Sulfur and nitrogen input-output budgets were estimated for five fores
ted Appalachian Plateau basins in Pennsylvania for the period October
1988 to March 1990. Wet and dry deposition inputs were determined on a
weekly basis from data collected at atmospheric deposition monitoring
stations located near the study sites. Stream export was estimated fr
om intensively sampled stream chemistry and continuous discharge data
collected on all five basins. On four of the five basins, deposited su
lfur was essentially in balance with stream flow export of sulfur (92-
120% exported) for the 1989 water year. The fifth basin had net retent
ion of deposited sulfur, with only 42% exported. All five basins retai
ned the vast majority of deposited nitrogen(only 3-18% exported). The
fraction of atmospherically deposited sulfur exported in stream flow w
as greater by a mean factor of 14 versus nitrogen, implying that sulfu
r dominates base cation leaching processes on these non-carbonate-base
d catchments; Although basins in the study were relatively homogeneous
in terms of topography, climate, geology and land use, local basin co
nditions caused significant differences in input-output budgets, point
ing to the need for replicated basin studies in a region. (C) 1997 by
John Wiley & Sons, Ltd.