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永定河对北京西山岩溶水和玉泉山泉的影响

秦大军 孙杰 郭艺 李露 Mohammed Haji 王东东 刘文才

工程地质学报2019,Vol.27Issue(1):162-169,8.
工程地质学报2019,Vol.27Issue(1):162-169,8.DOI:10.13544/j.cnki.jeg.2019-006

永定河对北京西山岩溶水和玉泉山泉的影响

IMPACTS OF YONGDING RIVER ON THE XISHAN KARST AQUIFER AND YUQUAN SPRING IN BEIJING, CHINA

秦大军 1孙杰 2郭艺 3李露 2Mohammed Haji 3王东东 2刘文才3

作者信息

  • 1. 三亚学院翟明国院士工作站, 三亚 572000
  • 2. 中国科学院地质与地球物理研究所, 中国科学院页岩气与地质工程重点实验室, 北京 100029
  • 3. 中国科学院地球科学研究院, 北京 100029
  • 折叠

摘要

Abstract

The karst water mixed with infitrated river water shows high Na, Cl and O-18 values and can be used to indicate the distribution of the infiltrated river water in karst aquifers. Individual flow path for three recharge sources was identified in the Xishan karst aquifer in Beijing, China using hydrochemical and isotopic methods. The recharge of rainfall in the Junzhuang area had two flow routes: one flows eastwards to the Yongfengtun; another flows southeastwards along east of the Yongding fault. The recharge of rainfall in Tanzhesi area flows along north of the Babaoshan fault northeastwards Sijiqing. The Yongdingriver infiltrates in the Junzhuang area and flows along the Yongding fault in the direction of southeast and turns to the diction of northeast near Gucheng, along a buried fault which is revealed this time. River water plays an important role in recharge to the karst aquifer and can be used to restore depleted karst flow systems by increasing the flow and infiltration of river water.

关键词

河水/岩溶水/水化学/同位素/水流路径/北京

Key words

River water/Karst water/Hydrochemistry/Isotope/Flow path/Beijing

分类

天文与地球科学

引用本文复制引用

秦大军,孙杰,郭艺,李露,Mohammed Haji,王东东,刘文才..永定河对北京西山岩溶水和玉泉山泉的影响[J].工程地质学报,2019,27(1):162-169,8.

基金项目

国家自然科学基金 (41172215) (41172215)

北京岩溶水资源勘查评价项目 (BJYRS-ZT-07) (BJYRS-ZT-07)

北京市西郊地区地下水战略储备前期勘察项目 (Z141100003614060) 资助 (Z141100003614060)

工程地质学报

OA北大核心CSCDCSTPCD

1004-9665

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