saturated soil hydraulic conductivity

基本解释

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典型土壤的飽和導水率的分析，研究了喀斯特地區不同植被退化類型下土壤的飽和導水率及其影響因素。
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.
結果表明含碎石土壤飽和水力傳導度可以通過對不同負壓下土壤穩定入滲速率進行非線性廻歸獲得。
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度與去除碎石後的土壤飽和水力傳導度及碎石形狀指數密切相關。