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Natural radioactivity in granites and gneisses of the Opava Mountains (Poland): a comparison between laboratory and in situ measurements

机译:Opava山(波兰)的花岗岩和片麻岩中的天然放射性:实验室测量与原位测量之间的比较

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摘要

The natural radioactivities of five characteristic igneous rocks of the eastern foreland of the Opava Mountains (Eastern Sudetes, Poland), obtained in the laboratory and under in situ conditions, are presented. The activity concentrations of 232Th, 238U, and 40K were measured using an HPGe gamma-ray spectrometry system. The ranges of the activity concentrations of 232Th were 7–71 Bq kg−1 in the laboratory and 6–68 Bq kg−1 for the in situ measurements. For 238U, the ranges of the activity concentrations were 5–52 Bq kg−1 in the laboratory and 9–48 Bq kg−1 for the in situ measurements, and for 40K, the ranges were 520–1560 Bq kg−1 in the laboratory and 537–1700 Bq kg−1 for the in situ measurements. These determined activity concentrations were compared with the average activity concentrations of the radionuclides in similar types of rocks and with data from the Sudetes available in the literature. No significant differences were found between the in situ and laboratory measurements.
机译:介绍了在实验室和现场条件下获得的奥帕瓦山脉东部前陆(东苏德特斯,波兰)的五种特征性火成岩的自然放射性。使用HPGeγ射线光谱系统测量 232 Th, 238 U和 40 K的活性浓度。实验室中 232 Th的活动浓度范围为7–71 Bq kg -1 ,而6–68 Bq kg -1 原位测量。对于 238 U,实验室中的活动浓度范围为5–52 Bq kg -1 和9–48 Bq kg -1 对于原位测量,对于 40 K,实验室范围为520-1560Bq kg -1 ,范围为537-1700Bq kg -1 < / sup>用于原位测量。将这些确定的活度浓度与相似类型岩石中放射性核素的平均活度浓度进行比较,并与文献中提供的Sudetes数据进行比较。在现场测量和实验室测量之间未发现明显差异。

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