Earth Science Frontiers ›› 2025, Vol. 32 ›› Issue (2): 469-483.DOI: 10.13745/j.esf.sf.2023.12.30

Previous Articles     Next Articles

The genesis of groundwater chemistry in Yellow River Delta: A case study of Gudao Town, Dongying City, Shandong Province

WANG Wei1(), CHENG Xing2, GAO Xubo2,*(), TIAN Zhenhuan1,*(), LIU Chunhua3, WU Zhanhui2, LI Chengcheng2, KONG Shuqiong2   

  1. 1. No.1 Institute of Geology and Mineral Resources of Shandong Province/Shandong Engineering Research Center for Iron-rich Ore Exploration and Exploitation Technology, Jinan 250109, China
    2. China University of Geosciences (Wuhan), Wuhan 430074, China
    3. Shandong Regional Geological Survey, Jinan 250013, China
  • Received:2023-10-12 Revised:2023-12-05 Online:2025-03-25 Published:2025-03-25

Abstract:

The Yellow River Delta is a key strategic economic zone in China, making it crucial to understand the characteristics and genetic mechanisms of groundwater quality for the sustainable utilization of groundwater resources and the protection of ecological and environmental health. Focusing on Gudao Town in the Yellow River Delta, this study systematically investigates groundwater quality and its formation mechanisms through field hydrogeological surveys, hydrogeochemical monitoring, and laboratory analysis. The findings are as follows: (1)The main hydrochemical types of different waters in the study area are HCO3·SO4-Na·Ca (Yellow River water), Cl-Na (seawater), Cl-Na (surface water), Cl·HCO3-Na (brackish groundwater), and Cl-Na (underground brackish water and brine).(2)Surface water and brackish groundwater are closely associated with silicate end members. The formation of brackish water is primarily influenced by cation exchange and the dissolution of silicate rocks, with dolomite and gypsum dissolution playing a dominant role. (3) Brackish water is mainly controlled by the dissolution of silicate and evaporite rocks, with its salinity primarily attributed to seawater intrusion. (4) The Cl- concentration in groundwater decreases progressively from the coastal area to the inland, while F concentration decreases from the estuary to the inland. The distribution patterns of Na+, Mg2+, Ca2+, and SO42- concentrations align with that of total dissolved solids (TDS), indicating that these elements are primarily derived from the intrusion of both ancient and modern seawater. Additionally, changes in NH4+ concentrations are largely influenced by human activities.

Key words: Yellow River Delta, groundwater chemistry, water pollution, hydrogeochemical processes

CLC Number: