ABOVEGROUND SULFUR CYCLING IN ADJACENT CONIFEROUS AND DECIDUOUS FORESTS AND WATERSHED SULFUR RETENTION IN THE GEORGIA PIEDMONT, USA

Atmospheric deposition and above-ground cycling of sulfur (S) were eva luated in adjacent deciduous and coniferous forests at the Panola Moun tain Research Watershed (PMRW), Georgia, U.S.A. Total atmospheric S de position (wet plus dry) was 12.9 and 12.7 kg ha(-1) yr(-1) for the dec iduous and coniferous forests, respectively, from October 1987 through November 1989. Dry deposition contributes more than 40% to the total atmospheric S deposition, and SO2 is the major source (similar to 55%) of total dry S deposition. Dry deposition to these canopies is simila r to regional estimates suggesting that 60-km proximity to emission so urces does not noticeably impact dry deposition at PMRW. Below-canopy S fluxes (throughfall plus stemflow) in each forest are 37% higher ann ually in the deciduous forest than in the coniferous forest. An excess in below-canopy S flux in the deciduous forest is attributed to leach ing and higher dry deposition than in the coniferous forest. Total S d eposition to the forest floor by throughfall, stemflow and litterfall was 2.4 and 2.8 times higher in the deciduous and coniferous forests, respectively, than annual S growth requirement for foliage and wood. A lthough S deposition exceeds growth requirement, more than 95% of the total atmospheric S deposition was retained by the watershed in 1988 a nd 1989. The S retention at PMRW is primarily due to SO42- adsorption by iron oxides and hydroxides in watershed soils. The S content in whi te oak and loblolly pine boles have increased more than 200% in the la st 20 yr, possibly reflecting increases in emissions.