新疆天山北麓中段孔隙水水化学特征及苏打水的成因

雷米; 周金龙; 梁杏; 周殷竹; 曾妍妍; 孙英

doi:10.3799/dqkx.2021.027

Volume 47 Issue 2

Feb. 2022

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Lei Mi, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Sun Ying, 2022. Hydrochemical Characteristics of Pore Water and Genesis of Soda Water in the Middle of the Northern Piedmont of Tianshan Mountain, Xinjiang. Earth Science, 47(2): 674-688. doi: 10.3799/dqkx.2021.027

Citation:

Lei Mi, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Sun Ying, 2022. Hydrochemical Characteristics of Pore Water and Genesis of Soda Water in the Middle of the Northern Piedmont of Tianshan Mountain, Xinjiang. Earth Science, 47(2): 674-688. doi: 10.3799/dqkx.2021.027

Citation:

Lei Mi, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Sun Ying, 2022. Hydrochemical Characteristics of Pore Water and Genesis of Soda Water in the Middle of the Northern Piedmont of Tianshan Mountain, Xinjiang. Earth Science, 47(2): 674-688. doi: 10.3799/dqkx.2021.027

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Hydrochemical Characteristics of Pore Water and Genesis of Soda Water in the Middle of the Northern Piedmont of Tianshan Mountain, Xinjiang

doi: 10.3799/dqkx.2021.027

Lei Mi^{1, 2
,
,},
Zhou Jinlong^{1, 2
,
,
,},
Liang Xing³,
Zhou Yinzhu⁴,
Zeng Yanyan^{1, 2},
Sun Ying^{1, 2}

1.
College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China
2.
Xinjiang Hydrology and Water Resources Engineering Research Center, Urumqi 830052, China
3.
School of Environment Studies, China University of Geosciences, Wuhan 430074, China
4.
Center for Hydrogeology and Environmental Geology, CGS, Baoding 071051, China

Received Date: 2021-07-03
Publish Date: 2022-02-25

Abstract

Abstract

The middle of the northern piedmont of Tianshan Mountain has complicated geological structure and developed faults. It is of great significance to ascertain the formation mechanism of soda water (NaHCO₃ type) for understanding the relationship between groundwater hydrogeochemical process and geological conditions in the middle of the northern piedmont of Tianshan Mountain. Based on 209 groups of groundwater samples in the middle plain of the northern piedmont of Tianshan Mountain, Xinjiang, combined with geological conditions, semi-variation model, multiple linear regression of absolute principal component score model (PCA/APCS-MLR) were used to identify the spatial distribution characteristics of hydrochemical types in unconfined water and confined water, source contribution of groundwater chemical components, and the hydrogeochemical process of soda water formation and the controlling factors of geological conditions. The results showed that Na₂SO₄, NaHCO₃ and Na₂SO₄ are the main types of unconfined groundwater in piedmont inclined plain, unconfined groundwater and confined groundwater in alluvial plain, respectively, the soda water in piedmont clinoplainun confined water, alluvial plain unconfined water and confined water accounted for 7.18%, 14.83% and 6.22% of the total water samples respectively. The spatial autocorrelation of Na⁺, HCO₃^- and TDS is strong in confined groundwater, but weak in unconfined groundwater, when TDS is less than 1 000 mg/L, NaHCO₃ type water will be formed. The contribution rates of dissolution-enrichment factor (F1), external input factor (F2), native geological factor (F3) and geological environment factor (F4) to groundwater chemical components were 29.44%, 15.99%, 7.70% and 6.71% respectively. The formation process of soda water is not only controlled by various hydrogeochemical processes such as mineral dissolution, cation exchange, mixing and desulphidation, but also affected by geological conditions such as geological environment, geological structure, hydrogeological conditions.
- pore water,
- soda water,
- hydrochemical characteristics,
- geological conditions,
- the middle of the northern piedmont of Tianshan Mountain,
- hydrogeology

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Hydrochemical Characteristics of Pore Water and Genesis of Soda Water in the Middle of the Northern Piedmont of Tianshan Mountain, Xinjiang

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