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We present a detailed investigation of observable properties associated with the relative stability of the rocksalt $(B1)$ and cesium chloride $(B2)$ phases in the AX (A=Li, Na, K, Rb, Cs; X=F, Cl, Br, I) crystal family. Thermodynamic B→1B2 transition pressures and ΔY=Y(B2)-Y(B1) differences in total energies, volumes, and bulk moduli at zero and transition pressures are computed following a localized Hartree-Fock method. The arrangement of the data in clear trends is shown to be mainly dominated by the cation atomic number. This behavior is well interpreted in terms of a variety of microscopic arguments that emerge from (i) the evaluation of the energy Hessian at the $B1$ and $B2$ points and (ii) the decomposition of the energy and pressure in anionic and cationic classical and quantum-mechanical contributions.
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Flórez et al. (2002) studied this question.
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