文章摘要
于丽莎.鲁中南泰莱盆地岩溶地下水赋存特征和找水规律[J].地质与勘探,2019,55(1):168-177
鲁中南泰莱盆地岩溶地下水赋存特征和找水规律
Occurrence characteristics of karst groundwater and the rule of water search in the Tailai basin, central-southern Shandong Province
投稿时间:2017-11-03  修订日期:2018-02-04
DOI:10.12134/j.dzykt.2019.01.017
中文关键词: 岩溶地下水 泰莱盆地 地下水赋存 钻井取水 地下水资源开发利用
英文关键词: Karst groundwater, Tailai basin, groundwater storage, water drilling, groundwater water resources exploitation and utilization
基金项目:中国地质调查局地质调查项目(编号:DD20160285)、水[2011]02-61-04和国家科技支撑计划课题(编号:2012BAJ11B04)联合资助
作者单位E-mail
于丽莎 中国地质科学院岩溶地质研究所,国土资源部岩溶动力学重点实验室, 广西桂林
联合国教科文组织国际岩溶研究中心,广西桂林 
panxiaodong@karst.ac.cn 
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中文摘要:
      结合泰安市岱岳区水文地质调查资料和实施27口钻井发现:在鲁中南泰莱盆地西部山区,碳酸盐岩裸露,崎岖不平的峰丛谷地、峰丛洼地地貌导致水力坡度大,地下水沿构造断裂呈线状快速径流,地下水非饱和,无统一水力联系,岩溶地下水分布极不均匀成为钻井取水的难点,寻找有利蓄水构造成为钻井找水关键;在盆地东部和南部靠近河谷的缓丘平原覆盖型岩溶分布区,水文地质单元上处于地下水径流排泄区,岩溶地下水丰富且呈层状、面状分布,水力联系密切,滞流形成饱水带,利于钻井开采地下水资源,但应着重关注火山侵入岩等隔水岩层的展布情况,综合分析岩溶含水层厚度、地下水水位和汇水条件。
英文摘要:
      This work is based on combining hydrogeological survey data of Daiyue district, Tai’an city and implementation of drilling 30 wells. The results show that the mountainous areas of the western Tailai basin, central-southern Shandong are characterized by exposed carbonate, rugged peak valleys and peak cluster depressions that resulted in large hydraulic gradients of landform, linear fast runoffs of groundwater along faults, non-saturated groundwater, no unified hydraulic connection of karst groundwater and extremely uneven distribution of karst groundwater, which make it difficult to find favorable water drilling sites. So to find favorable water storage structure becomes the key for water search by drilling. In the eastern and southern basin, gentle hilly plains near river valleys host karst zones of coverage type, where hydrogeological units lie in the discharge area of groundwater runoffs, with rich groundwater in layered and planar distribution, close hydraulic connections, and stagnation to form saturation zones, which are groundwater resources easy to drill. But it should focus on the distribution of volcano intrusive rocks and water resisting strata, as well as analysis of karst aquifer thickness, groundwater level and catchment conditions.
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