The Effect of Grain Size on Radon Exhalation Rate in Soil Samples of Dera Ismail Khan in Pakistan
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Keywords

 Radon concentration, Radon exhalation rate, grain size, soil texture.

How to Cite

Tabassum Nasir, & Nisar Ahmad. (2021). The Effect of Grain Size on Radon Exhalation Rate in Soil Samples of Dera Ismail Khan in Pakistan. Journal of Basic & Applied Sciences, 8(2), 430–436. https://doi.org/10.6000/1927-5129.2012.08.02.29

Abstract

Radon concentration and its exhalation rate has been measured from twenty five soil samples collected from seven different locations of Dera Ismail Khan, in the north west of Pakistan. These samples were crushed after drying and passed through sieves with different sizes of pores to get three grain sizes, £0.595 mm, 0.595-2.00 mm and 2.00-4.00 mm of soil. CR-39 based NRPB (National Radiological Protection Board) radon dosimeters have been used to measure the radon concentration and exhalation rates. The maximum average value of radon exhalation rate has found to be: (3.57±0.38) Bq m-2 hr-1 in the samples having grain size 2.00-4.00 mm and the minimum as: (2.21±0.26) Bq m-2hr-1, in the samples with grain size £ 0.0595 mm. This indicates that the radon exhalation rate increases with the grain size. The maximum average value of radon exhalation rate has been found in samples collected from river side where soil texture is silty clay loam. The obtained values of radon exhalation rate for all the samples are well below the world average value of 57.60 Bq m-2 hr-1.

https://doi.org/10.6000/1927-5129.2012.08.02.29
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References

Faheem M, Rahman SU, Nasir T, Rahman S, Matiullah. Assessment of lung cancer risk using weighted average indoor radon levels in six districts of the Punjab province in Pakistan. Indoor Built Environ 2010; 19(3): 382-90. http://dx.doi.org/10.1177/1420326X10367311

Shweikani R, Giaddai TG, Durrani SA. The effect of soil parameters on the radon concentration values in the environment. Radiat Meas 1995; 25: 581-84. http://dx.doi.org/10.1016/1350-4487(95)00188-K

Toxological Profile for radon, Agency for Toxic Substances and Disease Registry, 1990. U.S. Public Health Service, In collaboration with U. S. Environmental Protection Agency.

Durrani SA, Ilic R. Radon Measurements by Etch Track Detectors. World Scientific Publishing, Singapore 1997.

Bunzl K, Ruckerbaner F, Winkler R. Temporal and Small Scale Spatial Variability of 222Rn gas in a soil with a high gravel content. Sci Total Environ 1998; 220: 158-66. http://dx.doi.org/10.1016/S0048-9697(98)00256-3

Winkler R, Ruckerbaur F, Bunzl K. Radon concentration in soil gas: a comparison of the variability resulting from different method, spatial heterogeneity and seasonal fluctuations. Sci Total Environ 2001; 272: 273-82. http://dx.doi.org/10.1016/S0048-9697(01)00704-5

Graaf Van der ER, Witteman GAA, Spoel Van der WH, Andersen CE, Meijer de RJ. Measurements on, and modeling of diffusive and advective radon Transport in soil. Radiat Port Dosim 1994; 56: 167-70.

Rafique M, Qayyum S, Rahman S, Matiullah. The Influence of Geology on Indoor Radon Concentrations in Neelum Valley Azad Kashmir, Pakistan Indoor and Built Environment 1420326X11434181, first published on April 5, 2012 as doi:10.1177/1420326X11434181.

Jong Ede, Acton DF, Kozak LM. Naturally occurring gamma-emitting isotopes, radon release and properties of parent material of Saskatchewan Soils. Can J Soil Sci 1993; 74: 47-53.

Sun K, Guo Q, Zhuo W. Feasibility for mapping radon exhalation rate from soil in China. J Nucl Sci Technol 2004; 41: 86-90. http://dx.doi.org/10.1080/18811248.2004.9715462

Reimer GM, Gundersen LCS. A direct correlation among indoor Rn, soil gas Rn and geology in the reading prong near Boyertown, Pennsylvania. Health Phys 1989; 57 (1): 155-60.

LaBrecque JJ. Simple and rapid methods for on-site determination of radon and thoron in soil-gases for seismic studies. J Radiol Nucl Chem 2002; 254 (3): 439-44. http://dx.doi.org/10.1023/A:1021673601593

Rafique M, Rahman SU, Mahmood T, Rahman S, Matiullah, Rehman SU. Radon exhalation rate from soil, sand, bricks, and sedimentary samples collected from Azad Kashmir, Pakistan. Russian Geol Geophys 2011; 52(4): 450-57. http://dx.doi.org/10.1016/j.rgg.2011.03.007

Rehman S, Matiullah, Rahman S. Studing 222Rn exhalation rate from soil and sand samples using CR-39 detector. Radiat Meas 2006; 41(6): 708-13. http://dx.doi.org/10.1016/j.radmeas.2006.03.005

Faheem M, Matiullah. Radon exhalation and its dependence on moisture content from samples of soil and building materials. Radiat Meas 2008; 43: 1458-62. http://dx.doi.org/10.1016/j.radmeas.2008.02.023

Siddiqui S, Ali W, Khan M, Latif K, Abbass M, Mohmand H. Soil Erosion: Problem and Solutions of D. I. Khan 2010.

Howarth CB, Miles JCH. Results of the 2002 NRPB inter- comparison of passive radon detectors 2002. NRPB-W44, Chilton.

Report of the United Nations Scientific Committee on the Effects of Atomic Radiation to the General Assembly. UNSCEAR 2000. ANNEX B Exposures from natural radiation sources.