Abstract:
The importance of the use of low temperature data with the second Szigeti relation is shown for the fluorite structure; a comparison with the NaCl and CsCl structures is given. The volume dependence of the generalized first Szigeti relation is used to calculate the Grüneisen parameter γ1 with low temperature data; γ1 is calculated with different models. Values of the volume dependence of the effective ionic charge are obtained independently using Hardy's model. © 1983.
Referencias:
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Citas:
---------- APA ----------
Batana, A. & Soriano, M.R.
(1983)
. Volume dependence of the effective ionic charge of alkaline-earth fluorides. Journal of Physics and Chemistry of Solids, 44(8), 741-743.
http://dx.doi.org/10.1016/0022-3697(83)90004-5---------- CHICAGO ----------
Batana, A., Soriano, M.R.
"Volume dependence of the effective ionic charge of alkaline-earth fluorides"
. Journal of Physics and Chemistry of Solids 44, no. 8
(1983) : 741-743.
http://dx.doi.org/10.1016/0022-3697(83)90004-5---------- MLA ----------
Batana, A., Soriano, M.R.
"Volume dependence of the effective ionic charge of alkaline-earth fluorides"
. Journal of Physics and Chemistry of Solids, vol. 44, no. 8, 1983, pp. 741-743.
http://dx.doi.org/10.1016/0022-3697(83)90004-5---------- VANCOUVER ----------
Batana, A., Soriano, M.R. Volume dependence of the effective ionic charge of alkaline-earth fluorides. J Phys Chem Solids. 1983;44(8):741-743.
http://dx.doi.org/10.1016/0022-3697(83)90004-5