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锆石中辐射反冲形成轨迹的原子级模拟。

Atomistic simulation of track formation by energetic recoils in zircon.

机构信息

Instituto de Fisica Gleb Wataghin, Universidade Estadual de Campinas, Campinas, SP, 13083-970, Brazil.

出版信息

J Phys Condens Matter. 2010 Oct 6;22(39):395008. doi: 10.1088/0953-8984/22/39/395008. Epub 2010 Sep 17.

DOI:10.1088/0953-8984/22/39/395008
PMID:21403221
Abstract

We have performed classical molecular dynamics simulations of fission track formation in zircon. We simulated the passage of a swift heavy ion through crystalline zircon using cylindrical thermal spikes with energy deposition (dE/dx) of 2.5-12.8 keV nm( - 1) and a radius of 3 nm. At a low dE/dx of 2.55 keV nm( - 1), the structural damage recovered almost completely and a damage track was not produced. At higher values of dE/dx, tracks were observed and the radius of the track increased with increasing dE/dx. Our structural analysis shows amorphization in the core of the track and phase separation into Si-rich regions near the center of the track and Zr-rich regions near the periphery. These simulations establish a threshold dE/dx for fission track formation in zircon that is relevant to thermochronology and nuclear waste immobilization.

摘要

我们对锆石裂变径迹的形成进行了经典分子动力学模拟。我们使用能量沉积(dE/dx)为 2.5-12.8 keV nm(-1)且半径为 3nm 的圆柱形热刺,模拟了高速重离子穿过结晶锆石的过程。在低 dE/dx 值(2.55keVnm(-1))下,结构损伤几乎完全恢复,没有产生损伤轨迹。在更高的 dE/dx 值下,观察到了轨迹,并且轨迹的半径随着 dE/dx 的增加而增加。我们的结构分析表明,在轨迹的核心区域发生了非晶化,并且在轨迹的中心附近形成了富含 Si 的区域,在轨迹的外围附近形成了富含 Zr 的区域。这些模拟为锆石裂变径迹的形成建立了一个与热年代学和核废料固定化相关的阈值 dE/dx。

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