平原缺水区隐伏岩溶水的供水意义——以通州区龙旺庄隐伏灰岩水源地的勘查运行为例  

The Significance of Concealed Karst Water in Water-Deficient Plain Areas A Case Study of the Concealed Limestone Water-Source Area in Longwangzhuang,Tongzhou District,Beijing

作　　者：李海京[1] 

机构地区：[1]北京市地质工程勘察院,北京10037

出　　处：《城市地质》2007年第4期49-51,共3页Urban Geology

摘　　要：本文以通州区龙旺庄隐伏灰岩水源地的勘查及运行情况为例,提出以隐伏基岩地下水作为应惠水源来科学、适度地开采是具有一定现实意义的;像龙旺庄这种消耗性水源地,开采条件下补给量的增量(激发补给量)也不容忽视。With the concealed limestone water-source area in Longwangzhuang of Tongzhou District as a case study, this paper proposes that groundwater in concealed basic rocks can be exploited scientifically and rationally as emergency water, which is of practical significance. On the other hand, increased recharge （excitation recharge） during the exploitation should not be ignored in such an exhaustive water-source area as Longwangzhuang.

关 键 词：隐伏岩溶裂隙水 消耗性水源地 激发补给量 

分 类 号：P641.134[天文地球—地质矿产勘探]