Hygroscopic salts on the leaf surface as a possible cause of forest decline symptoms

Forest decline has been observed for about 20 years, especially in Central Europe and eastern North America. Whereas the direct effects of acid rain, acid fog and several trace gases on aerial parts of trees have been investigated, deposited atmospheric particles on leaf surfaces have been regarded as inert so far. By conductance measurements on the surface of coniferous needles an invisible wetness was observed over extended times. Washing experiments revealed this to be due to hygroscopic salts on the leaf surface, which will absorb water vapour mostly from leaf transpiration. The possible influence of salts on the microclimatic conditions on the leaf surface is outlined and it is concluded that they will act similar to a wick or a drying agent. This could form a direct link between air pollution and those forest decline symptoms which are connected with the water status of the trees.