六盘水矿区关键带岩溶水水化学演化特征及驱动因子

叶慧君; 张瑞雪; 吴攀; 韩志伟; 查学芳; 李学先; 覃应机; 石金芳

doi:10.3799/dqkx.2019.201

Volume 44 Issue 9

Sep. 2019

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Article Navigation > Earth Science > 2019 > 44(9): 2887-2898

Ye Huijun, Zhang Ruixue, Wu Pan, Han Zhiwei, Zha Xuefang, Li Xuexian, Qin Yingji, Shi Jinfang, 2019. Characteristics and Driving Factor of Hydrochemical Evolution in Karst Water in the Critical Zone of Liupanshui Mining Area. Earth Science, 44(9): 2887-2898. doi: 10.3799/dqkx.2019.201

Citation:

Ye Huijun, Zhang Ruixue, Wu Pan, Han Zhiwei, Zha Xuefang, Li Xuexian, Qin Yingji, Shi Jinfang, 2019. Characteristics and Driving Factor of Hydrochemical Evolution in Karst Water in the Critical Zone of Liupanshui Mining Area. Earth Science, 44(9): 2887-2898. doi: 10.3799/dqkx.2019.201

Citation:

Ye Huijun, Zhang Ruixue, Wu Pan, Han Zhiwei, Zha Xuefang, Li Xuexian, Qin Yingji, Shi Jinfang, 2019. Characteristics and Driving Factor of Hydrochemical Evolution in Karst Water in the Critical Zone of Liupanshui Mining Area. Earth Science, 44(9): 2887-2898. doi: 10.3799/dqkx.2019.201

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Characteristics and Driving Factor of Hydrochemical Evolution in Karst Water in the Critical Zone of Liupanshui Mining Area

doi: 10.3799/dqkx.2019.201

1.
School of Environmental Science and Engineering, Sun Yat-Sen University, Guangzhou 510006, China
2.
College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025, China
3.
Key Laboratory of Karst Environment and Geohazard, Ministry of Land and Resources, Guiyang 550025, China

Received Date: 2019-06-27
Publish Date: 2019-09-15

Abstract

Abstract

The surface water and groundwater which are critical resources for daily life, industrial and agricultural production exchange frequently in Liupanshui mining area.To ensure the security and sustainability of water system in the karst critical zone, thirty-three water samples were collected from the typical Liupanshui mining area in September 2015. They were analyzed by using the methods of hydrochemistry, correlation analysis and ion ratios. The results show most groundwater hydrochemical type was CaHCO₃ type, and some was Ca-SO₄ type. Most surface water was Ca-HCO₃ type and Ca-SO₄ type. Differently, the mine waste water was Na-HCO₃ type and the acid mine waste water was Ca-SO₄ type. There was a significant positive correlation between Ca²⁺, Mg²⁺ and HCO₃^- which was mainly controlled by reaction between water and carbonate, and some Na⁺ and K⁺ were controlled by reaction between water and silicate. The sources of Cl^- were mainly sewage, most of NO₃^- were affected by agricultural production, and SO₄^2- came from multiple sources. Mining activities, urbanization and agricultural production have affected the compositions of water ions, in addition mining activities have accelerated the dissolution of carbonate. These three factors have made significant changes in the hydrochemistry types. Under these compound influences affected by human activities, mining activities are the key driving factors for the changes of hydrochemical characteristics in water system of the karst critical zone.
- karst mining area,
- compound influence,
- hydrochemical evolution,
- driving factor,
- hydrogeology

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References(38)

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Characteristics and Driving Factor of Hydrochemical Evolution in Karst Water in the Critical Zone of Liupanshui Mining Area

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