The structure and atmosphere-dependent thermochemical reactivity of di
ammine copper carbonate, Cu(NH3)2CO3 has been investigated by means of
combined thermoanalytical/mass spectrometric measurements, single cry
stal and powder X-ray diffraction studies as well as scanning electron
microscopy. It could be shown that in reducing atmosphere a series of
different organic volatile species as well as Cu-degrees are formed.
This observation is explained in terms of the structural vicinity of p
otential volatile agents in the parent material, i.e. NH3 and CO2, as
well as the in situ formation of catalytically active solid products d
uring the thermochemical degradation.