Compensation points for gaseous exchange of ammonia (NH3) between stomata a
nd the atmosphere were determined in an oilseed rape (Brassica napus) canop
y by analysing the concentrations of NH4+ and H+ in leaf apoplastic solutio
n. This bioassay approach was applied for the first time in the field, allo
wing the first intercomparison with compensation points derived from microm
eteorological measurements.
Apoplastic NH4+ and H+ concentrations differed between leaf heights but val
ues were relatively stable over time, both diurnally and during a 2-week pe
riod. Stomatal NH3 compensation points calculated on the basis of apoplasti
c NH4+ and H+ concentrations and corrected for ambient leaf temperatures we
re found to correlate positively with the net NH3 emission from the canopy
estimated by micrometeorological measurements. As there was little diurnal
variability in apoplastic concentrations, this correlation was largely due
to the effect of temperature on NH3 solubility and NH4+ dissociation in the
apoplast, together with similar effects of temperature on the net NH3 flux
.
Very high NH4+ concentrations were also found in extracts of fallen litter
and resulted in NH3 partial pressures significantly exceeding NH3 levels in
the atmosphere close to the ground. By comparison of vertical atmospheric
NH3, concentration profiles in the plant canopy with the stomatal NH3 compe
nsation points determined here at three different plant heights, as well as
NH3 partial pressures in the litter, it is shown that plant residues on th
e soil surface would have been the primary NH3 source while attached leaves
acted as an NH3 sink. Although it was not possible to measure apoplastic c
oncentrations of siliques (seed cases), bulk tissue NH4+/H+ concentrations
and vertical atmospheric NH3 concentration profiles indicate that these may
have acted as an NH3 source. (C) 2000 Elsevier Science B.V. All rights res
erved.