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洞穴陨石中的宇宙成因放射性核素:伽马射线测量和探测效率模拟。

Cosmogenic radionuclides in the Cavezzo meteorite: Gamma-ray measurement and detection efficiency simulations.

机构信息

Universitá degli Studi di Torino, Via Pietro Giuria 1, Torino, 10125, Italy.

Universitá degli Studi di Torino, Via Pietro Giuria 1, Torino, 10125, Italy; INAF - Osservatorio Astrofisico di Torino, Via Osservatorio, 20, Pino Torinese (TO), 10025, Italy.

出版信息

Appl Radiat Isot. 2023 Apr;194:110651. doi: 10.1016/j.apradiso.2023.110651. Epub 2023 Jan 10.

DOI:10.1016/j.apradiso.2023.110651
PMID:36696750
Abstract

The Cavezzo meteorite was recovered on January 4, 2020, just three days after the fall observed over Northern Italy by the all-sky cameras of the Italian PRISMA fireball network. Two specimens, weighing 3.1 g (F1) and 52.2 g (F2), were collected in the predicted strewn-field and the meteorite has been classified as an L5 anomalous chondrite. The gamma-activity of the F2 sample was measured at the Monte dei Cappuccini underground Research Station (Torino, Italy) with a large-volume HPGe-NaI(Tl) spectrometer. Thanks to the high efficiency, selectivity, and low background of the spectrometer, we were able to detect fifteen cosmogenic radioisotopes. The presence of nuclides with half-lives down to a few days (Ca, Mn, and V) undoubtedly confirmed the recent fall of the sample. The very low activity of Ti and Co was revealed with a particular coincidence between the HPGe and NaI(Tl) detectors. To obtain the detection efficiency, we have simulated the response of the detector with the GEANT4 toolkit, once the spectrometer's dead layer thickness was estimated using standards of known activity. Moreover, the simulation of the Dhajala meteorite (H3/4 chondrite) measurement allowed us to verify that the self-absorption of the sample is correctly taken into account and validate our simulations. In this contribution, we focus on the coincidence optimization techniques and the detection efficiency computation.

摘要

卡韦佐陨石于 2020 年 1 月 4 日被回收,就在意大利北部被意大利 PRISMA 火球网络的全景摄像机观测到陨石坠落的三天后。在预测的散落场中收集了两个标本,重量分别为 3.1 克(F1)和 52.2 克(F2),陨石被归类为 L5 异常球粒陨石。在意大利都灵的蒙特 dei Cappuccini 地下研究站(Monte dei Cappuccini underground Research Station),用一个大体积的 HPGe-NaI(Tl)谱仪测量了 F2 样本的伽马活性。由于谱仪的高效率、选择性和低本底,我们能够探测到十五种宇宙成因放射性核素。半衰期短至几天的核素(Ca、Mn 和 V)的存在无疑证实了样本的近期坠落。Ti 和 Co 的非常低的活度与 HPGe 和 NaI(Tl)探测器之间的特别巧合有关。为了获得探测效率,我们使用 GEANT4 工具包模拟了探测器的响应,同时使用已知活度的标准估计了谱仪的死层厚度。此外,对 Dhajala 陨石(H3/4 球粒陨石)测量的模拟允许我们验证对样品的自吸收的正确考虑,并验证我们的模拟。在本研究中,我们重点关注符合优化技术和探测效率的计算。

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