The
Malaysian Journal of Analytical Sciences Vol 12 No 1 (2008): 160 – 166
AKTIVITI 226Ra DAN 228Ra
PADA PERMUKAAN SEDIMEN BAGAN LALANG, SELANGOR
Che Abd Rahim Mohamed1, Zaharuddin Ahmad2 dan Nioo
Siew Yew2
1Pusat Pengajian Sains Sekitaran Dan Sumber Alam, Fakulti Sains Dan Teknologi,
Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor,
Malaysia
2Agensi Nuklear Malaysia,
Bangi, 43000 Kajang,
Selangor, Malaysia
Abstract
Six stations had
selected from Sungai Sepang Kechil, Selangor during Mac, September and October
2004 for sediment analysis. The results
showed a significant difference among the 226Ra and 228Ra
activities (P < 0.01) with sampling period. The highest activities of 226Ra
and 228Ra have obtained during the sampling on Mac, which show the average activities 161.30
Bq kg-1 and 466.88 Bq kg-1,
respectively. Meanwhile, 226Ra activities obtained on September and
October are in the average of 24.77 Bq kg-1 and 69.22 Bq kg-1, respectively.
Average activities of 228Ra are 73.13 Bq kg-1 and 1284.58
Bq kg-1, respectively for September and October. Northeast Monsoon
effect might cause the higher activities of
radium isotopes during sampling on Mac. Sediments from Bagan Lalang are
sandy type with a limited size variation. Furthermore, radium isotopes are more
adsorbed on the particles sediments between size 63 – 125 µm, which usually
rich in alkaline feldspar.
Key words: 226Ra, 228Ra, sediment
References
1. Kim, Y.J., Kim, C.K., Kim, C.S., Yun, J.Y., Rho, B.H. 1999. Determination of 226Ra
in environmental samples using
high-resolution inductively coupled plasma mass spectrometry. J.
Radioanal. Nucl. Chem. 240: 613-618.
2. Nour,
S., El-Sharkawy, A., Burnett, W.C.,
Horwitz, E.P. 2004. Radium-228
determination of natural
waters via concentration on manganese dioxide and separation
using Diphonix ion exchange resin. Appl. Radiat. Isot. 61:1173 - 1178.
3. Eikenberg, J., Tricca,
A., Vezzu, G., Stille, P., Bajo,
S., Ruethi, M. 2001. 228Ra/226Ra/224Ra and
87Sr/86Sr
isotope relationships for determining interactions
between ground and river water in the upper Rhine
Valley. J. Environ.
Radioact. 54: 133-162.
4. Rama,
Moore, W.S. 1996. Using the radium
quartet to estimate
water exchange and ground
water input
in salt marshes. Geochim. Cosmochim. Act. 60:
4645 - 4652.
5. Dharmender, S. 2003. Rare sights at Bagan Lalang. http://www.allmalaysia.info/news/story.
(17 Januari 2005).
6. Sepang
Gold Coast dan Sepang
Water City. (atas talian) http://www.pnsb.com.my/n_jan03.htm. (17 Januari
2005).
7. DiToro, D.M. 1999. Sediment Flux Modelling. New York: John Wiley & Sons.
8. Pethick, J. 1984.
An introduction to coastal geomorphology. London: Edward Arnold.
9. Zhang,
C., Wang, L., Li, G., Dong, S., Yang, J., Wang, X. 2002. Grain size effect on multi-element concentrations in sediments from
the
intertidal flats of Bohai Bay, China. Appl.
Geochem. 17: 59-68.
10. Gotze,
J. 1998. Geochemistry and provenance of the Atlendrof feldspathic sandstone
in the Middle Bunter of the
Thuringian basin (Germany). Chemical Geol. 150: 43-61.