巴丹吉林沙漠湖泊水化学类型与钙华沉积关系

曹乐; 聂振龙; 申建梅; 王哲; 刘学全

doi:10.3799/dqkx.2021.172

Volume 48 Issue 10

Oct. 2023

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Cao Le, Nie Zhenlong, Shen Jianmei, Wang Zhe, Liu Xuequan, 2023. Relationship between Lakes' Hydrochemical Types and Tufa Deposition in Badain Jaran Desert. Earth Science, 48(10): 3844-3855. doi: 10.3799/dqkx.2021.172

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Cao Le, Nie Zhenlong, Shen Jianmei, Wang Zhe, Liu Xuequan, 2023. Relationship between Lakes' Hydrochemical Types and Tufa Deposition in Badain Jaran Desert. Earth Science, 48(10): 3844-3855. doi: 10.3799/dqkx.2021.172

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Relationship between Lakes' Hydrochemical Types and Tufa Deposition in Badain Jaran Desert

doi: 10.3799/dqkx.2021.172

Cao Le^{1, 2, 3
,
,},
Nie Zhenlong¹,
Shen Jianmei¹,
Wang Zhe¹,
Liu Xuequan¹

1.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China
2.
China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Groundwater Sciences and Engineering, Ministry of Natural Resources, Shijiazhuang 050061, China

Received Date: 2021-07-08
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

In order to find out the relationship between lake types and tufa deposition in Badain Jaran desert and explore the tufa deposition and water cycle process, in this paper it studies the relationship between ion composition, hydrochemical types and mineral saturation index (SI) of lake water and groundwater. The results show that the distribution of tufa lake accounts for about 1/5 of the total number of lakes, and these lakes have no obvious regularity in spatial distribution. There are 18 types of lake water chemistry, including Cl-Na type, Cl-CO₃-Na type and Cl-SO₄-Na type, and the distribution of lakes with tufa does not show the particularity of the type. The analysis of the tufa dating and paleoclimate records proves that tufa was a kind of chemical deposition under the Late Holocene arid climate background, which was caused by the evaporation and concentration of the lake water, and at the same time continuously receiving groundwater recharge and mixing with the lake water. The difference of chemical composition of groundwater leads to the difference of scale and location of tufa deposition in different lakes. The groundwater with lower SI of calcite and dolomite is more favorable to the mixed deposition of tufa with lake water, which type of groundwater is mainly derived from the weathering and dissolution of evaporite.
- salt lake,
- hydrochemical type of lake,
- groundwater,
- tufa,
- Badain Jaran Desert,
- hydrogeology

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References(51)

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Relationship between Lakes' Hydrochemical Types and Tufa Deposition in Badain Jaran Desert

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