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Parameter Identification Of Simplified Model Of Soil Evaporation With Numerical Experiments Using The Hygrothermal Dynamics Model A Study on simplified estimation of evaporation rate from soil surface Part 2

机译:利用湿热动力学模型进行数值模拟的土壤蒸发简化模型参数辨识简化估算土壤表层蒸发速率的研究第二部分

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摘要

Fundamental hygrothermal properties of soil were obtained by a series of numerical experiments in which the hygrothermal dynamics model was adopted as an exact solution. These properties as Evaporation Ratio, Hydraulic Transmittance and Moisture Diffusivity are simultaneously requisite in the simplified calculation model to estimate evaporation rate from soil surface, the authors developed. Time-series data of calculation led to the relationships between normalized weight water content of discrete soil surface layer and above-mentioned three properties, respectively.
机译:通过一系列数值实验获得了土壤的基本湿热特性,其中采用湿热动力学模型作为精确解。作者们开发了简化的计算模型中同时需要的这些特性,如蒸发率,水力透过率和水分扩散率,以估算土壤表面的蒸发速率。计算的时间序列数据分别导致离散的土壤表层的归一化重量水含量与上述三个特性之间的关系。

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