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2019 Vol. 46, No. 2
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CAO Jianwen, XIA Riyuan, FANG Shangwu, ZHAO Liangjie, WANG Zhe, WANG Ruofan, YI Rui. 2019. Model and mechanism of 'water exploration by cross layer' for high sulfate area in slope region of Yunnan-Guizhou Plateau[J]. Geology in China, 46(2): 235-243. doi: 10.12029/gc20190202
Citation: CAO Jianwen, XIA Riyuan, FANG Shangwu, ZHAO Liangjie, WANG Zhe, WANG Ruofan, YI Rui. 2019. Model and mechanism of "water exploration by cross layer" for high sulfate area in slope region of Yunnan-Guizhou Plateau[J]. Geology in China, 46(2): 235-243. doi: 10.12029/gc20190202
shu

Model and mechanism of "water exploration by cross layer" for high sulfate area in slope region of Yunnan-Guizhou Plateau

  • 1.

    Institute of Karst Geology, CAGS/Karst Dynamics Laboratory, MNR & GZAR, Guilin 541004, Guangxi, China

  • 2.

    No. 114 Geological Party, Guizhou Bureau of Geology and Mineral Resources, Zunyi 563000, Guizhou, China

    • Fund Project: Supported by China Geological Survey Program (No. DD20160300; DD20190342)
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  • Author Bio: CAO Jianwen, male, born in 1983, senior engineer, engages in karst geology and hydrogeology survey research; E-mail:caojianwen@karst.ac.cn
Received Date:  15 September 2018
Revised Date:  12 March 2019
Publish Date:  25 April 2019
    Abstract

  • Groundwater is an important drinking water source in Southwest China. However, there exists a large area of sulfate exceeding standard in groundwater in the northern part of Zhenning County in Central Guizhou Province, which leads to the problem of water shortage in local area. The following conclusions were obtained by methods of lithofacies palaeogeographic analysis, hydrochemical analysis, D, 18O, 34S isotope test, rock sample test, core observation and other technical methods:The main source of water supply in the study area is meteoric water; the concentration of sulfate (SO42-) in groundwater is in the range of 30-1100 mg/L, with an average value of 221.78 mg/L, showing the characteristics of highly enriched S042-; the concentration of S042- in different types of groundwater exhibits the law of well > rising spring > falling spring > karst pool > underground river > bedrock fissure spring > epikarst spring; the source of sulfate root in epikarst spring is mainly meteoric water, and the source of sulfate root in high sulfate samples such as J469, J585, ZK3-2 and C010 is mainly dissolved in gypsum. On such a basis and in combination with drilling data, the authors detected the distribution of gypsum rock layer and the characteristics of aquifer structure, and adopted the lower sulfate aquifers to obtain qualified drinking water source by establishing the "cross layer water finding" model, which can effectively solve the problem of water shortage in the study area.

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