DYNAMICS OF MATURE PEA RESIDUE NITROGEN TURNOVER IN UNPLANTED SOIL UNDER FIELD CONDITIONS

Authors
Citation
Es. Jensen, DYNAMICS OF MATURE PEA RESIDUE NITROGEN TURNOVER IN UNPLANTED SOIL UNDER FIELD CONDITIONS, Soil biology & biochemistry, 26(4), 1994, pp. 455-464
Citations number
34
Categorie Soggetti
Agriculture Soil Science
Journal title
ISSN journal
00380717
Volume
26
Issue
4
Year of publication
1994
Pages
455 - 464
Database
ISI
SICI code
0038-0717(1994)26:4<455:DOMPRN>2.0.ZU;2-O
Abstract
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.