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杭州市环西湖覆盖型岩溶地面塌陷成因及预防
引用本文:许领,金艳丽,简中华,梁河,吴守富,WU Shou-fu.杭州市环西湖覆盖型岩溶地面塌陷成因及预防[J].中国地质灾害与防治学报,2008,19(1):36-39.
作者姓名:许领  金艳丽  简中华  梁河  吴守富  WU Shou-fu
作者单位:1. 中国科学院地质与地球物理研究所,北京,100029
2. 浙江省地质调查院,浙江,杭州,311203
3. 中国地质大学(武汉)环境学院,湖北,武汉,430074
摘    要:覆盖型岩溶地面塌陷是西湖风景区潜在的工程地质问题之一。本文根据杭州市环西湖覆盖型岩溶地区多年水位观测资料和岩溶水开采强度资料,从时间上把岩溶水开采历史概化为3个阶段。不同开采阶段地下水位动态变化特征不同,因此岩溶地面塌陷表现为不同的塌陷形式,具有不同的成因机制。分析表明:研究区岩溶地面塌陷机制经历了扰动一压密、渗透一潜蚀、真空吸蚀3个演变阶段。本文根据研究区岩溶地面塌陷成因类型和现阶段岩溶水开采情况,提出岩溶地面塌陷预防措施。

关 键 词:开采岩溶水  覆盖型岩溶地面塌陷  成因  预防措施  杭州西湖周围
文章编号:1003-8035(2008)01-0036-04
修稿时间:2007年3月20日

Genesis of Karst Collapse in the over-laying karst Area around West Lake in Hangzhou
XU Ling,JIN Yan-li,HU Cheng,JIAN Zhong-hua,LIANG He,WU Shou-fu.Genesis of Karst Collapse in the over-laying karst Area around West Lake in Hangzhou[J].The Chinese Journal of Geological Hazard and Control,2008,19(1):36-39.
Authors:XU Ling  JIN Yan-li  HU Cheng  JIAN Zhong-hua  LIANG He  WU Shou-fu
Institution:XU Ling , JIN Yan-li , HU Cheng , JIAN Zhong-hua , LIANG He , WU Shou-fu (1. Institute of Geology and Geophysics, Chinese Academy of Sciecnes, Beining 100029, China; 2: Chain University of Geosciences(Wuhan), Wuhan 430074, China; 3. Zhejiang Institute of Geological Survey, Hangzhou 311203, China)
Abstract:Based on the grounderwater level data of last more than 40 years of the over-laying karst area around West Lake in Hangzhou, the history of exploiting karst water is classified into three periods. As the Variation of the volume of the discharge during different periods, over-laying-karst collapse has different characteristics. The analysis shows that the genetic evolution process of karst collapses experiences such three periods as: Disturbance-Consolidation Type, Infiltration- Underground-Erosion Type and Vacuum-Absorption Type. And now preventive measures for karst collapse should focus on avoiding Vacuum- Absorbing effects.
Keywords:Exploiting Karst Water  over-laying-karst Collapse  Genesis  preventing measures  around West Lake in Hangzhou
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