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An in situ method to measure the longitudinal and transverse dispersion coefficients of solute transport in soil

机译:原位法测量土壤中溶质运移的纵向和横向弥散系数

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The knowledge of hydraulic conductivity and solute transport parameters of topsoil is important in a variety of fields and their measurement has been an interest in both theory and practice. In this paper we present an in situ method to measure the longitudinal and transverse dispersion coefficients of solute movement by modifying the double-ring infiltrometer into a triple-ring infiltrometer. Water flow in the apparatus is controlled in one dimension and solute movement in three dimensions. The solute transport parameters can be measured simultaneously with the hydraulic conductivity. Analytical solutions are derived to describe the solute movement, and field experiment was carried out to calculate the solute parameters in homogeneous soil using a simple method developed based on the analytical solutions. Simulating results using these estimated parameters predict the observed breakthrough curves reasonably well. (c) 2006 Elsevier B.V. All rights reserved.
机译:表土的水力传导率和溶质运移参数的知识在许多领域都很重要,其测量在理论和实践中都引起了人们的兴趣。在本文中,我们提出了一种通过将双环渗透仪改为三环渗透仪来测量溶质运动的纵向和横向弥散系数的原位方法。装置中的水流在一维受到控制,溶质运动在三维受到控制。溶质传输参数可以与水力传导率同时测量。推导了描述溶质运移的解析解,并采用基于解析解的简单方法进行了野外实验,计算了均质土中的溶质参数。使用这些估计参数模拟结果可以很好地预测观察到的突破曲线。 (c)2006 Elsevier B.V.保留所有权利。

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