Abstract
Mining of kaolin deposits are common in Nigeria without considering the background radiation in such environment and the health risks it might pose on the miners. In this study, in-situ measurements of the naturally occurring radionuclides were carried out with the aim of determining the distribution of these radionuclides on the mining field and estimation of the hazard indices exposure risks (γ- and α-radiation risks) to the miners. The study was achieved with the aid of gamma ray detector Super-Spec (RS-125) and global positioning system. The detector used has ability to measure activity concentrations of 238U, 232Th and 40K and gamma doses. For the purpose of this study, only the concentrations of the three radionuclides were considered. For each location, measurements were taken four times, while its mean value was estimated for better accuracy. In all, nineteen locations were occupied in order to cover the study area. Basic kriging method was adopted for the production of spatial distribution of these radionuclides and their corresponding γ- and α-radiation hazard indices. The mean values of 238U, 232Th and 40K are 46.7, 71.8 and 108.7 Bq kg−1, respectively. When compared to the global standard, it was revealed that 238U and 232Th are greater than the global standard, while 40K fall below the permissible limit. The γ- and α-radiation exposure risks estimated revealed that the mean values of Iγ and Iα are 0.6 and 0.2 respectively. Though the estimated γ- and α-radiation indices showed that the kaolin field is safe for the miners, periodic check is required in order to monitor the rate at which these natural primordial radionuclides (238U and 232Th and their progenies) are being enhanced.
Highlights
The occurrence and distribution of radionuclides in soils is a function of the radionuclides’ compositions in their parent rocks [1]
Mining of kaolin deposits are common in Nigeria without considering the background radiation in such environment and the health risks it might pose on the miners
When compared to the global standard, it was revealed that 238U and 232Th are greater than the global standard, while 40K fall below the permissible limit
Summary
The occurrence and distribution of radionuclides in soils is a function of the radionuclides’ compositions in their parent rocks [1]. Enhancement or depletion of natural radionuclides have been recorded [2,3]. Effects of overexposure to these natural radionuclides have been documented by [7], [8], [9], [10] and [11]. Among these effects are cancers of various forms, hepatic, leukaemia, lung diseases, bone tumours and so on
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