Thoron activity concentration in Malaysian soil gas: geogenic impact assessment

Given the rather short half-life of thoron (220Rn), at 56 s, its contribution to radiation exposure is often overlooked. Nevertheless, in a thorium (232Th) rich environment potential hazard does exist, in particular regarding prolonged duration exposures to 220Rn and its short-lived alpha-particle e...

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Main Authors: Nuhu, Habila, Hashim, Suhairul, Mohd. Sanusi, Mohamad Syazwan, Ghoshal, Sib Krishna, Bradley, David A.
Format: Article
Published: Elsevier Ltd 2022
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Online Access:http://eprints.utm.my/103900/
http://dx.doi.org/10.1016/j.radphyschem.2022.110303
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spelling my.utm.1039002023-12-04T07:51:31Z http://eprints.utm.my/103900/ Thoron activity concentration in Malaysian soil gas: geogenic impact assessment Nuhu, Habila Hashim, Suhairul Mohd. Sanusi, Mohamad Syazwan Ghoshal, Sib Krishna Bradley, David A. QC Physics Given the rather short half-life of thoron (220Rn), at 56 s, its contribution to radiation exposure is often overlooked. Nevertheless, in a thorium (232Th) rich environment potential hazard does exist, in particular regarding prolonged duration exposures to 220Rn and its short-lived alpha-particle emitting progeny [polonium (216Po)]. Herein, concerning the geology and major soil types in the Malaysian state of Perak, an activity concentration map has been established for 220Rn in soil gas, with the use made of a RAD7 detector and the THORON protocol for in-situ measurements. The detector has been coupled to a soil probe driven to a depth of 0.8 m. The activity concentration of 220Rn in the soil ranged from undetectable to 563 kBq m−3 with a mean value of 38 ± 11 kBq m−3. Granite and Triassic-Jurassic formations in the region showed more elevated 220Rn activity while Quaternary and Silurian formations revealed low 220Rn values. Moreover, while elevated 220Rn activity concentrations were found in peat, riverine, and granite source soils, the activity concentrations in marine and other soils were low. A primary map of 220Rn in the soil gas has been developed based on geogenic impact assessment, with a greater 220Rn activity concentration in the central part of the state. Elsevier Ltd 2022-11 Article PeerReviewed Nuhu, Habila and Hashim, Suhairul and Mohd. Sanusi, Mohamad Syazwan and Ghoshal, Sib Krishna and Bradley, David A. (2022) Thoron activity concentration in Malaysian soil gas: geogenic impact assessment. Radiation Physics and Chemistry, 200 (NA). pp. 1-6. ISSN 0969-806X http://dx.doi.org/10.1016/j.radphyschem.2022.110303 DOI:10.1016/j.radphyschem.2022.110303
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
topic QC Physics
spellingShingle QC Physics
Nuhu, Habila
Hashim, Suhairul
Mohd. Sanusi, Mohamad Syazwan
Ghoshal, Sib Krishna
Bradley, David A.
Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
description Given the rather short half-life of thoron (220Rn), at 56 s, its contribution to radiation exposure is often overlooked. Nevertheless, in a thorium (232Th) rich environment potential hazard does exist, in particular regarding prolonged duration exposures to 220Rn and its short-lived alpha-particle emitting progeny [polonium (216Po)]. Herein, concerning the geology and major soil types in the Malaysian state of Perak, an activity concentration map has been established for 220Rn in soil gas, with the use made of a RAD7 detector and the THORON protocol for in-situ measurements. The detector has been coupled to a soil probe driven to a depth of 0.8 m. The activity concentration of 220Rn in the soil ranged from undetectable to 563 kBq m−3 with a mean value of 38 ± 11 kBq m−3. Granite and Triassic-Jurassic formations in the region showed more elevated 220Rn activity while Quaternary and Silurian formations revealed low 220Rn values. Moreover, while elevated 220Rn activity concentrations were found in peat, riverine, and granite source soils, the activity concentrations in marine and other soils were low. A primary map of 220Rn in the soil gas has been developed based on geogenic impact assessment, with a greater 220Rn activity concentration in the central part of the state.
format Article
author Nuhu, Habila
Hashim, Suhairul
Mohd. Sanusi, Mohamad Syazwan
Ghoshal, Sib Krishna
Bradley, David A.
author_facet Nuhu, Habila
Hashim, Suhairul
Mohd. Sanusi, Mohamad Syazwan
Ghoshal, Sib Krishna
Bradley, David A.
author_sort Nuhu, Habila
title Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
title_short Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
title_full Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
title_fullStr Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
title_full_unstemmed Thoron activity concentration in Malaysian soil gas: geogenic impact assessment
title_sort thoron activity concentration in malaysian soil gas: geogenic impact assessment
publisher Elsevier Ltd
publishDate 2022
url http://eprints.utm.my/103900/
http://dx.doi.org/10.1016/j.radphyschem.2022.110303
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score 13.211869