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2022 Vol. 49, No. 5
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Article navigation > Geology in China > 2022 > 49(5): 1527-1542
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JIN Yang, JIANG Yuehua, DONG Xianzhe, YANG Guoqiang, LIU Hongying, LEI Changzheng, ZHOU Quanping, ZHANG Hong, MEI Shijia, YANG Hui, LÜ Jinsong, LI Yun. 2022. Chemical characteristics and eco-environmental effect of groundwater in Ningbo Plain, Zhejiang Province[J]. Geology in China, 49(5): 1527-1542. doi: 10.12029/gc20220511
Citation: JIN Yang, JIANG Yuehua, DONG Xianzhe, YANG Guoqiang, LIU Hongying, LEI Changzheng, ZHOU Quanping, ZHANG Hong, MEI Shijia, YANG Hui, LÜ Jinsong, LI Yun. 2022. Chemical characteristics and eco-environmental effect of groundwater in Ningbo Plain, Zhejiang Province[J]. Geology in China, 49(5): 1527-1542. doi: 10.12029/gc20220511
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Chemical characteristics and eco-environmental effect of groundwater in Ningbo Plain, Zhejiang Province

  • 1. Chinese Academy of Geological Sciences, Beijing 100037, China;

  • 2. Nanjing Center, China Geological Survey, Nanjing 210016, Jiangsu, China;

  • 3. Key Laboratory of Watershed Eco-Geological Processes, Ministry of Natural Resources, Nanjing 210016, Jiangsu, China;

  • 4. Zhejiang Institute of Hydrogeology and Engineering Geology, Ningbo 315012, Zhejiang, China

More Information
  • Corresponding author: LI Yun
Received Date:  13 July 2020
Revised Date:  06 September 2020
    Abstract
  • This paper is the result of groundwater geological survey engineering.
    [Objective] In order to find out the characteristics of groundwater and its reason for evolution in Ningbo plain, and help to optimize the groundwater environment of Ningbo area. [Methods] Groundwater in Ningbo plain was analyzed comprehensively and systemically based on field survey and samples analysis, making full use of the previous data, then multiple methods including the mathematical statistics, the correlation matrices, Piper diagram, the ratio coefficient of main ions and environmental isotope were used for this study. [Results] The main of surface water and phreatic water were fresh water, however, confined water were mainly brackish water or salt water. HCO3- of phreatic water was the predominant anion and Cl-, Ca2+, Na+ were all secondary. Contrastly, the dominant ions of surface water and confined water were Cl- and Na+, HCO3- was the second. The four water were divided into twenty- three hydrochemical types, and surfer water and phreatic water were both influenced by precipitation evidently, whereas confined water deeply was closed in the aquifer during previous transgression, so there was little relationship with shallow water. [Conclusions] Compared with that in the 1970s, the distribution of fresh water body in confined aquifer Ⅰ of Ningbo urban area had no significant change, but that in confined aquifer Ⅱ was changing obviously by the influence of both human activities and natural water recycle. Salt water appeared in the scope of fresh water by hydrochemical evolution, and the scope of fresh water body expanded outside, overall, the distribution area increased by twelve square kilometer approximately, and the environmental effect was being towards positive tendency.
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