The fate of some components of acidic deposition in ombrotrophic mires

The ability of ombrotrophic Sphagnum species to immobilise inorganic nitrogen deposited from the atmosphere was investigated in a series of simple lysimeter experiments. In an unpolluted mire, Sphagnum fuscum mats retained all the nitrogen deposited to them in natural precipitation events. Sphagnum capillifolium mats, transplanted from an unpolluted site to the polluted southern Pennines in England, also initially retained a large proportion of deposited nitrate and ammonium. However, a laboratory experiment demonstrated that high rates of nitrogen supply cause a loss of the ability of the moss to retain nitrate, which suggests that this may occur as a result of increased nitrogen deposition in polluted regions, resulting in increased nitrate availability in the peat. Investigation of the volume of precipitation and amounts of sulphate and chloride passing through the Sphagnum mats in the southern Pennines, as compared to that collected in adjacent bulk deposition gauges, showed that conventional deposition monitoring grossly underestimates rates of deposition to vegetation. Efficient trapping of occult and dry deposition by the moss led to much greater volumes of precipitation and amounts of sulphate and chloride being measured in throughflow than in bulk precipitation samples. Physiological response of S. fuscum to occult precipitation and heavy rainfall was investigated by measuring nitrate reductase activity induced in the moss by nitrate supplied in 'fine mist' and 'large droplet' applications of solutions to moss in the field. Greater response was shown to occult deposition, suggesting that this form of precipitation may be important in vegetation damage in polluted regions.

Cloud Droplet Deposition in Subalpine Balsam Fir Forests: Hydrological and Chemical Inputs

Subalpine forests of the northern Appalachians are subject to significant deposition of water and chemicals via cloud droplet impaction. This deposition has been estimated by a method linking micrometeorological measures of turbulent transfer, a detailed representation of canopy structure, and experimentally derived capture efficiencies. Water inputs from clouds are about 46 percent, and chemical inputs range from 150 to 430 percent of the bulk precipitation.