Abstract

Human beings are persistently exposed to ionizing radiation caused by terrestrial, extra-terrestrial and anthropogenic radionuclides. In order to assess the risks associated with exposure due to the natural radioactivity in soil, a radiological environmental monitoring survey was carried out in district Chakwal. In the present study, activities of 226Ra, 232Th and 40K are measured in soil samples using an HPGe based gamma spectrometry system. The measured mean specific radioactivity concentration of 226Ra, 232Th and 40K in the studied samples was 31.08 ± 1.2 Bqkg-1, 47.67 ± 2.30 Bqkg-1 and 558.23 ± 17.52 Bqkg-1, respectively. From the measured activity concentration, radium equivalent activity, external and internal hazard indices, terrestrial absorbed dose and annual effective dose were calculated. Mean radium equivalent activity (Raeq), outdoor radiation hazard index (Hex), indoor radiation hazard index (Hin) and absorbed dose rate (D) for the area under study were determined as 142.18 Bqkg-1, 0.38, 0.47 and 66.13 nGyh-1 respectively. The annual effective dose equivalent (AEDE) varied in the range from 0.10 mSv y-1 to 0.16 mSv y-1. On the basis of measured activity and calculated values of hazards indices, it is concluded that the surveyed area does not pose any significant radiological risk to the population and environment.

Highlights

  • Occurring radioactive materials are ubiquitous on earth and their radioactivity may become concentrated in certain region/area as a result of human activities

  • The activity of 226Ra, 232Th and 40K in the soil samples have been calculated by High Purity Germanium (HPGe)

  • Gamma dose rates were calculated by using the formula given below: D = 0.427CRa + 0.662CTh + 0.043CK

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Summary

Introduction

Occurring radioactive materials are ubiquitous on earth and their radioactivity may become concentrated in certain region/area as a result of human activities. Natural radiation at the earth’s surface consists of two components, namely cosmic and terrestrial radiation. Terrestrial radiation mainly originates from the primordial radioactive nuclides originated in the early stage of the formation of the solar system. Thorium and potassium are the main elements contributing to natural terrestrial radioactivity. It is an established fact that radioactivity in the soil adds to the background level of radiation and human beings are exposed. The level of contribution to the background radiation depends on the concentration of the radioactive materials in the soil but this amount may vary from area to area [1,2,3]

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