We discuss situations where thermogravimetric/Fourier transform infrar
ed (TG/FT-IR) plots are obtained which differ substantially from the e
xpected ones. The most common of these situations involves samples tha
t release atmospheric components (H2O, CO2) at low temperatures. It is
shown that the phenomena are mainly related to the purging action of
the carrier gas, which strongly influences the spectroscopic portion o
f the TG/FT-IR plot. Such an influence, as well as the different situa
tions originating from it, is discussed and explained on the basis of
an analogy with the operational mode of a conventional dispersive spec
trometer.