The sequence of previously found phase transitions in
CsHSO4 at around
60, 122, and 141 °C
was carefully examined by using thermo-gravimetric analysis (TGA), mass
spectroscopy (MS), differential thermal analysis, ac calorimetry, impedance
spectroscopy, and x-ray diffraction (XRD). Our results show evidence that at all these
transition temperatures, the dehydration processes take place at or very near
the surface of the crystal. As a consequence, our results support the phase of
CsHSO4 above
141 °C
being not a superprotonic-conducting phase but rather a mixture of
CsHSO4 and
Cs2S2O7 caused
by a partial thermal decomposition that includes the break-up of hydrogen bonds and the formation
of H2O
molecules.