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首页> 外文期刊>Acta Geophysica >Mathematical Modeling and Practical Verification of Groundwater and Contaminant Transport in a Chosen Natural Aquifer
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Mathematical Modeling and Practical Verification of Groundwater and Contaminant Transport in a Chosen Natural Aquifer

机译:所选天然含水层中地下水和污染物运移的数学建模和实践验证

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The paper addresses the 2D mathematical equation of conservative contaminant transport in an aquifer for chosen contaminants. The contaminants (chlorides and sulfates) are subject to instantaneous reversible part of sorption process. The term of instantaneous reversible sorption in the presented equation has been described by the non-linear Freundlich adsorption isotherm, widely applied in practice in relation to static processes (for local equilibrium). The numerical solution (using the finite difference method) has been based on the previously calculated values of longitudinal and transverse dispersion coefficients and the non-linear adsorption parameters for the chosen contaminants. Based on this model, the values of chloride and sulfate concentration isolines have been calculated and compared with the measured maximal concentrations in the chosen natural aquifer (installed piezometers). Additionally, the values of chloride concentrations have been calculated taking into account the influence of radioactive decay term, using the numerical value of the first-order decay rate constant for an adopted theoretical radionuclide.
机译:本文针对选定污染物,讨论了在含水层中保守污染物传输的二维数学方程式。污染物(氯化物和硫酸盐)经受吸附过程的瞬时可逆部分。非线性方程式中的Freundlich吸附等温线描述了所提方程中的瞬时可逆吸附项,该等温线在实践中广泛应用于静态过程(用于局部平衡)。数值解法(使用有限差分法)是基于先前计算的纵向和横向色散系数值以及所选污染物的非线性吸附参数。基于此模型,已计算出氯化物和硫酸盐浓度等值线的值,并将其与所选天然含水层(已安装的压力计)中测得的最大浓度进行比较。另外,已经使用放射性衰变常数的影响值,采用了理论放射性核素的一阶衰变速率常数的数值,计算出了氯化物的浓度值。

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