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Advances in Earth Science >

2014 , Vol. 29 >Issue 3: 412 - 419

DOI: https://doi.org/10.11867/j.issn.1001-8166.2014.03.0412

Orginal Article

Karst Water System Boundaries and Hydrogeological Properties of Heilongguan Springshed in Xishan Region, Beijing

  • Chunhong Zhao ,
  • Qiang Li ,
  • Yongping Liang ,
  • Liang Xu ,
  • Weitai Wang ,
  • Haiping Lu ,
  • Chunlei Tang
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  • 1. Institute of Karst Geology, Chinese Academy of Geological Sciences / Karst Dynamiccs Laboratory, Ministry of Land and Resources & Guangxi Zhuang Autonomous Region, Guilin 541004, China
    2. Water Management Committee Office of Yuncheng, Yuncheng 044000, China
    3.Beijing Institute of Hydrogeology and Engineering Geology, Beijing 100195, China
梁永平(1962-),男,山西平遥人,研究员,主要从事中国北方岩溶地下水调查与研究.E-mail:lyp0261@karst.ac.cn

Received date: 2013-11-11

  Revised date: 2014-03-04

  Online published: 2014-03-10

Copyright

地球科学进展 编辑部, 2014, This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.本文支持CCAL协议的开放获取，允许读者在以下情况下免费获取和使用本文内容：科研、教学、数据库索引，并标明出处。但不得用于任何商业目的。版权属于地球科学进展 编辑部
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Abstract

With a fixed supplied scope and resource elements, karst groundwater system circulates as an independent unit in northern China, which controls karst water transport and enrichment, hydrochemical evolution, composition of water resources and environmental geological problems. In order to carry out karst groundwater system research, the primary task is determining the location and hydrogeological properties of boundaries. In this paper, we choose Heilongguan karst water system at Xishan region in Beijing as research object and determine the hydrogeological boundaries by geology, karst dynamics, fluid dynamics, hydro-geochemical, geophysical exploration and other methods. Finally, we conclude that Heilongguan karst water system is composed of two subsystems. The one is Dashihe anticline karst water subsystem, situated in the south and composed by the Upper Proterozoic aquifer;The other is Baihuashan syncline karst water subsystem, situated in the north and composed by Cambrian-Ordovician aquifer. According to hydrogeological properties of boundaries, there are surface water watershed boundary, underground watershed boundary, confining boundaries, karst aquifers deep stagnant boundary and other types.

Key words： Karst groundwater system; Hydrogeological boundaries; Heilongguan springshed.

Cite this article

Chunhong Zhao , Qiang Li , Yongping Liang , Liang Xu , Weitai Wang , Haiping Lu , Chunlei Tang . Karst Water System Boundaries and Hydrogeological Properties of Heilongguan Springshed in Xishan Region, Beijing[J]. Advances in Earth Science, 2014 , 29(3) : 412 -419 . DOI: 10.11867/j.issn.1001-8166.2014.03.0412

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