An integrated field experiment was organized as part of the EC EXAMINE project to quantify surface–atmosphere fluxes of ammonia (NH 3). Fluxes of NH 3, NH 4 + aerosol, HNO 3 and HCl were measured using the gradient method with several continuous and batch sampling systems. Within-canopy NH 3 was determined to quantify the contribution of leaf cuticles, sub-stomatal apoplastic (intercellular) fluids and other sources and sinks to net fluxes. The campaign included the first field measurements of apoplastic pH and [NH 4 +], providing independent estimates of the stomatal compensation point ( χ s) for comparison with micrometeorological results. The latter also compared fluxes before and after cutting. Under the clean conditions of the experiment, [NH 3][HNO 3] and [NH 3][HCl] were much less than values required for aerosol formation, while the NH 4 + aerosol size distribution indicated that aerosol evaporation would be much slower than the time-scale of turbulent exchange. Nevertheless, the measurements suggest that aerosol production/growth as well as formation of HCl may have occurred within the canopy. Apoplastic [NH 4 +] and pH of leaves showed no diurnal patterns, with the main control on χ s being the temperature dependence of the solubility equilibria. Fluxes of NH 3 were bi-directional (−200 to 620 ng m −2 s −1), with deposition generally occurring when the canopy was wet and emission when it was dry, particularly during the day. Nocturnal emissions indicated a non-stomatal NH 3 source, while daytime emissions were larger than indicated by the apoplastic estimates of χ s. The within-canopy data, together with an inverse Lagrangian source–sink analysis, showed decomposing litter to be a significant NH 3 source, explaining nocturnal NH 3 emissions and larger emissions following cutting. Daytime net fluxes were controlled by the top part of the canopy, due to χ s for siliques apparently being larger than for leaves. The measurements have been used to develop multi-layer resistance models of NH 3 exchange. A 3-layer ‘foliage–litter–silique model’ provides a detailed mechanistic treatment of the component fluxes, while a 2-layer ‘foliage–litter model’ is better suited to generalization in atmospheric transport models. Application of the new models should help improve estimates of regional atmospheric ammonia budgets.
Read full abstract