Elemental geochemistry of alto-cryic soils of Qinghai-Tibet Plateau in China - An example from the unpopulated Kekexili region | |
Huang, B; Gong, ZT; Gu, G | |
刊名 | GEOCHEMICAL JOURNAL |
2006 | |
卷号 | 40期号:2页码:211-218 |
关键词 | element geochemistry immature soil alto-cryic pedogenesis Qinghai-Tibet Plateau China |
ISSN号 | 0016-7002 |
通讯作者 | Gong, ZT(ztgong@issas.ac.cn) |
英文摘要 | The Qinghai-Tibet Plateau has developed immature soils since the late Pliocene period when it was uplifted. The objectives of this paper were (i) to investigate native major and trace elements of the immature soils in the Kekexili region in the Plateau; (ii) to evaluate the bioavailability of selected trace elements in the soils; (iii) to better understand the factors affecting accumulation and depletion of the elements and their bioavailability over a long history of alto-cryie pedogenesis. Cambosols and Aridosols are dominant soil types in this region while Gleyosols and Primosols are minor types. These coarse-textured soils have high soil pH and free carbonate content. The soil profile often developed a mattic or humic epipedon with high organic matter content in the topsoil. The contents of Ca, Mg, Na, and Sr in the Kekexili soils were significantly higher than the average values of Chinese soils, and also the world average, while the contents of Fe, Al, Ti, Mn, P, Co, Cr, and Ba in the former soils lower than those in the latter soils. The accumulation or depletion of elements was mainly dependent on soil carbonate content. The bioavailability of Fe, Zn, and Mn was positively related to the levels of organic matter in the surface soil. Results indicate that though these soils had a long history of pedogenesis, they were still relatively immature due to weak geocheirtical cycles but the bioavailability of nutrients in topsoil was high. |
收录类别 | SCI |
WOS关键词 | SEDIMENTS ; AREA |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | GEOCHEMICAL SOC JAPAN |
WOS记录号 | WOS:000236101300008 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2558583 |
专题 | 南京土壤研究所 |
通讯作者 | Gong, ZT |
作者单位 | Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China |
推荐引用方式 GB/T 7714 | Huang, B,Gong, ZT,Gu, G. Elemental geochemistry of alto-cryic soils of Qinghai-Tibet Plateau in China - An example from the unpopulated Kekexili region[J]. GEOCHEMICAL JOURNAL,2006,40(2):211-218. |
APA | Huang, B,Gong, ZT,&Gu, G.(2006).Elemental geochemistry of alto-cryic soils of Qinghai-Tibet Plateau in China - An example from the unpopulated Kekexili region.GEOCHEMICAL JOURNAL,40(2),211-218. |
MLA | Huang, B,et al."Elemental geochemistry of alto-cryic soils of Qinghai-Tibet Plateau in China - An example from the unpopulated Kekexili region".GEOCHEMICAL JOURNAL 40.2(2006):211-218. |
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