Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia

Sediment cores were collected from Kota Kinabalu and Labuan ports to determine the distribution of natural uranium isotopes, calcium (Ca), aluminium (Al) and total organic matter (TOM). A strong statistical correlation value between 234U/238U and Ca contents were shown at Kota Kinabalu (r2 = 0.811),...

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Main Authors: Abdul Hafidz Yusoff, Che Abd Rahim Mohamed
Format: Article
Language:English
Published: Thai Society of Higher Eduction Institutes on Environment 2015-07-01
Series:EnvironmentAsia
Subjects:
Online Access:http://www.tshe.org/ea/pdf/vol8no2-11.pdf
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spelling doaj-80bd4154b19b4736b0343d3e28d310a02020-11-25T01:59:21ZengThai Society of Higher Eduction Institutes on EnvironmentEnvironmentAsia1906-17142015-07-01828593Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, MalaysiaAbdul Hafidz Yusoff 0Che Abd Rahim Mohamed1School of Environmental and Natural Resource Sciences, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600, Bangi, Selangor, MalaysiaSchool of Environmental and Natural Resource Sciences, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600, Bangi, Selangor, MalaysiaSediment cores were collected from Kota Kinabalu and Labuan ports to determine the distribution of natural uranium isotopes, calcium (Ca), aluminium (Al) and total organic matter (TOM). A strong statistical correlation value between 234U/238U and Ca contents were shown at Kota Kinabalu (r2 = 0.811), and Labuan (r2 = 0.833) ports. Good statistical correlation r2 > 0.8 was also obtained between uranium isotopes and TOM at Kota Kinabalu port. Most activity ratio values of 234U/238U found in sediment cores from Kota Kinabalu port were more than 1.0; the major input of uranium at Kota Kinabalu port may be related to the sorptive process of authigenic uranium that occurs in the water column. In this case, the mobile U(VI) was reduced to immobile U(IV) by organic matter and scavenged to the sediment with co-precipitation of organic matter and calcium carbonate. On the other hand, a low activity ratio of 234U/238U (≤ 1) from Labuan was of detrital origin and also showed positive statistical correlation between calcium and aluminium.http://www.tshe.org/ea/pdf/vol8no2-11.pdfuraniumsediment coretotal organic matter (TOM)limestonedetrital
collection DOAJ
language English
format Article
sources DOAJ
author Abdul Hafidz Yusoff
Che Abd Rahim Mohamed
spellingShingle Abdul Hafidz Yusoff
Che Abd Rahim Mohamed
Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
EnvironmentAsia
uranium
sediment core
total organic matter (TOM)
limestone
detrital
author_facet Abdul Hafidz Yusoff
Che Abd Rahim Mohamed
author_sort Abdul Hafidz Yusoff
title Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
title_short Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
title_full Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
title_fullStr Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
title_full_unstemmed Vertical Profiles of Natural Uranium Isotopes in Sediment Cores from Kota Kinabalu and Labuan Ports, Malaysia
title_sort vertical profiles of natural uranium isotopes in sediment cores from kota kinabalu and labuan ports, malaysia
publisher Thai Society of Higher Eduction Institutes on Environment
series EnvironmentAsia
issn 1906-1714
publishDate 2015-07-01
description Sediment cores were collected from Kota Kinabalu and Labuan ports to determine the distribution of natural uranium isotopes, calcium (Ca), aluminium (Al) and total organic matter (TOM). A strong statistical correlation value between 234U/238U and Ca contents were shown at Kota Kinabalu (r2 = 0.811), and Labuan (r2 = 0.833) ports. Good statistical correlation r2 > 0.8 was also obtained between uranium isotopes and TOM at Kota Kinabalu port. Most activity ratio values of 234U/238U found in sediment cores from Kota Kinabalu port were more than 1.0; the major input of uranium at Kota Kinabalu port may be related to the sorptive process of authigenic uranium that occurs in the water column. In this case, the mobile U(VI) was reduced to immobile U(IV) by organic matter and scavenged to the sediment with co-precipitation of organic matter and calcium carbonate. On the other hand, a low activity ratio of 234U/238U (≤ 1) from Labuan was of detrital origin and also showed positive statistical correlation between calcium and aluminium.
topic uranium
sediment core
total organic matter (TOM)
limestone
detrital
url http://www.tshe.org/ea/pdf/vol8no2-11.pdf
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AT cheabdrahimmohamed verticalprofilesofnaturaluraniumisotopesinsedimentcoresfromkotakinabaluandlabuanportsmalaysia
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