2023
DOI: 10.1016/j.apradiso.2023.110716
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Measurement of radioactivity levels and determination of radiological hazard risks in areas of irrigated vegetable agriculture soils Southwestern Lake Hawassa, Sidama Region, Ethiopia

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Cited by 3 publications
(1 citation statement)
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“…Natural radioactive isotope values are determined by the physical, chemical, and biological properties of the soil. Natural radioactive isotopes are increased by rainfall, different types of cultivated plants, soil management techniques, and the use of fertilizers [2]. The most important terrestrial radionuclides to consider are 238 U, 232 Th, and 40 K because they are abundant in the Earth's crust and have a long half-life [3].…”
Section: Introductionmentioning
confidence: 99%
“…Natural radioactive isotope values are determined by the physical, chemical, and biological properties of the soil. Natural radioactive isotopes are increased by rainfall, different types of cultivated plants, soil management techniques, and the use of fertilizers [2]. The most important terrestrial radionuclides to consider are 238 U, 232 Th, and 40 K because they are abundant in the Earth's crust and have a long half-life [3].…”
Section: Introductionmentioning
confidence: 99%