土壤渗透 meaning in Chinese
soil percolate
Examples
- Test methods for permeability of saturated soils
饱和土壤渗透率的试验方法 - Test method for penetration test and split - barrel sampling of soils
土壤渗透试验和对开管取样的试验方法 - Acidity and inorganic nitrogen concentrations in soil solution in short - term response to n addition in subtropical forests
鼎湖山森林土壤渗透水酸度和无机氮含量对模拟氮沉降增加的早期响应 - Through this study and according to the law by which the soil moisture content changes with the time , the soil moisture is determined as consumptive , accumulative , fade - away and stabilization periods
对于土壤渗透，一般情况下初渗和稳渗速度是林内林外空地沼泽化迹地， a层b层。 - On the other hand for four main vegetation typies , which are picea crassifolia , forests sabina przewalskii forests , bushes and pastureland , whose soil permeability function was analyzed from angle of its physics , capacity of water , storing water in it . the results show as follow : permeability function of soil is controlled by quality of soil hole . the quality and quantity of soil hole under picea crassifolia forests are the best , and the permeability also is the best
另外，从土壤物理性质、蓄水量、贮水量等角度对祁连山苔藓云杉林、祁连圆柏林、亚高山灌丛林、牧坡草地4种主要植被类型的土壤渗透功能进行分析，结果表明：土壤的渗透功能主要由土壤非毛管孔隙度的质和量决定的，苔藓云杉林土壤非毛管孔隙度的质和量最好，它的渗透也最好；虽然亚高山灌丛林的渗透功能次之，但由于它所处的位置和面积大，现实贮水量在祁连山四种主要植被类型中最大。