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Geoscience ›› 2025, Vol. 39 ›› Issue (02): 440-446.DOI: 10.19657/j.geoscience.1000-8527.2022.028

• Monitoring, Modeling and Assessment of Supergene Resources • Previous Articles     Next Articles

Hydrochemical Characteristics and Genesis analysis of Shallow Groundwater in the Lower reaches of Nanfei River, Anhui Province

WANG Runtao(), QIAN Jiazhong(), WANG Xiuxuan, MA Haichun, WANG Xiaoyong   

  1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, Anhui 230009, China
  • Online:2025-04-10 Published:2025-05-08
  • Contact: QIAN Jiazhong

Abstract:

In order to explore the hydrochemical characteristics and genesis of shallow groundwater in the lower reaches of Nanfei River, Anhui Province, 87 groups of shallow groundwater samples were collected. By using Piper trigram, Shukalev classification, Gibbs model, ion ratio method and mathematical statistics, the hydrochemical characteristics and genesis of shallow groundwater in the lower reaches of Nanfei River were analyzed, and their genesis were further revealed. The results show that the average pH value of the shallow groundwater in the lower reaches of Nanfei River is 7.61, showing weak alkalinity. The average value of cation content is in the order of Na+ >Ca2+ >Mg2+ from high to low, and the average value of anion content is in the order of $\mathrm{HCO}_{3}^{-}>\mathrm{SO}_{4}^{2-}>\mathrm{Cl}^{-}$ from high to low. Na+ and $\mathrm{HCO}_{3}^{-}$ are the dominant ions in cations and anions respectively. In addition, the distribution of shallow groundwater chemical types in the lower reaches of Nanfei River is relatively rich, with a total of 15 hydrochemistry types, and the main hydrochemistry types can be divided into HCO3-Na·Ca, HCO3·Cl-Ca·Na, HCO3-Ca·Na·Mg, HCO3·SO4-Ca·Na, HCO3·SO4·Cl-Na·Ca. By considering the influence of water-rock interaction, we find that the hydrochemical composition of the shallow groundwater in the lower reaches of Nanfei River is mainly controlled by rock weathering and dissolution and affected by dissolution of carbonate mineral. Meanwhile, cation exchange plays an important role in the hydrochemical characteristics of shallow groundwater.

Key words: lower reaches of Nanfei river, shallow groundwater, hydrochemical characteristics, genesis analysis

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