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本文提出一种简单的方法,即:在土壤水入渗和再分配期间,根据原位测定数值,计算土壤的导水率,K(θ).计算方程K(θ)和K(h)的导出是假定以单位水势梯度为条
This paper presents a simple method of calculating soil water conductivity, K (θ), based on in situ measurements during soil water infiltration and redistribution. Calculating equations K (θ) and K (h) The export is assumed to be a unit of water potential gradient