1991
DOI: 10.2134/jeq1991.00472425002000020015x
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Modeling the Influence of Sorption and Transformation on Pesticide Leaching and Persistence

Abstract: Pesticide leaching to ground water at 1 m depth and pesticide persistence in the plow layer were calculated with a mathematical model for a sandy soil continuously cropped with maize (Zea mays L.) and exposed to weather conditions in a temperate climate. The pesticide was applied in spring. In the model, water flow was described by Darcy's law and water uptake by the crop was included. Dally averages of meteorological conditions (rainfall, evapotranspiration, soil temperature) were used as input. The model ass… Show more

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Cited by 237 publications
(139 citation statements)
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“…A change of a factor of two in herbicide sorption input parameters for modeling could result in a 10 times difference in herbicide leaching potential within a soil (Boesten and van der Linden, 1991). Such a difference in herbicide sorption occurred in this study with soil depth (Table 1), and among slope positions within the A horizon (Table 2).…”
Section: Discussionmentioning
confidence: 74%
“…A change of a factor of two in herbicide sorption input parameters for modeling could result in a 10 times difference in herbicide leaching potential within a soil (Boesten and van der Linden, 1991). Such a difference in herbicide sorption occurred in this study with soil depth (Table 1), and among slope positions within the A horizon (Table 2).…”
Section: Discussionmentioning
confidence: 74%
“…Parameter ranges related to potato crops, obtained by databases and tables included in the IPTM-CS program [41][42][43][44] are shown in Table 1. Other crops, less represented in the Plain, were not considered in this paper.…”
Section: Methodsmentioning
confidence: 99%
“…A complete water balance is simulated: root water uptake is calculated using the model described by Jarvis (1989); flow and transport to drainage systems is calculated by the Hooghoudt equation and seepage potential theory. Pesticide degradation is described by first-order kinetics, with the rate coefficient given as a function of soil temperature, according to the Arrhenius equation (Boesten and Van der Linden, 1991) and moisture content, following a modified Walker function (Walker, 1974). In this study, sorption is described with a linear isotherm, although MACRO can deal with non-linear Freundlich sorption isotherms.…”
Section: The Macro Model and Its Calibrationmentioning
confidence: 99%