Abstract

Uranium, perhaps the most strategically important component of heavy minerals, finds particular significance in the nuclear industry. In prospecting trenches, the radioactivity of 238U and 232Th provides a good signature of the presence of heavy minerals. In the work herein, the activity concentrations of several key primordial radionuclides (238U, 232Th, and 40K) were measured in prospecting trenches (each of the latter being of approximately the same geometry and physical situation). All of these are located in the Seila area of the South Eastern desert of Egypt. A recently introduced industry standard, the portable hand-held RS-230 BGO gamma-ray spectrometer (1024 channels) was employed in the study. Based on the measured data, the trenches were classified as either non-regulated (U activity less than 1000 Bq kg-1) or regulated (with 238U activity more than 1000 Bq kg-1). Several radiological hazard parameters were calculated, statistical analysis also being performed to examine correlations between the origins of the radionuclides and their influence on the calculated values. While the radioactivity and hazard parameters exceed United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) guided limits, the mean annual effective doses of 0.49 and 1.4 mSv y-1 in non-regulated and regulated trenches respectively remain well below the International Commission on Radiological Protection (ICRP) recommended 20 mSv/y maximum occupational limit. This investigation reveals that the studied area contains high uranium content, suitable for extraction of U-minerals for use in the nuclear fuel cycle.

Highlights

  • The radioactivity of the living environment is contributed to by terrestrial and extra-terrestrial sources

  • The Seila region in Egypt is considered as a potential area for exploration of heavy minerals, the prospecting trenches were drilled following some geological and radioactive studies

  • Present study forms an interest of measuring the concentrations of terrestrial radionuclides in some non-regulated and regulated trenches in this area

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Summary

Introduction

The radioactivity of the living environment is contributed to by terrestrial and extra-terrestrial sources. Terrestrial natural radionuclides (238U, 232Th and their progeny, and 40K) exist in all ground formations, forming the main sources of external gamma radiation exposure to humans [1,2,3]. Extra-terrestrial sources such as cosmogenic radionuclides (36Cl, 32Si, 26Al, 14C, 10Be, 7Be and 3H) exist at trace levels, forming a minor part of radiation exposure to humans, albeit at levels varying with altitude and location. Elevated levels of environmental radiation are contributed to by igneous rocks such as granite, with lower levels typically being associated with sedimentary rocks. Both are used as essential raw materials for building material purposes, landfill etc. The presence of terrestrial radionuclides in raw materials used for constructional intent may pose radiation risks within the living environment [5]

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