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皮埃蒙特塞尔沃岩体岩石中的天然放射性核素。

Natural radionuclides in the rocks of the Valle del Cervo Pluton in Piedmont.

作者信息

Sesana Lucia, Fumagalli Marco, Carnevale Mauro, Polla Giancarla, Facchini Ugo, Colombo Annita, Tunesi Annalisa, De Capitani Luisa, Rusconi Rosella

机构信息

Istituto di Fisica Generale Applicata, Università degli Studi di Milano, Via G. Celoria, 16-20133 Milano, Italy.

出版信息

Radiat Prot Dosimetry. 2006;118(3):337-44. doi: 10.1093/rpd/nci347. Epub 2006 Jan 12.

Abstract

Monitoring of the gamma radiation in Valle del Cervo Pluton was performed by determining U and Th contents in the main rock types cropping out over the entire area and pertaining to the granitic complex, syenitic complex and monzonitic complex. In particular, syenitic rocks were largely used as building and ornamental materials (e.g. Sienite della Balma). All the samples are fresh and do not present joints or fractures filled with U minerals. In the crushed samples the activity of uranium varies from 346 to 764 Bq/kg. Concentration of thorium varies from 202 to 478 Bq/kg. For all the analysed rocks uranium activity is higher than thorium one. The lowest value of radioactive concentration is referred to rocks of the granitic complex. The most active rocks are syenites. The data confirm the high activities of Valle del Cervo rock types, strongly connected with high K content of the source magma (geochemical signature); on the contrary, the activity seems to be not related to the location of the samples.

摘要

通过测定出露在整个区域且属于花岗岩杂岩、正长岩杂岩和二长岩杂岩的主要岩石类型中的铀和钍含量,对塞尔沃谷岩体的伽马辐射进行了监测。特别是,正长岩被大量用作建筑和装饰材料(例如巴尔马正长岩)。所有样品均为新鲜的,不存在充填有铀矿物的节理或裂缝。在粉碎后的样品中,铀的活度在346至764贝克勒尔/千克之间变化。钍的浓度在202至478贝克勒尔/千克之间变化。对于所有分析的岩石,铀的活度高于钍的活度。放射性浓度的最低值出现在花岗岩杂岩的岩石中。放射性最强的岩石是正长岩。数据证实了塞尔沃谷岩石类型的高放射性,这与源岩浆的高钾含量(地球化学特征)密切相关;相反,放射性似乎与样品的位置无关。

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