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2021 Vol. 48, No. 6
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LU Shiji, ZHOU Hong, LIU Wei, CHEN Qianlong, YAN Ziqi, CHEN Li. 2021. Distribution and enrichment of strontium in the Zigui karst watershed[J]. Geology in China, 48(6): 1865-1874. doi: 10.12029/gc20210616
Citation: LU Shiji, ZHOU Hong, LIU Wei, CHEN Qianlong, YAN Ziqi, CHEN Li. 2021. Distribution and enrichment of strontium in the Zigui karst watershed[J]. Geology in China, 48(6): 1865-1874. doi: 10.12029/gc20210616
shu

Distribution and enrichment of strontium in the Zigui karst watershed

  • 1.

    Geological Survey of China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

    SGIDI Engineering Consulting(Group) Co., Ltd, Shanghai 200433, China

  • 3.

    Karst Dynamics Laboratory, MNR, Guilin 541004, Guangxi, China

    • Fund Project: Supported by the project of China Geological Survey (No.DD20160304, No.DD20190824), Key Laboratory of Karst Dynamics, MNR and GZAR (Institute of Karst Geology, CAGS) Guilin (No.KDL201703), Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (No.CUGL180837)
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  • Author Bio: LU Shiji, male, born in 1993, master candidate, engaged in karst hydrogeological research; E- mail: lushiji@sgidi.com
  • Corresponding author: LIU Wei, male, born in 1985, assistant researcher, engaged in karst hydrogeology and environmental geology; E-mail: wliu@cug.edu.cn 
Received Date:  15 July 2019
Revised Date:  24 July 2020
Publish Date:  25 December 2021
    Abstract

  • In order to explore the distribution and enrichment of strontium in groundwater under the control of water flow system in karst area, the Maoping river and Jiuwanxi karst watershed in Zigui were taken as the study case, and 415 groups of water samples and 93 groups of rock samples were collected from typical springs, typical surface water and main water-bearing rocks during 2016-2018. The analytical results indicate that strontium is mainly enriched in the strata of the Jialingjiang Formation, Loushanguan Formation and Dengying Formation deposited in tidal flat and lagoon sedimentary facies, and mostly exists in the form of celestite, strontianite and other minerals. The water type of Sr-rich groundwater is mainly SO4 type, Cl type, and SO4-HCO3 type. In the water flow system, ,the strontium-rich minerals are less in strata above vadose zone, mainly affected by leaching; both celestite and strontianite are not saturated in shallow groundwater, but they tend to be saturated in a few deep groundwater. The closed reduction environment rich in gypsum and celestite is conducive to the enrichment of strontium in groundwater.

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