Spatial Distribution of Total 210Pb in the Marine Sediment of Peninsular Malaysia: Radioactivity Level Variations in the Sunda Shelf Seas

Authors

  • Nur Ashikin Zaini Department of Earth Sciences & Environment, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, Selangor 43600, Malaysia
  • Mohamad Arif Che Abd Rahim Department of Earth Sciences & Environment, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, Selangor 43600, Malaysia https://orcid.org/0000-0003-3571-1761
  • Shengfa Liu Key Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266000, China
  • Xuefa Shi Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266000, China
  • Che Abd Rahim Mohamed Department of Earth Sciences & Environment, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, Selangor 43600, Malaysia

DOI:

https://doi.org/10.48048/tis.2023.6790

Keywords:

210Pb, Sediment, Malacca Strait, Southern South China Sea, Andaman

Abstract

Radiochemical separation techniques were applied to measure 210Pb radioactivity in samples to determine spatial distribution of total 210Pb radionuclide in surface sediments and water column for the main waters on the Sunda Shelf. The average 210Pb radioactivity level recorded for the Malacca Strait (MS) is significantly higher than that of the southern South China Sea (sSCS); this is attributed to the supply of input from the Andaman Sea in its northern areas, and massive terrestrial processes from bordering land masses. The results reveal that the decreasing trend of total 210Pb in Peninsular Malaysia’s marine sediment starts with the north maritime zone of Malacca Strait (64.28 ± 5.97 Bq/kg) > south maritime zone of Malacca Strait (50.88 ± 6.15 Bq/kg) > east maritime zone of sSCS (41.01 ± 3.07 Bq/kg) > south maritime zone of sSCS (40.78 ± 3.16 Bq/kg). The Kelantan and Pahang Deltas have been identified as two of the main anthropogenic sources of input for total 210Pb in the sSCS with atmospheric transboundary mobilization affecting total 210Pb in the water column. In the Malacca Strait, however, the distribution of total 210Pb might be influenced mainly by in situ processes of the strait’s seafloor and sources origin of sediment.

HIGHLIGHTS

  • The Malacca Strait has a significantly higher level of 210Pb radioactivity compared to the southern South China Sea (sSCS), due to input from the Andaman Sea and terrestrial processes from adjacent land masses
  • The decreasing trend of total 210Pb in Peninsular Malaysia’s marine sediment starts with the north maritime zone of Malacca Strait > south maritime zone of Malacca Strait > east maritime zone of sSCS > south maritime zone of sSCS
  • The Kelantan and Pahang Deltas are identified as two of the main anthropogenic sources of input for total 210Pb in the sSCS, while in the sh Strait, the distribution of total 210Pb may be influenced mainly by in situ processes of the strait’s seafloor and sources origin of sediment


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Published

2023-04-26

How to Cite

Zaini, N. A. ., Che Abd Rahim, M. A. ., Liu, S. ., Shi, X. ., & Mohamed, C. A. R. . (2023). Spatial Distribution of Total 210Pb in the Marine Sediment of Peninsular Malaysia: Radioactivity Level Variations in the Sunda Shelf Seas. Trends in Sciences, 20(9), 6790. https://doi.org/10.48048/tis.2023.6790