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《Journal of Glaciology and Geocryology》 1983-02
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HYDROCHEMICAL FEATURES OF THE GLACIER N0.1 IN THE SOURCE REGION OF RMQI RIVER,TIANSHAN

Luo Hongzhen ( Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica )  
This paper deals with the hydrochemical features of the Glacier No.1 and the composite characteristics of the negative or positive ions in different waters and the water ion of low mineralization, analyzes the relations between ice crystal texture and the total content of ion from lower to higher in the evolution from snow,firn to ice,and discusses the relations between the content of trace element and climate as well as the source of aqueous vapour supplement in glaciated area. By studies on the relations between the contents of potassium,sodium,calcium,magnesium,manganese, iron and aluminium and their concentration coeffecient, it is supposed that the Glacier No,l is a glaciated area of extremely continental type influenced mainly by continental climate.As a result,the influence of the environment around the glacier to the chemical compounds in glacia 1 water and the vapour supplement is unnegligible.
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【References】
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1 ZHOU Cheng hu 1, LUO Ge ping 1, Li Ce 1, TANG Qi cheng 1, LI Hui guo 1, WANG Qin min 2, H. Fuikui 3 (1 State Key Laboratory of Resolrce and Environment Information System, Institute of Geographic Sciences and Natural Resources Reseach, C;Environmental change in Bosten Lake and its relation with the oasis reclamation in Yanqi Basin[J];Geographical Research;2001-01
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1 XIN Yu1, CHEN Hongwu1, LI Yuanpeng1, ZHANG Xin2, LU Ge2 1 Xinjiang Climate Center, Urumqi,Xinjiang China; 830002 2 Meteorological Bureau of Bortala Mongolia Autonomous Prefecture, Bole, Xinjiang 833400;The Analysis on Spatial-Temporal Change Characteristics and Multi-scale Abrupt Change of the Scorching Weather over North Xinjiang[A];[C];2007
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