Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay

Wu Run; Li Pei-quan; Miao Lu-tian; Zhang Shu-xin; Tian Wei-zhi

doi:10.1007/BF02850493

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Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay

OriginalPaper | Updated：2023-05-16

- Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay
- Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay
- 海洋湖沼学报（英文） 1994年12卷第4期页码：331-338
- Affiliations：
  
  1. Institute of Oceanology
  2. Institute of Atomic Energy
- Author bio：
- Funds：
- DOI：10.1007/BF02850493
  中图分类号：
- 纸质出版：1994
- Accepted：
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Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay[J]. 海洋湖沼学报（英文）, 1994,12(4):331-338.

Run, W., Pei-quan, L., Lu-tian, M. et al. Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay., Chin. J. Ocean. Limnol. 12, 331–338 (1994). https://doi.org/10.1007/BF02850493
Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay[J]. 海洋湖沼学报（英文）, 1994,12(4):331-338. DOI： 10.1007/BF02850493.

Run, W., Pei-quan, L., Lu-tian, M. et al. Geochemical studies of Fe, Mn, Co, As, Cr, Sb, Zn, Sc and V in surface sediments from Jiaozhou Bay., Chin. J. Ocean. Limnol. 12, 331–338 (1994). https://doi.org/10.1007/BF02850493 DOI：

摘要

Abstract

The contents of nearly forty-elements in surface sediments in Jiaozhou Bay were determined using a Neutron Activation Analysis Technique (Grancini

et al.

1976; Li Peiquan et al.

1985

1986; Li Xiuxia et al.

1986). This paper's detailed discussion on only nine elements (Fe

Zn and V) includes their distributions

concentrations

correlationships

material sources

background

etc. Based on Zavaristski's classification method

Cr and V belong to the second group; As and Sb to the eighth groups: Sc and Zn to the third and sixth groups. It was found that their notably good correlationship is mainly due to the similarity of their ionic structures and that their variation is controlled by the Fe content (except Mn). The source of sediments is mainly terristrial material

and the composition of sediment is similar to that of shale and shale+clay. The contents for a large number of elements are within the scope of the background level

but there still is pollution of Zn and Cr

at least in a few stations.

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references

Grancini, G., Stievano, M. B., et al., 1976. The capability of neutron activation for trace element analysis in sea and sediment samples of the Northern Adriatic Sea.J. Radioanal. Chem. 34: 65–78.

Li Peiquan, Li Xiuxia, Qian Xingzhen, et al., 1985. Neutron activation analysis of the sediments and geochemistry study of elements in Okinawa Trough: 1. The contents and distributions of elements.Oceanologia et Limnologia Sinica 16(6): 461–474. (in Chinese with English abstract)

Li Peiquan, Li Xiuxia, Qian Xingzhen et al., 1986. Neutron activation analysis of the sediments and geochemistry study of elements in Okinawa Trough: Discussion of elements, correlation, concentration coefficient, etc.Oceanologia et Limnologia Sinica (Suppl. 1986) 1–100. (in Chinese with English abstract)

Li Xiuxia, Qian Xingzhen, Li Peiquan et al., 1986. Neutron activation and analysis and geochemistry study of elements in sediment in East China Sea.Transactions of Oceanology 8(5): 566–572. (in Chinese)

Nanjing Geological College, 1987. Geochemistry. Science Press, Beijing. 1–514. (in Chinese)

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