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《Journal of Glaciology and Geocryology》 2006-02
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Hydrological and Hydrochemical Features of Kartamak Glacier Area in Muztag Ata

ZHAO Hua-biao~1, YAO Tan-dong~2,1, XU Bai-qing~2,1(1.Key Laboratory of Cryosphere and Environment,CAREERI,CAS,Lanzhou Gansu 730000,China;2.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China)  
Based on the measured hydrological data from 1 June to 25 August 2003,the variation characteristics of meltwater runoff draining from Kartamak Glacier in the Muztag Ata are discussed.The meltwater runoff is dependent mainly on ambient temperature and precipitation.Runoff and precipitation samples were collected from 10 to 23 August 2003.Their pH,EC(electric conductivity) were determined.Besides,the major ions(Na~+,K~+,Ca~2+,Mg~2+,Cl~-,NO~-\3,SO~2-_4) of runoff samples also determined.pH values show a positive correlation with EC for all samples.Runoff samples are slightly alkaline.Sulfate and calcium are the dominant anion and cation in the measured ions.The major ion concentrations have the similar variations in the samples collected whether on a single day or during the whole sampling period,except for NO~-_3,and have an inverse fluctuation with runoff or water level,because of dilution.In order to discuss the classification and origin of each dissolved chemical substance in the glacial meltwater,a principal component analysis is carried out.The results show that the fluctuations of Ca~2+ and SO~2-_4 are most similar in all measured cations and anions,and that water-rock interaction determines the ion components of the meltwater.
【Fund】: 中国科学院知识创新工程项目(KZCX3-SW-339);; 国家自然科学基金创新群体项目(40121101);; 国家重点基础研究规划项目(2005CB422004)资助
【CateGory Index】: P334.7
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