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Geoscience ›› 2022, Vol. 36 ›› Issue (02): 418-426.DOI: 10.19657/j.geoscience.1000-8527.2022.012

• Water Resources and Environmental Research • Previous Articles     Next Articles

Hydrochemical Characterization and Irrigation Suitability Analysis of Shallow Groundwater in Hetao Irrigation District, Inner Mongolia

LI Zeyan1,2,3(), CAO Wengeng1,2,3(), WANG Zhuoran4, LI Jincheng1,5, REN Yu1,2,3   

  1. 1. The Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang,Hebei 050061, China
    2. Key Laboratory of Groundwater Sciences and Engineering,Ministry of Natural Resources, Shijiazhuang,Hebei 050061, China
    3. Hebei Cangzhou Groundwater and Land Subsidence National Observation and Research Station, Shijiazhuang,Hebei 050061, China
    4. Water Information Center, Ministry of Water Resources, Beijing 100053, China
    5. School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
  • Received:2021-09-30 Revised:2022-03-10 Online:2022-04-10 Published:2022-06-01
  • Contact: CAO Wengeng

Abstract:

With the aggravation of conflict between supply and demand of water resources in the Yellow River basin, both Yellow River water and groundwater are used for agricultural irrigation in the Hetao region of Inner Mongolia (one of the large irrigation districts in China). In this paper, 499 groundwater samples and 1 Yellow River water sample were collected. Based on hydrogeochemical analysis of these samples, the irrigation suitabi-lity difference between groundwater and Yellow River water has been studied by SAR, PI, SC, RSC and Irrigation Water Quality Standard (GB 5084-2021). The results show that the environment of groundwater and Yellow River water are both weakly alkaline, and the major ions are Ca2+ and HC03-. The Gibbs diagram shows that the groundwater is affected by rock weathering/leaching and evaporation concentration, and the sodium salts (which have immense influence on irrigation suitability) come mainly from rock salt dissolution. According to the irrigation suitability analysis results about SAR, PI and RSC, the groundwater is suitable for irrigation. According to the SC evaluation result, the groundwater unsuitable for irrigation is mainly distributed in the main drainage channel in the northern irrigation area and along the Yellow River in the southern irrigation area. According to the irrigation water quality standard, except for the total arsenic and chloride, over 90% samples have other irrigation suitability indices. A total of 231 samples are suitable for irrigation. Comparing the irrigation suitability between groundwater and Yellow River water, we suggest that SAR and SC indices of the Yellow River water are better, while the PI and RSC indices of groundwater are better. The assessment result, using the irrigation water quality standard, shows that the Yellow River water is suitable for irrigation. This study gives data support for the irrigation water source selection, and provides a scientific basis for the future treatment and prevention of groundwater in the Hetao irrigation district in Inner Mongolia.

Key words: Hetao irrigation district, irrigation suitability, groundwater, Yellow River, hydrochemical characterization

CLC Number: