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    Volume 36 Issue 4
    Jul.  2011
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    LI Zhong-qin, DONG Zhi-wen, ZHANG Ming-jun, WANG Fei-teng, 2011. Chemical Characteristics and Seasonal Variation of Snow on Urumqi Glacier No.1 of the Eastern Tianshan, China. Earth Science, 36(4): 370-678. doi: 10.3799/dqkx.2011.068
    Citation: LI Zhong-qin, DONG Zhi-wen, ZHANG Ming-jun, WANG Fei-teng, 2011. Chemical Characteristics and Seasonal Variation of Snow on Urumqi Glacier No.1 of the Eastern Tianshan, China. Earth Science, 36(4): 370-678. doi: 10.3799/dqkx.2011.068

    Chemical Characteristics and Seasonal Variation of Snow on Urumqi Glacier No.1 of the Eastern Tianshan, China

    doi: 10.3799/dqkx.2011.068
    • Received Date: 2010-09-20
    • Publish Date: 2011-07-01
    • Alpine glacier and snow can record signals of surface earth. From September 2002 to October 2005, Surface snow samples were collected on Urumqi glacier No.1 and chemical characteristics and seasonal variations of major ions, dust, and metal were measured. Results show that the concentration of major ions is Ca2+ > SO42- > NO3- > Cl- > NH4+ > Mg2+ > Na+ > K+, Ca2+ is the dominant cation, SO42- is the dominant anion. All ions have good correlation except NO3-. δ18O shows minus correlation with air temperature change. Dust and major ionic concentrations in the snow show obvious seasonal change trend, with higher concentrations in spring but lower ones in summer, which indicates the chemical input of dust activities to snow. Temporal changes of heavy metal (Cd, Pb, Zn, Al, Fe) indicate that human activities also have effect on the snow chemistry.

       

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