Cong Zhiyuan, Kang Shichang, Qin Dahe
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China.
J Environ Sci (China). 2009;21(7):914-9. doi: 10.1016/s1001-0742(08)62361-x.
To assess the seasonality of aerosol deposition and anthropogenic effects on central Himalayas, a 1.85-m deep snow pit was dug on the northern slope of Mt. Qomolangma (Everest). Based on the morphology and energy dispersive X-ray (EDX) signal, totally 1500 particles were classed into 7 groups: soot; aluminosilicates; fly ash; calcium sulfates; Ca/Mg carbonates; metal oxides; and biological particles and carbon fragments. The size distribution and number fractions of different particle groups exhibited distinct seasonal variations between non-monsoon and monsoon periods, which are clearly related to the differences in air mass pathways. Specifically, the relative abundance of soot in non-monsoon period (25%) was much higher than that in monsoon period (14%), indicating Mt. Qomolangma region received more anthropogenic influence in non-monsoon than monsoon period.
为评估喜马拉雅山脉中部气溶胶沉降的季节性以及人为影响,在珠穆朗玛峰(珠峰)北坡挖掘了一个1.85米深的雪坑。基于形态学和能量色散X射线(EDX)信号,共1500个颗粒被分为7组: soot;铝硅酸盐;飞灰;硫酸钙;钙/镁碳酸盐;金属氧化物;以及生物颗粒和碳碎片。不同颗粒组的粒径分布和数量分数在非季风期和季风期之间呈现出明显的季节性变化,这与气团路径的差异密切相关。具体而言,非季风期soot的相对丰度(25%)远高于季风期(14%),表明珠穆朗玛峰地区在非季风期比季风期受到更多的人为影响。