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降雨对裂隙型岩溶含水系统演化影响的数值模拟研究

毛亮 于青春 王敬霞 李洪辉 赵帅维 贾梅兰

中国岩溶2017,Vol.36Issue(1):42-48,7.
中国岩溶2017,Vol.36Issue(1):42-48,7.DOI:10.11932/karst20170105

降雨对裂隙型岩溶含水系统演化影响的数值模拟研究

Numerical simulation of precipitation impact on fractured karst system evolution

毛亮 1于青春 2王敬霞 2李洪辉 2赵帅维 1贾梅兰1

作者信息

  • 1. 中国辐射防护研究院三废治理研究所,太原030006
  • 2. 中国地质大学(北京)水资源与环境学院,北京100083
  • 折叠

摘要

Abstract

The 10,000 years evolution of fractured karst system,which has precipitation infiltration and river recharge,is calculated using finite difference method,cubic law and Dreybort's (1996) empirical formula after building on the conceptual model of fractured karst system The result shows that the dissolution of karst aquifer system mainly occurs in the point of precipitation infiltration,recharge rivers and karst springs.With the dissolution of the karst aquifer system,the water tables were declining and some of the karst springs were dry.We found that the number of precipitation infiltration does not significantly affect the evolution of fractured karst system which has river recharge.

关键词

岩溶演化/裂隙渗流/碳酸盐溶蚀速率/数值模拟

Key words

karst evolution/fracture seepage/carbonate dissolution rate/numerical simulation

分类

天文与地球科学

引用本文复制引用

毛亮,于青春,王敬霞,李洪辉,赵帅维,贾梅兰..降雨对裂隙型岩溶含水系统演化影响的数值模拟研究[J].中国岩溶,2017,36(1):42-48,7.

基金项目

国家自然科学基金资助项目(40772208) (40772208)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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