摘要
本文介绍了在岩溶地区根据地下水动态观测资料,和地下水位重合时段的总排泄水量,直接推算地下水的补给量和渗入系数的方法。经验证,效果较好。
Method to calculate directly the recharge capacity of groundwater and infiltration coefficient in karst district based on dynamic observation of groundwater and the total drainage of groundwater during the period when the water level of groundwater coincided. It is verified that the result is perfect.
出处
《工程勘察》
CSCD
北大核心
1990年第6期39-41,共3页
Geotechnical Investigation & Surveying