A generalized van Genuchten model for unsaturated soil hydraulic conductivity

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Asghar Ghorbani, Morteza Sadeghi, Markus Tuller, Wolfgang Durner, Scott B. Jones
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引用次数: 0

Abstract

The hydrodynamics of variably saturated soils or porous media in general are described via nonlinear functions of water retention and hydraulic conductivity, which facilitate the simulation of various mass and energy transport processes (e.g., water, heat, contaminants, colloids) within the porous medium. We set out to derive improved functions for more accurate estimations of soil hydraulic functions to advance the simulation of porous medium hydrodynamics. A new model is proposed for estimating the unsaturated hydraulic conductivity (UHC) from a soil water retention (SWR) function that is parameterized via nonlinear regression of measured data. The function can be viewed as a generalized van Genuchten (1980) model (GVG). We tested the new SWR and UHC expressions for numerous data sets from literature that cover a wide range of soil textures. Our comparisons reveal more accurate estimations using the GVG model by comparison with the original van Genuchten model.
非饱和土壤导水性的广义范根努赫腾模型
可变饱和土壤或一般多孔介质的流体力学是通过保水性和导水率的非线性函数来描述的,这有助于模拟多孔介质中的各种质量和能量传输过程(如水、热、污染物、胶体)。我们着手推导改进的函数,以便更准确地估算土壤水力函数,从而推动多孔介质流体力学的模拟。我们提出了一个新模型,用于根据土壤水分滞留(SWR)函数估算非饱和水力传导率(UHC),该函数通过对测量数据的非线性回归进行参数化。该函数可视为广义的 van Genuchten(1980 年)模型(GVG)。我们对文献中的大量数据集测试了新的 SWR 和 UHC 表达式,这些数据集涵盖了广泛的土壤质地。比较结果表明,使用 GVG 模型与原始范-格努赫腾模型相比,估算结果更为准确。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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