河套灌区西部浅层地下水咸化机制

曾邯斌; 苏春利; 谢先军; 潘洪捷; 纪倩楠; 陶彦臻

doi:10.3799/dqkx.2020.259

Volume 46 Issue 6

Jun. 2021

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Article Navigation > Earth Science > 2021 > 46(6): 2267-2277

Zeng Hanbin, Su Chunli, Xie Xianjun, Pan Hongjie, Ji Qiannan, Tao Yanzhen, 2021. Mechanism of Salinization of Shallow Groundwater in Western Hetao Irrigation Area. Earth Science, 46(6): 2267-2277. doi: 10.3799/dqkx.2020.259

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Zeng Hanbin, Su Chunli, Xie Xianjun, Pan Hongjie, Ji Qiannan, Tao Yanzhen, 2021. Mechanism of Salinization of Shallow Groundwater in Western Hetao Irrigation Area. Earth Science, 46(6): 2267-2277. doi: 10.3799/dqkx.2020.259

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Mechanism of Salinization of Shallow Groundwater in Western Hetao Irrigation Area

doi: 10.3799/dqkx.2020.259

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
2.
Geological Survey Institute of Inner Mongolia Autonomous Region, Hohhot 011020, China

Received Date: 2020-07-09
Publish Date: 2021-06-15

Abstract

Abstract

High salinity and shallow level of shallow groundwater are the important causes of soil secondary salinization in Hetao irrigation area. In this paper, it takes the western part of Hetao irrigation area as the research area. The hydrochemical analysis, isotopic characteristics of hydrogen and oxygen and hydrogeochemical modeling were investigated to identify the recharge sources of shallow groundwater and the main water-rock interaction processes, and estimate quantitatively the effect of evaporation on shallow groundwater. The results show that shallow groundwater was weak alkaline salt water, the pH and total dissolved solids (total dissolved solids, TDS) are 7.23-8.45 and 371-7 599 mg/L respectively in the research area. With the accumulation of salt, the hydrochemical type of shallow groundwater changed from HCO₃-Na·Mg·Ca to Cl-Na. The main recharge resources of shallow groundwater are the irrigation by using Yellow River water and precipitation. The shallow groundwater was affected by evaporation and transpiration during the runoff process. The hydrochemical compositions of shallow groundwater mainly came from the dissolution of halite and silicate weathering, and experienced intense evaporation and the cation exchange. The results of hydrogeochemical modeling and principal component analysis show that evaporation and halite dissolution contributed the most part to the salinity of shallow groundwater; Na-Ca exchange, topography variations and dissolution of gypsum, dolomite and other minerals also contributed to the salinity of groundwater.
- hydrochemistry,
- isotope,
- principal component analysis,
- interaction of water-rock,
- hydrogeochemical modeling

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References(42)

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Mechanism of Salinization of Shallow Groundwater in Western Hetao Irrigation Area

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