Abstract

A study of terrestrial gamma radiation (TGR) dose rate was conducted in west of Sarawak, covering Kuching, Samarahan, Serian, Sri Aman, and Betong divisions to construct a baseline TGR dose rate level data of the areas. The total area covered was 20,259.2 km 2 , where in-situ measurements of TGR dose rate were taken using NaI(Tl) scintillation detector Ludlum 19 micro R meter NaI(Tl) approximately 1 meter above ground level. Twenty-nine soil samples were taken across the 5 divisions covering 26 pairings of 9 geological formations and 7 soil types. A hyperpure Germanium detector was then used to find the samples’ 238 U, 232 Th, and 40 K radionuclides concentrations producing a correction factor C f = 0.544. A total of239 measured data were corrected with Cf resulting in a mean Dm of 47 ± 1 nGy h -1 , with a range between 5 nGy h -1 - 103 nGy h -1 . A multiple regression analysis was conducted between geological means and soil types means against the corrected TGR dose rate Dm, generating D g,s = 0.847Dg+ 0.637Ds- 22.313 prediction model with a normalized Beta equation of D g,s = 0.605D g + 0.395 D s . The model has an 84.6% acceptance of Whitney- Mann test null hypothesis when tested against the corrected TGR dose rates.

Highlights

  • IntroductionHumans are bombarded with natural gamma radiation daily (IAEA, 1989), originating from solar radiation and terrestrial gamma radiation of geological background and soil (UNSCEAR, 2000)

  • Humans are bombarded with natural gamma radiation daily (IAEA, 1989), originating from solar radiation and terrestrial gamma radiation of geological background and soil (UNSCEAR, 2000).Radionuclides that have long half-lives that are formed during the formation of stars make up trace parts of today’s geological background (Valkovic, 2000) contributing to varying levels of gamma radiation

  • This study focuses on terrestrial gamma radiation of west Sarawak, covering 5 divisions, Kuching, Samarahan, Serian, Sri Aman, and Betong, and explores the relationship between gamma radiation dose rates with geological background and soil types of the areas

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Summary

Introduction

Humans are bombarded with natural gamma radiation daily (IAEA, 1989), originating from solar radiation and terrestrial gamma radiation of geological background and soil (UNSCEAR, 2000). Radionuclides that have long half-lives that are formed during the formation of stars make up trace parts of today’s geological background (Valkovic, 2000) contributing to varying levels of gamma radiation. These are naturally occurring radionuclides called primordial radionuclides. This study focuses on terrestrial gamma radiation of west Sarawak, covering 5 divisions, Kuching, Samarahan, Serian, Sri Aman, and Betong, and explores the relationship between gamma radiation dose rates with geological background and soil types of the areas

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