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Numerical simulation of salt leaching for the saline-alkali soil with clay interlayer Ⅰ: Models establishment and validation

机译:黏土夹层盐碱土盐分淋溶的数值模拟Ⅰ:模型建立与验证

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Salt-alkali-related soil degradation is a worldwide environmental problem that attracts researchers’ continuous attention for many years. In order to reclaim saline soil, slat leaching which is considered as the most direct method is always used. Models used to describe soil water and salt dynamics which are essential for establishing salt leaching theory are always absolutely necessary. In this paper, two-dimensional water flow and salt transport models were developed for researching salt transportation during leaching in a soil domain above a silo drilled throughout the clay subsoil. The corresponding boundary conditions were established and models were solved by finite difference method. Based on the experiment carried out in northwest China, the calibration and validation were realized and the result showed that the general trend of the simulated soil salt contents after leaching matched better with the observed values. The models could successfully simulate salt distribution of such leaching process and provided a reasonably good link for salt transportation research in saline-alkali soil.
机译:与盐碱有关的土壤退化是一个全球性的环境问题,多年来一直吸引着研究人员的持续关注。为了开垦盐渍土壤,总是使用被认为是最直接的方法的板条浸出。始终必须使用用于描述土壤水和盐动力学的模型,这些模型对于建立盐浸理论是必不可少的。在本文中,开发了二维水流和盐分运移模型,用于研究在整个粘土底土中钻取的筒仓上方的土壤区域中淋溶过程中的盐分运移。建立了相应的边界条件,并通过有限差分法求解了模型。在西北地区进行的实验基础上,实现了标定和验证,结果表明,浸出后模拟土壤盐分的总体趋势与实测值较为吻合。该模型可以成功模拟这种淋溶过程中的盐分分布,并为盐碱土中盐分运移研究提供了合理的良好链接。

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