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
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.