Yue Xiao-Ying, Li Zhong-Qin, Zhang Ming-Jun, Zhou Ping, Fan Jin
College of Geography and Environment Sciences, Northwest Normal University, Lanzhou 730070, China.
State Key Laboratory of Cryospheric Sciences/Tianshan Glaciological Station, Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou, China.
Huan Jing Ke Xue. 2013 Oct;34(10):3764-71.
Major soluble ions were measured in 26 aerosol samples collected at Glacier NO. 1 at the headwater of Urumqi River in Tianshan Mountains in April, August and October 2007. The concentration, seasonal change and source of aerosol were analyzed. The results showed that the mean concentration of total soluble major ions of aerosol was 2.76 microg.m-3, Ca2+, NO-(3) and SO2-(4) were the major soluble inorganic ion components. In spring, summer and autumn, the seasonal change of the mean concentration of total soluble inorganic ions was consistent with Ca2+ , SO2-(4) , NH+(4), Na+ , Mg2+ and Cl- , the highest concentration was in summer, followed by autumn and spring. While the maximum concentration of K and NO-(3) was observed in autumn, the minimum was in spring. Soluble inorganic ion source characteristics were that: Ca2+ , Na+, Mg2+ , K+ and Cl- were mostly the land source; NO-(3) and NH: were mainly from the anthropogenic source. SO2-(4) was mainly originated from both crustal surface and anthropogenic sources.
2007年4月、8月和10月,在天山乌鲁木齐河源1号冰川采集了26个气溶胶样品,测定了其中的主要可溶性离子。分析了气溶胶的浓度、季节变化和来源。结果表明,气溶胶中总可溶性主要离子的平均浓度为2.76μg·m-3,Ca2+、NO3-和SO42-是主要的可溶性无机离子成分。春、夏、秋三季,总可溶性无机离子平均浓度的季节变化与Ca2+、SO42-、NH4+、Na+、Mg2+和Cl-一致,最高浓度出现在夏季,其次是秋季和春季。而K和NO3-的最高浓度出现在秋季,最低浓度出现在春季。可溶性无机离子源特征为:Ca2+、Na+、Mg2+、K+和Cl-大多为陆源;NO3-和NH4+主要来自人为源。SO42-主要源于地壳表面和人为源。