Malaysian Journal of Analytical Sciencesw Vol 18 No
2 (2014): 284 298
ASSESSMENT
OF NATURALLY OCCURING RADIONUCLIDE IN THE SEDIMENT CORE IN SOUTHERN OF KUALA
SELANGOR COASTAL AREA
(Kajian
Radionuklida Tabii di dalam Teras Sedimen di Kawasan Pesisir Pantai Selatan
Kuala Selangor)
Zaini Hamzah, Umi Kalsum Abdul Karim*, Ahmad Saat, Sabarina
MD Yunus
Faculty
of Applied Sciences,
Universiti
Teknologi MARA, 40450, Shah Alam, Selangor, Malaysia
*Corresponding author: ikacome@yahoo.com
Abstract
This study is to
determine naturally occurring radionuclide activity concentrations of 226Ra, 228Ra
and 40K in sediment core using gamma-ray spectrometry with a
high-purity germanium (HPGe) detector. Sediment core was taken from 14
locations in two areas in Kuala Selangor which are Pantai Remis and Pantai
Jeram. Samples were taken during Northeast Monsoon in January and March 2011. 40K was measured via its 1460 keV
energy peak, 226Ra (of the 238U) and
228Ra (of the 232Th) through their γ-ray lines 609.3
keV (214Bi) and 911.1 keV (228Ac). The mean activity concentration of 226Ra
in Pantai Remis is 37.49±1.38 Bq/kg and ranged between 19.44-55.74
Bq/kg. For 228Ra the activity concentration ranged between 40.75-82.23 Bq/kg with a mean value of 58.64±2.60
Bq/kg; and that of 40K from 206.53-398.30Bq/kg
with a mean of 316.95 ± 10.88 Bq/kg. Meanwhile the mean activity concentration
of 226Ra in Pantai Jeram is 32.35±1.27 Bq/kg and ranged between 21.28-38.67 Bq/kg. For 228Ra the activity
concentration ranged between 34.25-106.72
Bq/kg with a mean value of 57.96±2.55Bq/kg; and that of 40K from 246.12-394.53 Bq/kg with a mean of 325.14±10.87
Bq/kg. Different vertical profile of 226Ra,
228Ra and 40K
activity concentration observed between sampling locations might due to the
sediment mineralogy, source of radioactivity, geochemistry of the area and
oceanic process. Plus, smaller 228Ra/226Ra activity ratio
range suggests that interaction on these two series with the surrounding were
very similar. Value of study radionuclides in present study were almost
comparable with study done in other part in Malaysia. Moreover, world mean
value of 226Ra, 228Ra and 40K provided by
UNSCEAR (1993) fall within the value range of radionuclides in present study.
Keywords: Natural radionuclides, activity
concentration, sediment core, coastal area, gamma spectrometer
Abstrak
Kajian ini adalah
untuk menentukan aras radionuklid tabii (226Ra,
228Ra dan 40K)
di dalam teras sedimen menggunakan spektrometer gama yang dilengkapkan dengan
pengesan germanium lampau tulen (HPGe). Teras sedimen telah di ambil daripada
14 lokasi di dua kawasan di Kuala Selangor iaitu Pantai Remis dan Pantai Jeram.
Sampel telah di ambil semasa monsun timur laut pada Januari dan Mac 2011. Radionuklid
40K diukur melalui puncak tenaga 1460 keV. Untuk 226Ra (daripada 238U) dan 228Ra
(daripada 232Th) garisan sinar gama 609.3 keV (214Bi) dan
911.1 keV (228Ac) digunakan. Purata kepekatan aktiviti 226Ra
di Pantai Remis ialah 37.49±1.38 Bq/kg dan julat di antara 19.44-55.74
Bq/kg. Untuk 228Ra, kepekatan aktiviti julat diantara
40.75-82.23Bq/kg dengan purata 58.64±2.60 Bq/kg; dan bagi 40K julat
di antara 206.53-398.30Bq/kg dengan purata 316.95 ± 10.88 Bq/kg. Sementara itu purata
kepekatan aktiviti 226Ra di
Pantai Jeram ialah is 32.35±1.27 Bq/kg dan julat diantara 21.28-38.67 Bq/kg.
Untuk 228Ra kepekatan
aktiviti berjulat diantara 34.25-106.72 Bq/kg dengan purata bernilai 57.96±2.55Bq/kg;
dan bagi 40K julat diantara 246.12-394.53 Bq/kg dengan purata
325.14±10.87 Bq/kg. Terdapat perbezaan profil mencangcang bagi kepekatan
aktiviti untuk 226Ra, 228Ra and 40K, yang mugkin
disebabkan oleh mineralogi sedimen, punca radioaktif, geokimia kawasan tersebut
serta proses lautan. Tambahan pula, nilai lingkungan kecil bagi nisbah activiti
untuk 228Ra/226Ra mengcadangkan bahawa interaksi di
antara dua siri ini dengan persekitaran adalah sama. Nilai radionuklida yang
dikaji di dalam kajian ini adalah sebanding dengan kajian yang dijalankan di kawasan lain di Malaysia. Nilai purata
dunia bagi 226Ra, 228Ra and 40K yang
dinyatakan oleh UNSCEAR (1993) jatuh di dalam lingkungan nilai radionuklida di
dalam kawasan kajian ini.
Kata
kunci:
Radionuklid tabii, kepekatan aktiviti, teras sedimen, kawasan pesisir pantai,
spektrometer gama
References
1.
Theng, T.L. & Mohamed, C. A. R. (2005). Activities of 210Po
and 210Pb in the water column at Kuala Selangor, Malaysia. Journal of Environmental Radioactivity, 80:
273-286.
2.
IAEA-TECDOC-1429. January (2005). Radionuclide levels in
oceans and seas. Worldwide marine
radioactivity studies (WOMARS). Final report of a coordinated research
project .
3.
IAEA.
1922 March (2007). Naturally occurring radioactive material NORM V. In:
Proceedings of an International Symposium, Seville, Spain.
4.
John R. C., Ranjeet, K. R. & Sokhi, S. (2003).
Radioactive Releases in the Environment: Impact and Assessment. John Wiley & Sons, Ltd. (1), England
5.
Alatise, O.O., Babalola, I. A. & Olowofela, J. A. (2008).
Distribution of some natural gamma-emitting radionuclides in the soils of the
coastal areas of Nigeria. Journal of
Environmental Radioactivity, 99: 1746-1749.
6.
Saat, A., Hamzah, Z., Yusop. M. F. & Zainal, M. A. (2010).
Experimental Determination of the HPGe Spectrometer Efficiency Calibration
Curves for Various Sample Geometry for Gamma Energy from50 keV to 2000 keV. Progress of Physic Research in Malaysia,
American Institute of Physic, 5: 39 42.
7.
Hamzah, Z., Saat, A., Mashuri, N. H. & Redzuan, S. D. (2008).
Surface Radiation Dose and Radionuclide
Measurement in Ex-Tin Mining Area, Kg Gajah Perak. The Malaysian Journal of Analytical Science, 12: 419-431.
8.
Brady, N.C. (1984). The Nature and Properties of Soils, 9. Macmillan Publishing Co., New York, 750.
9.
Avnimelec. Y, Ritvo. G, Meijer. L. E, & Kochba. M. (2001). Water content, organic carbon and dry bulk density
in flooded sediments. Aquacultural
Engineering 25: 2533.
10.
Opreanu. G. (2003). Porosity, density and other physical
properties of deep sea sediment from the black sea. National Institute of
Marine Geology and Geo-ecology Modern and Ancient Fluvial, Deltaic and Marine
Environments and Processes Proceedings of Euro-EcoGeoCentre-Romania:
GEO-ECO-MARINA 9-10/2003-2004.
11.
Molinari
& Snodgrass. (1990). The chemistry and radiochemistry of radium and the
other elements of the uranium and thorium and natural decay series. The environmental Behaviour of Radium, 1.
Technical Report Series No.310 IAEA.
12.
Choy, C. C.,
Zaharuddin. A. & Mohamed, C. A. R. (2007). Vertical profile of 210Pb
in the sediment core in Kuala Selangor Malaysia. The Malaysian Journal of Analytical Science,
11: 274-279.
13.
Jetter, H. H. (2000). Determining the Ages of Recent
Sediments Using Measurements of Trace Radioactivity. Terra et Aqua, 78 : 21 28.
14.
Lauria, D. C., Almeida,
R. M. R., Godoy, J. M. O. & Sracek, O. (2002). On the high radium
concentrations and low pH values in ground waters of a Brazilian coastal
region. Radioactivity in the Environment (Proc. Conf. Monaco).
15.
Godoy, J.M., Lauria,
D.C., Godoy, M.L.D.P. & Cunha, R.P. (1994). Development of a sequential
method for the determination of 238U, 234U, 232Th,
230Th, 228Th, 228Ra, 226Ra, and 210Pb
in environmental samples. J. Radioanalyt.
Nucl. Chem: Articles, 182 (1)165169.
16.
Sanders, L. M., Sanders, C. J., Luiz-Silva, W., Machado, W. E.,
Silva-Filho, V. & Patchineelam. S.
R. (2010). Anthropogenic source assessment of 226Ra and 210Pb
in a sediment core from the Cubatao River estuary (SE Brazil), Journal of Radioanalytical and Nuclear
Chemistry, 287:729 732.
17.
Chung, Y. C & Chen, C. T. A. (2007). Natural and
Anthropogenics Radionuclides. Encyclopedia
of Life Support Systems (EOLSS), Eolss Publishers, Oxford, UK, ISBN:
978-1-905839-62-9 e-Book, 1 : 359-388.
18.
Tavakoly Sany, S. B., Salleh, A., Sulaiman, A. B., Sasekumar,
A., Tehrani, G. M. & Rezayi, M. (2012). Distribution, characteristic and
ecological risk of heavy metals in surface sediments of West Port, Malaysia. Environment Protection Engineering,
38(4): 139 155.
19.
Saat, A., Hamzah, Z., Abu Bakar, Z., Ahmad, Z. &Wood, A.
B. (14 15 March 2009). Applicability of Pb-210 method for ages and
sedimentation study of a recent freshwater ex-minig lake. Conferences on
Scientific & Social Research (CSSR), paper number: 5281121.
20.
Hamzah, Z., Abdul Karim, U. K. & Saat, A. (2012).
Measurement of natural radioactivity level in surface sediment in southern
Kuala Selangor coastal area. Malaysian
Journal of Fundamental and Applied Sciences, 8:266 270.
21.
Yii, M.W., Wan Mahmood, Z., , Ahmad, Z, Md. Jaffary, N. A. I.
& Ishak, K. (2011). NORM activity concentration in sediment cores from the
Peninsular Malaysia East Coast Exclusive Economic Zone. Journal of Radioanalytical and Nuclear Chemistry, 289: 653-661.
22.
Omar M., Ibrahim M.Y., Hassan A., Mahmood C.S &
Sharifuddin M. A. (1991). Aras Sinaran
dan Keradioaktifan Alam Sekitar di Malaysia, Seminar Kebangsaan IRPA sektor
strategik.
23.
Turekian, K. K.; Wedepohl, K. H. (1961). Distribution of the
elements in some major units of the earths crust. Geol. Soc. Am. Bull., 72 : 175 192.
24.
Ismail, A. K., Ahmad, Z., Mohamed, N. & Yii, M. W. (2327
April 2007). Proceeding International Conference on Environmental
Radioactivity, International Atomic Energy Agency, Vienna, 255.
25.
Ahmad, Z., Ishak, A. K. & Yii M. W. (2007). Marine
Environment Related Activities in Malaysia Using Nuclear Technologies. Country Report Malaysia. Industrial
Technology Division, Malaysian Institute for Nuclear Technology Research
(MINT).
26.
Yii, M. W., Ahmad, Z. & Ishak, A. K. (2009). Distribution of
natural occurring radionuclides activity concentration in East Malaysia marine
sediment. Applied
Radiation and Isotopes, 67: 630-635.
27.
Li, D. M., Xu, M. Q., Liu, G. S. & Li, C. (2007).
Distribution of radioisotopes in sediment cores from nearshore off
Xinghua Baymouth, Fujian, China. Journal
of Radioanalytical and Nuclear Chemistry, 273: 151-155.
28.
UNSCEAR (1993). Sources and effects of ionizing radiation.
Report of the United Nations Scientific
Committee on the Effects of Atomic Radiation to the General Assembly, with Scientific Annexes,
United Nations, New York, USA.