In a laboratory incubation study, effect of various anions on net methane p
roduction in two rice soils (alluvial and acid sulphate) under flooded cond
itions was examined. Methane production was considerable in alluvial soil a
nd almost negligible in acid sulphate soil, albeit with a higher density of
viable methanogens, during 30-day incubation without salts. Sodium salts o
f hydroxide and phosphate further stimulated methane production in alluvial
soil and marginally in acid sulphate soil. But, addition of sodium molybda
te, a selective inhibitor of sulphate-reducing bacteria, increased the prod
uction of methane in acid sulphate soil. In contrast, nitrite, nitrate, sul
phite and sulphate suppressed the production of methane in both soils. Acet
ate served as an excellent substrate for methanogenesis in alluvial soil, b
ut not in acid sulphate soil. Succinate and citrate also stimulated methane
production especially in alluvial soil, but after a longer lag. In acid su
lphate soil, most of the added carbon in the form of sodium salts of carbox
ylic acids was converted to CO2 and not methane, which is consistent with t
heir preferential use by the sulphate-reducing bacteria. In general, none o
f the amendments could increase production of methane in acid sulphate soil
to the same level as in alluvial soil.