“…Nevertheless, inverse BCE was recently studied in ferroelectrics BaTiO 3 , (NH 4 ) 2 SO 4 , NH 4 HSO 4 and intermetallic compound La-Fe-Si-Co. [6,7,8,9] A different sign of the change of the unit cell volume is observed quite often at structural transformations in materials of the ferroelastic origin: fluorides, oxides and oxyfluorides with the perovskite-like structure. [5,10] Some of these crystals undergo at ambient pressure only one phase transition G 0 ↔ G 1 which is characterized by large entropy change ∆S and small change in the unit cell volume or in anomalous part of the β value. In such a case, in accordance with the Clausius-Clapeyron, dT /dp = δV · δS −1 , and Ehrenfest, dT /dp = T 0 · ∆β · ∆C −1 p , equations, baric coefficients dT G0−G1 /dp is also characterized by small magnitude.…”