摘要
根据岩性组合及岩溶发育规律研究,泰安城市供水水源地岩溶层组类型主要为均匀状石灰岩、均匀状白云岩和均匀状不纯碳酸盐岩等组成,岩溶水的边界条件决定了其处于一个相对独立的水文地质单元中,主要含水层类型为裂隙岩溶含水层、岩溶裂隙含水层。岩溶水文地质结构特征表明,岩溶水资源相对贫乏。
According to the characteristics of carbonate strata as well as karstified level, the karstified strata in Tai'an can be divided into three types: limestone, dolomite, and carbonate rocks with other minerals.The karstic water is preserved in an independent hydrogeologic unit due to it's horizontal boundary conditions. The fissure-karstic and karstic-fissure aquifers are two different types of aquifer. The hydrogeologic structure features indicate that the karstic water resource is limited in amount in the groundwater supply sites in Tai' an.
出处
《山东科技大学学报(自然科学版)》
CAS
2000年第2期79-81,84,共4页
Journal of Shandong University of Science and Technology(Natural Science)
关键词
碳酸盐岩
岩溶
水文地质结构
山东泰安
carbonate rocks
karst
hydrogeologic structure
karstic water dynamic unit