典型岩溶小流域水体中硝酸盐分布特征及成因:以普定后寨河流域为例

李耕; 韩志伟; 申春华; 曾祥颖

doi:10.3799/dqkx.2019.170

Volume 44 Issue 9

Sep. 2019

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Li Geng, Han Zhiwei, Shen Chunhua, Zeng Xiangying, 2019. Distribution Characteristics and Causes of Nitrate in Waters of Typical Small Karst Catchment: A Case of the Houzhai River Catchment. Earth Science, 44(9): 2899-2908. doi: 10.3799/dqkx.2019.170

Citation:

Li Geng, Han Zhiwei, Shen Chunhua, Zeng Xiangying, 2019. Distribution Characteristics and Causes of Nitrate in Waters of Typical Small Karst Catchment: A Case of the Houzhai River Catchment. Earth Science, 44(9): 2899-2908. doi: 10.3799/dqkx.2019.170

Citation:

Li Geng, Han Zhiwei, Shen Chunhua, Zeng Xiangying, 2019. Distribution Characteristics and Causes of Nitrate in Waters of Typical Small Karst Catchment: A Case of the Houzhai River Catchment. Earth Science, 44(9): 2899-2908. doi: 10.3799/dqkx.2019.170

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Distribution Characteristics and Causes of Nitrate in Waters of Typical Small Karst Catchment: A Case of the Houzhai River Catchment

doi: 10.3799/dqkx.2019.170

1.
Resource and Environmental Engineering College, Guizhou University, Guiyang 550025, China
2.
Key Laboratory of Karst Environment and Geohazard Prevention, Ministry of Natural Resources, Guiyang 550025, China

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

Abstract

Abstract

The water environment of karst catchment is very susceptible to human activities. Nitrate pollution is a prominent and common problem in karst catchment. It is important to clarify the source, distribution characteristics and formation mechanism of nitrate in waters of karst catchment, which can facilitate the nitrate pollution prevention in karst catchment. The Houzhai River catchment of Puding of Guizhou was selected as the study area. 53 samples of groundwater and surface water were collected for measuring water chemical parameters in May 2017. Water chemical parameters were determined for analyzing the NO₃^- source. Combined with the land use type, the influence of the nitrate spatial distribution was discussed along the flow path. The results show that the order of ion concentration in waters was Ca²⁺ > Mg²⁺ > Na⁺ > K⁺, HCO₃^- > SO₄^2- > NO₃^- > Cl^- in the study area, respectively. The type of water chemistry was HCO₃-Ca. The main source of NO₃^- was the chemical fertilizer. Variations of NO₃^- concentration along the flow path were mainly controlled by the mixing process, and the impact of nitrification and denitrification was not obvious. Waters of 6 sampling sites were obviously polluted by nitrate. The concentration of NO₃^- in waters of the catchment was obviously affected by the land use pattern. NO₃^- concentration increased when waters flowed through farmland or villages, and decreased when they flowed through forest land.
- karst,
- nitrate,
- distribution characteristics,
- formation mechnism,
- land use,
- mixing process,
- hydrogeology

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References(54)

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Distribution Characteristics and Causes of Nitrate in Waters of Typical Small Karst Catchment: A Case of the Houzhai River Catchment

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