中文核心期刊
CSCD来源期刊
中国科技核心期刊
RCCSE中国核心学术期刊

Journal of Chongqing Jiaotong University(Natural Science) ›› 2016, Vol. 35 ›› Issue (4): 83-87.DOI: 10.3969/j.issn.1674-0696.2016.04.17

• Port & Waterway · Hydraulic & Hydroelectric · Resources & Environment • Previous Articles     Next Articles

Study on the Enrichment Characteristics of Groundwater in Chongqing Southeast and Northeast Karst Areas

LV Yuxiang,HU Wei , ZHOU Jun   

  1. (Hydrogeology & Engineering Team 208, Chongqing Bureau of Geological Exploration, Chongqing 400700, P.R.China)
  • Received:2015-03-13 Revised:2015-09-29 Online:2016-08-20 Published:2016-08-20

渝东南渝东北岩溶区地下水富集特征研究

吕玉香,胡伟,周军   

  1. ( 重庆市地质矿产勘查开发局, 208水文地质工程地质队,重庆 400700)
  • 作者简介:第一作者:吕玉香(1984—),女,山东成武人,高级工程师,硕士,主要从事水文地质方面的研究。E-mail:lvyx02@163.com。
  • 基金资助:
    重庆市国土房管局2012年度科技计划项目(CQGT-KJ-2012014)

Abstract: Combining with the recent implementation in Chongqing Southeast and Northeast karst area of 1∶50 000 hydrogeological investigation and water demonstration project, karst groundwater enrichment characteristicswas studied, The influence degree of formation lithology, topography, geological structure and physiographic stages on karst groundwater enrichment; karst groudwater had uneven distribution of time and space. According to different stratum, topography, geological structure conditions, karst groundwater was divided into three types: extremely inhomogeneity, inhomogeneity, relatively uniform. According to karst groundwater circulation conditions and hydrodynamic characteristics, the study area of the water rich block was divided into confluence type, shunt type, discharge type, fractured type.The direction of developing and utilizing was proposed, and the basis for the development and utilization of karst waterwas provided .

Key words: environment engineering, Chongqing southeast and northeast, karst water, enrichment characteristics, inhomogeneity, enrichment model

摘要: 结合近年来在渝东南渝东北岩溶地区实施的1∶50 000水文地质调查及供水示范项目,对该区岩溶地下水富集特征开展研究。分析了地层岩性、地形地貌、地质构造、地文期等因素对岩溶地下水富集的影响程度;岩溶地下水时空分布不均,依据地层、地形地貌、地质构造条件不同,将岩溶地下水富集均一性分为极不均一、不均一、相对均一3类;根据岩溶地下水循环条件和水动力特征,将研究区内的富水模式分为汇流型、分流型、泄流型、断裂带型,提出了开发利用方向,为岩溶水的开发利用提供了依据。

关键词: 环境工程, 渝东南渝东北, 岩溶水, 富集特征, 不均一性, 富集模式

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