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Mineralogical and morphological properties of individual dust particles in ice cores from the Tibetan Plateau
Wu, GJ (Wu, Guangjian)1,2,6; Zhang, XL (Zhang, Xuelei)3; Zhang, CL (Zhang, Chenglong)4; Xu, TL (Xu, Tianli)1,5; Wu, GJ
Source PublicationJOURNAL OF GLACIOLOGY
2016
Volume62Issue:231Pages:46-53
DOI10.1017/jog.2016.8
AbstractUsing a field emission scanning electron microscope and energy-dispersive X-ray spectrometer (FESEM-EDS), individual insoluble dust particles in ice cores recovered from the northern (Dunde), western (Murtagata) and south-eastern (Palong-Zangbo) Tibetan Plateau were analysed in order to reveal the mineralogical and morphological characteristics of the analogue of long-range transported Asian dust. The results reveal that the dust particles are mainly composed of quartz (17-36%, number abundance), clay (37-48%) and feldspar (12-18%). Illite and chlorite are the dominant clay species, while kaolinite is rarely observed. For the three sites, regional differences in the mineral assemblages are significant, in particular the abundance of quartz, chlorite and muscovite species, reflecting the regional provenance of these dust particles and the climatic regime in their source areas. Oxide ratios in clays indicate different weathering strengths of the particles in their source regions, with a higher K2O/(SiO2 + Al2O3) in the western and northern Tibetan Plateau. The individual particles have modes of 1.48 and 1.53 in the aspect ratio and circularity distribution respectively. No significant relationship between aspect ratio and circularity was found. Quartz and feldspar particles have a narrow aspect ratio distribution. Muscovite particles have the coarsest grain size, while chlorite particles have the finest.
Subject Area自然地理学
WOS IDWOS:000376838400005
Language英语
Indexed BySCI
KeywordAce-asia Electron-microscopy Greenland Ice Soil Dust China Aerosol Chemistry Regions Shape Snow
Cooperation Status国内
Department环境
SubtypeArticle
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Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7867
Collection图书馆
Corresponding AuthorWu, GJ
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
2.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun 130102, Peoples R China
4.Chinese Acad Sci, Ecoenvironm Sci Res Ctr, Beijing 100085, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.Chinese Acad Sci, Inst Tibetan Plateau Res, 16 Courtyard,Lincui Rd, Beijing 100101, Peoples R China
Recommended Citation
GB/T 7714
Wu, GJ ,Zhang, XL ,Zhang, CL ,et al. Mineralogical and morphological properties of individual dust particles in ice cores from the Tibetan Plateau[J]. JOURNAL OF GLACIOLOGY,2016,62(231):46-53.
APA Wu, GJ ,Zhang, XL ,Zhang, CL ,Xu, TL ,&Wu, GJ.(2016).Mineralogical and morphological properties of individual dust particles in ice cores from the Tibetan Plateau.JOURNAL OF GLACIOLOGY,62(231),46-53.
MLA Wu, GJ ,et al."Mineralogical and morphological properties of individual dust particles in ice cores from the Tibetan Plateau".JOURNAL OF GLACIOLOGY 62.231(2016):46-53.
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