Mass spectrometric analysis of gases evolved during thermal decomposition o
f divalent metal hydroxides, hydroxysalts and hydrotalcites show that all t
hese compounds undergo dehydration in the temperature range 30 < T < 220 de
grees C followed by decomposition at temperatures above 250 degrees. The la
tter step involves simultaneous deanation and dehydroxylation of the layers
. Our observations conclusively prove that alternative mechanisms which env
isage CO2 evolution due to deanation at lower temperatures proposed by Kane
zaki to be wrong.