Abstract
The distribution of air-borne salt within a forest was investigated. Na deposition decreased rapidly for three canopy heights' from the windward edge of the forest. Deposition was constant throughout the remainder of the forest. Levels of deposition experienced near the edge of the forest may be expected to influence tree growth and development and possibly soil formation. Air-borne Mg and Ca show a similar, but much reduced, trend to Na but still have a major role in nutrient cycling systems.
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