长江口及邻近陆架沉积物中Pt、Pd分异的物源示踪

张霄宇; 张富元; 高爱根; 章伟艳

Volume 34 Issue 4

Jul. 2009

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Article Navigation > Earth Science > 2009 > 34(4): 604-612

ZHANG Xiao-yu, ZHANG Fu-yuan, GAO Ai-gen, ZHANG Wei-yan, 2009. Source Tracing Implication of Pt and Pd Fractionation in the Surface Sediment of Continental Shelf around Changjiang Estuary. Earth Science, 34(4): 604-612.

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Source Tracing Implication of Pt and Pd Fractionation in the Surface Sediment of Continental Shelf around Changjiang Estuary

1.
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Key Laboratory of Submarine Geoscience, State 0ceanic Administration, Hangzhou 310012, China

Received Date: 2008-06-03
Publish Date: 2009-07-25

Abstract

Abstract

Over the past decades extensive studies on the sediment source tracing and transporting routine of Yellow Sea and East China Sea have been carried out but not yet resolved completely.The present research suggests Pt/Pd ratio is a promising index to distinguish sediments transported from Changjiang and those from Huanghe drainage basins.The erosive sediment of old Huanghe Delta transported by southern Yellow Sea coastal current is characterized by Pt/Pd > 1;land source sediment carried by Changjiang River was characterized by Pt/Pd≤1.The two unique weathering regime in the Chanjiang and Huanghe drainage basins was the key factor causing the fractionation of Pt and Pd in the sediment.The element composition in the sediment of Pt/Pd≤1 corresponds well with that of Changjiang sediments, and the element composition in the sediment of Pt/Pd≤1 is in accordance with that of Huanghe sediments.The K/Na-Rb/Sr diagram suggests that the chemical composition of land source sediment varied during re-erosion and re-transportion and re-sedimentation.
- Yellow Sea and East China Sea,
- sediment,
- PGE,
- Pt/Pd,
- source tracing,
- sedimentology.

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References(66)

References

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Source Tracing Implication of Pt and Pd Fractionation in the Surface Sediment of Continental Shelf around Changjiang Estuary

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