吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 217-225.doi: 10.13278/j.cnki.jjuese.20180281

• 地质工程与环境工程 • 上一篇    

古堆泉岩溶地下水系统特征及系统圈划

申豪勇, 梁永平, 赵春红, 唐春雷, 王志恒   

  1. 自然资源部/广西壮族自治区岩溶动力学重点实验室(中国地质科学院岩溶地质研究所), 广西 桂林 541004
  • 收稿日期:2018-11-02 发布日期:2020-02-11
  • 通讯作者: 梁永平(1962-),男,研究员,主要从事北方岩溶地下水的调查与研究工作,E-mail:lyp0261@karst.ac.cn E-mail:lyp0261@karst.ac.cn
  • 作者简介:申豪勇(1988-),男,博士研究生,助理研究员,主要从事岩溶水文地质方面的研究,E-mail:shenhaoyong@karst.ac.cn
  • 基金资助:
    国家重点研发计划项目（2017YFC0406104）；国家自然科学基金项目（41672253，41902256）；中国地质调查局项目（DD20190334，DD20189807）

Hydro-Geological Characteristics and Demarcation of Gudui Spring Karst Groundwater System

Shen Haoyong, Liang Yongping, Zhao Chunhong, Tang Chunlei, Wang Zhiheng   

  1. Key Laboratory of Karst Dynamics, MNR&GZAR(Institute of Karst Geology, CAGS), Guilin 541004, Guangxi, China
  • Received:2018-11-02 Published:2020-02-11
  • Supported by:
    Supported by National Key R&D Program of China(2017YFC0406104),National Natural Science Foundation of China(41672253,41902256)and Project of China Geological Survey(DD20190334,DD20189807)

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摘要： 古堆泉是汾河流域内唯一的中低温地热泉，研究其水文地质特征、划定岩溶地下水系统边界是进行岩溶地下水资源评价和地热水成因研究的基础。通过对古堆泉岩溶地下水系统的地质结构特征、水文地质结构特征和岩溶地下水循环演化规律分析，初步圈划了古堆泉岩溶地下水系统及其子系统。研究结果表明：系统内地质结构复杂、火成岩侵入和隐伏断裂发育，总体上可以将其概括为南北和东西向均"三隆三陷"的地质格局；古堆泉岩溶地下水主要接受塔儿山、二峰山及中条山碳酸盐岩裸露区的降水入渗补给，南梁泉和海头泉是系统内2个岩溶地下水的局部排泄点，古堆泉是最终排泄点。根据水文地质结构特征和岩溶地下水循环特征确定了古堆泉岩溶地下水系统边界及其水文地质性质，圈定的古堆泉岩溶地下水系统面积为2 942 km2，并进一步将其划分为4个相对独立的岩溶地下水子系统：塔儿山-九原山古堆泉岩溶水子系统、佛岭山-高显海头泉岩溶水子系统、中条山南梁泉岩溶水子系统、侯马盆地深循环岩溶水子系统。

关键词: 水文地质结构, 岩溶水系统, 古堆泉, 锶钙比

Abstract: Gudui Spring is the only low medium temperature geothermal spring in Fenhe River basin. The research of hydro-geological characteristics and demarcation of karst groundwater system is the basis of karst groundwater resource evaluation. On the basis of the geological structural and hydro-geological characteristic analysis and karst groundwater circulation, the Gudui Spring karst groundwater system and subsystem are preliminarily delimited. The results show that the geological structures of the Gudui Spring karst system are complicated, and there are a lot of intrusive igneous rocks and buried faults. The overall geological structure of the system can be described as three uplifts and three subsides both in east-west and north-south directions. The recharge of karst groundwater is mainly from the precipitation of carbonate outcrop areas in Taer Mountain, Erfeng Mountain and Zhongtiao Mountain. Nanliang Spring and Haitou Spring are two local discharge areas;while Gudui Spring is the final discharge area. The boundary of Gudui Spring karst groundwater system and its hydrogeological nature are delimited by using the method of hydro-geological and groundwater circulation characteristic analysis. The area of Gudui Spring karst system is 2 942 km2 and can be divided into four relatively independent systems. The first is Taer Mountain-Jiuyuan Mountain Gudui Spring karst subsystem, the second is Foling Mountain-Gaoxian Haitou Spring karst subsystem, the third is Zhongtiao Mountain Nanliang Spring karst subsystem,and the last is Houma Basin deep circulation karst groundwater subsystem.

Key words: hydro-geological characteristic, karst groundwater system, Gudui Spring, c(Sr)/c(Ca)

中图分类号: 

  • P641
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[1] 姜光辉, 郭芳, 于奭. 岩溶水系统的水化学曲线及其在水文地质研究中的应用[J]. 吉林大学学报(地球科学版), 2015, 45(3): 899-907.
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