Measurements of Radioactivity Concentrations in Granites and Sedimentary- Rocks and their Leaching Components in Egyptian Deserts

Salha D. Y. Alsaadi, J. M. Ali, Areej Hazawi, A. M. Al-Abrdi
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Abstract

Concentrations of radionuclides in sediments and granite samples were determined by γ- ray spectrometer using High Pure Germanium Detector; HPGe, with a specially designed shield. Six different rock samples were collected from different sites: four samples of sediments from Um Bogma southwest Sinai, and two granite samples from Gabal Gattar, the northern part of the East- ern Desert of Egypt, where all samples were subject to investigation. Their samples were selected because the activity before being dissociated in sulfuric acid was less than after dissociation. The samples were dissolved in sulfuric acid with the same parameters of solid to liquid ratio; S/L, acid concentration, and leaching time. After the leaching process, the pregnant solution was separated from the residual, and the latter was dried. The two units, named the pregnant solutions and residu- als, were also measured radiometrically using the HPGe detector to determine the activity concen- trations (Bq/kg) of the different radionuclides of the six samples. The results showed that the rela- tion between the sum of activities of both pregnant solutions and residuals with the originals have different categories. In the sediment samples; the activity of solution+ residual was 72.37% from the original of siltstone, the activity of solution + residual was 90.02% from the original claystone sample, the activity of solution + residual was 92.6% from the original of shale, the activity of solu- tion + residual was 74.07% from the original claystone. In the granite samples, the activity of solu- tion + residual was 130.39% from the original of the first granite sample and 142.3% from the orig- inal of the second granite sample. This phenomenon varied in magnitude due to the different radio- nuclides in each sample. These variations depend mainly on the nature of the grain surfaces in the different rock types and their Pb content. As for leachability analysis, leaching experiments have been performed using sulfuric acid. The leaching efficiency (%) of uranium is estimated by the measurements of the HPGe detector. The result showed almost constant values for leachability. The non-frequent appearance of attenuation of gamma activities during leaching processes indicates that the acid solutions may have led to clean the grain surfaces and thus permit gamma activities of the inner grains to be measured. The treatment of the samples before measurements may have been needed.
埃及沙漠中花岗岩和沉积岩及其浸出成分中放射性浓度的测量
用高纯锗探测器γ射线谱仪测定了沉积物和花岗岩样品中放射性核素的浓度;HPGe,带有特殊设计的护罩。从不同的地点收集了六种不同的岩石样本:四个样本来自西奈西南部的Um Bogma沉积物,两个样本来自埃及东部沙漠北部的Gabal Gattar花岗岩样本,所有样本都被调查。选择他们的样品是因为在硫酸中解离前的活性低于解离后的活性。在相同的料液比参数下,将样品溶解于硫酸中;S/L,酸浓度,浸出时间。浸出过程结束后,将孕液与残液分离,残液干燥。用HPGe检测仪测定了6个样品中不同放射性核素的活度浓度(Bq/kg),分别命名为妊娠液和残余物。结果表明,两种孕液的活度和残差与原溶液的关系有不同的范畴。在沉积物样本中;原始粉砂岩的溶液+残余物活度为72.37%,原始粘土岩样品的溶液+残余物活度为90.02%,原始页岩样品的溶液+残余物活度为92.6%,原始粘土岩样品的溶液+残余物活度为74.07%。在花岗岩样品中,溶液+残余物的活度分别为第1样品的130.39%和第2样品的142.3%。这种现象的大小因每个样品中放射性核素的不同而不同。这些差异主要取决于不同岩石类型的颗粒表面性质及其Pb含量。在可浸性分析方面,进行了硫酸浸出试验。铀的浸出效率(%)是通过高温锗探测器的测量来估算的。结果表明,浸出率几乎是恒定的。在浸出过程中伽马活度衰减的不频繁出现表明,酸溶液可能导致颗粒表面清洁,从而允许测量内部颗粒的伽马活度。可能需要在测量前对样品进行处理。
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