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祁连山老虎沟12号冰川积雪中飞灰颗粒物的特征
引用本文:董志文,秦大河,秦翔,杜志恒,陈记祖,任贾文.祁连山老虎沟12号冰川积雪中飞灰颗粒物的特征[J].环境科学,2014,35(2):504-512.
作者姓名:董志文  秦大河  秦翔  杜志恒  陈记祖  任贾文
作者单位:中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 祁连山冰川与生态环境综合观测研究站, 兰州 730000;兰州大学西部环境教育部重点实验室, 兰州 730000;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 祁连山冰川与生态环境综合观测研究站, 兰州 730000;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 祁连山冰川与生态环境综合观测研究站, 兰州 730000;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 祁连山冰川与生态环境综合观测研究站, 兰州 730000;中国科学院大学, 北京 100049;兰州大学西部环境教育部重点实验室, 兰州 730000;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室, 祁连山冰川与生态环境综合观测研究站, 兰州 730000
基金项目:国家自然科学基金项目(41301065);中国博士后科学基金项目(2013T60898);兰州大学西部环境教育部重点实验室开放基金、中国沙漠气象科学研究基金项目(Sqj2012001);冰冻圈科学国家重点实验室开放基金项目(SKLCS2012-04)
摘    要:冰川积雪中的飞灰颗粒物可指示由大气沉降的人类活动污染物.本研究基于2012年6月在青藏高原东北缘的祁连山老虎沟12号冰川夏季野外观测取样、实验室扫描电子显微镜与X射线能谱仪联用系统(SEM-EDX)分析了积雪粉尘中球形颗粒物的特征信息,以弄清冰川区沉降的球形飞灰颗粒物的理化特征及其环境意义.结果表明,在所选取的雪层不同深度的9个积雪样品中,都存在着一定数量的飞灰颗粒,这些颗粒物通常是人类生产活动中的化石燃料高温燃烧所形成的.基于EDX能谱分析了飞灰颗粒物的化学元素成分组成,认为沉积在祁连山冰川积雪中的飞灰主要分为3种类型,分别为"富Si类"、"富Fe类"和"富Ti类"颗粒物.总体上,"富Si类"和"富Fe类"颗粒占了球形飞灰颗粒的绝大部分.这些不同组分的飞灰代表了污染物的不同生产活动来源,其平均粒径要相对大于雪层中自然来源的所有矿物粉尘颗粒物,反映了大气传输远距离中密度对粉尘颗粒的重要性.结合NOAA Hysplit气团后向传输轨迹分析认为,中亚地区和我国新疆地区城市、及研究区周边的工业燃烧物通过大气传输是祁连山老虎沟12号冰川积雪中飞灰颗粒的主要可能来源.

关 键 词:祁连山12号冰川  飞灰颗粒物  粉尘  扫描电镜  微观分析
收稿时间:6/9/2013 12:00:00 AM
修稿时间:2013/7/12 0:00:00

Characteristics of Fly Ash Particles Deposition in the Snowpack of Laohugou Glacier No.12 in Western Qilian Mountains, China
DONG Zhi-wen,QIN Da-he,QIN Xiang,DU Zhi-heng,CHEN Ji-zu and REN Jia-wen.Characteristics of Fly Ash Particles Deposition in the Snowpack of Laohugou Glacier No.12 in Western Qilian Mountains, China[J].Chinese Journal of Environmental Science,2014,35(2):504-512.
Authors:DONG Zhi-wen  QIN Da-he  QIN Xiang  DU Zhi-heng  CHEN Ji-zu and REN Jia-wen
Affiliation:State Key Laboratory of Cryospheric Sciences, Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;Key Laboratory of West China's Environmental System, Ministry of Education, Lanzhou University, Lanzhou 730000, China;State Key Laboratory of Cryospheric Sciences, Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;State Key Laboratory of Cryospheric Sciences, Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;State Key Laboratory of Cryospheric Sciences, Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;University of Chinese Academy of Sciences, Beijing 100049, China;Key Laboratory of West China's Environmental System, Ministry of Education, Lanzhou University, Lanzhou 730000, China;State Key Laboratory of Cryospheric Sciences, Qilian Shan Station of Glaciology and Ecologic Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Abstract:This research aimed to identify and characterize individual spherical fly ash particles extracted from surface snow at Laohugou Glacier No.12, western Qilian Mountains, China. Characterization of the spherical particles (i.e. morphology, chemical composition and genesis) was obtained by scanning electron microscopy coupled with energy dispersive X-ray spectrometer (SEM-EDX). Spherical particles and agglomerates were identified according to their morphology in nine snow samples. Prevalent particle types in all samples were granular spherical particles, hollow spherical particles, and agglomerates. The vast majority of spherical particles in our samples had mostly smooth and glossy surfaces. Individual particle analyses of elemental composition showed that particles formed in combustion were mainly composed of silicon, aluminum and trace elements. On the basis of chemical information obtained from EDX, the fly ash particles deposited in the snow could be classified into three types, which were Si-dominant particles, Fe-dominant particles, and Ti-dominant spherical particles. Backward air mass trajectory and dispersion analysis suggested that the developed urban regions of central Asia and surrounding Yumen city contributed the primary fly ash particles from industrial combustion to the study site through the high-level atmospheric circulation.
Keywords:Glacier No  12  fly ash  dust  SEM-EDX  morphology
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