Journal of Guangxi Normal University(Natural Science Edition) ›› 2020, Vol. 38 ›› Issue (4): 132-139.doi: 10.16088/j.issn.1001-6600.2020.04.016

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Hydrochemical Characteristics and Main Ion Sourcesof Shallow Groundwater in Zihe River Source Region, Shandong, China

YOU Jing1,2, QI Yueming1*, SHAO Guangyu3, MA Chao3, YANG Yaqi1, PEI Yifeng1   

  1. 1. School of Resources and Geosciences, China University of Mining and Technology, Xuzhou Jiangsu 221116, China;
    2. Shanghai Institute of Geological Engineering Exploration, Shanghai 200072, China;
    3. Shangdong Institute of GeologicalEngineering Exploration, Jinan Shandong 250014, China
  • Received:2019-04-28 Published:2020-07-13

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Abstract: The hydrogeological site investigation and hydrogeochemical methods were used to study the chemical characteristics and main ion sources of shallow groundwater in the source region of the Zihe River. The research showed that there are three types of shallow groundwater in the source region of the Zihe River:Quaternary loose pore water, carbonate rock karst groundwater and massive rock weathered fissure water. The water quality types are respectively:HCO3·SO4-Ca·Mg type, HCO3·SO4-Ca·Mg type and HCO3·SO4-Ca type. The concentrations of calcium, magnesium and bicarbonate ions in the three types of groundwater are relatively stable in the aquifer, while the concentrations of sodium, potassium, nitrate and chloride in the groundwater of the study area vary greatly, which are affected by environmental factors. As the main water supply target, the main chemical components of carbonate karst groundwater, calcium ions are mainly derived from the dissolution of dolomite and calcite, and partly from the infiltration of chloride ions and nitrate ions and the dissolution of gypsum. Magnesium ion is derived from the dissolution of dolomite; bicarbonate ion is mainly derived from the co-dissolution of calcite and dolomite, and secondly by rainfall replenishment; sulfate ion has three sources, but mainly from the dissolution of gypsum layer and the oxidation of pyrite. The comprehensive results showed that the groundwater quality in the source area of the Zihe River is good, and all the indicators have reached the groundwater Class III water quality standard. The shallow groundwater quality is mainly related to the precipitation, groundwater flow conditions and bare or shallow burial of the carbonate. The research will provide a scientific decision-making basis for the planning and construction of karst groundwater source areas in the source region of the Zihe River, and rational utilization and protection of karst groundwater resources.

Key words: Zihe River, karst groundwater, hydrochemical characteristics, hydrogeochemistry

CLC Number: 

  • X36
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