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Analysis of specific radionuclides activity variations in soil within geotectonic units of Republic of North Macedonia

机译:北马其顿共和国大地构造单元内土壤中特定放射性核素活度变化的分析

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To establish baseline values for concentrations of terrestrial radionuclides for the Republic of North Macedonia, a survey covering the entire territory was performed. The 213 soil samples were collected from regions around the major settlements and cities, approximately evenly distributed over the geotectonic units which constitute the country's geological foundation. The specific activities of radionuclides were measured by gamma spectrometry. The following geometric mean values and geometric standard deviations were obtained: 550 Bqkg–1 (1.47) for 40K, 37 Bqkg–1 (1.53) for 226Ra, 38 Bqkg–1 for 238U, and 38 Bqkg–1 (1.53) for 232Th in dry soil. The relation between specific activities of natural radionuclides and geology was investigated. Correlation between radionuclides, which may serve as additional geochemical indicators, and geology could not be found convincingly. Mutual correlations between 226Ra, 238U, and 232Th activities were found to be high (Spearman ρ about 0.8), whereas the ones between these and 40K are a bit lower, somewhat above ρ= 0.6.
机译:为了确定北马其顿共和国陆地放射性核素浓度的基线值,进行了覆盖整个领土的调查。从主要定居点和城市周围的地区收集了213个土壤样品,这些样品大致均匀地分布在构成该国地质基础的大地构造单元上。放射性核素的比活度通过γ光谱法测定。获得以下几何平均值和几何标准偏差:40K 550 Bqkg-1(1.47),226Ra 37 Bqkg-1(1.53),238U 38 Bqkg-1(232B)和38 Bqkg-1(1.53)。干燥的土壤。研究了天然放射性核素比活度与地质之间的关系。不能令人信服地发现放射性核素之间的相关性(可以用作其他地球化学指示剂)与地质之间的相关性。发现226Ra,238U和232Th活性之间的相互相关性很高(Spearmanρ约为0.8),而这些和40K之间的相互相关性较低,略高于ρ= 0.6。

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