1) penetrating recharge
渗入补给
2) infiltration recharge
入渗补给
1.
With the theory of runoff yield at natural storage and the computed restore method at separate layers,the variation law of the precipitation infiltration recharge with groundwater depth was investigated by using the measured data from the lysimeter in 8m fixed-depth at Ranzhuang.
利用冉庄8m定埋深地中蒸渗仪的观测资料,根据蓄满产流理论,采用分层计算还原的方法,研究降水入渗补给量随地下水埋深的变化规律。
3) precipitation recharge
降雨入渗补给
1.
Based on the physical process of soil water transfer,a calculated model esti mating the precipitation recharge is proposed.
基于土壤水运动的物理过程,提出了降雨入渗补给地下水的计算模型。
2.
Estimation of precipitation recharge is very important for regional water resources evaluation because it is a primary source of groundwater resources and is very useful for reasonable groundwater exploitation.
降雨入渗补给是平原区地下水补给的主要来源,降雨入渗补给量计算是地下水资源评价的重要部分。
6) vertical recharge
垂向入渗补给量
补充资料：渗入
分子式：
CAS号：
性质：土壤从降水中或流过地面的河流中吸收水的过程。在给定条件下，土壤能够吸收雨水或融雪的最大速率称为渗入量。
CAS号：
性质：土壤从降水中或流过地面的河流中吸收水的过程。在给定条件下，土壤能够吸收雨水或融雪的最大速率称为渗入量。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条