江汉平原东部地区浅层地下水水化学特征

於昊天; 马腾; 邓娅敏; 杜尧; 沈帅; 鲁宗杰

doi:10.3799/dqkx.2017.056

Volume 42 Issue 5

May 2017

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Article Navigation > Earth Science > 2017 > 42(5): 685-692

Yu Haotian, Ma Teng, Deng Yamin, Du Yao, Shen Shuai, Lu Zongjie, 2017. Hydrochemical Characteristics of Shallow Groundwater in Eastern Jianghan Plain. Earth Science, 42(5): 685-692. doi: 10.3799/dqkx.2017.056

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Yu Haotian, Ma Teng, Deng Yamin, Du Yao, Shen Shuai, Lu Zongjie, 2017. Hydrochemical Characteristics of Shallow Groundwater in Eastern Jianghan Plain. Earth Science, 42(5): 685-692. doi: 10.3799/dqkx.2017.056

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Hydrochemical Characteristics of Shallow Groundwater in Eastern Jianghan Plain

doi: 10.3799/dqkx.2017.056

Yu Haotian^{1,2
,},
Ma Teng^{1,2
,
,},
Deng Yamin³,
Du Yao^1,2,
Shen Shuai^1,2,
Lu Zongjie³

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
3.
Geological Survey, China University of Geosciences, Wuhan 430074, China

Received Date: 2017-01-15
Publish Date: 2017-05-15

Abstract

Abstract

The shallow groundwater is an important water supply source in the eastern Jianghan plain, but it is confronted with pollution and inferior quality of natural water. This study identifies the chemical characteristics, control processes and influencing factors of shallow groundwater in the study area based on the results of water chemistry, hydrogen and oxygen isotope, using methods of mathematical statistics and factor analysis. Results show that the shallow groundwater chemical types are mainly HCO₃-Ca, the contents of Ca²⁺ and Mg²⁺ in the phreatic water are close to those in confined water, the contents of the As, Fe, NH₄⁺ are lower than those in confined water, but the contents of the Cl^-, SO₄^2-, Mn and NO₃^- are higher than those in confined water. The shallow groundwater mainly originates from precipitation and the phreatic water has experienced a degree of evaporation and the mixture of surface water. Among the influencing factors of shallow groundwater chemical characteristics, the geologic origin may play a leading role; human activities have dramatically changed the chemical characteristics of the phreatic water, and the shallow confined water is mainly affected by water-rock interaction of the runoff process.
- eastern Jianghan plain,
- shallow groundwater,
- hydrochemistry,
- factor analysis,
- ion ratio method,
- hydrogeology

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References(26)

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