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Chinese Journal of Applied Ecology ›› 2024, Vol. 35 ›› Issue (11): 3149-3156.doi: 10.13287/j.1001-9332.202410.015

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Hydrochemical and isotopic characteristics and water transformation relationships in the Zhenglan Banner section of Shandian River Basin, China.

JI Mingyu1,2, JIA Debin1,2*, HAO Yusheng1,2, LIU Ting1,2, YANG Lina3, LI Xiaoyan4, LYU Chenge1,2, SHANG Ziqin1,2   

  1. 1College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China;
    2Key Laboratory of Eco-Hydrology and Efficient Use of Water Resources, Inner Mongolia Autonomous Region, Hohhot 010010, China;
    3Centre for Management of Baotou Reservoir, Baotou 014017, Inner Mongolia, China;
    4Hohhot Sub-Center for Hydrology and Water Resources, Hohhot 010010, China
  • Received:2024-04-18 Revised:2024-08-19 Online:2024-11-18 Published:2025-05-18

Abstract: Water resources are essential for sustaining life, driving economic development, and protecting the environment. We investigated the hydrochemical variations of surface water and groundwater in the Shandian River Basin to identify the driving factors and the transformation relationship between each water body. Precipitation data was collected from May to October 2023, while surface water and groundwater samples were collected in both August (wet season) and October (dry season). We analyzed water samples by Piper triplex diagram, Gibbs diagram, ion ratio method, hydrogen and oxygen isotope analysis, and MixSIAR mixed model. The results indicated that both groundwater and surface water were generally weakly alkaline. The dominant type of groundwater chemical composition was HCO3--Ca2+·Na+.During the process of surface water transitioning from the wet season to the dry season, the predominant surface water chemistry type shifted from HCO3--Ca2+-Na+ to HCO3--Na+-Mg2+, as well as HCO3--Ca2+-Na+-Mg2.Furthermore, the main hydrochemical types of surface water changed during the transition from wet season to dry season. The hydrochemical characteristics of different types of water were influenced by weathering of rocks, evaporation and concentration of water, as well as cation exchange. Additionally, significant enrichment of δD and δ18O isotopic values in surface water was observed during the wet season, and the ground-water remained in a depleted state during both wet and dry seasons. During the wet and dry seasons, the slope of surface water line was lower than that of the precipitation line, and the slope of groundwater line during the wet season was similar to that of the precipitation line and the surface water line, indicating the complexity of the conversion relationship between various water bodies during the wet season. The precipitation served as ~70% primary recharge source for surface waters, whereas underground aquifers contributed ~30%, being the secondary recharge source. During the dry season, groundwater replenished surface water. These findings would provide fundamental support for effective resource management and protection practices related to the basin.

Key words: Blue Flag section of Shandian River, stable isotopes of hydrogen and oxygen, hydrochemical characteristics, conversion of water bodies, MixSIAR model