Ej. Wilson et al., ARE CALCAREOUS GRASSLANDS IN THE UK UNDER THREAT FROM NITROGEN DEPOSITION - AN EXPERIMENTAL-DETERMINATION OF A CRITICAL LOAD, Journal of Ecology, 83(5), 1995, pp. 823-832
1 Nitrogen was applied to artificial chalk grasslands as either ammoni
um-N or nitrate-N to simulate recent increases in atmospheric N deposi
tion. 2 Inputs of nitrogen above ambient stimulated the growth of the
sward, but there was no further increase in growth when N inputs were
increased from 20 kg N ha(-1) year(-1) to over 80 kg N ha(-1) year(-1)
. The increase in dry weight of the sward was a result of a greater ab
ove-ground yield of certain forbs, particularly Filipendula, Scabiosa
and Thymus. N treatment did not significantly increase the growth of o
ther forbs, but there were no adverse effects even at N inputs as high
as 80 kg N ha(-1) year(-1). 3 The forbs which responded positively to
N addition had low Ellenberg Indicator Values. This index is unlikely
to be an accurate predictor of how a species will respond to increase
s in N deposition. 4 The growth of the grass Brachypodium pinnatum did
not increase significantly as a result of nitrogen addition. There wa
s no evidence that increases in atmospheric nitrogen deposition will r
esult in grass dominance and a loss of species diversity. 5 Growth of
both grasses and forbs was probably limited by the availability of pho
sphorus. In these circumstances, high levels of N deposition may prove
a greater threat to ground water quality than to species composition.
6 The growth of Brachypodium was adversely affected by a simulated gr
azing treatment. The response of forbs was variable; grazing reduced t
he growth of some species but had beneficial effects on others. Manage
ment practices such as grazing are likely to be a key factor in mainta
ining species diversity in chalk grasslands. 7 The critical load for a
grazed, P-limited chalk grassland is calculated to be between 42 and
55 kg N ha(-1) year(-1). Neither Brachypodium nor any of the forbs sho
wed different growth responses according to whether N was applied as a
mmonium or nitrate. A critical load for total N deposition should be c
alculated for chalk grasslands, and modified for local characteristics
such as past and present management practises, and factors which may
limit N assimilation (e.g. P status).