中国岩溶2018，Vol.37Issue(1)：1-8,8.DOI:10.11932/karst20180101
岩溶高原地下水径流系统垂向分带
Vertical zoning of groundwater runoff system in karst plateau
摘要
Abstract
The vertical zoning of groundwater runoff system in karst plateau have been discovered by large number of the exposed and observational studies of mineral resource exploitation,geological exploration,cave detection,tracer tests and so on.Based on burying condition of karst aquifer,spatial pattern of groundwater runoff,groundwater dynamics and the extent and depth of groundwater circulation,the groundwater runoff system can be divided into two types and six sub-classes in karst plateau.The details are as follow (Table 1).The zoning of groundwater runoff system in karst plateau is mainly determined by the sedimentary facies and sedimentary cycle of the strata,geologic structural association,topographic relief,zoning of karst development.The characteristics of shallow-circulating runoff zone are with shallower circulation underground,circulating period within one hydrogeological year and being obviously impacted by seasonal change.The deepcirculating runoff zones are with deeper circulation under ground,circulating period long as several to several decade years or more and being less or few impacted by seasonal change.The characteristics of six sub-classes are direct-viewing and distinct,which would be described in detail in the paper.关键词
岩溶高原/水循环/地下水/径流系统/垂向分带Key words
karst plateau/hydrological cycle/groundwater/runoff system/vertical zoning分类
天文与地球科学引用本文复制引用
王宇..岩溶高原地下水径流系统垂向分带[J].中国岩溶,2018,37(1):1-8,8.基金项目
国家重点研发计划项目课题:断陷盆地地表、地下水资源高效利用与优化调控(2016YFC0502502) （2016YFC0502502）
