Chemical characteristics and genesis analysis of groundwater in northwest Yili River Valley
Received date: 2020-04-13
Revised date: 2020-11-13
Online published: 2021-04-25
:To analyze groundwater genesis and chemical characteristics in Yili River Valley, Xinjiang China, we used descriptive statistical analysis, trilinear chart by Piper, Gibbs diagrams, ion ratio diagrams, and saturation index methods to systematically analyze 35 groundwater samples collected from June to October 2018. Groundwater in the study area is weakly alkaline, with a high total hardness level. The chemical components in groundwater showed little variation throughout the study area; Ca2+ was the main cation, and HCO3- the main anion. The hydrochemical characteristics in the study area can be divided into five groundwater types, HCO3-Ca, HCO3·SO4-Ca, HCO3·SO4-Ca·Mg, HCO3·SO4-Ca·Na, and HCO3-Ca·Mg. Although rock lixiviation is the main contributor to groundwater chemical composition, evaporation-concentration and cation exchange also contribute to the chemical composition of groundwater in the study area. Moreover, some groundwater samples might be affected by human activities. Na+, Cl-, and SO42- in groundwater are present due to the dissolution of rock salt, gypsum, and other evaporates; the dissolution of minerals such as calcite, dolomite, and gypsum contributes to Ca2+ and Mg2+ in groundwater.
Ailihamu Aikelamu,ZHOU Jinlong,ZHANG Jie,WEI Xing,YU Dong,CHEN Jinsong . Chemical characteristics and genesis analysis of groundwater in northwest Yili River Valley[J]. Arid Zone Research, 2021 , 38(2) : 504 -512 . DOI: 10.13866/j.azr.2021.02.22
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