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An Inverse Method to Estimate the Root Water Uptake Source-Sink Term in Soil Water Transport Equation under the Effect of Superabsorbent Polymer

机译:高吸收性聚合物作用下土壤水分运移方程中根吸源-库期的反演方法

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摘要

The widespread use of superabsorbent polymers (SAPs) in arid regions improves the efficiency of local land and water use. However, SAPs’ repeated absorption and release of water has periodic and unstable effects on both soil’s physical and chemical properties and on the growth of plant roots, which complicates modeling of water movement in SAP-treated soils. In this paper, we proposea model of soil water movement for SAP-treated soils. The residence time of SAP in the soil and the duration of the experiment were considered as the same parameter t. This simplifies previously proposed models in which the residence time of SAP in the soil and the experiment’s duration were considered as two independent parameters. Numerical testing was carried out on the inverse method of estimating the source/sink term of root water uptake in the model of soil water movement under the effect of SAP. The test results show that time interval, hydraulic parameters, test error, and instrument precision had a significant influence on the stability of the inverse method, while time step, layering of soil, and boundary conditions had relatively smaller effects. A comprehensive analysis of the method’s stability, calculation, and accuracy suggests that the proposed inverse method applies if the following conditions are satisfied: the time interval is between 5 d and 17 d; the time step is between 1000 and 10000; the test error is ≥ 0.9; the instrument precision is ≤ 0.03; and the rate of soil surface evaporation is ≤ 0.6 mm/d.
机译:超吸收性聚合物(SAPs)在干旱地区的广泛使用提高了当地土地和水的利用效率。但是,SAP重复吸收和释放水分对土壤的物理和化学性质以及植物根系的生长都具有周期性和不稳定的影响,这使用SAP处理过的土壤中水分运动的模型变得复杂。在本文中,我们提出了SAP处理过的土壤水分运移的模型。 SAP在土壤中的停留时间和实验持续时间被认为是相同的参数t。这简化了以前提出的模型,其中SAP在土壤中的停留时间和实验持续时间被视为两个独立的参数。在SAP的影响下,通过反演方法对土壤水分运移模型中根水吸收源/汇项的估计进行了反演。测试结果表明,时间间隔,水力参数,测试误差和仪器精度对反演方法的稳定性有显着影响,而时间步长,土壤分层和边界条件的影响相对较小。对方法的稳定性,计算和准确性的综合分析表明,如果满足以下条件,则建议的反方法适用:时间间隔在5 d至17 d之间;时间步长在1000到10000之间;测试误差≥0.9;仪器精度≤0.03;土壤表层蒸发率≤0.6mm / d。

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