中国“采水型”地裂缝特征和成因分析
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  • 英文篇名:Features and Mechanisms of Earth Fissures Induced Groundwater Withdrawal in China
  • 作者:王艺伟 ; 叶淑君 ; 于军 ; 龚绪龙
  • 英文作者:WANG Yiwei;YE Shujun;YU Jun;GONG Xulong;Department of Hydrosciences,School of Earth Science and Engineering,Nanjing University;Key Laboratory of Earth Fissure Geological Gazard of Land and Resources,institute of geological survey in Jiangsu;
  • 关键词:地裂缝 ; 地下水开采 ; 成因机制 ; 汾渭盆地 ; 华北平原 ; 苏锡常
  • 英文关键词:earth fissure;;groundwater withdrawal;;mechanism;;Fenwei Basin;;North China Plain;;Su-Xi-Chang area
  • 中文刊名:GXDX
  • 英文刊名:Geological Journal of China Universities
  • 机构:南京大学地球科学与工程学院水科学系;国土资源部地裂缝地质灾害重点实验室,江苏省地质调查研究院;
  • 出版日期:2016-12-20
  • 出版单位:高校地质学报
  • 年:2016
  • 期:v.22;No.86
  • 基金:国土资源部地裂缝地质灾害重点实验室开放课题(2014003);国土资源部公益项目(201411096);; 江苏省自然科学基金(批BK2012730);; 国家自然科学基金项目(41272259)联合资助
  • 语种:中文;
  • 页:GXDX201604017
  • 页数:12
  • CN:04
  • ISSN:32-1440/P
  • 分类号:155-166
摘要
过量开采地下水诱发的地裂缝("采水型"地裂缝)灾害对社会造成严重损失,受到人们普遍关注。近几十年来,国内外学者对其成因机制进行了大量研究,取得了丰硕成果。本文系统分析了前人的研究成果,归纳出"采水型"地裂缝的差异沉降成因、拉张性水平应变成因和四种成因模式;然后针对中国三个典型的"采水型"地裂缝发育区,即汾渭盆地、华北平原、苏锡常地区,阐述了各地地裂缝分布、发育特征和成因机理,并选择典型地段地裂缝进行成因分析,认为汾渭盆地和华北平原地区部分地裂缝属于"先期断层模式",而苏锡常地区地裂缝总体属于"基岩起伏模式",并阐述了该模式下导致地裂缝发育的差异性变形、水平应变作用机理。
        Excessive exploitation of groundwater in China has induced serious earth fissure hazards, which can cause significantdamage and heavy economic losses, and has received significant attention. In recent decades, mechanisms of earth fissures induced bygroundwater withdrawal have been studied by researchers worldwide and many remarkable achievements have been accomplished. Theresults of previous studies were analyzed in this article firstly and then the mechanisms of earth fissure induced by excessiveexploitation of groundwater were summarized and categorized as differential subsidence, horizontal tensile strain, and Four EarthFissure Formation Conceptual Models. Then the distribution of earth fissures, development features and mechanisms of earth fissures inthree regions(i.e., the Fenwei Basin, North China Plain and Su-Xi-Chang in China) where typical"groundwater-withdraw-induced"fissures developed, were elaborated, and a typical earth fissure was chosen to analyze its cause. Results indicate that earth fissures inthe Fenwei Basin and North China Plain were mainly caused by pre-existing faults and excessively ground water exploitation, while thefissures in the Su-Xi-Chang region were generally induced by a"bedrock ridge"below the aquifer and excessively ground waterexploitation. Differential compaction and horizontal strain mechanisms causing the development of such earth fissures were then explained.
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