Physicochemical Properties of Asian Dust Sources

In order to fully understand the chemical properties of Asian dust particles, especially their transformation and aging processes, it is desirable to investigate the nature of original sands collected at local source areas in China. This study presents the detailed properties of sands collected at f...

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Main Authors: Chang-Jin Ma, Mikio Kasahara, Susumu Tohno, Ki-Hyun Kim
Format: Article
Language:English
Published: Asian Association for Atmospheric Environment 2008-06-01
Series:Asian Journal of Atmospheric Environment
Subjects:
Online Access:http://asianjae.org/_common/do.php?a=full&b=11&bidx=1592&aidx=20026
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spelling doaj-d989193a1a804b2fa1ebd0c47a1c35302020-11-25T02:28:22ZengAsian Association for Atmospheric EnvironmentAsian Journal of Atmospheric Environment1976-69122287-11602008-06-0121263310.5572/ajae.2008.2.1.026Physicochemical Properties of Asian Dust SourcesChang-Jin Ma0Mikio Kasahara1Susumu Tohno2Ki-Hyun Kim3Department of Environmental Science, Fukuoka Women’s University, Fukuoka, JapanInstitute of Science and Technology Research, Chubu University, Aichi, JapanGraduate School of Energy Science, Kyoto University, Kyoto, JapanDepartment of Earth and Environmental Sciences, Sejong University, Seoul, KoreaIn order to fully understand the chemical properties of Asian dust particles, especially their transformation and aging processes, it is desirable to investigate the nature of original sands collected at local source areas in China. This study presents the detailed properties of sands collected at four different desert regions (Yinchuan, Wuwei, Dulan, and Yanchi) in China. Most of sands have irregular shape with yellowish coloration, whereas some of them show peculiar colors. The relative size distribution of sands collected at Yinchuan, Wuwei, and Dulan deserts exhibits monomodal with the maximum level between 200 and 300 μm, whereas that of Yanchi desert is formed between 100 and 200 μm. The mass concentration ratio of each element to that of Si (Z/Si) determined by PIXE analysis has a tendency towards higher Z/Si ratios for soil derived elements. It was possible to visually reconstruct the elemental maps on the surface of individual sands by XRF microprobe technique. In addition, the multielemental mass concentration could be quantitatively calculated for numerous spots of desert sands.http://asianjae.org/_common/do.php?a=full&b=11&bidx=1592&aidx=20026asian dustdesert sandx-ray fluorescencelong-range transportelement
collection DOAJ
language English
format Article
sources DOAJ
author Chang-Jin Ma
Mikio Kasahara
Susumu Tohno
Ki-Hyun Kim
spellingShingle Chang-Jin Ma
Mikio Kasahara
Susumu Tohno
Ki-Hyun Kim
Physicochemical Properties of Asian Dust Sources
Asian Journal of Atmospheric Environment
asian dust
desert sand
x-ray fluorescence
long-range transport
element
author_facet Chang-Jin Ma
Mikio Kasahara
Susumu Tohno
Ki-Hyun Kim
author_sort Chang-Jin Ma
title Physicochemical Properties of Asian Dust Sources
title_short Physicochemical Properties of Asian Dust Sources
title_full Physicochemical Properties of Asian Dust Sources
title_fullStr Physicochemical Properties of Asian Dust Sources
title_full_unstemmed Physicochemical Properties of Asian Dust Sources
title_sort physicochemical properties of asian dust sources
publisher Asian Association for Atmospheric Environment
series Asian Journal of Atmospheric Environment
issn 1976-6912
2287-1160
publishDate 2008-06-01
description In order to fully understand the chemical properties of Asian dust particles, especially their transformation and aging processes, it is desirable to investigate the nature of original sands collected at local source areas in China. This study presents the detailed properties of sands collected at four different desert regions (Yinchuan, Wuwei, Dulan, and Yanchi) in China. Most of sands have irregular shape with yellowish coloration, whereas some of them show peculiar colors. The relative size distribution of sands collected at Yinchuan, Wuwei, and Dulan deserts exhibits monomodal with the maximum level between 200 and 300 μm, whereas that of Yanchi desert is formed between 100 and 200 μm. The mass concentration ratio of each element to that of Si (Z/Si) determined by PIXE analysis has a tendency towards higher Z/Si ratios for soil derived elements. It was possible to visually reconstruct the elemental maps on the surface of individual sands by XRF microprobe technique. In addition, the multielemental mass concentration could be quantitatively calculated for numerous spots of desert sands.
topic asian dust
desert sand
x-ray fluorescence
long-range transport
element
url http://asianjae.org/_common/do.php?a=full&b=11&bidx=1592&aidx=20026
work_keys_str_mv AT changjinma physicochemicalpropertiesofasiandustsources
AT mikiokasahara physicochemicalpropertiesofasiandustsources
AT susumutohno physicochemicalpropertiesofasiandustsources
AT kihyunkim physicochemicalpropertiesofasiandustsources
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