vegetation regeneration around burned trees graph and explanation report

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  • 7/31/2019 Vegetation Regeneration Around Burned Trees Graph and Explanation Report

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    Vegetation Regeneration around Burned Trees, Stumps

    and Logs shown through Species Diversity and Richness in

    Slash Bust Sites, 2009

    SpeciesDiversity

    SpeciesRichness

    Logs (5) 4.20 57.60Stumps

    (47) 2.42 22.04Trees(105) 1.47 8.08

    During a forest fire approximately 8-10% of the heat generated is radiated

    downward to the forest floor (A. C., Cilimburg, and Short. K. C., 2005).

    Extensive soil heating takes time and is most likely to occur beneath heavy

    fuels, like large-diameter tree stumps and logs, which can smolder for days orweeks. In general, an enduring, low-intensity fire in logging slash will have

    more severe effects on forest soil than a fire that burns more intensely but

    rapidlythrough tree crowns (A. C., Cilimburg, and Short. K. C., 2005).

    Recovery to pre-fire conditions may take only as long as necessary for soil

    biota to reestablish and surface organic matter to reaccumulate. In the

    meantime, the physical, chemical, and biological changes in forest soil will be

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    manifest in post-fire plant establishment and growth (A. C., Cilimburg, and

    Short. K. C., 2005).

    Cited Literature:

    A. C., Cilimburg, and Short. K. C. . "Forest Fire in the Northern Rockies U.S. -

    Soils - Direct effect of fire." Forest Fire in the U. S. Northern Rockies - A

    Primer. 1 Aug. 2005. 8 Sep. 2009

    .

    Additional Available Literature:

    DeBano, L. F., S. M. Savage, and D. M. Hamilton. 1976 . The transfer of heat

    and hydrophobic substances during burning. Soil Science Society of America

    Journal 40:779-782.

    Hungerford, R. D. 1989. Modeling the downward heat pulse from fire in soils

    and in plant tissue. Pp. 148-154 in Proceedings of the 10th Conference on Fire

    and Forest Meteorology, Ottowa, Canada.

    Hungerford, R.D., M.G. Harrington, W.H. Frandsen, K.C. Ryan, and G.J. Niehoff.

    1991. Influence of fire on factors that affect site productivity. In A.E. Harveyand L. F. Neuenschwander, editors, Proceeding of the management and

    productivity of western Montane forest soils. USDA Forest Service,

    Intermountain Research Station, General Technical Report INT-280.

    Neary, D.G., C.C. Klopatek, L.F. DeBano, and P.F. Ffolliott. 1999. Fire effects on

    belowground sustainability: a review and synthesis. Forest Ecology and

    Management 122:51-71.

    Raison, R. J., P. K. Khanna, and P. V. Woods. 1985. Mechanisms of element

    transfer to the atmosphere during vegetation fires. Canadian Journal of ForestResearch 15:132-140.

    Steward, F. R. 1989. Heat penetration in soils beneath a spreading fire.

    Unpublished paper on file at: USDA Forest Service, Intermountain Forest and

    Range Experiment Station, Fire Sciences Laboratory, Missoula, Montana.

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    Wells, C. G., R. E. Campbell, L. F. DeBano, C. E. Lewis, R. L. Fredriksen, E. C.

    Franklin, R. C., Froelich, and P. H. Dunn. 1979. Effects of fire on soil, a state-of-

    knowledge review. USDA Forest Service, Washington Office, General Technical

    Report WO-7.