富勒石中光离子的能量损失和能量散失

J. Vacík, V. Hnatowicz, J. Červená, H. Naramoto, S. Yamamoto, D. Fink
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引用次数: 2

摘要

考虑到富勒石薄膜的高辐射敏感性和机械脆性,应采用一种可行的方法来确定富勒石的停止截面。在这项工作中,用卢瑟福后向散射、中子深度剖面和α光谱测量了几种选定能量下1H、3H、4He和7Li离子的停止截面,使用的是由沉积在坚固衬底(Si、钢)上的富勒石组成的夹层结构样品,中间标记物(Au、N、Li、B、Pu)。此外,还利用了离子通过支持富勒石层的薄C膜的传输。测量到的停止截面与碳的理论预测相符,但系统地(10-35%)高于理论预测(5 - 5.5 MeV 4He除外)。观察到的实验数据的偏差可以部分解释为富勒石中的化学状态效应,这约占差异的20-50%。测量到的能量分散在α光谱和离子透射上分别超过玻尔值约2倍,在卢瑟福后向散射和中子深度剖面上分别超过2.5或9.5倍。这种差异可以用厚度的变化来解释,比如富勒石薄膜的表面粗糙度。
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ENERGY LOSS AND ENERGY STRAGGLING OF LIGHT IONS IN FULLERITE
To determinate the stopping cross section in fullerite a feasible approach, taking into account the high radiation sensitivity and mechanical fragility of fullerite films, should be employed. In this work, the stopping cross sections of 1H, 3H, 4He and 7Li ions for several selected energies were measured by Rutherford backscattering, neutron depth profiling and alpha spectroscopy using sandwich structures of samples composed of fullerite deposited on a firm substrate (Si, steel) with an intermediate marker (Au, N, Li, B, Pu). In addition, ion transmission through a thin C film supporting a fullerite layer was also utilized. The measured stopping cross sections follow the theoretical predictions calculated for carbon, but are systematically (10–35%) higher than the theoretical ones (with the exception of 5 — 5.5 MeV 4He). The observed deviation of the experimental data can partly be explained by the chemical state effects in fullerite, which accounts for about 20–50% of the difference. The measured energy straggling exceeds Bohr's value by a factor of about 2 for alpha spectroscopy and ion transmission, and 2.5 or 9.5 for Rutherford backscattering and neutron depth profiling, respectively. The discrepancy can be explained by a thickness variation, such as surface roughness of the fullerite films.
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