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首页> 外文期刊>The Journal of Chemical Physics >Hydrogen diffusion in potassium intercalated graphite studied by quasielastic neutron scattering
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Hydrogen diffusion in potassium intercalated graphite studied by quasielastic neutron scattering

机译:准弹性中子散射研究插层石墨中氢的扩散

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摘要

The graphite intercalation compound KC_(24) adsorbs hydrogen gas at low temperatures up to a maximum stoichiometry of KC_(24)(H _2)_2, with a differential enthalpy of adsorption of approximately -9 kJmol~(-1). The hydrogen molecules and potassium atoms form a two-dimensional condensed phase between the graphite layers. Steric barriers and strong adsorption potentials are expected to strongly hinder hydrogen diffusion within the host KC_(24) structure. In this study, self-diffusion in a KC_(24)(H_2)_(0.5) sample is measured experimentally by quasielastic neutron scattering and compared to values from molecular dynamics simulations. Self-diffusion coefficients are determined by fits of the experimental spectra to a honeycomb net diffusion model and found to agree well with the simulated values. The experimental H _2 diffusion coefficients in KC_(24) vary from 3.6 × 10~(-9) m~2s~(-1) at 80 K to 8.5 × 10 ~(-9) m~2s~(-1) at 110 K. The measured diffusivities are roughly an order of magnitude lower that those observed on carbon adsorbents, but compare well with the rate of hydrogen self-diffusion in molecular sieve zeolites.
机译:石墨插层化合物KC_(24)在低温下吸附氢气,最大化学计量为KC_(24)(H _2)_2,吸附的焓差约为-9 kJmol〜(-1)。氢分子和钾原子在石墨层之间形成二维缩合相。立体势垒和强大的吸附潜力预计将严重阻碍主机KC_(24)结构内的氢扩散。在这项研究中,通过准弹性中子散射实验测量了KC_(24)(H_2)_(0.5)样品中的自扩散,并将其与分子动力学模拟的值进行了比较。自扩散系数是通过将实验光谱拟合到蜂窝网扩散模型确定的,并且发现其与模拟值非常吻合。 KC_(24)中的实验H _2扩散系数从80 K时的3.6×10〜(-9)m〜2s〜(-1)变化到80 K时的8.5×10〜(-9)m〜2s〜(-1) 110K。测得的扩散率比在碳吸附剂上测得的扩散率大约低一个数量级,但与分子筛沸石中氢的自扩散速率相比,效果很好。

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