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This article in SSSAJ

  1. Vol. 54 No. 1, p. 252-257
     
    Received: Feb 16, 1989


    * Corresponding author(s):
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doi:10.2136/sssaj1990.03615995005400010040x

Carbon Dioxide Dynamics in Acid Forest Soils in Shenandoah National Park, Virginia

  1. A. J. Castelle  and
  2. J. N. Galloway
  1. Coll. of Forest Resources, AR-10, Univ. of Washington, Seattle, WA 98195
    Dep. of Environmental Sciences, Clark Hall, Univ. of Virginia, Charlottesville, VA 22903

Abstract

Abstract

Carbonic acid, derived from soil CO2, may strongly affect stream-water chemistry. The spatial and temporal variability of soil CO2 levels was examined in the White Oak Run watershed of Shenandoah National Park, Virginia. This watershed is in a mountainous, forested region that is being studied to monitor the effects of atmospheric acidic deposition. Two soils—one comprised of alluvial infill on a valley bottom, the other covering a steep hillslope—were monitored for CO2 levels and soil temperature and moisture. Carbon dioxide concentrations varied from atmospheric levels during the winter to nearly two orders of magnitude higher in late summer. There were strong correlations of CO2 with soil air temperature, but correlations with soil moisture content were weak. The strong seasonal fluctuations of CO2 may explain variations in White Oak Run stream-water alkalinity and base-cation concentrations.

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