Sedimentation rate of trace elements in the surface sediment of the south China Sea

Trace elements contents in the surface sediments (about 5 cm depth) of the South China Sea were obtained during the Ekspedisi Matahari cruises. Their concentrations are slightly different from cruise to cruise and may be related to the content of water column and input from the land through river or...

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Main Authors: Che Abd Rahim Mohamed, Noor Azhar Mohamed Shzili
Format: Article
Published: Universiti Kebangsaan Malaysia 2000
Online Access:http://journalarticle.ukm.my/3796/
http://journalarticle.ukm.my/3796/
id ukm-3796
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spelling ukm-37962012-03-20T03:06:49Z http://journalarticle.ukm.my/3796/ Sedimentation rate of trace elements in the surface sediment of the south China Sea Che Abd Rahim Mohamed, Noor Azhar Mohamed Shzili, Trace elements contents in the surface sediments (about 5 cm depth) of the South China Sea were obtained during the Ekspedisi Matahari cruises. Their concentrations are slightly different from cruise to cruise and may be related to the content of water column and input from the land through river or wind. The range of accumulation rates of the heavy metals are also wide; 3.80 ­23.7 mg.cm2/kyr,8.89 - 24.7 mg.cm2/kyr, 3.78 - 14.4 mg.cm2/kyr and 20.1 ­30 mg.cm2/kyr for Cu, Ni, Pb and Zn, respectively. The metal/Fe ratios are slightly same with the preindustrial period and probably controlled by natural inputs from water column. Universiti Kebangsaan Malaysia 2000 Article PeerReviewed Che Abd Rahim Mohamed, and Noor Azhar Mohamed Shzili, (2000) Sedimentation rate of trace elements in the surface sediment of the south China Sea. Sains Malaysiana, 29 . pp. 225-232. ISSN 0126-6039 http://www.ukm.my/jsm/english_journals/vol29_2000/vol29_00page225-232.html
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institution_category Local University
institution Universiti Kebangasaan Malaysia
building UKM Institutional Repository
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description Trace elements contents in the surface sediments (about 5 cm depth) of the South China Sea were obtained during the Ekspedisi Matahari cruises. Their concentrations are slightly different from cruise to cruise and may be related to the content of water column and input from the land through river or wind. The range of accumulation rates of the heavy metals are also wide; 3.80 ­23.7 mg.cm2/kyr,8.89 - 24.7 mg.cm2/kyr, 3.78 - 14.4 mg.cm2/kyr and 20.1 ­30 mg.cm2/kyr for Cu, Ni, Pb and Zn, respectively. The metal/Fe ratios are slightly same with the preindustrial period and probably controlled by natural inputs from water column.
format Article
author Che Abd Rahim Mohamed,
Noor Azhar Mohamed Shzili,
spellingShingle Che Abd Rahim Mohamed,
Noor Azhar Mohamed Shzili,
Sedimentation rate of trace elements in the surface sediment of the south China Sea
author_facet Che Abd Rahim Mohamed,
Noor Azhar Mohamed Shzili,
author_sort Che Abd Rahim Mohamed,
title Sedimentation rate of trace elements in the surface sediment of the south China Sea
title_short Sedimentation rate of trace elements in the surface sediment of the south China Sea
title_full Sedimentation rate of trace elements in the surface sediment of the south China Sea
title_fullStr Sedimentation rate of trace elements in the surface sediment of the south China Sea
title_full_unstemmed Sedimentation rate of trace elements in the surface sediment of the south China Sea
title_sort sedimentation rate of trace elements in the surface sediment of the south china sea
publisher Universiti Kebangsaan Malaysia
publishDate 2000
url http://journalarticle.ukm.my/3796/
http://journalarticle.ukm.my/3796/
first_indexed 2023-09-18T19:39:48Z
last_indexed 2023-09-18T19:39:48Z
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