地球科学进展

地球科学进展 >

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

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

北京西山黑龙关泉域岩溶水系统边界与水文地质性质

  • 赵春红 ,
  • 李强 ,
  • 梁永平 ,
  • 许亮 ,
  • 王维泰 ,
  • 卢海平 ,
  • 唐春雷
展开
  • 1.中国地质科学院岩溶地质研究所/国土资源部、广西壮族自治区岩溶动力学重点实验室, 广西 桂林 541004
    2.山西省运城市水资源管理委员会办公室,山西 运城 044000
    3.北京市水文地质工程地质大队,北京 100195

赵春红(1986-),女,河南项城人,研究实习员,主要从事岩溶水文地质调查与研究、水资源评价等研究.

收稿日期: 2013-11-11

  修回日期: 2014-03-04

  网络出版日期: 2014-03-10

基金资助

中国地质调查局地质调查项目“北方岩溶区水文地质环境地质调查示范”(编号:1212011220940);北京市岩溶地下水勘查评价工程(编号:BJYRS-ZT)资助

版权

, 2014,
收起

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
Expand
  • 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
Fold

摘要

北方岩溶水系统具有固定补给范围和资源要素,是岩溶地下水进行独立循环的基本单元,控制了岩溶水的运移富集、水化学演化特征、资源构成以及环境地质问题。开展岩溶水系统研究的首要任务是确定系统边界位置及其水文地质性质。以北京西山黑龙关泉域岩溶水系统为研究对象,采用地质学、岩溶动力学、流体动力学、水文地球化学、地球物理勘探等方法,确定黑龙关泉域岩溶水系统是由南部大石河背斜岩溶水子系统和北部百花山向斜南翼岩溶水子系统2个次级系统组成;其含水岩层分别为蓟县系铁岭组、雾迷山组和青白口系景儿峪组、奥陶系、寒武系碳酸盐岩。根据边界的水文地质性质可以划分为地表分水岭边界、地下分水岭边界、隔水边界、岩溶含水层深埋滞流性边界等类型。

关键词： 岩溶水系统; 水文地质边界; 黑龙关泉域

本文引用格式

赵春红 , 李强 , 梁永平 , 许亮 , 王维泰 , 卢海平 , 唐春雷 . 北京西山黑龙关泉域岩溶水系统边界与水文地质性质[J]. 地球科学进展, 2014 , 29(3) : 412 -419 . DOI: 10.11867/j.issn.1001-8166.2014.03.0412

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.

参考文献

[1] Zhou Zongjun. The investigation of groundwater systems division in Shaanxi Province[J]. Geology of Shaanxi, 1985, (1): 100-107.
[2] Liang Yongping, Wang Weitai. The division and characteristics of karst water systems in Northern China[J]. Acta Geoscientica Sinica, 2010, 31(6):860-868.
[2] [梁永平,王维泰.中国北方岩溶水系统划分与系统特征[J].地球学报,2010, 31(6):860-868.]
[3] Chen Mengxiong,Ma Fengshan. China Groundwater Resources and Environment[M]. Beijing: Seismological Press, 2002.
[3] [陈梦熊,马凤山. 中国地下水资源与环境[M].北京:地震出版社, 2002.]
[4] Liu Qiren, Zhang Fengqi, Qin Yisu, et al. The formation, distribution, rational development and utilization of karst groundwater resource in Northern China[J]. Hydrogeology and Engineering Geology, 1992, 19(4):41-44.
[4] [刘启仁, 张凤岐, 秦毅苏, 等.中国北方岩溶水资源的形成、分布与合理开发利用[J].水文地质工程地质,1992, 19(4):41-44.]
[5] Han Xingrui,Lu Rongan,Li Qingsong. Karst Groundwater System—Resarch on Big Springs in Shanxi[M]. Beijing: Geological Publishing House, 1993.
[5] [韩行瑞,鲁荣安,李庆松. 岩溶水系统——山西岩溶大泉研究[M].北京: 地质出版社,1993.]
[6] Han Xingrui,Liang Yongping,Shi Jian. Research on Typical Karst Groundwater System at Loess Region in Northwest China[M]. Guilin: Guangxi Normal University Press, 2002.
[6] [韩行瑞,梁永平,时坚. 中国西北黄土地区典型岩溶水系统研究[M]. 桂林: 广西师范大学出版社, 2002.]
[7] Li Wenpeng, Hao Aibing. The formation and evolution model of groundwater and its significance in inland arid basin, Northwest China[J]. Hydrogeology and Engineering Geology,1999, 26(4): 28-32.
[7] [李文鹏,郝爱兵.中国西北内陆干旱盆地地下水形成演化模式及其意义[J].水文地质工程地质,1999, 26(4):28-32.]
[8] Wu Xuanmin, Shi Shengsheng, Li Zhiheng, et al. Systemic research of groundwater in Ejina Basin in the lower Heihe River(up)[J].Hydrogeology & Engineering Geology, 2002,29(1):16-20.
[8] [武选民, 史生胜, 黎志恒,等. 西北黑河下游额济纳盆地地下水系统研究(上)[J].水文地质工程地质, 2002, 29(1):16-20.]
[9] Wu Xuanmin, Shi Shengsheng, Li Zhiheng, et al. Systemic research of groundwater in Ejina Basin in the lower Heihe River(down)[J].Hydrogeology & Engineering Geology, 2002,29(2):30-33.
[9] [武选民, 史生胜, 黎志恒, 等.西北黑河下游额济纳盆地地下水系统研究(下)[J].水文地质工程地质,2002, 29(2):30-33.]
[10] Wang Zhanhe, Zhan Tiande, Yu Desheng, et al. Division of groundwater systerm of Tarim Basin[J]. Xinjiang Geology, 2004, 22(3):262-264.
[10] [王占和, 谌天德, 于德胜, 等. 塔里木盆地地下水系统划分[J].新疆地质,2004, 22(3):262-264.]
[11] Pan Shulan. Using stable isotopic to study karst water resources in taiyuan area[J]. Carsologica Sinica, 1989,8(2):66-70.
[11] [潘曙兰.稳定同位素在太原地区岩溶水资源研究中的应用[J].中国岩溶,1989, 8(2):66-70.]
[12] Ma Zhiyuan, Niu Guangliang, Dang Xueya, et al. Supply environm ent from Ordovician karst groundwater in eastern Weibei of Ordos Basin, Shaanxi Province[J]. Advances in Earth Science, 2004, (Suppl.): 161-165.
[12] [马致远, 牛光亮, 党学亚, 等.鄂尔多斯盆地渭北东部奥陶系岩溶地下水的补给环境[J].地球科学进展,2004, (增刊):161-165.]
[13] Yang Jilong, Han Dongmei, Su Xiaosi, et al. Environmental tracers as indicators of seawater intrusion processes in the coastal karst area[J]. Advances in Earth Science, 2012, 27(12):1 344-1 352.
[13] [杨吉龙, 韩冬梅, 苏小四, 等.环境同位素特征对滨海岩溶地区海水入侵过程的指示意义[J].地球科学进展,2012, 27(12):1 344-1 352.]
[14] Hong Yiguo. Marine nitrogen cycle recorded by nitrogen and oxygen isotope fractionation of nitrate[J]. Advances in Earth Science, 2013,28(7):751-764.
[14] [洪义国.硝酸盐氮氧稳定同位素分馏过程记录的海洋氮循环研究进展[J].地球科学进展,2013, 28(7):751-764.]
[15] Li Xiangquan, Hou Xinwei, Zhang Hongda, et al. Study on the geochemistry-isotope characteristics of the groundwater systems in Taiyuan Basin[J]. Journal of Arid Land Resources and Environment, 2006,20(5):109-114.
[15] [李向全, 侯新伟, 张宏达, 等. 太原盆地地下水系统水化学—同位素特征研究[J].干旱区资源与环境,2006, 20(5):109-114.]
[16] Deng Yinger, Jia Shuyuan, Huang Runqiu, et al. Groundwater systerm of karst fracture-cave media[J]. Advances in Earth Science,2008, 23(5):489-494.
[16] [邓英尔, 贾疏源, 黄润秋, 等. 岩溶缝洞系统地下水系研究[J]. 地球科学进展,2008, 23(5):489-494.]
[17] Beijing Buraeu of Geology. Beijing Regional Geology[M]. Beijing: Geological Publishing House, 1991.
[17] [北京市地质矿产局. 北京市区域地质志[M]. 北京: 地质出版社, 1991.]
[18] Beijing Buraeu of Geology. Beijing Lithostratigraphic[M]. Beijing: China University of Geosciences Press, 1996.
[18] [北京市地质矿产局. 北京市岩石地层[M]. 北京:中国地质大学出版社, 1996.]
Options
文章导航

/

〈 〉

地址：甘肃省兰州市天水中路8号
QQ：114723517
电话：0931-8762293　E-mail：adearth@lzb.ac.cn
陇ICP备2021001824号-5　 甘公网安备62010202000687