又称土壤渗透速率单位时间内地表单位面积土壤的入渗水量。渗透速率与入渗过程有关。...田间土壤水分渗透速率与入渗时间的关系，在入渗的初始阶段速率较快，到一定时间后速率趋于稳定，此时的渗透速率称为稳定入渗率，可用以表征土壤的渗透特性。
芦苇能改变土壤入渗率和根际土壤的理化性质，从而影响湿地土壤对苯酚的吸附能力。
Through changing soil infiltration and physicochemical properties of rhizosphere, reed can affect adsorption ability of wetland soil on phenol.
建立像素颜色RGB值与土壤含水率之间的数学关系，是染色入渗法的应用基础。
It is necessary to quantify the relationship between pixel color RGB value and soil water content for the application of dye infiltration.
不同矿化度的水入渗后，土壤表层含水率基本相近，接近饱和含水率。
The surface soil water content was close with different mineralization degree levels water, which approached saturated water content.
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