The paper analyzed the difference and the error of trans-mechanism of moisture between the lysimeter and the natural unconfinedgroundwater system.
对地中蒸渗计与自然潜水水分运移机理存在的差异及误差进行了分析。
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While groundwater flows through an unconfined aquifer due to heterogeneity, the vertical average saturated hydraulic conductivity is a function of hydraulic head.