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Numerical Simulation of Salt Transportation During Leaching Through Layered Saline Soil

机译:盐水土壤浸出过程中盐运输的数值模拟

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Salt-related soil degradation is considered a major threat to sustainable agriculture under semi-arid conditions. It 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. In this paper, HYDRUS-2D was used for researching salt transportation during leaching in a soil domain above a silo drilled throughout the clay subsoil. Based on the experiment carried out in Shule River basin 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. HYDRUS-2D could successfully simulate salt distribution of such leaching process and provided a reasonably good link for salt transportation research in saline soil. The results of salt transportation characteristics during the leaching demonstrated that with same water quota of leaching and same radius of silo, different existence and depth of clay interlayer needed different time for salt leaching down the soil profile. Additional applies will be carried out to illustrate the models' capacity for application to a broad range of soils.
机译:与盐相关的土壤退化被认为是在半干旱条件下对可持续农业的重大威胁。这是一个全球环境问题,吸引了研究人员多年的持续注意。为了回收盐渍土,始终使用被认为是最直接方法的板条浸出。本文中,Hydrus-2d用于在整个粘土底土钻的土壤域中浸出过程中的盐水运输。基于中国西北地区舒尔河流域的实验,实现了校准和验证,结果表明,浸出后模拟土壤盐含量的一般趋势与观察到的值更好。 Hydrus-2D可以成功地模拟这种浸出过程的盐分布,并为盐渍土壤盐运输研究提供了合理良好的联系。浸出过程中盐运输特性的结果证明,具有相同的浸出水分和相同的筒仓半径,不同的存在和粘土中间层的深度需要不同的时间盐浸出土壤轮廓。将进行额外的适用,以说明模型的应用能力施加到广泛的土壤中。

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