1) Recharge rate
补给强度
1.
However,the large spatial and temporal variation makes it difficult to measure directly the groundwater recharge rate and hence it is very difficult to reconstruct the groundwater recharge history and estimate the changes of recharge rate.
以滹沱河冲洪积扇河北省正定试验场包气带剖面为研究对象,利用环境示踪剂(氚和氯)方法,估算了该区地下水近三十多年来的天然补给强度。
3) recharge degree
补给程度
1.
The recharge degree and the influence of river pollution on the groundwater quality were discussed.
在地下水开采井正常运行和全部关闭两种情况下,分别对现状年和设计典型年,运用所建模型求解松花江水对研究区地下水的补给量,分析补给程度,从一个侧面探讨江水污染对地下水水质的影响程度。
4) supply temperature
补给温度
1.
The new method of determining groundwater supply temperature and rainfall by dissolved noble gases;
测定地下水补给温度与降雨量的最新方法——惰性气体法
5) recharge depth
补给深度
1.
A preliminary study of the recharge depth of the Yellow River to groundwater;
黄河水对地下水补给深度的初步研究
6) Subsidy System
补给制度
1.
Fragment of Sino-Japanese Relations in the Early 20th Century——Study of the“Oriental Cultural Undertakings”Foreign Student Tuition Subsidy System by Sun Ying PhD, Foreign Language College, Northeast Normal University;
20世纪上半叶中日文化关系的一个片断——“东方文化事业”留学生学费补给制度考略
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