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This article in SSSAJ

  1. Vol. 67 No. 6, p. 1909-1919
     
    Received: Nov 7, 2002


    * Corresponding author(s): ivanjf@maine.edu
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doi:10.2136/sssaj2003.1909

Experimental Acidification Causes Soil Base-Cation Depletion at the Bear Brook Watershed in Maine

  1. Ivan J. Fernandez *a,
  2. Lindsey E. Rustadb,
  3. Stephen A. Nortonc,
  4. Jeffrey S. Kahld and
  5. Bernard J. Cosbye
  1. a Dep. of Plant, Soil, and Environmental Sciences, Univ. of Maine, Orono, ME 04469
    b USDA Forest Service, Northeastern Experiment Station, Durham, NH 03824
    c Dep. of Geological Sciences, Univ. of Maine, Orono, ME 04469
    d Senator George J. Mitchell Center for Env. & Watershed Research, Univ. of Maine, Orono, ME 04469
    e Dep. of Environmental Sciences, University of Virginia, Charlottesville, VA 22904

Abstract

There is concern that changes in atmospheric deposition, climate, or land use have altered the biogeochemistry of forests causing soil base-cation depletion, particularly Ca. The Bear Brook Watershed in Maine (BBWM) is a paired watershed experiment with one watershed subjected to elevated N and S deposition through bimonthly additions of (NH4)2SO4 Quantitative soil excavations in 1998 measured soil pools of exchangeable base cations 9 yr after treatments began. Stream sampling at the weirs on a weekly and event basis, and weekly precipitation sampling, were used for input-output estimates. The treated watershed had lower concentrations of exchangeable Ca and Mg in all horizons, with evidence for the greater depletion in the O horizon compared to underlying mineral soils, and in softwoods compared to hardwoods. This difference between watersheds is interpreted to be treatment-induced base-cation depletion, which was reinforced by model simulations. The difference between watersheds was 66 and 27 kg ha−1 of exchangeable Ca and Mg, respectively, after accounting for soil mass differences between watersheds. This was comparable with the total cumulative excess stream Ca and Mg export in West Bear after 9 yr of treatment of 55 and 11 kg ha−1, respectively. Model simulations of watershed response to treatments predicted excess soil exchangeable Ca and Mg losses in the treated watershed of 47 and 9 kg ha−1, respectively. These results indicate that the response to a step-increase in N and S deposition during the first decade of treatments in this experimental forested watershed was to invoke cation-exchange buffering, resulting in a net decline in soil exchangeable base cations.

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