Water Quality Information Center of the National Agricultural Library
Agricultural Research Service, U.S. Department of Agriculture


Simulation Models, GIS and Nonpoint-Source Pollution (I)

 January 1991 - December 1993
 Quick Bibliography Series:  QB 94-06 (Updates QB 92-69)
 337 citations from AGRICOLA
 
 Joe Makuch and Bonnie Emmert
 Water Quality Information Center
 
 Quick Bibliography Series 
 Bibliographies in the Quick Bibliography series of the
 National Agricultural Library (NAL), are intended primarily for
 current awareness, and as the title of the series implies, are
 not in-depth and exhaustive. However, the citations are a
 substantial resource for recent investigations on a given topic. 
 They also serve the purpose of bringing the literature of
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 access it by any other means.  The bibliographies are derived
 from online searches of the AGRICOLA database.  Timeliness of
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 criteria.  Send suggestions for Quick Bibliography topics to
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 index is provided along with the search strategy.
 
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      Simulation Models, GIS and Nonpoint-Source Pollution
 
 1                                    NAL Call. No.: 56.8 SO3
 An accurate and numerically stable model for one-dimensional
 solute transport in soils.
 Moldrup, P.; Yamaguchi, T.; Hansen, J.A.; Rolston, D.E.
 Baltimore, Md. : Williams & Wilkins; 1992 Apr.
 Soil science v. 153 (4): p. 261-273; 1992 Apr.  Includes
 references.
 
 Language:  English
 
 Descriptors: Soil solution; Solutes; Transport processes;
 Simulation models; Mathematical models; Soil water movement;
 Convection; Dispersion; Comparisons; Accuracy; Soil testing;
 Soil water content; Loam soils
 
 
 2                                    NAL Call. No.: QH540.N3
 Adsorption-desorption methodologies and selected estimation
 techniques for transport-modeling parameters.
 Roy, W.R.
 Berlin, W. Ger. : Springer-Verlag; 1993.
 NATO ASI series : Series G : Ecological sciences v. 32: p.
 169-188; 1993.  In the series analytic: Migration and fate of
 pollutants in soils and subsoils / edited by D. Petruzzelli
 and F.G. Helfferich. Proceedings of the NATO Advanced Study
 Institute, May 24-June 5, 1992, Maratea, Italy.  Includes
 references.
 
 Language:  English
 
 Descriptors: Soil pollution; Pollutants; Adsorption;
 Desorption; Transport processes; Computer simulation; Vapor;
 Organic compounds; Volatilization; Groundwater pollution;
 Trichloroethylene; Microbial degradation
 
 
 3                                 NAL Call. No.: HD1773.A2N6
 Aggregate analysis of site-specific pollution problems: the
 case of groundwater contamination from agriculture.
 Opaluch, J.J.; Segerson, K.
 Morgantown, W.Va. : The Northeastern Agricultural and Resource
 Economics Association; 1991 Apr.
 Northeastern journal of agricultural and resource economics v.
 20 (1): p. 83-97; 1991 Apr.  Paper submitted in response to
 call for papers on the theme "The Effects of Agricultural
 Production on Environmental Quality.".  Includes references.
 
 Language:  English
 
 Descriptors: Groundwater; Contamination; Water pollution;
 Agricultural sector; Agricultural policy; Microeconomic
 analysis; Aggregate data; Site factors; Spatial distribution;
 Information systems; Mathematical models
 
 
 4                                    NAL Call. No.: S900.R39
 Analysing water quality policy using microeconomic models of
 production practices and biophysical flow models of
 environmental processes. Weaver, R.D.; Harper, J.K.
 London : Harwood Academic Publishers; 1993.
 Resource management and optimization v. 9 (2): p. 95-105;
 1993.  Includes references.
 
 Language:  English
 
 Descriptors: U.S.A.; Water quality; Water policy;
 Microeconomics; Technology; Environmental factors;
 Mathematical models
 
 
 5                                  NAL Call. No.: 292.8 W295
 An analytical solution for one-dimensional transport in porous
 media with an exponential dispersion function.
 Yates, S.R.
 Washington, D.C. : American Geophysical Union; 1992 Aug.
 Water resources research v. 28 (8): p. 2149-2154; 1992 Aug. 
 Includes references.
 
 Language:  English
 
 Descriptors: Transport processes; Solutes; Hydrodynamic
 dispersion; Subsurface layers; Equations; Mathematical models
 
 Abstract:  An analytical solution describing the transport of
 dissolved substances in heterogeneous porous media with an
 asymptotic distance-dependent dispersion relationship has been
 developed. The solution has a dispersion function which is
 linear near the origin (i.e., for short travel distances) and
 approaches an asymptotic value as the travel distance becomes
 infinite. This solution can be used to characterize
 differences in the transport process relative to both the
 classical convection-dispersion equation which assumes that
 the hydrodynamic dispersion in the porous medium remains
 constant and a dispersion solution which has a strictly linear
 dispersion function. The form of the hydrodynamic dispersion
 function used in the analytical solution is D(x) = alpha(x)
 average pore water velocity + D(diff), where a(x) = a L[1 -e(-
 bx/L)]. The proposed model may provide an alternate means for
 obtaining a description of the transport of solutes in
 heterogeneous porous media, when the scale dependence of the
 dispersion relationship follows the behavior given by
 alpha(x). The overall behavior of the model is illustrated by
 several examples for constant concentration and flux boundary
 conditions.
 
 
 6                                    NAL Call. No.: 56.9 SO3
 Analytical solution of solute diffusion and biodegradation in
 spherical aggregates.
 Priesack, E.
 Madison, Wis. : The Society; 1991 Sep.
 Soil Science Society of America journal v. 55 (5): p.
 1227-1230; 1991 Sep. Includes references.
 
 Language:  English
 
 Descriptors: Microbial degradation; Soil flora; Organic
 compounds; Solutes; Diffusion; Soil solution; Aggregates;
 Spatial distribution; Mathematical models; Soil pore system;
 Pores; Transport processes; Movement in soil; Diffusivity;
 Growth rate; Adsorption; Biomass; Substrates
 
 Abstract:  Microbial degradation and transformation of
 substances in soils plays a crucial role ii the nutrient
 turnover of ecosystems. To quantify these processes, a
 mathematical description is needed. For this purpose, an
 analytical solution to a model of solute diffusion and
 biodegradation in soil aggregates was developed. The model is
 a first approach toward understanding the influence of
 geometric arrangement of microorganisms and substrates in
 structured soils. These soils are considered to consist of
 uniformly sized and shaped aggregates surrounded by surface
 films of the soil solution. The model simulates transient
 diffusion of finite substrate amounts from the surface films
 into spherical aggregates. Biodegradation is considered for
 the special case of unlimited microbial growth, and adsorption
 is assumed to follow a linear Freundlich isotherm. The system
 is represented by a composite sphere, the outer sphere being
 the solution film and the inner sphere representing the soil
 aggregate. The diffusion equations are solved by Laplace
 transformation. The model solution gives a direct relationship
 between the initial substrate and biomass concentrations, the
 diffusion coefficient, the specific growth rate, and the
 adsorption coefficient. Good agreement between this closed
 form solution and numerical solutions is obtained for
 diffusion with and without biodegradation. Since the substrate
 is exhausted by organisms close to the surface, the centers of
 large aggregates are not reached by the diffusing substrate.
 These unaffected centers become lager as the growth rate is
 higher, the diffusion constant is lower, and adsorption of the
 substrate is stronger.
 
 
 7                                  NAL Call. No.: 292.8 W295
 Analytical solutions for solute transport in three-dimensional
 semi-infinite porous media.
 Leij, F.J.; Skaggs, T.H.; Van Genuchten, M.T.
 Washington, D.C. : American Geophysical Union; 1991 Oct.
 Water resources research v. 27 (10): p. 2719-2733; 1991 Oct. 
 Includes references.
 
 Language:  English
 
 Descriptors: Transport processes; Solutes; Flow; Mathematical
 models; Prediction
 
 Abstract:  This paper presents several analytical solutions
 for three-dimensional solute transport in semi-infinite porous
 media with unidirectional flow using first-type (or
 concentration) and third-type (or flux) boundary conditions at
 the inlet location of the medium. The solutions may be used
 for predicting solute concentrations in homogeneous media,
 verification of more comprehensive numerical models, and
 laboratory or field determination of solute transport
 parameters. The transport equation incorporates terms
 accounting for advection, dispersion, zero-order production,
 and first-order decay. General solutions were derived for an
 arbitrary initial distribution and solute input with the help
 of Laplace, Fourier, and Hankel transforms. Specific solutions
 are presented for rectangular and circular solute inflow
 regions, as well as for solutes initially present in the form
 of parallelepipedal or cylindrical regions of the medium. The
 solutions were mathematically verified against simplified
 analytical solutions. Examples of concentration profiles are
 presented for several solute transport parameters using both
 first- and third-type boundary conditions. A mass balance
 constraint is defined based on a prescribed solute influx; the
 third-type condition is shown to conserve mass whereas the
 first-type condition was found to always overestimate resident
 solute concentrations in the medium.
 
 
 8                                  NAL Call. No.: 292.8 W295
 Applicability of the steady state flow assumption for solute
 advection in field soils.
 Destouni, G.
 Washington, D.C. : American Geophysical Union; 1991 Aug.
 Water resources research v. 27 (8): p. 2129-2140; 1991 Aug. 
 Includes references.
 
 Language:  English
 
 Descriptors: Agricultural soils; Solutes; Transport processes;
 Transient flow; Soil water movement; Soil texture; Soil depth;
 Plant water relations; Simulation models
 
 Abstract:  A comparison between solute travel times predicted
 by a transient and a steady state flow model is made. Data for
 five different soil profiles with detailed measurements of
 their hydraulic properties and their variation with depth are
 used. Daily measurements of meteorological data are used as
 input parameters in the transient simulations that include
 snow and frost dynamics, interception of precipitation, and
 evapotranspiration. The parameters of the steady state flow
 model are related to the measured soil properties and the
 hydrological characteristics of each transient simulation.
 Furthermore, the influence of solute injection time on the
 predicted travel time is analyzed, and the effect of root
 water uptake on the applicability, of the steady state flow
 assumption for solute advection is investigated. The results
 indicate that the steady, state flow model may provide
 estimates of the mean solute advection that are compatible
 with those of the transient flow model. The constant rate of
 recharge in the steady state flow, model should then be
 interpreted as the average annual effective infiltration
 (i.e., infiltration minus actual evapotranspiration). When
 root water uptake is accounted for, an arithmetic depth-
 averaging of the soil parameters appears to yield steady state
 estimates of arrival time that are closest to the transient
 predictions. When root water uptake is neglected, a harmonic
 depth-averaging of the soil parameters provides the best
 steady state results. The discrepancy between the arrival
 times predicted with the two flow models decreases with the
 travel distance from the soil surface.
 
 
 9                            NAL Call. No.: 100 G29So no.372
 Application and enhancement of hydrologic/water quality
 models..  S-211 final report
 Thomas, Daniel L.; Shirmohammadi, Adel,_1952-; Engel, Bernard
 A. Tifton, Ga. : Biological and Agricultural Engineering Dept.
 : University of Georgia-Coastal Plain Experiment Station,;
 1992.
 xi, 114 p. : ill. ; 28 cm. (Southern cooperative series
 bulletin ; no. 372). Running title: S-211 final report.  June,
 1992.  Includes bibliographical references.
 
 Language:  English; English
 
 Descriptors: Hydrology; Water quality
 
 
 10                                  NAL Call. No.: SB951.P47
 Application and validation of pesticide leaching models.
 Klein, M.
 Essex : Elsevier Applied Science Publishers; 1991.
 Pesticide science v. 31 (3): p. 389-398; 1991.  Includes
 references.
 
 Language:  English
 
 Descriptors: German federal republic; Bentazone; Cloethocarb;
 Simulation models; Environmental factors; Leaching;
 Lysimeters; Pesticide residues; Soil properties; Climatic
 factors
 
 Abstract:  Two lysimeter studies with the pesticides
 cloethocarb and bentazone were used to validate a modified
 version of the computer model SESOIL (Seasonal Soil
 Compartment Model), developed by Bonazountas and Wagner and to
 transfer the results of the lysimeter study to another climate
 scenario. For cloethocarb, an experimental insecticide without
 marked mobility in the soil, as indicated by the lysimeter
 study, the simulations were in excellent agreement with the
 lysimeter study. Calculations for bentazone revealed higher
 leaching than found in the lysimeter study. This discrepancy
 was resolved by a more careful and realistic inclusion of
 sorption in the lysimeter soil into the simulation model.
 
 
 11                                  NAL Call. No.: 292.8 J82
 An application of a physically based semi-distributed model to
 the Balquhidder catchments.
 Robson, A.J.; Whitehead, P.G.; Johnson, R.C.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1993 May15.
 Journal of hydrology v. 145 (3/4): p. 357-370; 1993 May15. 
 Special Issue: The Balquhidder Catchment and Process Studies /
 edited by P.G. Whitehead and I.R. Calder.  Includes
 references.
 
 Language:  English
 
 Descriptors: Scotland; Watersheds; Simulation models;
 Catchment hydrology; Rain; Runoff; Flow
 
 Abstract:  A physically based semi-distributed model,
 TOPMODEL, is applied to the two catchments at Balquhidder. The
 model uses a topographic index which highlights hydrologically
 significant areas within the catchments. The model is used to
 simulate runoff and to compare the behaviour of the two
 catchments. The results indicate that a large proportion of
 stream water is generated from saturated contributing areas
 (source areas); the Monachyle has higher contributions of
 water of this type. The results may also indicate that the
 hydrology of the Monachyle catchment has changed following
 agricultural improvement by increased drainage; a damped
 subsurface response is observed.
 
 
 12                              NAL Call. No.: QA76.76.E95A5
 Application of case-based reasoning concepts to the WEPP soil
 erosion model. Meyer, C.R.; Flanagan, D.C.
 Moscow, Idaho : AI Applications; 1992.
 AI applications v. 6 (3): p. 63-71; 1992.  Includes
 references.
 
 Language:  English
 
 Descriptors: U.S.A.; Water erosion; Prediction; Simulation
 models; Information retrieval; Usda; Improvement; Management;
 Practice; Information storage; Data banks; Program
 development; Computer techniques
 
 
 13                                   NAL Call. No.: 56.9 SO3
 Applications of a laser scanner to quantify soil
 microtopography. Huang, C.H.; Bradford, J.M.
 Madison, Wis. : The Society; 1992 Jan.
 Soil Science Society of America journal v. 56 (1): p. 14-21;
 1992 Jan. Includes references.
 
 Language:  English
 
 Descriptors: North Carolina; Hapludults; Inceptisols; Surface
 roughness; Measurement; Quantitative techniques; Surface
 layers; Topography; Height; Spatial variation; Mathematical
 models; Mathematics; Transport processes; Soil boundaries;
 Artificial precipitation; Tillage; Interrill erosion; Soil
 water content; Size; Lasers
 
 Abstract:  Many transport processes on or across the soil
 surface boundary are controlled by surface microtopography, or
 roughness. How roughness affects the transport process depends
 on the length scale of the process. The most commonly used
 method of expressing soil surface roughness, the roughness
 length or random roughness, is constrained by the measurement
 technique and does not embody the concept of scale. The
 structural function, or variogram, plotted on a log-log scale
 was used in this study to express the surface roughness at
 different scales. With the aid of a laser scanner, surface
 topography was measured down to 0.5-mm grid spacing. Data
 collected from a variety of surface conditions showed that
 soil roughness can be quantified by a combination of fractal
 and Markov-Gaussian processes at different scales. Potential
 applications of the roughness quantification were also
 discussed.
 
 
 14                                  NAL Call. No.: TD426.J68
 An approach to estimating uncertainties in modeling transport
 of solutes through soils.
 Zhang, H.; Haan, C.T.; Nofziger, D.L.
 Amsterdam : Elsevier; 1993 Feb.
 Journal of contaminant hydrology v. 12 (1/2): p. 35-50; 1993
 Feb.  Includes references.
 
 Language:  English
 
 Descriptors: Soil pollution; Groundwater pollution;
 Pollutants; Chemicals; Solutes; Movement in soil; Uncertainty;
 Rain; Variation; Prediction; Simulation models
 
 
 15                                 NAL Call. No.: 292.8 W295
 Approximate analytical solution for soil chemical transfer to
 runoff: a modified boundary condition.
 Wallach, R.
 Washington, D.C. : American Geophysical Union; 1993 May.
 Water resources research v. 29 (5): p. 1467-1474; 1993 May. 
 Includes references.
 
 Language:  English
 
 Descriptors: Agricultural chemicals; Soil solution; Surface
 water; Runoff water; Overland flow; Boundaries; Transport
 processes; Equations; Mathematical models; Comparisons
 
 Abstract:  Two mass balance equations were used to model the
 transfer of dissolved chemicals from the soil solution to the
 surface runoff water and the transport of these chemicals to
 the field outlet. One mass balance equation was written for
 chemicals dissolved in the overland water, the other for
 chemicals within the soil profile. Chemical input into the
 surface water (upper boundary condition) was expressed as a
 rate-limited convective mass transfer, depending on both soil
 surface and runoff concentrations. Isolating a slow and fast
 time scale and scaling the mass balance equations to the slow
 one yielded a parameter, epsilon, which multiplies the time
 derivative of the mass balance equation written for overland
 flow. In most cases epsilon << 1, providing a singular
 perturbation problem that was solved by using the method of
 matched asymptotic expansion. The approximate solution,
 uniformly valid over the entire domain, was made up of two
 terms: a leading-order solution and a first-order solution,
 the latter of which was relatively small, even for epsilon =
 O(1). The leading-order solution was compared with that for a
 simpler case, in which the convective mass transfer (upper
 boundary condition) depends only on the soil surface
 concentration. The comparison indicated those limited cases to
 which the simpler boundary condition can be applied resulting
 in a very small error. Although it is not possible to get a
 strictly analytical solution for a problem involving a
 modified upper boundary condition, the approximate analytical
 solution is easily obtained.
 
 
 16                                 NAL Call. No.: 292.9 AM34
 Assessing ground water pollution potential from nitrogen
 fertilizer using a geographic information system.
 Halliday, S.L.; Wolfe, M.L.
 Bethesda, Md. : American Water Resources Association; 1991
 Mar. Water resources bulletin v. 27 (2): p. 237-245; 1991 Mar. 
 Includes references.
 
 Language:  English
 
 Descriptors: Texas; Groundwater pollution; Nitrogen
 fertilizers; Pollutants; Susceptibility; Expert systems
 
 Abstract:  A geographic information system (GRASS 3.1) was
 used to correlate the availability of nitrogen fertilizer with
 the susceptibility of ground water to pollution in Texas to
 identify potential ground water quality problems. An
 agricultural pollution susceptibility map, produced by the
 Texas Water Commission using the DRASTIC methodology, was
 combined with information on cropped areas, recommended
 nitrogen fertilizer application rates, and aquifer outcrops. A
 Nitrogen Fertilizer Pollution Potential Index was generated,
 identifying 24 percent or Texas within the high pollution
 potential category. An analysis of the susceptibility of major
 aquifer outcrops to potential pollution from nitrogen
 fertilizer indicated that 34 percent of the outcrop areas fall
 in the high pollution potential range. It is proposed that
 correlating the availability of a pollutant with an assessment
 of the susceptibility of ground water to pollution yields a
 more accurate screening tool for identifying potential
 pollution problems than considering susceptibility alone.
 
 
 17                                 NAL Call. No.: S542.A8A34
 Assessment and alleviation of the impact of runoff and erosion
 on crop production.
 Okwach, G.E.; Williams, J.; Wambua, J.
 Canberra : Australian Centre for International Agricultural
 Research; 1992. ACIAR proceedings (41): p. 72-82; 1992.  In
 the series analytic: A search for strategies for sustainable
 dryland cropping in semi-arid eastern Kenya / edited by M.E.
 Probert. Paper presented at a symposium held Dec 10-11, 1990,
 Nairobi, Kenya.  Includes references.
 
 Language:  English
 
 Descriptors: Kenya; Runoff; Erosion; Soil fertility; Tillage;
 Mulches; Soil conservation; Semiarid zones; Simulation models
 
 
 18                                  NAL Call. No.: 292.8 J82
 An assessment of the dynamic response characteristics of
 streamflow in the Balquhidder catchments.
 Jakeman, A.J.; Littlewood, I.G.; Whitehead, P.G.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1993 May15.
 Journal of hydrology v. 145 (3/4): p. 337-355; 1993 May15. 
 Special Issue: The Balquhidder Catchment and Process Studies /
 edited by P.G. Whitehead and I.R. Calder.  Includes
 references.
 
 Language:  English
 
 Descriptors: Scotland; Watersheds; Stream flow; Catchment
 hydrology; Clearcutting; Afforestation; Rain; Runoff;
 Simulation models
 
 Abstract:  The method of rainfall-runoff modelling and
 hydrograph separation developed in an earlier paper is applied
 to the Kirkton and Monachyle catchments situated near
 Balquhidder, Scotland. Using daily rainfall and streamflow
 data, natural differences between the quick and slow flow
 responses for the Kirkton and Monachyle catchments are
 quantified, and an attempt is made to detect the impact of
 land-use changes on these natural regimes (clear-felling in
 part of the Kirkton and drainage ditching and conifer planting
 in part of the Monachyle). Dynamic response characteristics
 for the quick and slow flow components are defined in terms of
 time constants, relative throughput volumes and unit
 hydrograph peaks. These response characteristics are estimated
 and compared for annual periods before and after the land-use
 changes. For both the Kirkton and Monachyle, the effects of
 the land-use changes (affecting part of each catchment) on the
 hydrological response are not detectable at the catchment
 outlets. The interannual variation of the dynamic response
 characteristics falls within the inherent uncertainty expected
 if no land-use changes had occurred.
 
 
 19                              NAL Call. No.: aS21.A8U5/ARS
 Basin scale water quality model.
 Arnold, J.G.
 Washington, D.C. : The Service; 1993.
 Reprints - U.S. Department of Agriculture, Agricultural
 Research Service [512]: 9 p.; 1993.  Indexed from reprint:
 Proceedings of the CREAMS and GLEAMS Conference. p. 192-200. 
 Includes references.
 
 Language:  English
 
 Descriptors: Catchment hydrology; Simulation models; Water
 quality; Climatic factors; Geological sedimentation; Runoff;
 Agricultural chemicals
 
 
 20                                  NAL Call. No.: S612.I756
 Best management of pesticide--furrow irrigation systems.
 Ranjha, A.Y.; Peralta, R.C.; Requena, A.M.; Deer, H.M.;
 Ehteshami, M.; Hill, R.W.; Walker, W.R.
 Berlin, W. Ger. : Springer International; 1992.
 Irrigation science v. 13 (1): p. 9-14; 1992.  Includes
 references.
 
 Language:  English
 
 Descriptors: Utah; Furrow irrigation; Design; Simulation
 models; Pesticides; Leaching; Losses from soil systems; Water
 management; Groundwater pollution; Soil texture
 
 Abstract:  Effects of furrow irrigation designs, water
 management practices (irrigation scheduling, etc.), soil types
 and pesticide parameters on pesticide leaching were simulated.
 A hydraulic kinematic-wave irrigation model was used to
 estimate water infiltration for alternative furrow lengths and
 inflow rates. A one-dimensional simulation model then
 simulated the movement of pesticides through soils following
 furrow irrigation. Potential ground-water contamination by
 pesticides can be reduced by an integrated use of the best
 management practices (BMPs) such as careful selection and use
 of pesticides, efficient furrow irrigation designs and
 improved water management techniques (irrigation scheduling,
 etc.). Procedures for designing an appropriate furrow
 irrigation system for a particular site and pesticide, and
 selecting pesticides for a particular site, crop and furrow
 irrigation system are illustrated. These procedures are being
 used to develop decision support computer models for
 developing different BMPs for pesticide-agricultural
 management decisions.
 
 
 21                      NAL Call. No.: GB701.W375 no.91-4055
 Calibration, verification, and use of a steady-state stream
 water-quality model for Monument and Fountain Creeks, east-
 central Colorado. Kuhn, Gerhard
 Pikes Peak Area Council of Governments, Geological Survey
 (U.S.) Denver, CO : U.S. Dept. of the Interior, U.S.
 Geological Survey : Books and Open-File Reports Section
 [distributor],; 1991.
 vii, 149 p. : ill. ; 28 cm. (Water-resources investigations
 report ; 91-4055).  Includes bibliographical references (p.
 139-142).
 
 Language:  English
 
 Descriptors: Water quality
 
 
 22                                NAL Call. No.: 290.9 AM32T
 Characterization of macropore transport studied with the ARS
 root zone water quality model.
 Ahuja, L.R.; DeCoursey, D.G.; Barnes, B.B.; Rojas, K.W.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1993 Mar. Transactions of the ASAE v. 36 (2): p.
 369-380; 1993 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Macropores; Movement in soil; Root zone flux;
 Soil water; Water flow; Fertilizers; Pesticides; Simulation
 models
 
 Abstract:  The ARS Root Zone Water Quality Model components
 dealing with preferential water and chemical transport are
 presented and used to study macropore flow and transport in a
 silty clay loam soil. Macroporosity of the soil was assumed to
 be 0.05% by volume, half of which was continuous and the rest
 discontinuous. Two rainfall sequences with two initial soil
 water contents, evaporation versus transpiration, macropore
 radius ranging from 1.0 to 0.125 mm, and three different
 chemicals were evaluated. Over a five-week period, weekly
 rainfall of 25.4 mm in one hour, with soil water
 redistribution and evaporation or transpiration occurring
 between storms, generated no macropore flow when the soil was
 initially dry (-1500 kPa). A slight amount of macropore flow
 was generated under the same rainfall when the soil was
 initially wet (-33 kPa). Doubling the weekly rainfall amount
 and intensity generated macropore flow varying between 30 to
 50% of rainfall depending on initial and boundary conditions.
 Chemicals transported with this flow were 0.05 to 8% of the
 surface-applied amount, depending on conditions and type of
 chemical. A moderately adsorbed chemical (Atrazine) was the
 most susceptible to macropore transport, followed in order by
 a strongly adsorbed chemical (Prometryn), and a mobile
 chemical (Nitrate). The flow entering the macropores was
 partially absorbed by soil at progressively deeper depths; it
 increased the water content of the root zone, and created a
 tail of low concentrations in the soil chemical content
 distributions. The macropore size had very little effect on
 macropore flow and transport, but the smallest size pores
 retarded the downward chemical movement by wall adsorption a
 little more than the largest size pores. Surface evaporation
 decreased macropore flow, soil water contents, and downward
 chemical movement, but increased chemical content of the
 macropore flow. Transpiration, on the other hand, decreased
 both macropore flow and its chemical content. Thu
 
 
 23                                  NAL Call. No.: HC79.E5E5
 Classification and spatial mapping of riparian habitat with
 applications toward management of streams impacted by nonpoint
 source pollution. Delong, M.D.; Brusven, M.A.
 New York, N.Y. : Springer-Verlag; 1991 Jul.
 Environmental management v. 15 (4): p. 565-571; 1991 Jul. 
 Includes references.
 
 Language:  English
 
 Descriptors: Idaho; Habitats; Riparian vegetation; Erosion;
 Pollution; Information systems; Mapping; Watersheds; Farmland
 
 
 24                                  NAL Call. No.: 56.8 J822
 Classifying remotely sensed data for use in an agricultural
 nonpoint-source pollution model.
 Jakubauskas, M.E.; Whistler, J.L.; Dillworth, M.E.; Martinko,
 E.A. Ankeny, Iowa : Soil and Water Conservation Society of
 America; 1992 Mar. Journal of soil and water conservation v.
 47 (2): p. 179-183; 1992 Mar. Includes references.
 
 Language:  English
 
 Descriptors: Kansas; Water quality; Water pollution; Remote
 sensing; Watersheds; Simulation models; Landsat; Thematic
 mapper; Data collection
 
 
 25                                  NAL Call. No.: SB610.W39
 Combining computer simulation with physical simulation: an
 attempt to validate turf runoff models.
 Lin, J.C.; Graney, R.L.
 Champaign, Ill. : The Society; 1992 Jul.
 Weed technology : a journal of the Weed Science Society of
 America v. 6 (3): p. 688-695; 1992 Jul.  Paper presented at a
 Symposium on the, "Role of Modeling in Regulatory Affairs," at
 the Weed Science Society of America, February 4, 1991,
 Louisville, Kentucky.  Includes references.
 
 Language:  English
 
 Descriptors: Agricultural chemicals; Pesticides; Simulation
 models; Runoff; Risk; Aquatic environment; Calibration; Field
 tests; Prediction
 
 
 26                                   NAL Call. No.: 56.9 SO3
 Comparison of models for describing the transport of dissolved
 organic carbon in aquifer columns.
 Jardine, P.M.; Dunnivant, F.M.; Selim, H.M.; McCarthy, J.F.
 Madison, Wis. : The Society; 1992 Mar.
 Soil Science Society of America journal v. 56 (2): p. 393-401;
 1992 Mar. Includes references.
 
 Language:  English
 
 Descriptors: Aquifers; Sediment; Organic matter; Carbon;
 Transport processes; Adsorption; Sorption isotherms; Kinetics;
 Contaminants; Movement in soil; Mathematical models;
 Comparisons
 
 Abstract:  Dissolved organic carbon (DOC) is a reactive
 constituent in aquifer and soil media and equilibrates between
 the mobile aqueous phase and the immobile solid phase. Since
 DOC is believed to accelerate the transport of associated
 contaminants, yet is known to interact with aquifer and soil
 material, our objective was to define and model those
 processes governing DOC adsorption to porous media that may
 affect the cotransport of contaminants. Column displacement
 experiments of DOC through aquifer sediments were modeled with
 various formulations of the convective-dispersive equation,
 which considered time-dependent adsorption reactions and
 linear or nonlinear adsorption processes. Batch equilibrium
 adsorption isotherm and kinetic studies for DOC interaction
 with the sediments were used to parameterize the transport
 models. The equilibrium DOC-adsorption isotherm was nonlinear
 and was adequately described by the Langmuir equation. The
 adsorption of DOC to the aquifer sediment was also time
 dependent and the batch results could be described by two
 simultaneous reaction rates for solution concentrations
 greater than or equal to 19 mg DOC L-1 and a slow reaction
 rate for solution concentrations < 10 mg DOC L-1. Observed DOC
 breakthrough curves (BTCs) with influent concentrations
 greater than or equal to 10 mg DOC L-1, were adequately
 modeled as two-site, non-linear adsorption processes, with DOC
 interactions with both types of sites being time dependent.
 Batch adsorption and kinetic parameters were generally
 successful in describing DOC transport; however, the magnitude
 of the initial batch rate coefficient was significantly larger
 than that observed for the displacement experiments. The
 extended tailing of the observed DOC BTCs was influenced more
 by the slow, time-dependent adsorption of DOC during transport
 than to the nonlinear features of the adsorption isotherms.
 Observed DOC BTCs with influent concentrations < 10 mg DOC L-1
 did not exhibit extensive tailing and were
 
 
 27                                NAL Call. No.: QH545.A1E58
 Comparison of PRZM and GLEAMS computer model predictions with
 field data for alachlor, metribuzin and norflurazon leaching.
 Mueller, T.C.; Jones, R.E.; Bush, P.B.; Banks, P.A.
 Elmsford, N.Y. : Pergamon Press; 1992.
 Environmental toxicology and chemistry v. 11 (3): p. 427-436;
 1992.  Includes references.
 
 Language:  English
 
 Descriptors: Alachlor; Norflurazon; Metribuzin; Herbicide
 residues; Leaching; Computer simulation; Simulation models;
 Soil depth; Sandy loam soils
 
 
 28                                  NAL Call. No.: 292.8 J82 A
 comprehensive surface-groundwater flow model.
 Arnold, J.G.; Allen, P.M.; Bernhardt, G.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1993 Feb.
 Journal of hydrology v. 142 (1/4): p. 47-69; 1993 Feb. 
 Includes references.
 
 Language:  English
 
 Descriptors: Texas; Groundwater; Groundwater flow; Groundwater
 level; Surface water; Runoff; Flow; Stream flow; Watersheds;
 Catchment hydrology; Land management; Climate; Vegetation;
 Water management; Simulation models
 
 Abstract:  In this study, a simple groundwater flow and height
 model was added to an existing basin-scale surface water
 model. The linked model is: (1) watershed scale, allowing the
 basin to be subdivided; (2) designed to accept readily
 available inputs to allow general use over large regions; (3)
 continuous in time to allow simulation of land management,
 including such factors as climate and vegetation changes, pond
 and reservoir management, groundwater withdrawals, and stream
 and reservoir withdrawals. The model is described, and is
 validated on a 471 km2 watershed near Waco, Texas. This linked
 model should provide a comprehensive tool for water resource
 managers in development and planning.
 
 
 29                                  NAL Call. No.: 1.98 AG84
 Computer model helps ensure clean water.
 Cooke, L.
 Washington, D.C. : The Service; 1991 Apr.
 Agricultural research - U.S. Department of Agriculture,
 Agricultural Research Service v. 39 (4): p. 10-12; 1991 Apr.
 
 Language:  English
 
 Descriptors: Michigan; Groundwater pollution; Nitrates;
 Leaching; Prevention; Computer simulation; Computer techniques
 
 
 30                                  NAL Call. No.: SB610.W39
 Computer models for fate assessment during the registration
 process: data needs.
 Behl, E.
 Champaign, Ill. : The Society; 1992 Jul.
 Weed technology : a journal of the Weed Science Society of
 America v. 6 (3): p. 696-700; 1992 Jul.  Paper presented at a
 Symposium on the, "Role of Modeling in Regulatory Affairs," at
 the Weed Science Society of America, February 4, 1991,
 Louisville, Kentucky.  Includes references.
 
 Language:  English
 
 Descriptors: Pesticides; Registration; Simulation models;
 Groundwater; Water quality
 
 
 31                      NAL Call. No.: GB701.W375 no.90-4200
 Computer software for converting ground-water and water-
 quality data from the National Water Information System for
 use in a geographic information system..  Software for
 converting data from NWIS for use in GIS
 Scott, J. C.
 Geological Survey (U.S.)
 Oklahoma City, Okla. : U.S. Geological Survey ; Denver, Colo.
 : Books and Open-File Reports [distributor],; 1991.
 iv, 55 p. : ill. ; 28 cm. (Water-resources investigations
 report ; 90-4200). Spine title: Software for converting data
 from NWIS for use in GIS.  Includes bibliographical references
 (p. 38-39).
 
 Language:  English
 
 Descriptors: Geographic information systems; Water
 
 
 32                                NAL Call. No.: 290.9 AM32T
 Computing watershed storage probabilities from rainfall and
 runoff data. Mills, W.C.; Thomas, A.W.; Dillard, A.L.; Snyder,
 W.M.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1992 May. Transactions of the ASAE v. 35 (3): p.
 891-897; 1992 May.  Includes references.
 
 Language:  English
 
 Descriptors: Rain; Runoff; Water conservation; Watersheds;
 Mathematical models; Probability
 
 Abstract:  This article describes the development and
 application of a computational procedure for obtaining
 watershed storage probabilities that are corrected for bias
 toward lower storage, which is inherent in storage values
 computed directly from rainfall and runoff data. The developed
 procedure makes use of rainfall and runoff data from
 watersheds, and also incorporates probabilities for rainfall
 needed to produce runoff for various storages. The procedure
 is derived mathematically using basic probability concepts and
 employs numerical integration and nonlinear least squares
 optimization in the solution. The procedure is applied to
 rainfall and runoff data collected from a Southern Piedmont
 field watershed over a 10-year period during which a
 conventional tillage system for crops was followed by two
 successive conservation tillage systems. Results of the
 application show that the developed computational procedure
 performs adequately in providing bias-corrected watershed
 storage probabilities that reflect effects of the three
 cropping/tillage systems on watershed storage.
 
 
 33                                  NAL Call. No.: TD426.J68
 Conditional simulation of flow and transport.
 Rogowski, A.S.; Wolf, J.K.; Simmons, D.E.
 Amsterdam : Elsevier; 1991 Jan.
 Journal of contaminant hydrology v. 7 (1/2): p. 95-121; 1991
 Jan.  Includes references.
 
 Language:  English
 
 Descriptors: Groundwater pollution; Leachates; Movement in
 soil; Groundwater recharge; Clay; Subsoil; Infiltration;
 Spatial distribution; Simulation models; Spatial variation
 
 
 34                                  NAL Call. No.: aSD11.A42
 The conservation reserve program: effects on soil, water and
 environmental quality.
 Blackburn, W.H.; Newman, J.B.; Wood, J.C.
 Fort Collins, Colo. : The Station; 1991 May.
 General technical report RM - Rocky Mountain Forest and Range
 Experiment Station, U.S. Department of Agriculture, Forest
 Service (203): p. 27-36; 1991 May.  Includes references.
 
 Language:  English
 
 Descriptors: U.S.A.; Soil conservation; Erosion control;
 Federal programs; Reserved areas; Simulation models;
 Percolation; Evapotranspiration; Water erosion; Runoff
 
 
 35                                 NAL Call. No.: TD420.A1E5
 Convective transport of gases in moist porous media: effect of
 absorption, adsorption, and diffusion in soil aggregates.
 McCoy, B.J.; Rolston, D.E.
 Washington, D.C. : American Chemical Society; 1992 Dec.
 Environmental science & technology v. 26 (12): p. 2468-2476;
 1992 Dec. Includes references.
 
 Language:  English
 
 Descriptors: Soil pollution; Groundwater pollution; Volatile
 compounds; Mathematical models
 
 
 36                                  NAL Call. No.: TC401.W27 A
 coupled rainfall-runoff and runoff-routing model for adaptive
 real-time flood forecasting.
 Habaieb, H.; Troch, P.A.; Troch, F.P. de
 Hingham, Mass. : Kluwer Academic Publishers; 1991.
 Water resources management v. 5 (1): p. 47-61; 1991.  Includes
 references.
 
 Language:  English
 
 Descriptors: Belgium; Floods; Forecasting; Rain; Runoff;
 Models; On line; Identification; Case studies
 
 
 37                                  NAL Call. No.: 292.8 J82
 Coupled simulations of water flow from a field-investigated
 glacial till slope using a quasi-two-dimensional water and
 heat model with bypass flow. Espeby, B.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1992 Feb.
 Journal of hydrology v. 131 (1/4): p. 105-132; 1992 Feb. 
 Includes references.
 
 Language:  English
 
 Descriptors: Sweden; Glacial till soils; Forest soils;
 Coniferous forests; Picea abies; Pinus sylvestris; Slopes;
 Water flow; Macropore flow; Meltwater; Precipitation; Runoff;
 Soil water retention; Saturated hydraulic conductivity;
 Macropores; Soil temperature; Soil depth; Physical models;
 Simulation models
 
 Abstract:  Substantial field investigations of soil physical
 properties and stratification in a forested slope (10 degrees
 slope) covered with glacial till revealed that macropores in
 the form of old root channels as well as coarse structures in
 the form of well-sorted layers dominate a very permeable upper
 solid horizon. Rapid response and quick recessions during
 snowmelt and heavy rains in 1986 were observed in the runoff
 from the slope. Based on field tracer experiments it was found
 that such macropores and macrostructures played an important
 role on these occasions. In order to verify these findings
 one-dimensional water and heat models were coupled in a serial
 manner to simulate the formation of runoff from the slope,
 using a quasi-two-dimensional approach. Both a strict Darcian
 concept and a Darcian concept with a simple bypass flow
 concept introduced were tested. The drainage gradient in the
 model was made equal with the angle of the slope. Coupled
 slope simulations, with water retention properties and
 hydraulic conductivities taken from three different levels on
 the slope, indicated that the conditions in the lower region
 of the slope were most important in explaining the discharge
 rate. With a shallow groundwater table in the lower region of
 the slope and low hydraulic conductivity of the deeper layers,
 rapid water flows are routed to the uppermost layers where the
 conductivity is higher. Most of the flow is well described by
 Richards' equation, although smaller peaks cannot be
 represented for small rain events, when the measured runoff
 and recession showed a more rapid response than that
 simulated, however, the introduction of a simple bypass flow
 improved the ability of the model to simulate the
 observations. Much of the simulated surface runoff generated
 in the Darcian simulation during the winter of 1986, could be
 diverted through a frost layer in the humus horizon and in the
 humus-impregnated mineral horizon with a silty-sand character,
 down to a more conductiv
 
 
 38                                   NAL Call. No.: QH540.J6
 Coupling groundwater contamination with economic returns when
 applying farm pesticides.
 Hoag, D.L.; Hornsby, A.G.
 Madison, Wis. : American Society of Agronomy; 1992 Oct.
 Journal of environmental quality v. 21 (4): p. 579-586; 1992
 Oct.  Includes references.
 
 Language:  English
 
 Descriptors: North Carolina; Groundwater pollution;
 Methodology; Pesticides; Usage; Economic impact; Returns;
 Profitability; Environmental impact; Glycine max; Weed
 control; Costs; Crop yield; Weed competition; Leaching;
 Simulation models
 
 Abstract:  A methodology is presented that permits
 simultaneous consideration of the economics of production and
 groundwater contamination hazard of pesticide use. An example
 is constructed for weed control in soybean (Glycine max L.)
 production at Clayton, NC. A cost/groundwater hazard frontier
 is developed that can be used to identify and illustrate the
 cost tradeoffs of selecting alternative weed control
 strategies that reduce the risk of adverse health effects from
 drinking contaminated groundwater. The methodology relies on
 models to estimate costs, crop yields, pest competition, and
 leaching of pesticides; thus, its applicability depends on
 availability of local data and appropriately validated models
 for the site considered. The cost/groundwater hazard frontier
 provides a useful decision aid to assist pesticide users in
 making cost-effective and environmentally favorable production
 decisions. It is also useful in evaluating policy or the value
 of new pest control technologies, as it indicates a farmer's
 ability to substitute alternatives for currently used
 practices.
 
 
 39                                  NAL Call. No.: 381 J8224
 Criteria to assess when biodegradation is kinetically limited
 by intraparticle diffusion and sorption.
 Chung, G.Y.; McCoy, B.J.; Scow, K.M.
 New York, N.Y. : John Wiley & Sons; 1993 Mar15.
 Biotechnology and bioengineering v. 41 (6): p. 625-632; 1993
 Mar15.  Includes references.
 
 Language:  English
 
 Descriptors: Soil flora; Microbial degradation; Pollutants;
 Transport processes; Diffusion; Sorption; Desorption; Polluted
 soils; Soil pollution; Mathematical models; Bioremediation
 
 Abstract:  To determine when intraparticle diffusion and
 sorption can influence the rate of biodegradation, we consider
 the biodegradation of a pollutant diffusing into or out of
 porous aggregates suspended in a liquid medium, where the
 reactant is metabolized by bacteria. The pollutant that
 diffuses into the aggregates obeys a sorption-desorption
 equilibrium isotherm at sites on inner pore surfaces. The
 governing partial differential equations for the transient
 process describe (a) the local equilibrium sorption-desorption
 and the diffusion of the pollutant in the porous aggregate,
 (b) the mass transfer of the pollutant from the external
 surface of the spherical aggregates to the reaction medium,
 and (c) the biodegradation of the pollutant in the external
 medium. Illustrative calculations are presented for a linear
 sorption isotherm and first-order biodegradation kinetics. A
 dimensionless group, comprised of the diffusion coefficient,
 biodegradation rate coefficient, aggregate characteristic
 length (radius), and adsorption capacity, serves as a
 criterion for determining when intraparticle diffusion
 resistance can be ignored. The model provides a realistic
 description of experimental data for biodegradation of a
 pollutant subject to intraparticle diffusion and sorption.
 
 
 40                                 NAL Call. No.: TD420.A1P7
 DBAPE--a database and model parameter analysis system for
 agricultural soils to support water quality management.
 Imhoff, J.C.; Carsel, R.F.; Kittle, J.L. Jr; Hummel, P.R.
 Oxford : Pergamon Press; 1991.
 Water science and technology : a journal of the International
 Association on Water Pollution Research and Control v. 24 (6):
 p. 331-337; 1991.  In the series analytic: Watermatex '91 /
 edited by T.O. Barnwell, P.J. Ossenbruggen and M.B. Beck.
 Proceedings of the "Second International Conference on Systems
 Analysis in Water Quality Management," June 3-6, 1991, Durham,
 New Hampshire. Includes references.
 
 Language:  English
 
 Descriptors: Soil properties; Water quality; Management;
 Agricultural soils; Computer software; Subsurface runoff;
 Models; Databases
 
 
 41                                   NAL Call. No.: QH540.J6
 Degradation and transport of dicamba in a clay soil.
 Comfort, S.D.; Inskeep, W.P.; Macur, R.E.
 Madison, Wis. : American Society of Agronomy; 1992 Oct.
 Journal of environmental quality v. 21 (4): p. 653-658; 1992
 Oct.  Includes references.
 
 Language:  English
 
 Descriptors: Dicamba; Clay soils; Degradation; Leaching; Soil
 water movement; Soil temperature; Persistence; Half life;
 Precipitation; Irrigation scheduling; Simulation models
 
 Abstract:  Dicamba (3,6-dichloro-2-methoxybenzoic acid) has
 been identified as one of five pesticides present in Montana
 groundwaters. We determined the effects of degradation and
 time of water application on the transport of dicamba in a
 Lohmiller clay soil (fine, montmorillonitic, mesic Ustic
 Torrifluvent). Carbon 14-labeled dicamba was surface applied
 (0.35 kg ha-1) to disturbed soil columns (5.0 cm diam; 29 cm
 length) previously conditioned with 3 mM CaCl2. The columns
 were allowed to incubate (23.5 degrees C) in triplicate for 0,
 14, 21, 28, and 42 d. Following incubation, the columns were
 attached to a vacuum chamber containing a fraction collector
 and leached with 3 mM CaCl2 under unsaturated conditions.
 Dicamba breakthrough curves were determined for each
 incubation period. The percentage of dicamba recovered in the
 column effluent decreased from 85% (of total applied) after no
 incubation to 9.5% after 42 d of incubation. The decline of
 dicamba in the effluent coincided with an accumulation of
 dichlorosalicyclic acid at the soil surface. Dicamba half-
 lives determined under batch conditions were 23.5 d at 28
 degrees C, 38 d at 20 degrees C, and 151 d at 12 degrees C,
 and were all higher than the half-life estimated from the
 decrease in column effluent concentrations over time (13.5 d).
 The simulation model, LEACHM, was used to predict transport of
 dicamba after the different incubation periods. LEACHM
 adequately estimated the mass of dicamba leached, but
 underestimated the maximum dicamba concentrations observed in
 the effluent. Both simulated and observed results indicated
 that the transport of dicamba can be greatly reduced if
 sufficient degradation of dicamba is allowed to occur before
 irrigation or precipitation.
 
 
 42                                  NAL Call. No.: QC851.J62 A
 description of rainfall interception over large areas.
 Eltahir, E.A.B.; Bras, R.L.
 Boston, MA : American Meteorological Society, c1988-; 1993
 Jun. Journal of climate v. 6. (6): p. 1002-1008; 1993 Jun. 
 Includes references.
 
 Language:  English
 
 Descriptors: Rain; Ground vegetation; Canopy; Drainage; Runoff
 water; Interception; Evaporation; Models; Climatic factors
 
 Abstract:  A new scheme is developed for describing
 interception at spatial scales comparable to the typical
 resolution of climate models. The scheme is based on the
 Rutter model of interception and statistical description of
 the subgrid-scale spatial variability of canopy storage and
 rainfall. The interception loss simulated by the new scheme is
 significantly smaller than those simulated by other schemes
 that do not include considerations for spatial variability.
 The explanation of this result is partly in the enhancement of
 spatially averaged canopy drainage due to the large local
 drainage from the few buckets of large canopy storage. The
 relative reduction in interception loss simulated by the new
 scheme may explain the overestimation of interception loss by
 climate models that do not include the effects of spatial
 variability on interception processes.
 
 
 43                                   NAL Call. No.: TD403.G7
 Design and evaluation of a mesoscale model vadose zone and
 ground-water system.
 Lawrence, J.R.; Zanyk, B.N.; Hendry, M.J.; Wolfaardt, G.M.;
 Robarts, R.D.; Caldwell, D.E.
 Dublin, Ohio : Ground Water Pub. Co; 1993 May.
 Ground water v. 31 (3): p. 446-455; 1993 May.  Includes
 references.
 
 Language:  English
 
 Descriptors: Groundwater pollution; Soil pollution;
 Contaminants; Movement in soil; Chemical degradation;
 Microbial degradation; Models; Agricultural chemicals
 
 Abstract:  A mesoscale model soil and ground-water system was
 constructed and instrumented to study physical, chemical, and
 microbial processes, including transport and degradation of
 contaminants. The model system was 4.6 m in height by 2.4 m in
 diameter and contained up to 65 tonnes of soil and geologic
 materials. The model was filled with Ap (11 cm), B (20 cm), Cl
 and C2 (369 cm) horizons; the water table was 3.3 m from the
 soil surface. A rain simulation system applied uniform
 coverage of rain and/or chloride tracer to the model. Sampling
 of soil, sediment, pore waters, and gas phase was carried out
 using a series of in situ collectors and sampling ports. Major
 anions, metals, pH, alkalinity, CO2, N2, O2, CH4, microbial
 numbers, microbial biomass and heterotrophic potential (14 C-
 amino-acid uptake) were monitored over time (120 days) and
 depth. The system approached steady state with respect to
 solution chemistry and gases after approximately 60-70 days.
 During this interval, carbon dioxide rose from atmospheric to
 3-5% of total gas volume measured at each sampling depth above
 the water table. Physical, chemical, and biological conditions
 in the model system after the initial 120 days were comparable
 to those reported for vadose and saturated zones during field
 studies on shallow phreatic aquifers. These results indicated
 that the mesoscale model preserved many of the features of
 natural systems while providing controlled conditions for
 studies such as evaluating the fate, and ground-water
 contamination potential, of agricultural and industrial
 chemicals.
 
 
 44                                   NAL Call. No.: TD201.A4
 Design of optimal pump-and-treat strategies of contaminated
 groundwater remediation using the simulated annealing
 algorithm.
 Kuo, C.H.; Michel, A.N.; Gray, W.G.
 Essex : Elsevier Science Publishers Ltd; 1992.
 Advances in water resources v. 15 (2): p. 95-105; 1992. 
 Includes references.
 
 Language:  English
 
 Descriptors: Groundwater pollution; Problem solving; Pumps;
 Placement; Optimization methods; Hydraulics; Constraints;
 Simulation models; Algorithms
 
 
 45                                   NAL Call. No.: TD403.G7
 Designing a nitrate monitoring program in a heterogeneous,
 carbonate aquifer. Smith, R.T.; Ritzi, R.W. Jr
 Dublin, Ohio : Ground Water Pub. Co; 1993 Jul.
 Ground water v. 31 (4): p. 576-584; 1993 Jul.  Includes
 references.
 
 Language:  English
 
 Descriptors: Ohio; Aquifers; Carbonates; Hydraulic
 conductivity; Finite element analysis; Simulation models;
 Nitrates; Movement in soil; Zea mays; Glycine max; Rotations;
 Groundwater pollution
 
 
 46                                 NAL Call. No.: 292.9 AM34
 Determination of best timing for poultry waste disposal: a
 modeling approach. Edwards, D.R.; Daniel, T.C.; Marbun, O.
 Bethesda, Md. : American Water Resources Association; 1992
 May. Water resources bulletin v. 28 (3): p. 487-494; 1992 May. 
 Includes references.
 
 Language:  English
 
 Descriptors: Arkansas; Poultry manure; Waste disposal;
 Application to land; Application date; Timing; Surface water;
 Runoff water; Water quality; Nitrogen; Phosphorus; Losses from
 soil systems; Grasses; Crop production; Crop yield
 
 Abstract:  Confined production of poultry results in
 significant volumes of waste material which are typically
 disposed of by land application. Concerns over the potential
 environmental impacts of poultry waste disposal have resulted
 in ongoing efforts to develop management practices which
 maintain high quality of water downstream of disposal areas.
 The timing of application to minimize waste constituent losses
 is a management practice with the potential to ensure high
 quality of streams, rivers, and lakes downstream of receiving
 areas. This paper describes the development and application of
 a method to identify which time of year is best, from the
 standpoint of surface water quality, for land application of
 poultry waste. The procedure consists of using a mathematical
 simulation model to estimate average nitrogen and phosphorus
 losses resulting from different application timings, and then
 identifying the timings which minimize losses of these
 nutrients. The procedure was applied to three locations in
 Arkansas, and three different criteria for optimality of
 application timing were investigated. One criterion was
 oriented strictly to water quality, one was oriented only to
 crop production, and the last was a combination. The criteria
 resulted in different windows of time being identified as
 optimal. Optimal windows also varied with location of the
 receiving area. The results indicate that it is possible to
 land-apply poultry waste at times which both minimize nutrient
 losses and maximize crop yield.
 
 
 47                                  NAL Call. No.: SB951.P47
 Development and validation of a modified fugacity model of
 pesticide leaching from farmland.
 Brooke, D.; Matthiessen, P.
 Essex : Elsevier Applied Science Publishers; 1991.
 Pesticide science v. 31 (3): p. 349-361; 1991.  Includes
 references.
 
 Language:  English
 
 Descriptors: England; Mecoprop; Simazine; Concentration;
 Leaching; Measurement; Models; Monitoring; Soil properties;
 Water pollution; Agricultural soils
 
 Abstract:  To test whether a simple model could provide
 reasonable quantitative estimates of chemical concentrations
 in a dynamic situation, Mackay's fugacity model was adapted to
 represent an agricultural field. The intention was to
 determine the extent of modification required to obtain
 reasonable agreement with experimental results, or indeed if
 such agreement could be achieved. The validity of the model
 was tested at Rosemaund Experimental Husbandry Farm in
 Herefordshire, where the chemical input and output could be
 monitored and meteorological and other parameters measured
 regularly. Results from monitoring concentrations of two
 pesticides at this site in recent years. and changes that have
 been made to the model in attempting to fit the observed
 behaviour are described.
 
 
 48                                   NAL Call. No.: QH540.J6
 Development of a database and model parameter analysis system
 for agricultural soils.
 Carsel, R.F.; Imhoff, J.C.; Kittle, J.L. Jr; Hummel, P.R.
 Madison, Wis. : American Society of Agronomy; 1991 Jul.
 Journal of environmental quality v. 20 (3): p. 642-647; 1991
 Jul.  Includes references.
 
 Language:  English
 
 Descriptors: Water quality; Water management; Databases;
 Computer software; Water flow
 
 Abstract:  An interactive computer program was developed for
 obtaining soils data for geographic analyses and estimation of
 soil water retention data for simplistic and classical water
 flow models. The soils data base contains 8080 soil series
 identified from the USDA-SCS. The data are organized in
 sequential files that contain textural, morphological crop
 support, and geographical location (at a county level) and
 density (ha/county). The computer program allows the
 exploration of the database, clarifying the impact of data on
 modeled processes, screening geographically based data to
 identify potential sites for model application or testing, and
 developing initial guidance on alternative water quality
 management strategies. The program allows the display of data
 in the form of generated reports and production of geographic
 maps and plots of soil water functional relationships.
 Indirect methods are used in the program for estimating soil
 water retention characteristics using textural information
 from the soil data base. Estimates of variability can be
 developed within a soil series or among series by using
 reported ranges for textural information on each series
 contained in the soil database.
 
 
 49                                NAL Call. No.: S592.7.A1S6
 Dispersion effect on the apparent nitrogen isotope
 fractionation factor associated with denitrification in soil;
 evaluation by a mathematical model. Kawanishi, T.; Hayashi,
 Y.; Kihou, N.; Yoneyama, T.; Ozaki, Y. Exeter : Pergamon
 Press; 1993 Mar.
 Soil biology and biochemistry v. 25 (3): p. 349-354; 1993 Mar. 
 Includes references.
 
 Language:  English
 
 Descriptors: Denitrification; Quantitative analysis;
 Agricultural soils; Solutes; Dispersion; Transport processes;
 Soil water; Water flow; Mathematical models; Nitrate;
 Groundwater pollution
 
 Abstract:  An analytical model is constructed to investigate
 the effect of dispersion on the apparent 15N/14N fractionation
 factor associated with denitrification in soil. The steady
 input of solute with a fixed isotope ratio, uniform flow of
 the solute, and the first-order reaction for each isotope are
 assumed, and the relationship between the concentration
 distribution and the change of isotope ratio in the steady
 state is examined. The only dimensionless parameter, kl4ND/v2,
 the product of the first-order reaction rate constant and the
 dispersion coefficient divided by the square of the
 superficial velocity, determines the effect of dispersion, and
 if its value is larger than 0.01, the dispersion will affect
 the apparent isotope fractionation factor. As kl4ND/v2
 increases, the effect becomes more prominent, and when it
 approaches infinity, the ratio of the apparent per mille
 enrichment factor to the true one, (alpha ap-1)/(alpha tr-1),
 reaches 0.5.
 
 
 50                      NAL Call. No.: GB701.W375 no.93-4015
 Documentation of geographic-information-system coverages and
 data-input files used for analysis of the geohydrology of the
 Virginia Coastal Plain.. Documentation of geographic
 information system coverages and data input files used for
 analysis of the geohydrology of the Virginia Coastal Plain
 Focazio, Michael J.; Samsel, Theodore B.
 Geological Survey (U.S.),Hampton Roads Planning District
 Commission (Va.),Virginia Water Control Board
 Richmond, Va. : U.S. Geological Survey ; Denver, CO : Books
 and Open-File Reports Section [distributor],; 1993; I
 19.42/4:93-4015.
 vi, 53 p. : maps ; 28 cm. (Water-resources investigations
 report ; 93-4015). Shipping list no.: 93-0451-P.  Includes
 bibliographical references (p. 11).
 
 Language:  English; English
 
 Descriptors: Hydrogeology; Geographic information systems
 
 
 51                                 NAL Call. No.: 292.8 W295 A
 dual-porosity model for simulating the preferential movement
 of water and solutes in structured porous media.
 Gerke, H.H.; Van Genuchten, M.T.
 Washington, D.C. : American Geophysical Union; 1993 Feb.
 Water resources research v. 29 (2): p. 305-319; 1993 Feb. 
 Includes references.
 
 Language:  English
 
 Descriptors: Transport processes; Solutes; Water flow;
 Saturated flow; Transient flow; Leaching; Porous media;
 Physicochemical properties; Deterministic models; Mathematical
 models; Equations
 
 Abstract:  A one-dimensional dual-porosity model has been
 developed for the purpose of studying variably saturated water
 flow and solute transport in structured soils or fractured
 rocks. The model involves two overlaying continua at the
 macroscopic level: a macropore or fracture pore system and a
 less permeable matrix pore system. Water in both pore systems
 is assumed to be mobile. Variably saturated water flow in the
 matrix as well as in the fracture pore system is described
 with the Richards' equation, and solute transport is described
 with the convection-dispersion equation. Transfer of water and
 solutes between the two pore regions is simulated by means of
 first-order rate equations. The mass transfer term for solute
 transport includes both convective and diffusive components.
 The formulation leads to two coupled systems of nonlinear
 partial differential equations which were solved numerically
 using the Galerkin finite element method. Simulation results
 demonstrate the complicated nature of solute leaching in
 structured, unsaturated porous media during transient water
 flow. Sensitivity studies show the importance of having
 accurate estimates of the hydraulic conductivity near the
 surface of soil aggregates or rock matrix blocks. The proposed
 model is capable of simulating preferential flow situations
 using parameters which can be related to physical and chemical
 properties of the medium.
 
 
 52                                 NAL Call. No.: 100 C12CAG
 Dupuit-Forchheimer approximation may underestimate groundwater
 flow to San Joaquin River.
 Grismer, M.E.; Rashmawi, E.A.
 Oakland, Calif. : Division of Agriculture and Natural
 Resources, University of California; 1993 Jan.
 California agriculture v. 47 (1): p. 12, 13-15; 1993 Jan.
 
 Language:  English
 
 Descriptors: California; Groundwater flow; River water; Water
 quality; Water management; Salinity; Estimation; Water table;
 Errors; Mathematical models
 
 
 53                                  NAL Call. No.: GB746.W33
 Dynamic-probabilistic models for the formation of rainfall and
 snowmelt runoff.
 Kuchment, L.S.; Gel'fan, A.N.
 New York, N.Y. : Consultants Bureau; 1992 May.
 Water resources v. 18 (4): p. 335-343; 1992 May.  Translated
 from: Vodnye Resursy, v. 18 (4), 1991, p. 5-14, (GB746.V55). 
 Includes references.
 
 Language:  English; Russian
 
 Descriptors: U.S.S.R.in europe; Rain; Meltwater; Floods;
 Runoff water; Watersheds; Forest steppe; Zoning; Probabilistic
 models; Dynamic models; Physical models; Mathematical models;
 Weather data
 
 
 54                                   NAL Call. No.: HD101.S6
 Economic impacts of chemical use reduction on the South.
 Taylor, C.R.; Penson, J.B. Jr; Smith, E.G.; Knutson, R.D.
 Experiment, Ga. : The Association; 1991 Jul.
 Southern journal of agricultural economics - Southern
 Agricultural Economics Association v. 23 (1): p. 15-23; 1991
 Jul.  Discussion by J.R. Schaub, p. 25-26.  Includes
 references.
 
 Language:  English
 
 Descriptors: Southern states of U.S.A.; Agricultural
 chemicals; Pesticide residues; Water quality; Groundwater;
 Contamination; Food safety; Agricultural policy; Models;
 Economic impact; Income
 
 
 55                                     NAL Call. No.: HD1.A3
 The economics of water harvesting and supplementary irrigation
 in the semi-arid tropics of India.
 Pandey, S.
 Essex : Elsevier Applied Science Publishers; 1991.
 Agricultural systems v. 36 (2): p. 207-220; 1991.  Includes
 references.
 
 Language:  English
 
 Descriptors: Madhya pradesh; Soybeans; Wheat; Water
 harvesting; Irrigation; Cropping systems; Semiarid zones;
 Agricultural regions; Economic evaluation; Feasibility; Risk;
 Simulation models; Soil water balance; Yield response
 functions; Water relations; Decision making; Rain; Runoff
 water
 
 
 56                                   NAL Call. No.: 56.8 SO3
 The effect of soil P sorption kinetics on parameters used for
 modeling P uptake.
 Shnek, M.; Shaviv, A.; Ravina, I.
 Baltimore, Md. : Williams & Wilkins; 1991 May.
 Soil science v. 151 (5): p. 333-342; 1991 May.  Includes
 references.
 
 Language:  English
 
 Descriptors: Calcareous soils; Soil physics; Phosphorus;
 Sorption; Kinetics; Diffusion models; Desorption; Mathematical
 models; Soil solution; Equilibrium; Buffering capacity;
 Nutrient uptake; Prediction; Equations; Solubility; Nutrient
 availability; Transport processes
 
 
 57                                   NAL Call. No.: 56.8 SO3
 The effect of soil properties on phosphorus sorption by
 everglades histosols. Porter, P.S.; Sanchez, C.A.
 Baltimore, Md. : Williams & Wilkins; 1992 Nov.
 Soil science v. 154 (5): p. 387-398; 1992 Nov.  Includes
 references.
 
 Language:  English
 
 Descriptors: Florida; Histosols; Agricultural soils;
 Phosphorus; Sorption; Movement in soil; Leaching; Losses from
 soil systems; Soil chemistry; Soil properties; Water
 pollution; Indexes; Models
 
 
 58                                  NAL Call. No.: 292.8 J82
 The effect of transverse dispersion on solute transport in
 soils. Leij, F.J.; Dane, J.H.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1991 Jan.
 Journal of hydrology v. 122 (1/4): p. 407-422; 1991 Jan. 
 Includes references.
 
 Language:  English
 
 Descriptors: Solutes; Transport processes; Horizontal flow;
 Two dimensional flow; Transverse distribution; Permeability;
 Simulation; Mathematical models
 
 Abstract:  Most theoretical and experimental investigations of
 solute transport involve one-dimensional problems (i.e. soil
 column studies), whereas in reality many soil pollution
 problems concern transport and flow in more than one
 dimension. This study investigates two-dimensional transport,
 with emphasis on the contribution of transverse dispersion to
 solute transport. Three problems were studied with a finite
 element code. The first problem involved one-dimensional flow
 parallel to the interface of two layers with differing pore-
 water velocity. The early arrival of the solute at the end of
 the low-permeability layer and the increase-in solute
 spreading for both layers, as a result of transverse
 dispersion, were demonstrated. The two other problems
 concerned transport of a pollutant from a point source and a
 diffuse source, respectively, located at the soil surface. The
 magnitude of the transverse dispersion coefficient influenced
 the region to which the pollution extended as well as the
 intensity of the pollution.
 
 
 59                                 NAL Call. No.: 292.8 W295
 The effect of vertical soil heterogeneity on field scale
 solute flux. Destouni, G.
 Washington, D.C. : American Geophysical Union; 1992 May.
 Water resources research v. 28 (5): p. 1303-1309; 1992 May. 
 Includes references.
 
 Language:  English
 
 Descriptors: Solutes; Transport processes; Flow; Saturated
 hydraulic conductivity; Soil depth; Stochastic models
 
 Abstract:  Vertical heterogeneity is incorporated in a
 stochastic transport model, in which the soil is viewed as
 consisting of an ensemble of essentially vertical, independent
 stream tubes. The saturated hydraulic conductivity in each
 stream tube is defined as the vertical average of the
 corresponding point random process. The statistics of the
 vertically averaged hydraulic conductivity and the resulting
 statistics of solute travel time are depth dependent. The
 evolution of the field scale breakthrough curve with depth is
 analyzed in terms of the first two moments of solute travel
 time to an arbitrary depth below the soil surface. The arrival
 time of the solute center of mass, quantified by the expected
 travel time, grows linearly with depth also for vertically
 heterogeneous soil. The temporal solute spreading around its
 center, quantified by the travel time variance, may exhibit a
 compression-expansion that is qualitatively analogous to the
 solute plume behavior in the studies of Butters and Jury
 (1989), Russo (1991), and Ellsworth and Jury (1991). The
 relative solute spreading, quantified by the travel time
 coefficient of variation, decreases with increasing depth.
 
 
 60                                   NAL Call. No.: QH540.J6
 Effects of climatic variations over 11 years on nitrate-
 nitrogen concentrations in the Raccoon River, Iowa.
 Lucey, K.J.; Goolsby, D.A.
 Madison, Wis. : American Society of Agronomy; 1992 Jan.
 Journal of environmental quality v. 22 (1): p. 38-46; 1992
 Jan.  Includes references.
 
 Language:  English
 
 Descriptors: Iowa; Nitrate nitrogen; Drinking water; Seasonal
 variation; Precipitation; Stream flow; Water quality; Water
 pollution; Nitrogen fertilizers; Mathematical models
 
 Abstract:  Nitrate-nitrogen (NO3-N) concentrations at public
 water-supply intakes on the Des Moines and Raccoon Rivers in
 Iowa exceeded the maximum contaminant level (MCL) of 10 mg L-1
 for public water supplies established by the USEPA for
 extended periods of time from March through early August 1990.
 The excessive NO3-N levels followed 2 yr of less than normal
 precipitation in 1988 and 1989. The largest daily NO3-N load
 (771 t) transported during the last 17 yr in the Raccoon River
 occurred in June 1990. The streamflow hydrograph for the
 Raccoon River for March 1990 prior to seasonal fertilizer
 application indicates that high NO3-N concentrations
 characterize the recession side of the hydrograph. High NO3-N
 concentrations in streamflow persisted as streamflow decreased
 to baseflow conditions. This implies that substantial
 quantities of NO3-N were being leached from the soil and
 transported by subsurface flow during early 1990. A multiple
 linear-regression model was developed to predict NO3-N
 concentrations in the Raccoon River from readily-obtainable
 streamflow and climatic data. The four-variable model
 explained about 70% of the variability in the concentration of
 NO3-N. The mean streamflow for the previous 7-d period
 accounted for about 50% of the total variability.
 
 
 61                                NAL Call. No.: 290.9 AM32T
 Effects of pesticide, soil, and rainfall characteristics on
 potential pesticide loss by percolation--a GLEAMS simulation.
 Truman, C.C.; Leonard, R.A.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1991 Nov. Transactions of the ASAE v. 34 (6): p.
 2461-2468; 1991 Nov.  Includes references.
 
 Language:  English
 
 Descriptors: Georgia; Pesticides; Percolation; Leaching;
 Losses from soil systems; Water pollution; Groundwater;
 Computer simulation; Zea mays
 
 Abstract:  Potential pesticide loss in soil percolate is
 influenced by pesticide persistence and sorption by soil
 constituents (organic matter). Pesticide persistence,
 expressed as half-life (t1/2), changes with soil depth as
 microbial activity and soil properties change. Little is
 known, however, how these changes influence potential
 pesticide transport out of the root zone. Objectives of this
 study were to investigate relative differences in potential
 pesticide losses from the root zone by percolation due to 1)
 different soil surface and subsurface textures and pesticide
 t1/2, and 2) interactions between pesticide t1/2 arid timing
 of rainfall after pesticide application. The GLEAMS
 (Groundwater Loading Effects of Agricultural Management
 Systems) model and a 50-year historical rainfall record at
 Tifton, Georgia, were used to simulate pesticide losses by
 percolation from three soils ranging in surface texture from
 sand to sandy clay loam. Hypothetical pesticides had surface
 t1/2 of 5, 15, 30, and 60 d and a range of subsurface t1/2
 (2.5-360 d), and were applied to continuous corn (Zea maize,
 L.) at 2 kg ha-1 as surface spray at planting each year on 1
 April. Simulated pesticide losses by percolation increased
 with increased surface and subsurface t1/2, and decreased with
 increased KOC (adsorption constant based on soil organic
 matter) values. Potential pesticide leaching was greatest for
 Lakeland sand and least for Greenville sandy clay loam.
 Rainfall timing affected simulated pesticide loss by
 percolation, especially for nonpersistent pesticides. For
 short pesticide t1/2 (0-5 d), excessive rainfall events within
 1 t1/2 were largely responsible for simulated pesticide loss
 by percolation. Results indicate that changes in pesticide
 t1/2 in surface and subsurface horizons of different soils
 influence potential pesticide leaching from the root zone, and
 models (i.e., GLEAMS) can be used to provide comparative
 analysis of soil-pesticide-climate interactions. For example,
 dependi
 
 
 62                                 NAL Call. No.: 292.8 W295
 Effects of rainfall, vegetation, and microtopography on
 infiltration and runoff.
 Dunne, T.; Zhang, W.; Aubry, B.F.
 Washington, D.C. : American Geophysical Union; 1991 Sep.
 Water resources research v. 27 (9): p. 2271-2285; 1991 Sep. 
 Includes references.
 
 Language:  English
 
 Descriptors: Soil water; Infiltration; Runoff; Rain; Hill
 grasslands; Slope; Plant density; Hydraulic conductivity;
 Mathematical models
 
 Abstract:  Apparent, or effective, infiltration rates on
 grassland hillslopes vary with rainfall intensity and flow
 depth because of the interaction between rainfall, runoff, and
 vegetated microtopography. The higher parts of the
 microtopography are occupied by greater densities of
 macropores and therefore have much greater hydraulic
 conductivities than the intervening microdepressions. On short
 hillslopes and plots the apparent infiltration rate is simply
 the spatial average of the saturated and unsaturated
 conductivities of this surface. The proportion of the surface
 which is saturated and the value to which the unsaturated
 conductivity is raised depends on the rainfall intensity. On
 longer hillslopes the downslope increase in flow depth in
 microtopographic depressions progressively inundates more
 permeable, vegetated mounds so that the hydraulic conductivity
 of a greater proportion of the surface is raised to its
 saturated value. For this reason the apparent infiltration
 rate increases downslope, even in the absence of spatial
 trends in any of the surface characteristics that affect
 infiltration. Apparent, or effective, infiltration rate
 depends on hillslope length. Consequently, steady state
 discharge does not increase linearly with distance downslope.
 These two fundamental relationships between infiltration,
 rainfall intensity, and runoff are analyzed on the basis of
 sprinkling-infiltrometer measurements and a mathematical
 model.
 
 
 63                                 NAL Call. No.: 292.8 W295
 Effects of soil heterogeneity on pesticide leaching to
 groundwater. Zee, S.E.A.T.M. van der; Boesten, J.J.T.I.
 Washington, D.C. : American Geophysical Union; 1991 Dec.
 Water resources research v. 27 (12): p. 3051-3063; 1991 Dec. 
 Includes references.
 
 Language:  English
 
 Descriptors: Pesticides; Groundwater; Leaching; Hydrodynamic
 dispersion; Sorption; Transformation; Uptake; Physicochemical
 properties; Spatial variation; Stochastic models; Monte carlo
 method
 
 Abstract:  Pesticide leaching was simulated numerically
 assuming Freundlich adsorption, first-order transformation and
 passive plant uptake, taking transient flow, hydrodynamic
 dispersion, and depth as well as temperature dependence of
 (bio)chemical parameters into account. The dependency of the
 leached fraction on sorption and transformation parameters
 appeared to be in good general agreement with the model
 developed by Jury et al. (1987). We incorporated spatial
 variability of (bio)chemical parameters into the piston flow
 model and showed how spatial variability may be accounted for
 without having to resort to demanding Monte Carlo techniques.
 Such spatial variability affects the leached fraction
 significantly. The data requirement of the simple stochastic
 model is small and the versatility relatively high. For
 parameter values often not of prime practical interest for
 pesticide screening this model fails. Considering transport by
 convection and dispersion in the semi-infinite domain, this
 spatial variability can be easily accounted for using
 parameter ranges for which our original analytical model for
 spatially variable piston transport failed. In this revised
 model, hydrodynamic dispersion, preferential flow, and spatial
 variability of transformation, sorption and soil thickness are
 dealt with in a similar fashion, while both correlation or the
 absence of correlation of parameters can be incorporated
 through an approximation of apparent residence time variance.
 
 
 64                                   NAL Call. No.: QH540.J6
 Effects of spatial accumulation of runoff on watershed
 response. Garbrecht, J.
 Madison, Wis. : American Society of Agronomy; 1991 Jan.
 Journal of environmental quality v. 20 (1): p. 31-35; 1991
 Jan.  Literature review.  Includes references.
 
 Language:  English
 
 Descriptors: Watersheds; Drainage; Hydrology; Rain; Runoff;
 Simulation models
 
 Abstract:  The drainage network accumulates upstream
 subwatershed runoff into a single downstream response, with
 runoff accumulating at network junctions. The effects of this
 accumulation on the magnitude and spatial variability of the
 downstream response are reviewed for simplified boundary
 conditions. Runoff parameters are runoff depth and
 corresponding unit area peak runoff rate. At the subwatershed
 level these parameters are referred to as d and q,
 respectively, and they vary from one subwatershed to another.
 At a downstream location, after accumulation by the drainage
 network, corresponding parameters are referred to as D and Q.
 Equations expressing the effects of runoff accumulation are
 formulated and discussed for uniform rainfall conditions. The
 review shows that the effects of runoff accumulation gain in
 importance as the number of upstream subwatersheds and the
 size of the watershed increase in the downstream direction.
 The accumulation process cancels extreme values of d and q to
 yield a representative D and Q value for the entire upstream
 drainage area. The impact of individual d and q values on the
 downstream D and Q values in the channel diminishes as the
 number of upstream subwatersheds increases. This results in a
 decrease in the spatial variability of D and Q in the
 downstream direction. The review suggests that the role of
 spatial variability of upstream d and q in the determination
 of downstream D and Q diminishes as watershed size increases.
 However, nonuniform rainfall distributions and storm movement
 may overshadow the effects of runoff accumulation when
 watershed size increases beyond the size of the storm.
 
 
 65                                 NAL Call. No.: 325.28 P56
 Effects of suspended particle size and concentration on
 reflectance measurements.
 Bhargava, D.S.; Mariam, D.W.
 Bethesda, Md. : American Society of Photogrammetry and Remote
 Sensing; 1991 May.
 Photogrammetric engineering and remote sensing v. 57 (5): p.
 519-529; 1991 May.  Includes references.
 
 Language:  English
 
 Descriptors: Soil types; Suspensions; Particle size; Sediment;
 Concentration; Reflectance; Responses; Prediction; Models;
 Turbidity; Water quality; Equations; Remote sensing
 
 
 66                                   NAL Call. No.: TD403.G7
 Effects of waste-water irrigation on aqueous geochemistry near
 Paris, Texas. Tedaldi, D.J.; Loehr, R.C.
 Dublin, Ohio : Ground Water Pub. Co; 1992 Sep.
 Ground water v. 30 (5): p. 709-719; 1992 Sep.  Includes
 references.
 
 Language:  English
 
 Descriptors: Texas; Waste water; Irrigation; Long term
 experiments; Groundwater; Water quality; Soil chemistry;
 Geochemistry; Prediction; Thermodynamics; Equilibrium; Models;
 Aquifers; Saline water; Recharge; Infiltration; Hydraulic
 conductivity
 
 
 67                                 NAL Call. No.: TD420.A1E5
 Elution of aged and freshly added herbicides from a soil.
 Pignatello, J.J.; Ferrandino, F.J.; Huang, L.Q.
 Washington, D.C. : American Chemical Society; 1993 Aug.
 Environmental science & technology v. 27 (8): p. 1563-1571;
 1993 Aug. Includes references.
 
 Language:  English
 
 Descriptors: Connecticut; Soil pollution; Herbicide residues;
 Atrazine; Metolachlor; Leaching; Profiles; Models
 
 
 68                                 NAL Call. No.: S539.5.J68
 Environmental and economic impacts of pesticide and irrigation
 practices: EPIC-PST simulation.
 Sabbagh, G.J.; Norris, P.E.; Geleta, S.; Bernado, D.J.;
 Elliott, R.L.; Mapp, H.P.; Stone, J.F.
 Madison, Wis. : American Society of Agronomy; 1992 Jul.
 Journal of production agriculture v. 5 (3): p. 312-317; 1992
 Jul.  Includes references.
 
 Language:  English
 
 Descriptors: Oklahoma; Groundwater pollution; Crop management;
 Environmental impact; Economic impact; Pest control;
 Irrigation; Computer techniques; Simulation models;
 Pesticides; Movement in soil; Runoff
 
 
 69                                 NAL Call. No.: 292.8 W295
 Estimating changes in recreational fishing participation from
 national water quality policies.
 Ribaudo, M.O.; Piper, S.L.
 Washington, D.C. : American Geophysical Union; 1991 Jul.
 Water resources research v. 27 (7): p. 1757-1763; 1991 Jul. 
 Includes references.
 
 Language:  English
 
 Descriptors: Water quality; Water policy; Water pollution;
 Angling; Participation; Estimation; Models
 
 Abstract:  The complete evaluation of the offsite effects of
 national policies or programs that affect levels of
 agricultural nonpoint source pollution requires linking
 extensive water quality changes to changes in recreational
 activity. A sequential decision model is specified to describe
 an individual's decisions about fishing. A participation model
 for recreational fishing that includes a water quality index
 reflecting regional water quality is developed and estimated
 as a logit model with national level data. A visitation model
 for those who decide to fish that also includes the water
 quality index is estimated using ordinary least squares. The
 water quality index is found to be significant in the
 participation model but not in the visitation model. Together,
 the two models provide a means of estimating how changes in
 water quality might influence the number of recreation days
 devoted to fishing. The model is used to estimate changes in
 fishing participation for the Conservation Reserve Program.
 
 
 70                                  NAL Call. No.: TC401.W27
 Estimating low flow characteristics in ungauged catchments.
 Nathan, R.J.; McMahon, T.A.
 Dordrecht : Kluwer Academic Publishers; 1992.
 Water resources management v. 6 (2): p. 85-100; 1992. 
 Includes references.
 
 Language:  English
 
 Descriptors: New South Wales; Victoria; Watersheds; Rural
 areas; Flow; Characteristics; Water yield; Rain; Runoff;
 Models; Multivariate analysis; Climatic factors; Hydrological
 data; Equations
 
 
 71                                  NAL Call. No.: 292.8 J82
 Estimating transport parameters at the grid scale: on the
 value of a single measurement.
 Beven, K.J.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1993 Mar01.
 Journal of hydrology v. 143 (1/2): p. 109-123; 1993 Mar01. 
 Special Issue: Modelling Flow and Transport in the Unsaturated
 Zone: Scale Problems and Spatial Variability.  Includes
 references.
 
 Language:  English
 
 Descriptors: Solutes; Transport processes; Soil water; Flow;
 Spatial variation; Hydrodynamic dispersion; Prediction;
 Estimation; Probabilistic models
 
 Abstract:  Distributed models of solute transport at the field
 and catchment scales require the specification of effective
 parameters at the model grid scale. The grid scale will
 generally be much larger than the scale at which it is
 possible to make measurements to derive parameter values but
 may be of the same order as the scale of variability of such
 'point' values. In addition, measurements are usually
 expensive and time consuming to make and where, for example,
 'undisturbed' soil cores are used, may be destructive. This
 paper describes a conditional probability based approach for
 estimating grid scale effective parameter values in the light
 of expected spatial heterogeneity, given only one or a small
 number of available measurements. Initial results show,
 somewhat surprisingly, that despite the integrative nature of
 the spatial averaging involved in moving to the grid scale,
 the variance of the effective grid element values does not
 decrease. There is a small shift in the location of the
 distribution, as a result of the macrodispersive effect of the
 grid scale variability.
 
 
 72                                  NAL Call. No.: GB746.W33
 Estimation of possible anthropogenic changes in the runoff and
 removal of biogenic elements from small watersheds of the
 forest zone on the basis of a mathematical model.
 Kondrat'ev, S.A.
 New York, N.Y. : Consultants Bureau; 1991 Mar.
 Water resources v. 17 (3): p. 240-248; 1991 Mar.  Tranlated
 from: Vodnye Resursy, V. 17, No. 3, May/June 1990, p. 24-32.
 (GB746.V55).  Includes references.
 
 Language:  English; Russian
 
 Descriptors: U.S.S.R.in europe; Rsfsr; Runoff water; Sediment;
 Formation; Water pollution; Nutrients; Removal; Phosphorus;
 Nitrogen; Agricultural production; Effects; Watersheds;
 Forests; Hydrology; Mathematical models
 
 
 73                                  NAL Call. No.: 292.8 J82
 Evaluating the green and ampt infiltration parameter values
 for tilled and crusted soils.
 Mohamoud, Y.M.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1991 Feb.
 Journal of hydrology v. 123 (1/2): p. 25-38; 1991 Feb. 
 Includes references.
 
 Language:  English
 
 Descriptors: Illinois; Agricultural soils; Rain; Infiltration;
 Soil water content; Runoff; Surface layers; Tillage; Crop
 residues; Crusts; Permeability; Capillary rise; Wetting front;
 Hydraulic conductivity; Mathematical models; Green and ampt
 equation
 
 Abstract:  Methods for determining Green-Ampt infiltration
 parameter values for tilled and crusted soils are not well
 established. A two-stage method is developed to determine the
 Green and Ampt parameter values for soils under different
 management practices. The first stage is aimed at calculating
 rainfall infiltration from rainfall and runoff data of small
 field plots which had different soil surface conditions (e.g.
 tillage, residue cover and crusting). To determine accurate
 rainfall infiltration rates from field plots, we employed a
 water balance model which accounted for depression storage,
 detention storage as well as surface routing of runoff. The
 second stage is aimed at evaluating the values of the Green
 and Ampt infiltration equation parameters by the linear least
 squares parameter estimation technique. The Green and Ampt
 parameter values determined were the effective capillary
 suction at the wetting front and the effective hydraulic
 conductivity. The results of this study indicated that this
 procedure is sufficiently sensitive to reflect the effects of
 tillage, residue cover and crusting on infiltration data.
 Raindrop impact reduced infiltration rates by crusting the
 soil surface. However, most of the management systems that
 left about 30% of residue cover protected the soil from
 raindrop impact as evidenced by the higher effective hydraulic
 conductivity. It is concluded that the model developed by
 Green and Ampt in 1911 satisfactorily fitted the infiltration
 data obtained from protected and crusted soil profiles. Also,
 residue cover and crusting greatly influenced the Green and
 Ampt infiltration parameter values.
 
 
 74                                 NAL Call. No.: TP995.A1I5
 Evaluating transport of organic chemicals in soil resulting
 from underground fuel tank leaks.
 Lee, D.Y.; Chang, A.C.
 Chelsen, Mich. : Lewis Publishers; 1992.
 Proceedings of the Industrial Waste Conference (46): p.
 131-140; 1992. Meeting held May 14-16, 1991, West Lafayette,
 Indiana.  Includes references.
 
 Language:  English
 
 Descriptors: Polluted soils; Soil pollution; Organic
 compounds; Petroleum; Petroleum hydrocarbons; Transport
 processes; Fuel tanks; Leakage; Underground storage;
 Simulation models; Equations; Mathematics; Groundwater
 pollution; Soil water movement; Movement in soil
 
 
 75                      NAL Call. No.: GB701.W375 no.91-4142
 Evaluation of a ground-water flow and transport model of the
 upper Coachella Valley, California..  Evaluation of a ground
 water flow and transport model of the upper Coachella Valley,
 California
 Reichard, Eric George; Meadows, J. Kevin
 Geological Survey (U.S.),California Regional Water Quality
 Control Board--Colorado River Basin Region
 Sacramento, Calif. : U.S. Geological Survey ; Denver, CO :
 Books and Open-File Reports Section [distributor],; 1992.
 vi, 101 p. : ill., maps ; 28 cm. (Water-resources
 investigations report ; 91-4142).  Includes bibliographical
 references (p. 42).
 
 Language:  English
 
 Descriptors: Groundwater flow; Water, Underground
 
 
 76                                  NAL Call. No.: TD426.J68
 Evaluation of a pesticide mobility index: impact of recharge
 variation and soil profile heterogeneity.
 Kleveno, J.J.; Loague, K.; Green, R.E.
 Amsterdam : Elsevier; 1992 Oct.
 Journal of contaminant hydrology v. 11 (1/2): p. 83-99; 1992
 Oct.  Includes references.
 
 Language:  English
 
 Descriptors: Hawaii; Soil pollution; Pesticides; Profiles;
 Movement in soil; Attenuation; Leaching; Assessment;
 Simulation models; Errors; Movement to roots; Rain
 
 
 77                                NAL Call. No.: 290.9 AM32T
 Evaluation of fluvial sediment transport equations for
 overland flow. Guy, B.T.; Dickinson, W.T.; Rudra, R.P.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1992 Mar. Transactions of the ASAE v. 35 (2): p.
 545-555. ill; 1992 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Geological sedimentation; Overland flow; Rain;
 Runoff; Splash erosion; Simulation models
 
 Abstract:  Sediment transport capacity was measured under a
 range of conditions in two types of overland flow: shallow
 uniform flow in the absence of rainfall, and shallow flow
 affected by rainfall impact. The abilities of six fluvial
 sediment transport equations to represent each dataset are
 evaluated. For both flow types, common aspects of equation
 performance include poor representation of sediment transport
 thresholds, underprediction of transport rates, and
 significant scatter about measured values. These problems,
 particularly the equations' inability to predict transport
 threshold, are more evident with the rain-impacted now data.
 Only the Schoklitsch equation is suitable for uniform overland
 flow without rain-impact, and none am suitable for rain-
 impacted overland flow.
 
 
 78                                NAL Call. No.: 290.9 AM32T
 Evaluation of PRZM and LEACHMP on intact soil columns.
 Smith, W.N.; Prasher, S.O.; Barrington, S.F.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1991 Nov. Transactions of the ASAE v. 34 (6): p.
 2413-2420; 1991 Nov.  Includes references.
 
 Language:  English
 
 Descriptors: Atrazine; Computer simulation; Leaching; Soil
 properties; Water pollution
 
 Abstract:  Limiting factors towards the utilization of
 pesticide transport models are lack of both detailed data and
 cognizant personnel available to test and validate model
 predictions. In this study, computer simulations were carried
 out to test the performance of PRZM (a management model) and
 LEACHMP (a research model) on leaching characteristics of
 atrazine in long intact soil columns. Also, in an attempt to
 evaluate model uncertainty, a sensitivity analysis of several
 parameters for each model was considered. LEACHMP was found to
 be superior in predicting hydrological characteristics in the
 soil columns as compared to PRZM which required calibration.
 Both models underestimated levels of atrazine near the soil
 surface and in the leachate (115 cm depth) and over-estimated
 them throughout most of the range in-between. Inaccurate
 predictions for the two models are attributed to simplistic
 linear adsorption equations and lack of a macropore flow
 subroutine. In increasing order, PRZM was most sensitive to
 rate of application, distribution coefficient, bulk density
 and field capacity, whereas LEACHMP was sensitive to rate of
 application, organic carbon distribution coefficient, air
 entry value, and bulk density.
 
 
 79                                  NAL Call. No.: 292.8 J82
 Evaluation of the accuracy and precision of annual phosphorus
 load estimates from two agricultural basins in Finland.
 Rekolainen, S.; Posch, M.; Kamari, J.; Ekholm, P.
 Amsterdam : Elsevier Scientific Publishers, B.V.; 1991 Nov.
 Journal of hydrology v. 128 (1/4): p. 237-255; 1991 Nov. 
 Includes references.
 
 Language:  English
 
 Descriptors: Finland; Agricultural land; Drainage; Runoff;
 Pollution; Phosphorus; Transport processes; Flow; Estimates;
 Sampling; Frequency; Monitoring; Mathematical models;
 Comparisons
 
 Abstract:  The accuracy and precision of phosphorus load
 estimates from two agricultural drainage basins in western
 Finland were evaluated, based on continuous flow measurements
 and frequent flow-proportional sampling of total phosphorus
 concentration during a 2 year period. The objective was to
 compare different load calculation methods and to evaluate
 alternative sampling strategies. An hourly data set of
 concentrations was constructed by linear interpolation, and
 these data were used in Monte Carlo runs for producing
 replicate data sets for calculating the accuracy and precision
 of load estimates. All estimates were compared with reference
 values computed from the complete hourly data sets. The load
 calculation methods based on summing the products of regularly
 sampled flows and concentrations produced the best precision,
 whereas the best accuracy was achieved using methods based on
 multiplying annual flow by flow-weighted annual mean
 concentration. When comparing different sampling strategies,
 concentrating sampling in high runoff periods (spring and
 autumn) was found to give better accuracy and precision than
 strategies based on regular interval sampling throughout the
 year. However, the best result was obtained by taking samples
 flow-proportionally within the highest peak flows plus
 additional regular interval (e.g. biweekly) samples outside
 these flow peaks. Using this strategy, which calls for
 automatic sampling equipment, accuracies better than 5% and
 precisions better than 10% can be achieved with only 30-50
 samples per year.
 
 
 80                                NAL Call. No.: 290.9 AM32T
 Evaluation of the hydrologic component of the ADAPT water
 table management model.
 Chung, S.O.; Ward, A.D.; Schalk, C.W.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1992 Mar. Transactions of the ASAE v. 35 (2): p.
 571-579; 1992 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Tile drainage; Water management; Water table;
 Evapotranspiration; Hydrology; Macropore flow; Runoff;
 Seepage; Simulation models
 
 Abstract:  A subsurface, water table management model ADAPT
 (Agricultural Drainage and Pesticide Transport) has been
 developed by combining drainage and subirrigation algorithms
 from DRAINMOD with the GLEAMS model. In addition, the model
 incorporates improved snow melt and runoff algorithms,
 macropore flow due to cracking, and deep seepage. Theory for
 the hydrologic components of the model is presented together
 with an evaluation of the model using data from a long-term
 field experiment at Castalia in North Central Ohio. Predicted
 surface runoff, subsurface drainage, and combined surface and
 subsurface drainage are compared with the field observations.
 In general, the model predictions are within the range of the
 variations of the observed replications. Sensitivity analysis
 shows that surface runoff estimates are sensitive to changes
 in curve number, while subsurface drainage flows are sensitive
 to deep seepage estimates. Model input requirements are not
 excessive and the model gives reasonable estimates of the
 hydrologic component of water table management systems. ADAPT
 can be used in designing water table management systems and
 does not require extensive calibration. The pesticide
 component of ADAPT is currently being evaluated and
 development of a nutrient component has been initiated.
 
 
 81                                    NAL Call. No.: 4 AM34P
 Evaluation of the nitrogen submodel of CERES-maize following
 legume green manure incorporation.
 Bowen, W.T.; Jones, J.W.; Carsky, R.J.; Quintana, J.O.
 Madison, Wis. : American Society of Agronomy; 1993 Jan.
 Agronomy journal v. 85 (1): p. 153-159; 1993 Jan.  Includes
 references.
 
 Language:  English
 
 Descriptors: Simulation models; Prediction; Nutrient uptake;
 Nitrogen; Green manures; Nutrient availability;
 Mineralization; Leaching; Nitrate; Losses from soil; Nitrogen
 balance
 
 Abstract:  Crop simulation models that accurately predict the
 availability of N from decomposing plant residues would
 provide a powerful tool for evaluating legume green manures as
 potential N sources for nonlegume crops. Using measured data
 from a series of field experiments conducted on an Oxisol in
 central Brazil, we conducted this study to test the N submodel
 of CERES-Maize for its ability to simulate N mineralization,
 nitrate leaching, and N uptake by maize (Zea Mays L.)
 following the incorporation of 10 different legume green
 manures. Legume or weed residue N at the time of incorporation
 varied from 25 to 300 kg ha-1 with C/N ratios varying from 13
 to 37. Comparison of predicted and measured accumulation of
 inorganic N in uncropped soil showed that the model usually
 provided a realistic simulation of legume N release, although
 N release was overpredicted for some legumes. For all legumes,
 both simulated and measured data showed that about 60% of the
 organic N applied was recovered as inorganic N within 120 to
 150 d after incorporation. To realistically simulate N
 availability when rainfall was excessive, we modified the
 model to account for delayed leaching due to nitrate retention
 in the subsoil. Nitrogen uptake by maize was generally
 overpredicted at high levels of available N. The N submodel
 was shown to realistically simulate legume N release, but
 further work is needed to determine the importance of subsoil
 nitrate retention in other soils and how best such retention
 might be described in the model.
 
 
 82                                NAL Call. No.: 290.9 AM32T
 An evaluation of unit stream power theory for estimating soil
 detachment and sediment discharge from tilled soils.
 McIsaac, G.F.; Mitchell, J.K.; Hummel, J.W.; Elliot, W.J. St.
 Joseph, Mich. : American Society of Agricultural Engineers;
 1992 Mar. Transactions of the ASAE v. 35 (2): p. 535-544; 1992
 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Illinois; Water erosion; Aggregates; Runoff;
 Sediment yield; Simulation models; Soil properties; Streams;
 Tillage
 
 Abstract:  Unit Stream Power (USP) and the associated Yang
 (1973) sediment transport equations were compared to soil
 detachment rates and sediment concentrations in runoff from
 eroding soils. Although USP was significantly correlated with
 rill detachment rates, potential energy dissipation rate per
 unit rill area was a better predictor of soil detachment
 rates. The Yang (1973) equations estimated sediment
 concentrations within a factor of 10 of the observed
 concentrations, if the median soil aggregate diameter was
 within the range of diameters used by Yang to estimate the
 equation parameters. When median aggregate sizes were less
 than 0.15 mm, the lower limit of Yang's (1973) calibration
 range, the equations tended to produce unrealistically large
 estimates of sediment concentration.
 
 
 83                NAL Call. No.: ViBlbVLD5655.V856 1992.J663
 Evaluation of water distribution system monitoring using
 stochastic dynamic modeling.
 Jones, Philip Edward James,
 1992; 1992.
 xiv, 215 leaves : ill. ; 28 cm.  Vita.  Abstract. 
 Bibliography: leaves 181-191.
 
 Language:  English
 
 Descriptors: Water quality management; Water
 
 
 84                                   NAL Call. No.: 56.8 SO3
 Exit condition for miscible displacement experiments.
 Parlange, J.Y.; Starr, J.L.; Van Genuchten, M.Th; Barry, D.A.;
 Parker, J.C. Baltimore, Md. : Williams & Wilkins; 1992 Mar.
 Soil science v. 153 (3): p. 165-171; 1992 Mar.  Includes
 references.
 
 Language:  English
 
 Descriptors: Transport processes; Solutes; Soil solution; Soil
 analysis; Mathematical models; Determination; Convection;
 Dispersion; Length; Movement in soil; Kinetics
 
 
 85                                   NAL Call. No.: 56.8 SO3
 Experimental and simulated B transport in soil using a
 multireaction model. Mansell, R.S.; Bloom, S.A.; Burgoa, B.;
 Nkedi-Kizza, P.; Chen, J.S. Baltimore, Md. : Williams &
 Wilkins; 1992 Mar.
 Soil science v. 153 (3): p. 185-194; 1992 Mar.  Includes
 references.
 
 Language:  English
 
 Descriptors: Florida; Spodosols; Acid soils; Sandy soils; B
 horizons; Subsurface layers; Phosphorus; Movement in soil;
 Transport processes; Soil water movement; Determination;
 Laboratory methods; Simulation models; Mathematical models;
 Sorption; Kinetics; Sorption isotherms; Comparisons; Fixation;
 Soil organic matter; Aluminum oxide; Iron oxides
 
 
 86                                  NAL Call. No.: HC79.E5E5
 Exploring the effects of multiple management objectives and
 exotic species on Great Lakes food webs and contaminant
 dynamics.
 Fontaine, T.D.; Stewart, D.J.
 New York, N.Y. : Springer-Verlag; 1992 Mar.
 Environmental management v. 16 (2): p. 225-229; 1992 Mar. 
 Includes references.
 
 Language:  English
 
 Descriptors: Fishery management; Lakes; Water quality; Food
 chains; Objectives; Simulation models
 
 
 87                                 NAL Call. No.: S539.5.J68
 Farm-level economic and environmental impacts of eastern Corn
 Belt cropping systems.
 Foltz, J.C.; Lee, J.G.; Martin, M.A.
 Madison, WI : American Society of Agronomy, c1987-; 1993 Apr.
 Journal of production agriculture v. 6 (2): p. 290-296; 1993
 Apr.  Includes references.
 
 Language:  English
 
 Descriptors: Corn belt states of U.S.A.; Cabt; Zea mays;
 Medicago sativa; Glycine max; Microeconomic analysis; Economic
 impact; Alternative farming; Environmental impact; Rotations;
 Continuous cropping; Simulation models; Computer simulation;
 Erosion; Runoff; Pesticides; Water pollution
 
 
 88                                   NAL Call. No.: TD201.A4 A
 fast and accurate method for solving subsurface contaminant
 transport problems with a single uncertain parameter.
 Ahlfeld, D.P.; Pinder, G.F.
 Essex : Elsevier Science Publishers Ltd; 1992.
 Advances in water resources v. 15 (2): p. 143-150; 1992. 
 Includes references.
 
 Language:  English
 
 Descriptors: Groundwater pollution; Contaminants; Transport;
 Equations; Random sampling; Stochastic models; Groundwater
 flow; Hydraulic conductivity
 
 
 89                                NAL Call. No.: QH545.A1E58
 Fate, dissipation and environmental effects of pesticides in
 southern forests: a review of a decade of research progress.
 Neary, D.G.; Bush, P.B.; Michael, J.L.
 Tarrytown, N.Y. : Pergamon Press; 1993 Mar.
 Environmental toxicology and chemistry v. 12 (3): p. 411-428;
 1993 Mar.  Paper presented at the "Symposium on Pesticides in
 Forest Management, 11th Annual Meeting of the Society of
 Environmental Toxicology and Chemistry," November 11-15, 1990,
 Arlington, Virginia.  Literature review.  Includes references.
 
 Language:  English
 
 Descriptors: Southern states of U.S.A.; Pesticides; Forestry;
 Ecosystems; Watersheds; Environmental impact; Water quality;
 Air quality; Groundwater pollution; Silviculture; Species
 diversity; Simulation models; Nontarget effects; Literature
 reviews
 
 
 90                                   NAL Call. No.: QH540.N3
 Fate of non-aqueous phase liquids: modeling of surfactant
 effects. Harwell, J.H.; Sabatini, D.A.; Soerens, T.S.
 Berlin, W. Ger. : Springer-Verlag; 1993.
 NATO ASI series : Series G : Ecological sciences v. 32: p.
 309-328; 1993.  In the series analytic: Migration and fate of
 pollutants in soils and subsoils / edited by D. Petruzzelli
 and F.G. Helfferich. Proceedings of the NATO Advanced Study
 Institute, May 24-June 5, 1992, Maratea, Italy.  Includes
 references.
 
 Language:  English
 
 Descriptors: Soil pollution; Groundwater pollution;
 Pollutants; Organic compounds; Transport processes;
 Groundwater flow; Soil water movement; Equations; Mathematics
 
 
 91                                 NAL Call. No.: TP963.A1F4
 Fertilization under drip irrigation.
 Bar-Yosef, B.
 New York, N.Y. : Marcel Dekker; 1991.
 Fertilizer science and technology series v. 7: p. 285-329;
 1991.  In the series analytic: Fluid fertilizer science and
 technology / edited by D.A. Palgrave.  Includes references.
 
 Language:  English
 
 Descriptors: Fertigation; Liquid fertilizers; Fluids; Trickle
 irrigation; Fertilizer requirement determination; Irrigation
 water; Ph; Salinity; Plant nutrition; Nutrient requirements;
 Nutrient uptake; Temporal variation; Nitrogen; Movement in
 soil; Transport processes; Spatial distribution; Root systems;
 Soil water content; Soil solution; Mathematical models;
 Monitoring; Fertilizer technology; Management; Crop production
 
 
 92                                    NAL Call. No.: QD1.A45
 Field and model estimates of pesticide runoff from turfgrass.
 Rosenthal, W.D.; Hipp, B.W.
 Washington, D.C. : The Society; 1993.
 ACS Symposium series - American Chemical Society (522): p.
 208-213; 1993.  In the series analytic: Pesticides in urban
 environments: Fate and significance / edited by K.D. Racke and
 A.R. Leslie. Paper presented at the 203rd National Meeting of
 the American Chemical Society, April 5-10, 1992, San
 Francisco, California.  Includes references.
 
 Language:  English
 
 Descriptors: Chlorpyrifos; Carbaryl; Diazinon; 2,4-d; Dicamba;
 Atrazine; Fertilizers; Herbicide residues; Insecticide
 residues; Runoff water; Mathematical models; Simulation
 models; Cynodon dactylon; Buchloe dactyloides
 
 Abstract:  Environmental awareness of surface runoff water
 quality is increasing. A study was conducted to analyze the
 impact of different turfgrass fertilizer and pesticide
 management systems on runoff water quality. A hydrologic and
 water quality model, Erosion Productivity Impact Calculator
 (EPIC), was used to estimate pesticide and nutrient
 concentrations in runoff from turfgrass on a Houston Black
 Clay. Nutrient and pesticide concentrations in the surface
 runoff increased significantly for highly maintained turfgrass
 systems. A larger fraction of the amount applied was observed
 in runoff for the moderate application rate treatments.
 Simulated results are being validated from measured runoff of
 turfgrass plots at Dallas, TX.
 
 
 93                          NAL Call. No.: S478.S68T43 no.31
 Field measurement and modelling of runoff and erosion response
 of small agricultural catchments in the mid north of South
 Australia. Punthakey, J.F.
 Adelaide, South Australia : Dept. of Agriculture,; 1992.
 v, 137 p. : ill. ; 30 cm. (Technical paper (South Australia.
 Dept. of Agriculture) ; no. 31.).  May 1992.  AGDEX 572. 
 Includes bibliographical references (p. 134-137) and index.
 
 Language:  English
 
 
 94                                   NAL Call. No.: 56.9 SO3
 Field study of bromacil transport under continuous-flood
 irrigation. Jaynes, D.B.
 Madison, Wis. : The Society; 1991 May.
 Soil Science Society of America journal v. 55 (3): p. 658-664;
 1991 May. Includes references.
 
 Language:  English
 
 Descriptors: Bromacil; Flood irrigation; Herbicide residues;
 Leaching; Movement in soil; Transport processes; Agricultural
 soils; Mathematical models
 
 Abstract:  The transport processes of sorbing chemicals in
 field soils are poorly understood. This study characterized
 the leaching behavior of the weakly sorbing herbicide bromacil
 (5-bromo-3-sec-butyl-6-methyluracil) in comparison to Br-
 during continuous-flood irrigation of a small field plot.
 Twenty-four solution samplers were used to periodically
 collect in situ samples from seven depths within four 1.83 by
 1.83 m subplots. Estimates of the pore water velocity (vs) and
 dispersion coefficient (D) were made by fitting an analytical
 solution of the convection-dispersion (CD) equation to the Br-
 data. Estimates of retardation (R) were made by fitting the CD
 equation to the bromacil data using the vs and D estimates
 from the Br- data and letting R be a fitting parameter.
 Estimates of R were also made from the results of batch
 equilibration studies using soil from seven depths. Best-fit
 vs and D values exhibited considerable variability from
 sampler to sampler (CV = 1.25 and 1.30, respectively) and
 showed no significant trends with depth. Retardation values
 estimated from the CD equation averaged 1.88, but varied from
 1.21 to 3.35 and also showed no significant trend with depth.
 In contrast, batch equilibration studies showed the absorption
 properties of the surface 0.6 m of soil to be significantly
 different than the 0.6- to 3-m depth, with R values decreasing
 from 1.62 for the surface 0.6 m to 1.31 at 3 m. Although the
 two methods gave the same estimate of R in the surface soil
 neither the lower R values at deeper depths nor the tendency
 to decrease with depth as predicted from the batch studies was
 apparent in the transport data. Using D as an additional
 fitting parameter to the bromacil data resulted in an average
 increase of 1.96 for this parameter, indicating more
 dispersion for the sorbing solute. Increased dispersion and
 increased tailing of the sorbed solute may be attributed to
 spatially variable adsorption and to a negative correlation
 between vs and R (r = -0.524)
 
 
 95                                NAL Call. No.: 290.9 AM32T
 Field testing and comparison of the PRZM and GLEAMS models.
 Smith, M.C.; Bottcher, A.B.; Campbell, K.L.; Thomas, D.L. St.
 Joseph, Mich. : American Society of Agricultural Engineers;
 1991 May. Transactions of the ASAE v. 34 (3): p. 838-847; 1991
 May.  Includes references.
 
 Language:  English
 
 Descriptors: Georgia; Alachlor; Atrazine; Bromides; Field
 tests; Leaching; Groundwater; Pesticides; Precipitation;
 Runoff; Simulation models; Soil properties; Soil water
 
 Abstract:  The root/vadose zone transport models PRZM and
 GLEAMS were tested against an experimental data set.
 Parameters were not optimized or calibrated to produce the
 best fit. In all cases the measured and predicted peak
 concentrations agreed within an order of magnitude, and in
 most cases agreed within a factor of 2 to 3. This level of
 agreement between the models and the measured data is within
 the criteria for model acceptance suggested by the EPA. The
 small differences noted in simulated transport between the
 models are thought to be a result of differences in
 computational layering and chemical transport calculation
 methods.
 
 
 96                                  NAL Call. No.: TD426.J68
 Fluid flow and solute transport processes in unsaturated
 heterogeneous soils: Preliminary numerical experiments.
 Liu, C.C.K.; Loague, K.; Feng, J.S.
 Amsterdam : Elsevier; 1991 Feb.
 Journal of contaminant hydrology v. 7 (3): p. 261-283; 1991
 Feb.  Includes references.
 
 Language:  English
 
 Descriptors: Movement in soil; Pollutants; Unsaturated flow;
 Mathematical models; Finite element analysis; Prediction;
 Aquifers
 
 
 97                                 NAL Call. No.: S539.5.J68
 Functional form selection for regional crop response to
 salinity, water application, and climate.
 Lee, D.J.
 Madison, Wis. : American Society of Agronomy; 1992 Oct.
 Journal of production agriculture v. 5 (4): p. 445-454; 1992
 Oct.  Includes references.
 
 Language:  English
 
 Descriptors: Zea mays; Sorghum bicolor; Triticum aestivum;
 Triticum turgidum; Irrigation; Application rates; Saline
 water; Water quality; Mathematical models; Crop yield; Soil
 salinity; Climatic factors
 
 
 98                                   NAL Call. No.: QH540.J6 A
 functional model of solute transport that accounts for bypass.
 Corwin, D.L.; Waggoner, B.L.; Rhoades, J.D.
 Madison, Wis. : American Society of Agronomy; 1991 Jul.
 Journal of environmental quality v. 20 (3): p. 647-658; 1991
 Jul.  Includes references.
 
 Language:  English
 
 Descriptors: Groundwater; Water quality; Transport processes;
 Solutes; Water management; Mathematical models
 
 Abstract:  Public awareness of groundwater contamination has
 created renewed interest in solute transport models that can
 be practically applied as groundwater quality management
 tools. Because of their simplicity with regard to input
 requirements, functional models of solute transport are
 excellent groundwater quality management tools. A functional
 model of one-dimensional solute transport that accounts for
 hydraulic bypass is presented. The transport model TETrans,
 simulates the vertical movement of nonvolatile solutes (i.e.,
 trace elements and nonvolatile organic chemicals) through the
 vadose zone. Plant water uptake is taken into account assuming
 no solute uptake by the plant. TETrans requires minimal input
 data for its operation. Since TETrans uses a mass-balance
 approach to solute transport, it offers the speed of an
 analytical solution and the versatility of a numerical
 approach without the need for input parameters, which are
 difficult to measure. TETrans is able to account for bypass
 with a single term, the mobility coefficient. The mobility
 coefficient, gamma, represents the fraction of the soil liquid
 phase, which is subject to piston-type displacement;
 therefore, 1 - gamma represents the fraction of the liquid
 phase that is bypassed. The mobility coefficient is a
 temporally and spatially variable parameter (within a range of
 0 to l) which is calculated from the deviation of the measured
 chloride concentration from the predicted concentration
 assuming piston displacement and assuming complete mixing of
 the resident soil solution and incoming water for a given
 irrigation and volume of soil. A constant mobility coefficient
 for a given depth or entire profile can be determined by
 averaging temporally varying mobility coefficients or
 averaging spatially and temporally varying mobility
 coefficients, respectively. In essence, the mobility
 coefficient simplistically accounts for three physical
 transport phenomena in a single term. On a microscopic level
 there is flow thr
 
 
 99                                NAL Call. No.: 290.9 AM32T
 Generic anaerobic digestion model for the simulation of
 various reactor types and substrates.
 Thomas, M.V.; Nordstedt, R.A.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1993 Mar. Transactions of the ASAE v. 36 (2): p.
 537-544; 1993 Mar.  Literature review. Includes references.
 
 Language:  English
 
 Descriptors: Florida; Agricultural wastes; Animal wastes;
 Hyacinths; Manures; Straw; Waste disposal; Anaerobic
 digestion; Literature reviews; Mathematical models; Methane
 production
 
 Abstract:  A mathematical model was developed to represent a
 wide variety of anaerobic reactor types and substrates. The
 model is a generic, anaerobic digestion process model, using
 lumped substrate parameters, and was developed for use as
 type-specific reactor model operating within the sphere of a
 larger system model. Three types of anaerobic reactors were
 simulated: fixed-bed reactors, conventional stirred tank
 reactors, and continuously expanding reactors. The generic
 anaerobic digestion model provided a tool for testing various
 values of conversion efficiency and kinetic parameters for a
 wide range of substrate types and reactor designs.
 
 
 100                                NAL Call. No.: 292.8 W295 A
 geochemical transport model for redox-controlled movement of
 mineral fronts in groundwater flow systems: a case of nitrate
 removal by oxidation of pyrite. Engesgaard, P.; Kipp, K.L.
 Washington, D.C. : American Geophysical Union; 1992 Oct.
 Water resources research v. 28 (10): p. 2829-2843; 1992 Oct. 
 Includes references.
 
 Language:  English
 
 Descriptors: Denmark; Groundwater flow; Transport processes;
 Denitrification; Pyrites; Oxidation; Nitrate; Reduction; Redox
 reactions; Geochemistry; Spatial distribution; Algorithms;
 Mathematical models; Simulation
 
 Abstract:  A one-dimensional prototype geochemical transport
 model was developed in order to handle simultaneous
 precipitation-dissolution and oxidation-reduction reactions
 governed by chemical equilibria. Total aqueous component
 concentrations are the primary dependent variables, and a
 sequential iterative approach is used for the calculation. The
 model was verified by analytical and numerical comparisons and
 is able to simulate sharp mineral fronts. At a site in
 Denmark, denitrification has been observed by oxidation of
 pyrite. Simulation of nitrate movement at this site showed a
 redox front movement rate of 0.58 m yr-1, which agreed with
 calculations of others. It appears that the sequential
 iterative approach is the most practical for extension to
 multidimensional simulation and for handling large numbers of
 components and reactions. However, slow convergence may limit
 the size of redox systems that can be handled.
 
 
 101                                 NAL Call. No.: 56.9 SO32
 Geographic information system for differentiating unused
 wells. Tan, Y.R.; Shih, S.F.
 S.l. : The Society; 1991.
 Proceedings - Soil and Crop Science Society of Florida v. 50:
 p. 110-116; 1991.  Paper presented at the "Symposium on
 Reality of Sustainable Agriculture in Florida, September
 26-28, 1990, Daytona Beach, FLorida.  Includes references.
 
 Language:  English
 
 Descriptors: Florida; Groundwater; Wells; Water management;
 Geographical distribution
 
 
 102                                    NAL Call. No.: QE1.E5
 Geostatistical modeling of salinity as a basis for irrigation
 management and crop selection--a case study in central
 Tunisia.
 Soderstrom, M.
 New York, N.Y. : Springer; 1992 Sep.
 Environmental geology and water sciences v. 20 (2): p. 85-92;
 1992 Sep. Includes references.
 
 Language:  English
 
 Descriptors: Tunisia; Groundwater; Saline water; Irrigation
 water; Spatial distribution; Soil salinity; Irrigated soils;
 Wells; Water; Soil; Sampling; Maps; Leaching; Models;
 Irrigation scheduling; Crop yield; Yield losses; Crops;
 Selection
 
 
 103                              NAL Call. No.: QH541.5.D4J6 A
 GIS approach to desertification assessment and mapping.
 Grunblatt, J.; Ottichilo, W.K.; Sinange, R.K.
 London : Academic Press; 1992 Jul.
 Journal of arid environments v. 23 (1): p. 81-102; 1992 Jul. 
 Includes references.
 
 Language:  English
 
 Descriptors: Kenya; Desertification; Remote sensing; Satellite
 imagery; Models; Geography
 
 
 104                                  NAL Call. No.: S671.A66
 GIS-assisted input data set development for the Finite Element
 Storm Hydrograph Model (FESHM).
 Wolfe, M.L.
 St. Joseph, Mich. : American Society of Agricultural
 Engineers; 1992 Mar. Applied engineering in agriculture v. 8
 (2): p. 221-227; 1992 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Hydrology; Simulation models; Automation;
 Computer techniques
 
 Abstract:  A study was conducted to develop an automated
 proceedings to assist in the development of input data sets
 for the FESHM hydrologic model using the GRASS geographic
 information system. Shell scripts (executable sequences of
 commands in the UNIX operating system) were developed to
 overlay soils and land use maps to generate hydrologic
 response unit (HRU) maps and to compute the fractional areas
 of HRUs in overland flow elements. The automated procedures
 decreased the input data set development time significantly,
 by approximately 250% (from five to two hours) for a 122 ha
 (303 ac) watershed. The time savings on larger, more variable
 watersheds would be even greater. The input data set
 development procedure provides an efficient manner for
 considering alternative land use and management scenarios.
 
 
 105                                NAL Call. No.: 292.9 AM34
 Ground water quality implications of soil conservation
 measures: an economic perspective.
 Setia, P.; Piper, S.
 Bethesda, Md. : American Water Resources Association; 1991
 Mar. Water resources bulletin v. 27 (2): p. 201-208; 1991 Mar. 
 Includes references.
 
 Language:  English
 
 Descriptors: Corn belt of U.S.A.; Soil conservation;
 Groundwater; Water quality; Pesticides; Runoff; Leaching;
 Agricultural economics; Usda; Federal programs
 
 Abstract:  An evaluation of the intermedia movement of
 pesticides applied under various land management systems
 already in place, or to be implemented, under the Conservation
 Reserve and Conservation Compliance programs is presented. The
 simulation modeling approach followed in this analysis
 consists of a mathematical programming model and
 leaching/surface runoff, Pesticide Root Zone Model (PRZM)
 models. Special care was taken to ensure that the physical
 model was sensitive to the chemical characteristics of
 individual pesticides and the important physical changes
 brought about by different agricultural practices. Results
 show that, although these programs as now planned, increase
 farm income and achieve soil conservation goals, they may
 adversely affect ground water quality. Also, depending on soil
 and location characteristics, there are tradeoffs between
 surface and ground water quality implications. Hence, if these
 programs are to address water quality problems, the
 recommended practices must be evaluated for their impact on
 water quality, particularly in potentially vulnerable areas.
 
 
 106                                   NAL Call. No.: QD1.A45
 Groundwater and surface water risk assessments for proposed
 golf courses. Cohen, S.Z.; Durborow, T.E.; Barnes, N.L.
 Washington, D.C. : The Society; 1993.
 ACS Symposium series - American Chemical Society (522): p.
 214-227; 1993.  In the series analytic: Pesticides in urban
 environments: Fate and significance / edited by K.D. Racke and
 A.R. Leslie. Paper presented at the 203rd National Meeting of
 the American Chemical Society, April 5-10, 1992, San
 Francisco, California.  Includes references.
 
 Language:  English
 
 Descriptors: Hawaii; Massachusetts; Golf courses; Golf green
 soils; Herbicide residues; Insecticide residues; Leaching;
 Leachates; Runoff; Surface water; Water pollution; Groundwater
 pollution; Mathematical models; Simulation models; Risk;
 Fungicides; Pesticide residues; Fertilizers; Nitrogen
 
 Abstract:  Proposed golf course developments usually require
 environmental impact statements in the U.S. Concerns about
 ground water, surface water, and near-shore coastal water
 quality and wetlands often require state-of-the-art risk
 assessments and complex computerized simulation modeling. It
 is extremely important to obtain site-specific data for these
 risk assessments. Thus soil sampling, test borings, stream
 surveys, and coastal surveys are often done. Daily weather
 records are obtained or generated. The new PRZM-VADOFT model
 pair is used for leaching assessments, even though nonlinear
 adsorption isotherms cannot be used. The SWRRBWQ model is
 difficult to use but it is appropriate for the modeling of
 complex drainage patterns at the basin and sub-basin scale, as
 with golf courses. Annual and storm-event runoff values are
 computed for pesticides, nutrients, runoff water, and
 sediments. It is best used for areas expected to experience
 appreciable runoff. EXAMS II provides useful predictions of
 stream water quality. An uncertainty analysis is a critical
 but often overlooked part of modeling. These results help fine
 tune proposed turf management programs and may indicate the
 need for design changes. Risk assessments in Hawaii are
 especially complex; they often indicate the need for detention
 basins.
 
 
 107                                NAL Call. No.: TD420.A1E5
 Herbicide transport in rivers: importance of hydrology and
 geochemistry in nonpoint-source contamination.
 Squillace, P.J.; Thurman, E.M.
 Washington, D.C. : American Chemical Society; 1992 Mar.
 Environmental science & technology v. 26 (3): p. 538-545; 1992
 Mar.  Includes references.
 
 Language:  English
 
 Descriptors: Iowa; Minnesota; Herbicide residues; Water
 pollution; River water; Groundwater pollution; Concentration;
 Models; Overland flow
 
 
 108                                  NAL Call. No.: S601.A34
 High bed-low ditch system in the Pearl River Delta, South
 China. Ming, L.S.; Jian, L.R.
 Amsterdam : Elsevier; 1991 Jun14.
 Agriculture, ecosystems and environment v. 36 (1/2): p.
 101-109; 1991 Jun14. Includes references.
 
 Language:  English
 
 Descriptors: China; Delta soils; Alluvial soils; Deltas;
 Subtropics; Saccharum officinarum; Musa paradisiaca; Citrus
 reticulata; Oryza sativa; Sustainability; Ditches; High water
 tables; Soil depth; Roots; Growth; Erosion; Sediment;
 Nutrients; Losses from soil systems; Cycling; Flow; Models;
 Crop production; Agricultural byproducts; Irrigation water;
 Rain; Runoff water; Drainage water; Fertilizers; Dry matter
 accumulation; Decomposition; Crop residues; Nitrogen;
 Phosphorus pentoxide; Potassium; Nutrient content; Temporal
 variation; Dry season; Rainy season; Water quality; Organic
 matter
 
 
 109                            NAL Call. No.: TC163.I54 1992
 Hydraulic and environmental modelling--estuarine and river
 waters proceedings of the Second International Conference on
 Hydraulic and Environmental Mod