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1)  rainfall recharge
降雨补给
2)  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。
3)  subrainfall infiltration coefficient
次降雨入渗补给系数
1.
Study on spatial variability of subrainfall infiltration coefficient and simulation of the stochastic field;
次降雨入渗补给系数空间变异性研究及模拟
4)  the coefficient of rainfall infiltration
降雨入渗补给系数
1.
The water resource infiltrated by rainfall is an important part of the underground water resource,which is affected by the coefficient of rainfall infiltration.
降雨入渗补给量是干旱地区地下水资源的重要组成部分,降雨入渗补给系数取用的正确与否直接关系到降雨入渗补给量的估算。
5)  compensation and rehabilitation
降雨补偿
1.
However, studies on root functions under soil water deficit, compensation and rehabilitation characteristics after rainy seasons in differ.
采用单株平衡法 ,通过定位监测与对比分析 ,对黄土高原半湿润落叶阔叶林区 ,持续干旱期末人工林地土壤水分亏缺度、雨季末降雨补偿深度及土壤贮水亏缺补偿度的时空分布进行了研究。
6)  precipitation recharge
降水补给
补充资料:贺李观察祷河神降雨
【诗文】:
质明斋祭北风微,驺驭千群拥庙扉。玉帛才敷云淡淡,
笙镛未撤雨霏霏。路边五稼添膏长,河上双旌带湿归。
若出敬亭山下作,何人敢和谢玄晖。



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【出处】:
全唐诗:卷269_32
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