新疆昌吉州东部平原区地下水水文地球化学演化分析

Abstract

Abstract:

In this paper, the test data of 63 groundwater samples in 2016 and 54 water quality monitoring data from 2012 to 2015 in the eastern plains in Changji Hui Autonomous Prefecture, Xinjiang were analyzed by the mathematical statistics, Piper diagrams, Gibbs figures, ion ratios, etc. The purposes of this study was to explore the evolution process of groundwater in the study area. The results showed that the average cationic concentrations of groundwater in the study area in 2012 were in an order of Ca²⁺> K⁺+Na⁺> Mg²⁺, and the average anionic concentrations were in an order of HCO₃^-> SO₄^2-> Cl^-. After 2013, the concentration of SO₄^2- was gradually increased but that of Ca²⁺ was gradually decreased. By 2016, the average cationic concentrations of groundwater were in an order of Ca²⁺> K⁺+Na⁺> Mg²⁺, and the average anionic concentrations were in an order of HCO₃^-> SO₄^2-> Cl^-. The hydrochemical type evolved from HCO₃—Ca·Mg (Ca·Na, Ca·Na·Mg) in 2012 to HCO₃·SO₄—Ca·Na·Mg (Ca·Mg, Ca·Na) in 2016, which was mainly related to the evaporation and rock weathering of aquifer medium, and the evaporation was reflected more in unconfined groundwater. Na⁺, K⁺and Cl^-in groundwater came mainly from the dissolution of rock salt; SO₄^2-came mainly from the dissolution of gypsum (CaSO₄·2H₂O) and mirabilite (Na₂SO₄·10H₂O). In addition to the dissolution of rock salt, Cl^- and SO₄^2-are also affected by human activities.

Key words: plain, groundwater; hydrogeochemistry, evolution, Changji, Xinjiang

LEI Mi, ZHOU Jin-long, WU Bin, FAN Wei, ZHANG Jie. Hydrogeochemical Evolution Process of Groundwater in the Eastern Plains in Changji Hui Autonomous Prefecture,Xinjiang[J].Arid Zone Research, 2020, 37(1): 105-115.

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Hydrogeochemical Evolution Process of Groundwater in the Eastern Plains in Changji Hui Autonomous Prefecture,Xinjiang

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