山西晋祠泉复流——地球物理应用研究
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1.中国地质大学地球物理与空间信息学院,武汉;2.中国地质大学(武汉);3.中国地质大学地质调查研究院,武汉

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P631.3

基金项目:

国家自然科学(41804122);国家重点研发计划(2018YFC0604303)


Reflow Project of Jinci Spring in Shanxi Province—— Application Research of Comprehensive Geophysical Prospecting Methods
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Affiliation:

1.Institute of Geophysics Geomatics,China University of Geoscience,Wuhan ,China;2.China University of Geoscience, Wuhan;3.Institute of Geophysics&Geomatics, China University of Geoscience, Wuhan

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    摘要:

    1994年晋祠泉断流后,广大人民群众热切期盼千古名泉能早日重现昔日风采,晋祠泉复流工程由此提上议程。明仙沟位于晋祠泉西北侧,是复流工程最重要的研究区之一。因此,查明重点区域地质构造与水文地质条件,确定最佳岩溶水补给地点和方法,实现岩溶地下水资源有效补给成为本项目的重要课题,地球物理方法是研究该课题的一种重要手段。音频大地电磁法在探测深大断裂结构特征、基底构造及其影响范围等方面具有良好效果;高密度电法对150m以浅的次级断裂、地下水水位、基岩面和岩溶发育情况识别度高;充电法在测定地下水流向和流速,查明明仙沟与晋祠泉水力联系方面优势明显。根据三种地球物理方法的特点及测区实况,确立了上述三种地球物理方法联合勘查的策略。音频大地电磁法与高密度电法反演所得电阻率断面图显示的主要断裂构造与该区1:50000地质图吻合得很好,边山断裂响应明显且对边山断裂位置和倾向刻画清晰;高密度电法不同测线对相同地质体反映的一致性增加了解释的可信度;三种地球物理方法综合勘查表明明仙沟与晋祠泉之间存在较好的水力联系,为该区生态补水工程选址提供了地球物理依据。

    Abstract:

    Since the cutoff of Jinci Springs in 1994, a large amount of people eagerly hoped that these ancient and famous springs could regain their former demeanours, and therefore the Jinciquan reflow project was put on the agenda. Mingxiangou is located on the northwest side of Jinci Spring and is one of the most important research areas for the reflow project. Therefore, identifying the geological structure and hydrogeological conditions in key areas, determining the best karst water replenishment sites and methods, and realizing the effective recharge of karst groundwater resources have become important topics of this project. Geophysical method is an important means to study this topic. Audiomagnetotelluric method has good effects in detecting the structural characteristics of deep and large faults, the basement structure and its influence range. High-density electrical method is sensitive to shallow secondary fractures within 150m, groundwater level, bedrock surface and karst development. The charging method is effective in determining the flow direction and flow rate of the groundwater, and finding out the water connection between Mingxiangou and Jinci Spring. According to the characteristics of the three geophysical methods and the actual situation of the survey area, the strategy of joint exploration of the above three geophysical methods was established. The main deep and shallow fault structures shown by the audiomagnetotelluric method and high-density electrical method inversion resistivity profiles are in good agreement with the 1:50000 geological map in this area. The Bianshan fault response is obvious and the location and tendency of which are clearly defined; The consistency of the same geological body in different profiles of high-density electrical method increases the credibility of the interpretation; Meanwhile, the comprehensive exploration of the three geophysical methods shows that there is a good hydraulic connection between Mingxianou and Jinxi Spring, which lays a theoretical foundation for the ecological water replenishment project in the area.

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刘盼,李鹏翔,陈斌,等. 山西晋祠泉复流——地球物理应用研究[J]. 科学技术与工程, 2019, 19(25): 58-67.
LIU pan, LI Pengxiang,,et al. Reflow Project of Jinci Spring in Shanxi Province—— Application Research of Comprehensive Geophysical Prospecting Methods[J]. Science Technology and Engineering,2019,19(25):58-67.

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  • 收稿日期:2018-12-13
  • 最后修改日期:2019-05-15
  • 录用日期:2019-04-01
  • 在线发布日期: 2019-09-19
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