1983
DOI: 10.2134/jeq1983.00472425001200040025x
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Behavior Assessment Model for Trace Organics in Soil: I. Model Description

Abstract: A mathematical model is introduced for describing transport and loss of soil‐applied organic chemicals. The model assumes linear, equilibrium partitioning between vapor, liquid, and adsorbed chemical phases, net first order degradation, and chemical movement to the atmosphere by volatilization loss through a stagnant air boundary layer at the soil surface. From these assumptions and the assumption of steady state upward or downward water flow, an analytic solution is derived for chemical concentration and vola… Show more

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Cited by 613 publications
(148 citation statements)
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“…In porous solids (such as plant tissue), the diffusion is hampered by a "labyrinth factor", named tortuosity T. This tortuosity is estimated by the method of Millington and Quirk [37], for diffusion in root water and gas pores:…”
Section: Discussionmentioning
confidence: 99%
“…In porous solids (such as plant tissue), the diffusion is hampered by a "labyrinth factor", named tortuosity T. This tortuosity is estimated by the method of Millington and Quirk [37], for diffusion in root water and gas pores:…”
Section: Discussionmentioning
confidence: 99%
“…Many researchers have documented groundwater contamination due to toxic organic compounds in runoff (German, 1989;Wilson, et al, 1990;Ku and Simmons, 1985;Wilde, 1994). Many of these were associated with source areas where toxic organic pollutant concentrations exceeded typical stormwater concentrations.…”
Section: Other Organic Compoundsmentioning
confidence: 99%
“…Factors such as temperature, pH, metal concentration, nutrient availability and other factors affect the ability of a bacterial colony to survive in the water or soil (Ku and Simmons, 1985). Bacteria survive longer in acid soils and when large amounts of organic matter are present.…”
Section: Pathogens and Indicator Organismsmentioning
confidence: 99%
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“…In detail the volatilization models selected are: -Jury's model [9,10], assuming a contamination source with semi-infinite dimensions and time-varying concentrations (estimation of VF ss,J1 and VF ss,J2 for surface soil and VF ds,J for deep soil), -Farmer's model [11], with steady-state assumption (estimation of VF ss,F for surface soil, VF ds,F1 , VF ds,F2 for deep soil and VF gw for groundwater).…”
Section: Volatilization Factorsmentioning
confidence: 99%