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Experimental study and numerical simulation of soil water and salt transport under dry drainage conditions

机译:干排水条件下土壤水盐运移的实验研究与数值模拟

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In this research, the effect of dry drainage on the distribution of soil water content and salinity were experimentally and numerically investigated for 84 days. In the experimental study, soil water content and salinity were measured at different soil depths and four times after planting. Numerical simulation was carried out with HYDRUS-2D which was calibrated and validated using measured data from the experimental study based on different assumptions. Results showed that dry drainage could not only control the soil water content of the irrigated area but also transfers large amounts of salts from this area to the fallow area. So that at the end of the experiment, soil surface salinity of the irrigated and fallow area increased up to 145% and 270% more than initial values, respectively. Based on statistical indices, the accuracy of HYDRUS-2D simulation was improved by considering differences between parameters of the irrigated and the fallow areas including soil hydraulic and solute transport parameters. Furthermore, this accuracy was increased due to the application of the multiplicativity approach for combining water and salinity stresses. In addition, two indices of variations, soil surface salinity percent and soil salinity ratio, are recommended as suitable criteria for determining salt scratching time from soil surface of the fallow area and ensuring the sustainability of the dry drainage system.
机译:在这项研究中,实验和数值研究了干排水对土壤水分和盐分分布的影响,为期84天。在实验研究中,在不同土壤深度和种植后四次测量土壤水分和盐分。使用HYDRUS-2D进行了数值模拟,该HYDRUS-2D使用了基于不同假设的来自实验研究的测量数据进行校准和验证。结果表明,干排水不仅可以控制灌溉区的土壤含水量,而且可以将大量盐分从灌溉区转移到休闲区。因此,在实验结束时,灌溉区和休耕区的土壤盐分分别比初始值增加了145%和270%。基于统计指标,通过考虑灌溉区和休耕区参数(包括土壤水力和溶质运移参数)之间的差异,提高了HYDRUS-2D模拟的准确性。此外,由于应用了将水和盐分应力相结合的乘法方法,因此提高了精度。另外,建议使用两个变化指数,即土壤表面盐度百分比和土壤盐度比,作为确定休耕区土壤表层盐分刮擦时间并确保干排水系统可持续性的合适标准。

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