紫荆关断裂构造对燕川水库渗漏的影响
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摘要
紫荆关断裂是保定西部山区区域性深大断裂,经过了多期复杂的地质作用,形成独特的地质构造,对区域地下水的赋存、运动、排泄规律起了明显控制作用。根据地质调查、钻探、压水试验等勘察资料,分析了紫荆关深断裂在燕川水库库区的构造特征、破碎带及其周围不同岩性的导水性,查明了燕川水库渗漏原因及渗漏部位,为水库除险加固提供可靠依据。
Zijingguan fracture is a regional deep fault located in the western mountain area of Baoding.It formed a unique geological structure after more than a period of complex geological processes,such as compressive shear,transtension,and lift.It has significant controlling effects on the storage,movement,discharge of regional groundwater.According to the regional geological data from geological survey,drilling,and pressure water test,the tectonic characteristics,hydraulic conductivities in different areas and strata of Zijingguan deep fracture in the Yanchuan reservoir were analyzed.The leakage causes and positions of Yanchuan reservoir were analyzed,which can provide reference for the reservoir reinforcement.
引文
[1]曲阳县水利志[M].河北省曲阳县水利志编纂委员会,1999.(Water conservancy volunteers of Quyang county[M].Hebei Qu-yang County Water Conservancy Compilation Committee,1999.(in Chinese))
    [2]曲阳县燕川水库大坝安全鉴定报告[R].保定市水利局,2008.(Dam safety appraisal report of Qu-yang YanChuan reservoir[R].Baoding City′s Water,2008.(in Chinese))
    [3]曲阳县燕川水库除险加固工程地质勘察报告[R].保定市水利局,2010.(Engineering geological investigation report of Quyang YanChuan reservoir[R].Baoding City′s Water,2010.(in Chinese))
    [4]河北省、北京市、天津市区域地质志[M].北京:地质出版社,1982.(Regional geology of Hebei,Beijing,Tianjin[M].Beijing:Geological Publishing House,1982.(in Chinese))
    [5]詹志佳,刘志远,高金田,等.紫荆关断裂构造磁效应的观测研究[A].中国地震学会第七次学术大会论文摘要集[C],1998.(ZHAN Zhi-jia,LIU Zhi-yuan,GAO Jin-tian,et al.Zijingguan active faults structure of magnetic experimental observation research[A].The Geomagnetic Observation and Research[C],1999.(in Chinese))
    [6]鞠紫云.紫荆关断裂在太行山北段的特征及其发生发展过程的推论[J].中国区域地质,1983(1).(JU Zi-yun.Zijingguan fracture in north taihang mountain characteristics and development process of reasoning[J].China′s Regional Geological,1983(1).(in Chinese))
    [7]陈桂华.紫荆关断裂带构造活动特征—以太行山北段为例[D].北京:中国地质大学,2003年.(CHEN Gui-hua.Zijingguan fracture zone characteristics of tectonic activity-in the northern section of taihang mountain,for example[D].Beijing:China University of Geosciences,2003.(in Chinese))
    [8]邢卫国.保定西部山区地下水赋存环境与勘察方法研究[D].北京:中国地质大学环境工程系,2009.(XING Wei-guo.Baoding groundwater environment and prospecting method research in the western mountainous areas[D].Beijing:China University of Geosciences Environmental Engineering,2009.(in Chinese))
    [9]水利水电工程钻孔压水试验规程[S].北京:中国计划出版社,2003.(Water resources and hydropower engineering drilling pressure water test procedure[S].Beijing:China planning press,2003.(in Chinese))
    [10]水文地质手册[M].北京:地质出版社,2012.(Hydrogeological manual[M].Beijing:Geological Publishing House,2012.(in Chinese))
    [11]水文地质学基础[M].北京:地质出版社,2011.(Hydrogeology basis[M].Beijing:Geological Publishing House,2011.(in Chinese))
    [12]杨进,韩金明.钻孔压水试验技术的应用与探讨[J].甘肃水利水电技术,2005(6).(YANG Jin,Han Jin-ming.The application of the drilling pressure water test technology and discusses[J].Water Resources and Hydropower Technology in Gansu Province,2005(6).(in Chinese))
    [13]韩爱民,白玉华,孙家齐.断层透水性工程地质评价[J].南京建筑工程学院学报,2002(1).(HAN Ai-min,Bai Yu-hua,Son Jia-qi.Fault permeability engineering geology evaluation[J].Journal of Nanjing Architectural Engineering Institute,2002(1).(in Chinese))
    [14]王清.渔洞河水库岩溶发育特征与渗漏研究[D].成都:成都理工大学,2013年.(WANG Qing.Yudong reservoir leakage of karst development characteristics and research[D].Chengdu:Chengdu University of Technology,2013.(in Chinese))
    [15]孙维兵.黄河羊曲水电站坝址岩溶发育特征及对工程影响研究[D].成都:成都理工大学,2008年.(SON Wei-bing.Huang Heyang qu hydropower station dam site karst development characteristics and influence on engineering research[D].Chengdu:Chengdu University of Technology,2008.(in Chinese))

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