Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.9719/EEG.2012.45.1.009 |
Geochemical Characteristics and Trace Metal Speciation of Soils in Major Source Area of Asian Dust | |
Lee, Pyeong-Koo; Youm, Seung-Jun; An, Gi-O | |
通讯作者 | Lee, PK |
来源期刊 | ECONOMIC AND ENVIRONMENTAL GEOLOGY
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ISSN | 1225-7281 |
EISSN | 2288-7962 |
出版年 | 2012 |
卷号 | 45期号:1页码:9-21 |
英文摘要 | In this study, we investigated the chemical characteristics of soils collected from the several deserts and loess in China known as the typical source areas of Asian dust (the Taklamakan desert, the Alashan desert, the Ordos desert and the Loess Plateau). Based on our analysis, we examined the possibility of adverse effects on environments and human health. In each desert and loess, major elemental compositions of soils did not show large variations, implying that the long-periodic mixing of soils in each area made their chemical compositions homogeneous. Minor elements of soils in each desert and loess showed more complicated patterns with strong correlations each other (e. g., Cr, Cu, As, Co, Ni, V, Y, Sc, Sn, Pb, Zn, Cd, Cs, Li, Th, U). These results thus enable us to discriminate the soil of the Loess Plateau from those of the other deserts in China. The results of sequential extraction experiments for soils showed that the chemical speciation of Fe was dominant in residual fraction (> 85%) in all deserts and loess, but the fractions of Mn and Ca chemical speciations were very different in each area. In the case of Mn, the fraction of amorphous Fe-Mn hydroxides (55.4%) in the Central Loess Plateau and the carbonate fraction (33.8%) in Taklamakan desert were higher as much as 2 to 5 times than other deserts. The chemical speciations of Ca are dominant in carbonate fraction in Taklamakan (75.9%) and Alashan (50.5%) deserts, but carbonate fractions of Ca in the Loess Plateau and Ordos deserts were low (6.6% and 2.1%, respectively). According to the mobility of trace elements inferred from the results of sequential extraction procedure, we could classify them into five groups, and the mobility of Cd, Pb and Cu are more than 87%, 33% and 30%, respectively. Therefore, Cd, Pb and Cu in soils of deserts and loess could be easily dissolved when interacted with surface water. As such, they could give adverse effects on surficial environments and human health. |
英文关键词 | Asian dust source areas soils of desert & loess geochemical characteristics |
类型 | Article |
语种 | 其他 |
开放获取类型 | Bronze |
收录类别 | ESCI |
WOS记录号 | WOS:000439560000002 |
WOS类目 | Geology |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/330199 |
作者单位 | [Lee, Pyeong-Koo; Youm, Seung-Jun; An, Gi-O] Korea Inst Geosci & Mineral Resources, Geol Environm Div, Daejeon, South Korea |
推荐引用方式 GB/T 7714 | Lee, Pyeong-Koo,Youm, Seung-Jun,An, Gi-O. Geochemical Characteristics and Trace Metal Speciation of Soils in Major Source Area of Asian Dust[J],2012,45(1):9-21. |
APA | Lee, Pyeong-Koo,Youm, Seung-Jun,&An, Gi-O.(2012).Geochemical Characteristics and Trace Metal Speciation of Soils in Major Source Area of Asian Dust.ECONOMIC AND ENVIRONMENTAL GEOLOGY,45(1),9-21. |
MLA | Lee, Pyeong-Koo,et al."Geochemical Characteristics and Trace Metal Speciation of Soils in Major Source Area of Asian Dust".ECONOMIC AND ENVIRONMENTAL GEOLOGY 45.1(2012):9-21. |
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