祁连山东端地表及地下水水化学时空变化特征

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Abstract

Surface water and undergroundwater were collected from the eastern part of Qilian Mountains (Wushaoling, Gulang, Tianzhu) from May to September, 2016~2017. Water chemical analysis, statistical analysis, Piper three-line diagram, Gibbs diagram and ion ratio were used to explore the main ion composition, source and temporal & spatial variation of surface water and undergroundwater in the area. The result shows that the main cations of theeastern part of the surface water and undergroundwater in Qilian Mountainsare Ca²⁺ and Na⁺. The average concentration of Ca²⁺ is 76.897mg/L, accounting for 73.89%.AndNa⁺ is 16.592mg/L, accounting for 15.94%. The dominant anions are HCO₃^- and SO₄^2-. The concentration of HCO₃^- is 190.117mg/L, accounting for 68.71%. SO₄^2- is 67.565mg/L, accounting for 24.42%. The water hydrochemistry type is HCO₃^--Ca²⁺ concerning Wushaoling River water, Wushaoling undergroundwater, Tianzhu riverand Tianzhuunderground water.In the light of Gulangriver water and its underground water, the type is HCO₃^--Ca²⁺-Mg²⁺. Ions ofdifferent waters are from rock weathering, meanwhile affected by carbonate and silicate weathering and dissolution combined, and human activity is alsocontributed. The time-varying characteristics of the main ions concentration in different water bodies are different.In general, the ions concentration of most water bodies does not change significantly with time, and the overall trend is relatively flat.

Key words： water chemistry ion source temporal-spatial variation the eastern part of Qilian Mountains

Received: 09 September 2019

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X523

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	Articles by authors
	CAO Yan-feng
	ZHANG Ming-jun
	QU De-ye
	WANG Sheng-jie
	QIU Xue
	MA Zhuan-zhuan
	DU Qin-qin
	CHE Cun-wei

Cite this article:

CAO Yan-feng,ZHANG Ming-jun,QU De-ye等. Temporal-spatial variation of surface and undergroundwater chemistry in the eastern part of Qilian Mountains[J]. CHINA ENVIRONMENTAL SCIENCECE, 2020, 40(4): 1667-1676.

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http://www.zghjkx.com.cn/EN/ OR http://www.zghjkx.com.cn/EN/Y2020/V40/I4/1667

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