The interaction between haematite powder and formic acid has been studied a
t atmospheric pressure by FTIR and under high-vacuum conditions by X-ray ph
otoelectron spectroscopy (XPS) and mass spectroscopy (MS). At room temperat
ure formic acid is adsorbed mainly molecularly whereas dissociative chemiso
rption is prevalent at higher temperatures. Heating to >500 K causes decomp
osition of the formate with the formation of carbon monoxide, carbon dioxid
e, hydrogen and water. Suggestions are made concerning the surface acid sit
es in connection with the chemisorption and the reaction pathway. The resul
ts obtained are compared with those previously achieved by the chemisorptio
n of methanol on iron oxide.