伊犁河谷西北部地下水化学特征及成因分析

doi:10.13866/j.azr.2021.02.22

Abstract

Abstract:

：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 SO₄^2- 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.

Key words: northwest area of Yili River Valley, groundwater, hydrochemical characteristics, Gibbs diagram, ion ratio diagram, Xinjiang

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.

Figures/Tables 8

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References 31

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项目	K⁺	Na⁺	K⁺+Na⁺	Ca²⁺	Mg²⁺	Cl^-	SO₄^2-	HCO₃^-	pH	总硬度	TDS	NO₃^-
最大值	9.01	247.01	251.76	248.89	179.35	267.01	1109.24	523.17	8.10	2920.00	2318.92	26.52
最小值	0.87	3.03	4.10	26.11	6.43	2.82	26.50	60.76	6.90	151.00	111.00	0.84
平均值	2.77	42.43	45.20	79.15	31.32	43.47	154.57	235.32	7.66	604.07	448.73	10.19
中位数	2.35	27.95	31.94	63.78	24.30	35.98	117.77	214.81	7.78	435.00	320.02	3.11
标准差	1.79	45.20	46.14	44.96	30.73	48.83	183.57	103.81	0.37	494.74	387.65	10.42
变异系数	0.65	1.06	1.02	0.57	0.98	1.12	1.19	0.44	0.05	0.82	0.86	1.02

地下水类型	SI值	文石	方解石	白云石	石膏	岩盐	地下水类型	SI值	文石	方解石	白云石	石膏	岩盐
	最大值	0.71	0.86	1.41	-0.51	-5.84		最大值	0.75	0.90	1.74	-1.27	-6.62
	最小值	-0.68	-0.54	-1.28	-2.30	-9.09		最小值	-0.10	0.05	-0.30	-2.25	-9.42
承压水	平均值	0.16	0.31	0.45	-1.57	-7.60	潜水	平均值	0.17	0.32	0.39	-1.71	-7.98
	SI>0占比/%	77.5	82.0	82.0	0.0	0.0		SI>0占比/%	69.6	100.0	62.0	0.0	0.0
	SI<0占比/%	22.5	18.0	18.0	100.0	100.0		SI<0占比/%	30.4	0.0	38.0	100.0	100.0

Chemical characteristics and genesis analysis of groundwater in northwest Yili River Valley

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