RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2016, Vol. 25 >> Issue (07): 1121-1128.doi: 10.11870/cjlyzyyhj201607014

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HYDROCHEMICAL CHARACTERISTICS IN THE SANCHAHE RIVER BASIN AND THE POSSIBLE CONTROLS

HOU Yi-liang1,2, AN Yan-ling1,2, WU Qi-xin1,2,3, WU Jing-tao1,2, HUANG Juan2, DUAN Shao-qiong1,2, LIU Xiao1,2   

  1. 1. Key Laboratory of Karst Environment and Geohazard Prevention, Guizhou University, Guiyang 550025, China;
    2. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China;
    3. State Key Laboratory of Environment Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
  • Received:2016-03-17 Revised:2016-05-18 Online:2016-07-20
  • Supported by:
    Postdoctoral Fund(No.2014M552388);Key Laboratory Construction Project of Guizhou Province(Qiankehe SY20133133, Qiankehe Z20124012);The Natural Science Foundation of Guizhou Province(QiankeheJ20132130, Qiankehe J20132298);Guizhou University Graduate Innovation FundProject(Yanligong 2015077)

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Abstract: The analysis of ion concentration and composition characteristics was conducted based on samples from the Sanchahe River Basin, which were collected in dry and wet seasons from the Wujiang source area. The results showed that the dominate anion and cation were HCO3-and Ca2+ in the samples, accounting for 55% and 70% of the total anions and total cations, respectively, suggesting that the ion composition was similar with that of the karst area river basins. The comparison of temporal variations of the concentrations of major ions showed that, the concentrations of Ca2+、Mg2+、Na+、HCO3-、Cl- in dry seasons were slightly higher than they were in wet seasons, while the concentrations of K+、SO4-2、NO3- were almost the same in these two seasons. And the spatial distribution types of the ions were diversified, showing that different small basins have different geological background, ecological environment, and different human activities, all of these could affect the concentration and composition of water ions. The Gibbs diagram indicated that the river water chemistry was mainly influenced by rock weathering. Triangle diagram showed that the river water chemistry was mainly affected by the carbonate rock, and sulfuric acid was widely involved in the rock weathering. Human activities also have some influences on the composition of water chemistry.

Key words: Sanchahe River, water chemistry, ion sources, impact factors

CLC Number: 

  • X36
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