Seasonal variation in ammonia compensation point and nitrogen pools in beech leaves (Fagus sylvatica)

Ammonia (NH₃) fluxes between beech leaves (Fagus sylvatica) and the atmosphere were investigated in a 90-year-old forest canopy and related to leaf nitrogen (N) pools and glutamine synthetase (GS) activities. The stomatal ammonia compensation point, ?? _NH3, was measured by both a twig cuvette and bioassay techniques involving measurements of pH and ammonium (NH ₄ ⁺ ) concentration in the leaf apoplastic solution. The ?? _NH3 determined on the basis of the gas exchange measurements followed a seasonal variation with early-season peaks during leaf expansion (9.6 nmol NH₃ mol^?1 air) and late-season peaks during leaf senescence (7.3 nmol NH₃ mol^?1 air). In the mid-season, the ?? _NH3 of mature green leaves was much lower (around 3 nmol NH₃ mol^?1 air) and dropped below the NH₃ concentration in the ambient atmosphere. For comparison, ?? _NH3 obtained by the apoplastic bioassay were 7.0, 3.7 and 6.4 nmol NH₃ mol^?1 air in early-, mid-, and late -season, thus agreeing reasonably well with ?? _NH3 values derived from the gas exchange measurements. Potential NH₃ emission fluxes during early and late season were 1.31 and 0.51 nmol m^?2 leaf surface area s^?1, respectively, while leaves were a sink for NH₃ during mid-season. During leaf establishment and senescence, both apoplastic and bulk tissue NH ₄ ⁺ concentrations were relatively high coinciding with low activities of glutamine synthetase, which is a key enzyme in leaf N metabolism. In conclusion, the exchange of NH₃ between beech leaves and the atmosphere followed a seasonal variation with NH₃ emission peaks being related to N mobilization during early leaf establishment and remobilization during late leaf senescence.