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Physical and numerical modelling of solute transport in unsaturated soils

机译:不饱和土壤溶质运输的物理和数值模拟

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In this paper, the study of conservative solutes released into unsaturated homogeneous and layered soils has been addressed through physical modelling in a geoenvironmental centrifuge. Because independent long term modelling under a variety of controlled boundary conditions can be performed without the need to establish soil properties, centrifugation is an ideal technique for obtaining data sets for numerical simulation validation or calibration. Physical testing in the centrifuge was used to calibrate soil-water characteristic curve, hydraulic conductivity function, and molecular diffusion function predictions from the commercially available program SoilVision. Centrifuge modelling was used to simulate the 2-D transport of NaCl solution releases into unsaturated soil systems. Pore water concentrations were measured during centrifugation (in-flight) at various depths and were determined, along with volumetric water content, at the end of each modelling sequence. Two model series were performed and the results compared to predictions from the commercially available software SEEP/W and CTRAN/W.
机译:本文通过在地理环境离心机中的物理建模解决了释放到不饱和均匀和层状土壤中的保守溶质的研究。由于可以在无需建立土壤性质的情况下进行多种受控边界条件下的独立长期建模,因此离心是获取用于数值模拟验证或校准的数据集的理想技术。离心机中的物理测试用于校准土壤 - 水特征曲线,液压导电功能和来自市售的程序的土壤植物的分子扩散函数预测。离心式建模用于模拟NaCl溶液释放到不饱和土壤系统的二维转运。在各种深度离心(飞行中)的离心(飞行中)期间测量孔水浓度,并在每个建模序列结束时与体积含水含量一起测定。进行了两种模型系列,结果与来自商业上可用的软件SEEP / W和CTRAN / W的预测相比。

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