Sea flux of trace metals in Saanich Inlet

Zhan Binqiu; C. S. Wong; K. W. Johnson

doi:10.1007/BF02846267

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Sea flux of trace metals in Saanich Inlet

OriginalPaper | Updated：2023-05-16

- Sea flux of trace metals in Saanich Inlet
- Sea flux of trace metals in Saanich Inlet
- 海洋湖沼学报（英文） 1989年7卷第4期页码：345-354
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Contribution No. 1650 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02846267
  中图分类号：
- 纸质出版：1989
- Accepted：
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Sea flux of trace metals in Saanich Inlet[J]. 海洋湖沼学报（英文）, 1989,7(4):345-354.

Binqiu, Z., Wong, C.S. & Johnson, K.W. Sea flux of trace metals in Saanich Inlet., Chin. J. Ocean. Limnol. 7, 345–354 (1989). https://doi.org/10.1007/BF02846267
Sea flux of trace metals in Saanich Inlet[J]. 海洋湖沼学报（英文）, 1989,7(4):345-354. DOI： 10.1007/BF02846267.

Binqiu, Z., Wong, C.S. & Johnson, K.W. Sea flux of trace metals in Saanich Inlet., Chin. J. Ocean. Limnol. 7, 345–354 (1989). https://doi.org/10.1007/BF02846267 DOI：

摘要

Abstract

The sea fluxes of trace metals

POC

and settled material were studied in anoxic seawater

Saanich Inlet

B. C.

Canada with sediment traps. This paper discusses the change of mass fluxes of sediment

trace metals and POC for various seasons and depths. The annual mean of settled material is 1.56 g.m−2.a−1

84.6 mg. m−2.a−1 for POC

60.0 mg. m−2.a−1 for Cu

16.5 mg.m−2.a−1 for Pb

189 mg.m−2.a−1 for Zn

2.20 mg.m−2.a−1 for Cd

699 mg.m−2.a−1 for Fe

38.8 mg.m−2.a−1 for Co

and 84.6 mg.m−2.a−1 for Ni. The relations between the average fluxes of trace metals and POC

the fluxes of trace metals and settled matter

and the sea fluxes of trace metals and Fe are in linear progression. The resident times of elements as calculated from sea flux

are 1.1 a. for Cu

0.014 a. for Pb

0.50 a. for Zn

3.8 a. for Cd

0.16 a. for Fe

0.39 a. for Co

and 1.14 a. for Ni. The order of resident times is as follows: Pb−Fe−Co−Zn−Cu−Ni−Cd. The metal resident times in Saanich Inlet are shorter than the values estimated for the open ocean. It illustrates that the biochemical processes in shallow Saanich Inlet are faster than those in the open ocean

and that debries of plankton and fecal pellets of zooplankton play an important role in vertical transport of organic carbons.

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Keywords

references

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