An investigation was made of the effect of chemical and biological pro
cesses on ammonium immobilisation. Three soils, autoclaved and unautoc
laved, were used. Labelled ((NH4)-N-15)(2)SO4, was added to soils that
were then incubated at 25 degrees C for 0, 1, 5, 10 or 20 days. At th
e end of incubation, clay-fixed (NH4+)-N-15, organic N-15 and KCl-extr
actable mineral N-15 was determined. In autoclaved soil, fixation by c
lay accounted for up to 31% of applied (NH4+)-N-15 over a 20 day incub
ation. In unautoclaved soils (NH4+)-N-15-N fixed by clay decreased whe
n nitrification reduced the quantity of KCl-extractable (NH4+)-N-15-N.
Incorporation of (NH4+)-N-15 into organic matter in unautoclaved soil
accounted for 6-13% of applied N, whereas in autoclaved soil, only 2-
7% was recovered in the organic N pool. The data show that both chemic
al and biological processes play important roles in immobilisation of
(NH4+)-N-15 in soils. Copyright (C) 1996 Elsevier Science Ltd