Es. Jensen, DYNAMICS OF MATURE PEA RESIDUE NITROGEN TURNOVER IN UNPLANTED SOIL UNDER FIELD CONDITIONS, Soil biology & biochemistry, 26(4), 1994, pp. 455-464
The dynamics of N-15-labelled mature, pea (Pisum sativum L.) residue t
urnover in soil were studied in two 3 yr experiments, using residue si
zes of < 10 mm or < 3 mm in unplanted soil in the field. During the in
itial 10 days of decomposition there was a sharp decline in the amount
of N-15 in organic form in the topsoil in the two experiments, i.e. 1
4% (Expt 1) and 28% (Expt 2). Simultaneously, 14% (Expt 1) and 22% (Ex
pt 2) of the residue N-15 was incorporated into the microbial biomass.
The labelled N incorporated in the biomass was estimated to account f
or 66 and 100% of the increase in the biomass N, indicating that unlab
elled soil N was immobilized in the biomass in the second experiment,
despite the high residue N concentration. The total residual organic N
-15 and the N-15 in the biomass declined with average decay constants
of 0.44 and 0.65 yr-1, respectively, for the 10 d to 1 yr period, and
0. 15 and 0.29 yr-1, respectively for 1-3 yr period, showing a faster
turnover rate of the biomass N-15 than of the total residual organic N
-15 pool. The pool of potentially-mineralizable organic N-15, as deter
mined by an anaerobic incubation procedure, varied with time in a simi
lar way to the biomass N-15, but the size of the potentially-mineraliz
able N-15 pool was much smaller than the biomass N-15 pool. After 3 yr
of decomposition, 28% (Expt 1) and 45% (Expt 2) of the residue N-15 i
nput was present in the topsoil in organic forms. Only 1-2% of the res
idual organic N-15 was potentially mineralizable after 2 yr of decompo
sition, indicating that the remaining residue N-15 was present in rath
er recalcitrant soil organic matter. After 90 days of decomposition N-
15 unaccounted for corresponded to 10% of the input, increasing to 20-
30% after 2-3 yr of decomposition. The main part of the N unaccounted
for may have been lost by leaching of organic N and denitrification, s
ince the soil had high nitrate concentrations during the late summer a
nd autumn.