Nj. Hutchings et Is. Kristensen, MODELING MINERAL NITROGEN ACCUMULATION IN GRAZED PASTURE - WILL MORE NITROGEN LEACH FROM FERTILIZED GRASS THAN UNFERTILIZED GRASS CLOVER, Grass and forage science, 50(3), 1995, pp. 300-313
A model of herbage growth and nitrogen dynamics for grazed pasture was
developed. Grazed herbage nitrogen is partitioned between animal grow
th, urine and faeces. After allowing for ammonia volatilization, the r
ate and area covered by urinary nitrogen is simulated. The fate of eac
h day' s urinary nitrogen deposition is followed separately through ti
me. The mineral nitrogen remaining in the soil at the end of the growi
ng season is assumed to be leached over winter. Leaching from fertiliz
ed grass-only and unfertilized grass/clover pastures are compared at v
arying levels of dry matter (DM) production. Biological fixation is as
sumed to provide sufficient nitrogen to allow the grass/clover pasture
to achieve the same seasonal distribution of production as the fertil
ized grass-only pasture. There was a non-linear increase in predicted
leaching with increasing DM production owing to the aggregation of uri
nary nitrogen into urine patches; Leaching was lower from grass/clover
than the grass-only pasture and the difference increased with DM prod
uction. At levels of production common in the UK, the difference in le
aching between the two pasture types was small and the spatial distrib
ution of soil mineral nitrogen was uneven, so differences in leaching
may be small and difficult to detect.