Spreading of chemical substance after its accidental spillage onto the soil surface under unsaturated conditions and variable porosity

O. Kozhushko, P. Martyniuk
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Abstract

In this paper we study a mathematical model of soil moisture transport with variable porosity. The problem is set for the case of highly concentrated solute spilled onto soil surface. We investigate the way solute transfer, adsorption of contaminant by soil particles and variable porosity influence infiltration of solute into the soil profile. For that purpose, two models are used: a classical one and the one with consideration of mentioned factors. By comparing the results of both models, we established that high concentration of solute causes moisture transport to transpire more slowly, and the pollutant to remain on the soil surface for longer time. Numerical results indicate that porosity can vary considerably under the conditions of intensive contamination with salts.
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非饱和条件下变孔隙率下化学物质意外泄漏到土壤表面后的扩散
本文研究了变孔隙率下土壤水分运移的数学模型。这个问题是针对高浓度溶质溢出到土壤表面的情况设置的。我们研究了溶质转移、土壤颗粒对污染物的吸附和孔隙度变化对溶质渗入土壤剖面的影响。为此,使用了两个模型:一个是经典模型,另一个是考虑了上述因素的模型。通过对比两种模型的结果,我们发现高浓度的溶质会导致水分的输送更慢,污染物在土壤表面停留的时间更长。数值结果表明,在盐的强烈污染条件下,孔隙度会发生很大的变化。
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