saturated soil hydraulic conductivity

基本解釋

The soil saturated hydraulic conductivity in different vegetation degeneration type and its influential factors in southwest karst region of China were studied.
通過對西南喀斯特地區(qū)典型土壤的飽和導(dǎo)水率的分析，研究了喀斯特地區(qū)不同植被退化類型下土壤的飽和導(dǎo)水率及其影響因素。
Results indicate that saturated hydraulic conductivity of soil containing rock fragments can be calculated through nonlinearly regressing steady infiltration rates at different negative water heads.
結(jié)果表明含碎石土壤飽和水力傳導(dǎo)度可以通過對不同負(fù)壓下土壤穩(wěn)定入滲速率進行非線性回歸獲得。
Saturated hydraulic conductivity of soil containing rock fragments is closely correlated to the hydraulic conductivity of soil without rock fragments and the shape coefficient of the rock fragments.
含碎石土壤飽和水力傳導(dǎo)度與去除碎石后的土壤飽和水力傳導(dǎo)度及碎石形狀指數(shù)密切相關(guān)。