soil hydraulic conductivity

基本解釋

A model for the unsaturated soil hydraulic conductivity is established based on an assumption that the soil can be represented as a continuum fractal porous medium.
土壤的孔隙是具有連續(xù)分形性質(zhì)的物理結(jié)構(gòu)，根據(jù)土壤孔隙分形結(jié)構(gòu)建立了非飽和水力傳導(dǎo)度模型。
Soil hydraulic conductivity is closely related to the movement of water and salts in soil profiles and is highly affected by solution salt concentration and its composition.
水力傳導(dǎo)度的變化直接影響土壤剖面的水鹽運(yùn)動，并和土壤溶液的鹽分濃度及其組成有很大關(guān)系。
The theories and application about methods of parameter determination on soil hydraulic conductivity in fields are reviewed, and the advantages and disadvantages of those methods are analyzed.
綜述田間測定土壤導(dǎo)水參數(shù)的幾種方法的原理及應(yīng)用，并對各種方法的優(yōu)缺點(diǎn)進(jìn)行對比分析。