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首页> 外文期刊>Journal of Physics. Condensed Matter >Theory of self-diffusion in alkali metals: I. Results for monovacancies in Li, Na, and K
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Theory of self-diffusion in alkali metals: I. Results for monovacancies in Li, Na, and K

机译:碱金属自扩散理论:I. Li,Na和K中单空位的结果

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The phonon dispersion curves for perfect crystals of bcc Li, Na, and K are calculated by the db initio Force-constant method in a supercell approach. It is shown that the coupling constants of Li decay much more slowly in space than those for Na and K, so for Li the phonon spectrum could not be reliably determined with the supercell sizes used in the calculations. From the phonon spectra of the perfect supercell and the supercell with a monovacancy the vacancy formation entropy is calculated for Na (1.36 k(B)) and K (0.78 k(B)). Furthermore, the formation energy (0.53, 0.34, and 0.30 eV) and the formation volume (about 0.5 Omega(0)) are obtained for Li, Na, and K, and the temperature and pressure dependences of the formation entropy and volume are investigated for the case of Na; a strong decrease of the formation volume with increasing pressure is found. The migration energies acid volumes are determined within the framework of the transition-state theory. The migration energies are small (about 0.05 eV) for Li, Na, and K, and the migration volumes are small and negative for Li and Na. The calculated activation energies for self-diffusion (0.58, 0.39, and 0.35 eV) agree well with experimental data. Neglecting the migration entropy and inserting Flynn's ansatz for the attempt frequency, the absolute values of the self-diffusion coefficients are determined as a function of temperature. For Na these values agree well with experimental data, whereas for K the calculated values are too small except for low temperatures. [References: 73]
机译:bcc Li,Na和K完美晶体的声子色散曲线是通过db初始力恒方法在超级电池方法中计算的。结果表明,Li的耦合常数在空间中的衰变要比Na和K的慢得多,因此对于Li,声子谱无法通过计算中使用的超级单元尺寸可靠地确定。根据完美超级电池和具有单空位的超级电池的声子谱,计算Na(1.36 k(B))和K(0.78 k(B))的空位形成熵。此外,获得了Li,Na和K的地层能量(0.53、0.34和0.30 eV)和地层体积(约0.5 Omega(0)),并研究了地层熵和体积的温度和压力依赖性。就Na而言;发现随着压力的增加,地层体积大大减少。迁移能的酸体积是在过渡态理论的框架内确定的。 Li,Na和K的迁移能小(约0.05 eV),Li和Na的迁移量小且为负。计算出的自扩散活化能(0.58、0.39和0.35 eV)与实验数据非常吻合。忽略迁移熵并将弗林的ansatz插入尝试频率,根据温度确定自扩散系数的绝对值。对于Na,这些值与实验数据非常吻合,而对于K,除低温外,计算值都太小。 [参考:73]

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