Volume 44 Issue 9
Sep.  2019
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Su Chunli, Zhang Ya, Ma Yanhua, Liu Wenbo, 2019. Hydrochemical Evolution Processes of Karst Groundwater in Guiyang City: Evidences from Hydrochemistry and 87Sr/86Sr Ratios. Earth Science, 44(9): 2829-2838. doi: 10.3799/dqkx.2019.214
Citation: Su Chunli, Zhang Ya, Ma Yanhua, Liu Wenbo, 2019. Hydrochemical Evolution Processes of Karst Groundwater in Guiyang City: Evidences from Hydrochemistry and 87Sr/86Sr Ratios. Earth Science, 44(9): 2829-2838. doi: 10.3799/dqkx.2019.214
shu

Hydrochemical Evolution Processes of Karst Groundwater in Guiyang City: Evidences from Hydrochemistry and 87Sr/86Sr Ratios

doi: 10.3799/dqkx.2019.214
  • 1.

    School of Environmental Studies, China University of Geosciences, Wuhan 430074, China

  • 2.

    Hainan Institute of Environmental Sciences, Haikou 570026, China

  • 3.

    China Geological Environment Monitoring Institute, Beijing 100081, China

  • Received Date: 2019-06-29
  • Publish Date: 2019-09-15
    Abstract
  • Study on hydrochemical characteristics and water-rock interaction is of great significance to ascertain the causes of groundwater pollution and the sustainable use of karst water. Hydrochemical components and types, ion ratios, strontium content, 87Sr/86Sr ratio and inverse hydrogeochemical modelling were employed to identify hydrochemical evolutional processes of karst groundwater in Guiyang City. The results show that the hydrochemical types of groundwater are mainly HCO3·SO4-Ca and HCO3-Ca·Mg, and the hydrochemical compositions of groundwater varied with time and space due to the dissolution/precipitation of different minerals. The mixing of surface water and groundwater has a certain influence on the hydrochemical characteristics of groundwater. Strontium isotope analysis and inverse hydrogeochemical modeling indicate that the hydrochemical characteristics of groundwater are mainly controlled by rock weathering. The dissolution-precipitation of carbonate dominated by calcite and dolomite as well as the dissolution of sulfate and halite are important processes to control the hydrochemical characteristics of groundwater in the study area, and are also affected by the hydrolysis of silicate minerals in the overlying porous aquifer.

     

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