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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 3, issue 2
Hydrol. Earth Syst. Sci., 3, 223–231, 1999
https://doi.org/10.5194/hess-3-223-1999
© Author(s) 1999. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Hydrol. Earth Syst. Sci., 3, 223–231, 1999
https://doi.org/10.5194/hess-3-223-1999
© Author(s) 1999. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  30 Jun 1999

30 Jun 1999

Distribution of bog and heath in a Newfoundland blanket bog complex: topographic limits on the hydrological processes governing blanket bog development

P. A. Graniero1 and J. S. Price2 P. A. Graniero and J. S. Price
  • 1Department of Geography, University of Toronto at Mississauga, 3359 Mississauga Road N, Mississauga, Ontario, Canada L5L 1C6
  • 2Department of Geography, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
  • e-mail for corresponding authors: graniero@eratos.erin.utoronto.ca
  • jsprice@watserv1.uwaterloo.ca

Abstract. This research quantified the role of topography and hydrological processes within and, hence, the development of, blanket bogs. Topographic characteristics were derived from digital elevation models (DEMs) developed for the surface and underlying substrate at three blanket bog sites on the southeastern lobe of the Avalon Peninsula, Newfoundland. A multinomial logit (MNL) model of the probability of bog occurrence was constructed in terms of relevant topographic characteristics. The resulting model was then used to investigate the probabilistic boundary conditions of bog occurrence within the landscape. Under average curvatures for the sites studied, substrate slopes up to 0.065 favoured blanket bog development. However, steeper slopes could, theoretically, be occupied by blanked bog where water is concentrated by convergent curvatures or large contributing areas. Near community boundaries, bog and heath communities both occupied similar topographic conditions. Since these boundary locations are capable of supporting the hydrological conditions necessary for bog development, the heath is likely to be encroached upon by bog.

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