LOSS OF NITROGEN IN COMPACTED GRASSLAND SOIL BY SIMULTANEOUS NITRIFICATION AND DENITRIFICATION

Citation
Mk. Abbasi et Wa. Adams, LOSS OF NITROGEN IN COMPACTED GRASSLAND SOIL BY SIMULTANEOUS NITRIFICATION AND DENITRIFICATION, Plant and soil, 200(2), 1998, pp. 265-277
Citations number
39
Categorie Soggetti
Agriculture Soil Science","Plant Sciences",Agriculture
Journal title
ISSN journal
0032079X
Volume
200
Issue
2
Year of publication
1998
Pages
265 - 277
Database
ISI
SICI code
0032-079X(1998)200:2<265:LONICG>2.0.ZU;2-S
Abstract
The soils of mid-Wales in grazed permanent pasture usually exhibit sta gnogley features in the top 4-10 cm even though on sloping sites, they are freely drained. Nitrogen is often poorly recovered under these co nditions. Our previous studies suggest that continuing loss of availab le N through concurrent nitrification and denitrification might provid e an explanation for poor response to fertilizer N. The work described was designated to further test this proposition. When NH4+-N was appl ied to the surface of intact cores, equilibrated at -5kPa matric poten tial, about 70% of NH4+-N initially present was lost within 56 days of incubation. Study of different sections of the cores showed a rise in NO3- level in the surface 0-2.5 cm soil layer but no significant chan ges below this depth. The imbalance between NO3- accumulation and NH4 disappearance during the study indicated a simultaneous nitrification and denitrification in the system. Furthermore. the denitrification p otential of the soil was 3-4 times greater than nitrification potentia l so no major build-up of NO3- would be expected when two processes oc cur simultaneously in micro-scale. When nitrification was inhibited by nitrapyrin, a substantial amount of NH4+-N remained in the soil and p ersisted till the end of the incubation. The apparent recovery of appl ied N increased and of the total amount of N applied, 50% more was rec overed relative to without nitrapyrin. It appears that addition of nit rapyrin inhibited nitrification, and consequently denitrification, by limiting the supply of NO3- for denitrifying organisms. Emission of N2 O from the NH4+ amended soil cores further confirmed that loss of appl ied N was the result of both nitrification and denitrification, which occurred simultaneously in adjacent sites at shallow depths. This N lo ss could account for the poor response to fertilizer N often observed in pastoral agriculture in western areas of the UK.