长江科学院院报 ›› 2016, Vol. 33 ›› Issue (8): 22-33.DOI: 10.11988/ckyyb.20150972

• 水资源与环境 • 上一篇    下一篇

贵州修文县陶家龙潭水源地水文地质特征

曾红彪1,邵莲芬2,余宏明1,李亚1   

  1. 1.中国地质大学武汉 工程学院, 武汉 430074;
    2.黄淮学院 建筑工程学院,河南 驻马店 463000
  • 收稿日期:2015-11-16 修回日期:2015-12-13 出版日期:2016-07-25 发布日期:2016-07-25
  • 通讯作者: 余宏明(1952-),男,湖北咸宁人,教授,博士生导师,主要从事地质灾害分析与防治及岩土工程领域的教学与科研工作,(电话)18627871639(电子信箱)yuhongming55@sohu.com。
  • 作者简介:曾红彪(1988-),男,河南商丘人,博士研究生,主要从事水文地质及地质灾害设计、防治方面的研究,(电话)18202761986(电子信箱)zhb2012xqd@126.com。
  • 基金资助:
    国家自然科学基金项目(41272377);贵州省试点地区地下水基础环境状况调查评估(2012A054)

Hydrogeological Characteristics of Taojialongtan Water Source Area in Xiuwen County of Guizhou

ZENG Hong-biao1, SHAO Lian-fen2, YU Hong-ming1, LI Ya1   

  1. 1.Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;
    2.School of Architectural Engineering, Huanghuai University, Zhumadian 463000,China
  • Received:2015-11-16 Revised:2015-12-13 Published:2016-07-25 Online:2016-07-25

摘要: 为了研究贵州省岩溶区水源地水文地质特征,以修文县陶家龙潭水源地为研究对象,结合水文地质测绘等调查方法及岩溶地下水的发育规律,得到其地质概况及岩溶发育影响因素、边界条件等特征。划分其隔水边界条件的依据主要为隔水边界阻水性质、边界沿线岩溶现象发育情况、地下水出露点,并以地形分水岭为依据研究其补给边界。研究表明水源地发育区域具有独立的水文地质单元的特征;陶家龙潭水文地质单元的发育主要受岩性和裂隙构造的影响;排泄形式主要为岩溶泉和人工开采,并最终排泄于地表河流;水源地地下水水化学类型为HCO3·SO4—Ca·Mg水,适合作为饮用水源。

关键词: 水文地质单元, 水源地, 岩溶地下水, 边界条件, 陶家龙潭

Abstract: In order to study the hydrogeological characteristics of water source in the karst area of Guizhou Province, we take Taojialongtan water source area in Xiuwen country as study object. In association with investigation methods like hydrological surveying and according to the development law of karst groundwater, we obtain the characteristics such as general geological situation, factors affecting karst development, and boundary conditions. We divide impervious boundary conditions according to three aspects water blocking property of the boundary, development situation of karst along the boundary, and the groundwater emergence location.Moreover on this basis, we study the recharge boundary. Results show that the development area of water source has the characteristics of an independent hydrogeological unit; meanwhile, the development of Taojialongtan hydrogeological unit is mainly influenced by lithology and fissure structures; furthermore, discharges mainly takes the form of karst spring and artificial mining, which ultimately flows into the surface river; finally, the hydrochemistry type of Taojialongtan water source area is of HCO3·SO4-Ca·Mg, suitable for drinking water source.

Key words: hydrogeological unit, water source area, karst groundwater, boundary conditions, Taojialongtan

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