Temporal and Spatial Distributions and Controlling Factors of Hydrochemistry at Wuyishan National Park Water Body

YE Hongmeng; GAN Juan; LI Guoping; HU Jiapeng; SU Liman; WU Jinping; WANG Shengyan

doi:10.19303/j.issn.1008-0384.2022.010.016

Volume 37 Issue 10

Oct. 2022

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Article Navigation > Fujian Journal of Agricultural Sciences > 2022 > 37(10): 1362-1370

YE H M, GAN J, LI G P, et al. Temporal and Spatial Distributions and Controlling Factors of Hydrochemistry at Wuyishan National Park Water Body [J]. Fujian Journal of Agricultural Sciences，2022，37（10）：1362−1370 doi: 10.19303/j.issn.1008-0384.2022.010.016

Citation:

YE H M, GAN J, LI G P, et al. Temporal and Spatial Distributions and Controlling Factors of Hydrochemistry at Wuyishan National Park Water Body [J]. Fujian Journal of Agricultural Sciences，2022，37（10）：1362−1370 doi: 10.19303/j.issn.1008-0384.2022.010.016

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Temporal and Spatial Distributions and Controlling Factors of Hydrochemistry at Wuyishan National Park Water Body

doi: 10.19303/j.issn.1008-0384.2022.010.016

1.
Fujian Provincial Key Laboratory of Eco-Industrial Green Technology, College of Ecology and Resources Engineering, Wuyi University, Wuyishan, Fujian　354300, China
2.
Library of Wuyi University, Wuyi University, Wuyishan, Fujian　354300, China
3.
Taizhou Hydrology and Water Resources Investigation Bureau of Jiangsu Province, Taizhou, Jiangsu　225300, China

Received Date: 2021-10-31
Rev Recd Date: 2022-06-13

Available Online: 2022-10-21

Publish Date: 2022-10-30

Abstract

Abstract

Objective Contents of major anions and cations in the Jiuquxi River at the Wuyishan National Park were analyzed to unveil the spatial and temporal distributions, action mechanism, and lithological control of the surface water. Method Thirty water samples from different river sections were collected at different hydrological periods for chemical determination. Gibbs, triangle, and endmember diagrams were applied to analyze the hydrochemical mechanism and lithological control. Principal component analysis and model calculation were applied to quantify the hydrochemical contributions. Result The river water was weakly acidic with an average total dissolved solids (TDS) of 25.30 mg·L⁻¹, which was well below the world average of 100.00 mg·L⁻¹. The contents of major cations in the water ranked in the order of Ca²⁺＞Na⁺＞K⁺＞Mg²⁺, while that of anions HCO₃⁻＞Cl⁻＞NO₃⁻＞SO₄²⁻. In different hydrological periods, TDS and most of the ions were dry period＞normal period＞wet period and increased from upstream to downstream of the river. Conclusion The hydrochemistry of Jiuquxi water in the national park was HCO3⁻-Ca²⁺+Na⁺ type and, basically, of a rock weathering action mechanism that affected by precipitation, and to a certain extent, human activities. The rock weathering altered the hydrochemistry more on the upper reach than the middle or lower reach of the river. Precipitation affected the hydrochemistry most greatly in wet season. The lithological control on the area waters was largely weathering of carbonate and silicate rocks that contributed 58.82% of the controlling factors of the hydrochemistry.
- Hydrochemical characteristics,
- spatial and temporal distributions,
- rock weathering,
- Wuyishan National Park,
- Jiuquxi

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References(36)

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