ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
典型岩溶包气带洞穴滴水水文过程研究—以桂林硝盐洞为例
  
关键词:Xiaoyan Cave  vadose zone  epikarst aquifer  hydrological process  precipitation threshold  residence time
基金项目:国家自然科学基金项目(编号: 41172231; 41502176; 41302211)、中国地质调查局地质调查项目(编号: DD20160285)和广西院士顾问项目(编号: 2002371310009)联合资助
作者单位E-mail
郭小娇 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
联合国教科文组织国际岩溶研究中心 
lguo2010@163.com 
龚晓萍 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
广西水文地质工程地质队 
 
袁道先 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
联合国教科文组织国际岩溶研究中心 
dxyuan@karst.edu.com 
殷建军 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
联合国教科文组织国际岩溶研究中心 
 
姜光辉 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室  
林玉石 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室  
白 冰 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
联合国教科文组织国际岩溶研究中心 
 
汤庆佳 中国地质科学院岩溶地质研究所, 国土资源部/广西岩溶动力学重点实验室
联合国教科文组织国际岩溶研究中心 
 
陈长杰 中国地质大学(北京)  
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摘要:
Research on Hydrological Processes of Cave Dripping Water in a Typical Karst Vadose Zone: A Case Study of Xiaoyan Cave, Guilin
      The high resolution monitoring of hydrochemistry and tracing test were conducted to determine recharge sources and study hydrological response processes of cave dripping water to precipitation in Xiaoyan Cave. The results indicate that the dripping water of Xiaoyan Cave is mainly recharged by two different flow components, i.e., conduit flow characterized by concentrated recharge and diffuse flow. The epikarst aquifer probably exists in the upper vadose zone of Xiaoyan Cave, which continuously maintains the drip flow. The peak of drip flow, electrical conductivity and tracer concentration all show a rapid response with conduit flow during the intensive precipitation events, and there is a threshold arousing the dripping water response to the precipitation in Xiaoyan Cave. The pre-even karst aquifer hydrological conditions are main factors that cause hydrological response differences of karst vadose zones. Two response modes of dripwater to infiltration event was identified as the retention function of soil and epikarst, with the result of a 10-hour rapid response in wet season and a 9.8-day lagged-time response in dry season. 74.4 mm rainfall is the threshold for precipitation response from dry to rainy season. The integration of cave dripwater hydrodynamic variation and tracer test technology proves to have a significant influence on studying hydrological processes in vadose zone, acquiring the structure and characteristics of karst aquifer and revealing the mechanism of precipitation infiltration recharge in karst area.
GUO Xiao-jiao,GONG Xiao-ping,YUAN Dao-xian,YIN Jian-jun,JIANG Guang-hui,LIN Yu-shi,BAI Bing,TANG Qing-jia,CHEN Chang-jie.2017.Research on Hydrological Processes of Cave Dripping Water in a Typical Karst Vadose Zone: A Case Study of Xiaoyan Cave, Guilin[J].Acta Geoscientica Sinica,38(4):537-548.
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