SSSAJ Journal of Natural Resources and Life Sciences Education
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Published online 2 December 2005
Published in Soil Sci Soc Am J 70:141-152 (2006)
DOI: 10.2136/sssaj2005.0073
© 2005 Soil Science Society of America
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Forest, Range & Wildland Soils

Acid-base Characteristics of Soils in the Adirondack Mountains, New York

Timothy J. Sullivana,*, Ivan J. Fernandezb, Alan T. Herlihyc, Charles T. Driscolld, Todd C. McDonnelle, Nancy A. Nowickie, Kai U. Snydera and James W. Sutherlandf

a E&S Environmental Chemistry, Inc., P.O. Box 609, Corvallis, OR 97339
b Dep. of Plant Soil and Environmental Sciences, Univ. of Maine, Orono, ME 04469
c Dep. of Fisheries and Wildlife, Oregon State Univ., Corvallis, OR 97331
d Dep. of Civil and Environmental Engineering, Syracuse Univ., Syracuse, NY 13244
e SUNY College of Environmental Science and Forestry, Syracuse, NY 13210
f NYS Dep. of Environmental Conservation, Bureau of Watershed Management, Albany, NY 12233

* Corresponding author (tim.sullivan{at}ESenvironmental.com)

It is believed that atmospheric deposition of S and N in the Adirondack Mountains of New York has depleted soil-base cation pools, reduced soil base saturation (BS), and contributed to enhanced acidification of soils and surface waters. However, data to determine changes in soil characteristics are generally lacking. It is expected that soil acid-base status will improve as acidic deposition declines in response to atmospheric emissions controls. We studied edaphic characteristics at 199 locations within 44 statistically selected Adirondack lake-watersheds, plus 26 additional watersheds that are included in long-term lakewater monitoring programs. The statistically selected watersheds were chosen to be representative of Adirondack watersheds containing lakes larger than 1 ha and deeper than 1 m that have lakewater acid neutralizing capacity (ANC) less than or equal to 200 µmolc L–1. Results of soil analyses were extrapolated to the watersheds of 1320 low ANC lakes. In general, the concentrations of exchangeable base cations, base saturation, and soil pH were low. More than 75% of the target lakes received drainage from watersheds having average B horizon exchangeable Ca concentrations < 0.52 cmolc kg–1, base saturation < 10.3%, and pH (H2O) < 4.5. Variations in the effective cation exchange capacity in both O and B horizons were closely correlated with soil organic matter content. These data provide a baseline against which to compare future changes in regional soil chemistry, and provide input data for aquatic and terrestrial effects models intended to project future changes in surface water chemistry, biological conditions, and forest health.

Abbreviations: AEAP, Adirondack effects assessment program • ALSC, Adirondack Lakes Survey Corporation's survey • ALTM, Adirondack Long-term monitoring project • ANC, acid neutralizing capacity • BS, base saturation • CECe, effective cation-exchange capacity • DDRP, Direct Delayed Response Project • ELS, Eastern Lakes Survey • EMAP, Environmental Monitoring and Assessment Program • LOI, loss on ignition • NY-GAP, New York State Gap Analysis Project







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