scholarly journals Wildfire and Prescribed Fire Effects on Forest Floor Properties and Erosion Potential in the Central Appalachian Region, USA

Forests ◽  
2019 ◽  
Vol 10 (6) ◽  
pp. 493
Author(s):  
Emma Georgia Thompson ◽  
Thomas Adam Coates ◽  
Wallace Michael Aust ◽  
Melissa A. Thomas-Van Gundy
Keyword(s):  
West Virginia ◽  
Prescribed Fire ◽  
Forest Floor ◽  
Fire Severity ◽  
Fire Intensity ◽  
National Forest ◽  
Appalachian Region ◽  
Litter Depth ◽  
Burned Forest

Short- and long-term impacts of wildland fires on forest floor properties and erosion potential were examined at three locations in the Central Appalachian region, U.S.A. In 2018, two wildfires were investigated within six months of burning on the George Washington–Jefferson National Forest (GWJNF) in Bland County, Virginia and the Monongahela National Forest (MNF) in Grant County, West Virginia. An additional wildfire was studied eight years post-fire on the Fishburn Forest (FF) in Montgomery County, Virginia. A 2018 prescribed fire was also studied within six months of burning on the MNF in Pendleton County, West Virginia. Litter and duff consumption were examined to evaluate fire severity and char heights were measured to better understand fire intensity. The Universal Soil Loss Equation for forestlands (USLE-Forest) was utilized to estimate potential erosion values. For the 2018 comparisons, litter depth was least as a result of the wildfires on both the MNF and GWJNF (p < 0.001). Wildfire burned duff depths in 2018 did not differ from unburned duff depths on either the MNF or GWJNF. Eight years after the FF wildfire, post-fire litter depth was less than that of an adjacent non-burned forest (p = 0.29) and duff depth was greater than that of an adjacent non-burned forest (p = 0.76). Mean GWJNF wildfire char heights were greatest of all disturbance regimes at 10.0 m, indicating high fire intensity, followed by the MNF wildfire and then the MNF prescribed fire. USLE-Forest potential erosion estimates were greatest on the MNF wildfire at 21.6 Mg soil ha−1 year−1 due to slope steepness. The next largest USLE-Forest value was 6.9 Mg soil ha−1 year−1 on the GWJNF wildfire. Both the prescribed fire and the 2010 wildfire USLE-Forest values were approximately 0.00 Mg soil ha−1 year−1. Implications for potential long-term soil erosion resulting from similar wildfires in Central Appalachian forests appeared to be minimal given the 2010 wildfire results.

scholarly journals Vegetative and Edaphic Responses in a Northern Mixed Conifer Forest Three Decades after Harvest and Fire: Implications for Managing Regeneration and Carbon and Nitrogen Pools

Forests ◽  
2020 ◽  
Vol 11 (10) ◽  
pp. 1040
Author(s):  
R. Kasten Dumroese ◽  
Martin F. Jurgensen ◽  
Deborah S. Page-Dumroese
Keyword(s):  
Prescribed Fire ◽  
Forest Floor ◽  
Fire Severity ◽  
Mineral Soil ◽  
Habitat Type ◽  
Larix Occidentalis ◽  
Shrub Species ◽  
Silvicultural Practices ◽  
C And N ◽  
C And N Pools

Research Highlights: This experiment compares a range of combinations of harvest, prescribed fire, and wildfire. Leveraging a 30-year-old forest management-driven experiment, we explored the recovery of woody species composition, regeneration of the charismatic forest tree species Larix occidentalis Nutt., and vegetation and soil carbon (C) and nitrogen (N) pools. Background and Objectives: Initiated in 1967, this experiment intended to explore combinations of habitat type phases and prescribed fire severity toward supporting regeneration of L. occidentalis. At onset of the experiment, a wildfire affected a portion of the 60 research plots, allowing for additional study. Our objective was to better understand silvicultural practices to support L. occidentalis regeneration and to better understand the subsequent impacts of silvicultural practices on C and N pools within the vegetation and soil. Materials and Methods: We categorized disturbance severity based on loss of forest floor depth; 11 categories were defined, including controls for the two habitat type phases involved. We collected abundance, biomass, and C and N concentrations for the herbaceous layer, shrubs, and trees using nested quadrats and 6 to 10 experimental units per disturbance category plot. Moreover, we systematically sampled woody residue from transects, and forest floor, soil wood, and mineral soil with a systematic grid of 16 soil cores per disturbance category plot. Results: We found that (1) disturbance severity affected shrub species richness, diversity, and evenness within habitat type phases; (2) L. occidentalis regenerates when fire is part of the disturbance; (3) N-fixing shrub species were more diverse in the hotter, drier plots; (4) recovery levels of C and N pools within the soil had surpassed or were closer to pre-disturbance levels than pools within the vegetation. Conclusions: We confirm that L. occidentalis regeneration and a diverse suite of understory shrub species can be supported by harvest and prescribed fire, particularly in southern and western aspects. We also conclude that these methods can regenerate L. occidentalis in cooler, moister sites, which may be important as this species’ climate niche shifts with climate change.

scholarly journals Growth of Eastern White Pine (Pinus strobus L.) Related to Forest Floor Consumption by Prescribed Fire in the Southern Appalachians

2002 ◽  
Vol 26 (1) ◽  
pp. 18-25 ◽  
Author(s):  
Katherine J. Elliott ◽  
James M. Vose ◽  
Barton D. Clinton
Keyword(s):  
Forest Floor ◽  
Fire Severity ◽  
The Other ◽  
Size Difference ◽  
Southern Appalachians ◽  
White Pine ◽  
Eastern White Pine ◽  
Growing Seasons ◽  
Humus Layer

Abstract Chainsaw felling, burning, and planting of eastern white pine (Pinus strobusL.) have been prescribed on degraded pine/hardwood stands in the Southern Appalachians to improve overstory composition and productivity. The desired future condition of the overstory is a productive pine/hardwood mixture, with white pine, which is resistant to southern pine beetle (Dendroctonus frontalis), as the dominant pine. We evaluated the growth of white pine planted after fell-and-burn treatments through eight growing seasons after planting on three sites that differed in their fire characteristics and carbon and nitrogen losses. The three sites (JE, JW, and DD) differed in heat penetration and forest floor consumption. Although very little consumption of the Oe+Oa humus layer occurred during burning, consumption of the Oi litter layer was 94%, 94%, and 63% at JE, JW, and DD, respectively. Corresponding to the forest floor layer consumption (Oi and Oe+Oa combined), 46% of forest floor N was lost at JE, 45% of forest floor N was lost at JW, and less than 0.1% of the forest floor N was lost at DD. Biomass and density of woody competitor species were not significantly related to white pine size or growth. By the eighth growing season, no differences in white pine size or growth were detected between JE and JW, but DD had significantly smaller white pine trees. The size difference between DD and the other two sites was attributed to the replanting of seedlings at DD in 1992. However, relative growth rate (RGR) was significantly higher on DD in 1998 than the other two sites. Eight growing seasons after planting, white pine growth was negatively related to percent Oi layer consumed on the JE and JW sites. We also found significant relationships between white pine RGR and percent Oi consumed using data from all three sites. Although fire severity had a long-term effect on pine growth, fire severity was considered low overall on these sites because there were limited losses from the forest floor Oe+Oa layer. However, white pine increment and RGR were significantly related to percent forest floor Oi mass and N loss. This loss of site N capital could have a significant negative effect on growth of planted white pine over the long term. South. J. Appl. For. 26(1):18–25.

Fire and False Brome: How Do Prescribed Fire and Invasive Brachypodium sylvaticum Affect Each Other?

2015 ◽  
Vol 8 (2) ◽  
pp. 122-130 ◽  
Author(s):  
Lauren P. Poulos ◽  
Bitty A. Roy
Keyword(s):  
Prescribed Fire ◽  
Fire Severity ◽  
Seedling Emergence ◽  
Fire Regimes ◽  
National Forest ◽  
Invasive Grass ◽  
Brachypodium Sylvaticum ◽  
High Severity ◽  
Forest Sites ◽  
Noxious Weed

Brachypodium sylvaticum, a shade-tolerant, forest dwelling, and aggressive invasive grass native to Eurasia, is a noxious weed in California, Oregon, and Washington. This species could cause ecosystem collapse by altering forest fire regimes. To examine interactions with fire, we divided two Willamette National Forest sites into eight units and randomly selected half for treatment with prescribed fire in spring 2011. We assessed the effect of B. sylvaticum on fire (severity and intensity) as well as the effect of fire on B. sylvaticum (cover, seedling emergence, and dispersal). We found that B. sylvaticum cover decreased fire severity but had no effect on intensity. Furthermore, fire severity influenced B. sylvaticum cover; in areas receiving low-severity fire, the grass increased from 21 ± 15.05 to 34 ± 15.81%, but in areas of high-severity fire, cover remained consistently around 0% (0 ± 0% cover in yr 1 to 0.2 5± 0.25% in yr 3). In the field, prescribed fire decreased seedling emergence by 32% compared to controls, but not in an associated greenhouse experiment. However, in the greenhouse, severely burned plots had zero emergence, compared to 0.29 ± 0.14 seedlings low-severity m−2 plot. Fire severity also influenced dispersal in the field; we monitored plots with < 0.5% cover B. sylvaticum initially; when these plots experienced low severity fire, they had greater B. sylvaticum cover (increasing 1,200%), suggesting increased dispersal with less severe fires. High-severity dispersal plots did not experience increased cover. High severity fires have the potential to control the grass, but low-severity fires will likely increase its cover.

Effects of fire intensity on survival and recovery of soil microarthropods after a clearcut burning

2008 ◽  
Vol 38 (9) ◽  
pp. 2465-2475 ◽  
Author(s):  
Anna Malmström ◽  
Tryggve Persson ◽  
Kerstin Ahlström
Keyword(s):  
Heat Transfer ◽  
Soil Fauna ◽  
Fire Severity ◽  
Fire Intensity ◽  
Soil Microarthropods ◽  
Logging Residues ◽  
Burnt Soil ◽  
Living Species ◽  
Experimental Plots

We studied responses of soil microarthropods to different burning intensities at a clearcut that was burnt in May 2002. Fire intensity was manipulated by adding or removing logging residues as fuel from the experimental plots. Samples were taken 1 week before and 1 week after burning as well as during autumn of the same year. Samples were taken in the 2 following years to estimate long-term recovery. No difference in humus combustion could be detected between burning intensities, but most microarthropod species showed lower abundances in the hard-burnt than in the light-burnt plots immediately after fire. Surface-living species also declined in light-burnt plots, whereas soil-living species were particularly affected in hard-burnt plots. This is probably explained by greater heat transfer into the hard-burnt soil. Total abundances of Oribatida and Protura remained low for several years in the burnt plots, whereas abundances of Collembola and Mesostigmata recovered within 1 year, which indicates that at least these groups had enough habitat space and food resources after fire. The study indicates that fire severity (depth of burn) is more decisive than fire intensity (heat release) for the long-term recovery of soil fauna, whereas fire intensity determines the acute survival of animals.

When It's Hot, It's Hot... Or Maybe It's Not! (Surface Flaming May Not Portend Extensive Soil Heating)

1992 ◽  
Vol 2 (3) ◽  
pp. 139 ◽  
Author(s):  
RA Hartford ◽  
WH Frandsen
Keyword(s):  
Forest Floor ◽  
Fire Severity ◽  
Mineral Soil ◽  
Soil Surface ◽  
Fire Effects ◽  
Fire Intensity ◽  
Surface Moisture ◽  
Long Duration ◽  
Key Variables ◽  
Duration Of Heating

Fire effects on aplant community, soil, and air are not apparent when judged only by surface fire intensity. The fire severity or fire impact can be described by the temperatures reached within the forest floor and the duration of heating experienced in the vegetation, forest floor, and underlying mineral soil. Temporal distributions of temperatures illustrate heat flow in duff and mineral soil in three instrumented plots: two with slash fuel over moist duff and one with litter fuel over dry duff. Fires in the two slash fuel plots produced substantial flame lengths but minimal heating in the underlying mineral soil. In contrast, smoldering combustion in the dry duff plot produced long duration heating with nearly complete duff consumption and lethal temperatures at the mineral soil surface. Moisture content of duff and soil were key variables for determining f i e impact on the forest floor.

Long-term interdisciplinary research on the Goosenest Adaptive Management Area, Klamath National Forest, California

1999 ◽  
Vol 75 (3) ◽  
pp. 453-456 ◽  
Author(s):  
M. W. Ritchie ◽  
K. A. Harcksen
Keyword(s):  
Adaptive Management ◽  
Prescribed Fire ◽  
Ponderosa Pine ◽  
Interdisciplinary Research ◽  
National Forest ◽  
Mixed Stands ◽  
Treatment Unit ◽  
White Fir ◽  
Management Area

The Goosenest Adaptive Management Area (AMA) was established on the Klamath National Forest in northern California in 1994. The AMA was created to encourage development and testing of management strategies so as to improve the planning and implementation of management activities on the National Forest. A primary objective for the Goosenest AMA is to evaluate the extent to which different silvicultural treatments (specifically tree harvesting and prescribed fire) can accelerate development of late-successional forest attributes in mixed stands of ponderosa pine and white fir. A long-term research project was initiated to evaluate changes in response to a suite of treatments. Treatments include two different thinning regimes, prescribed fire, and a control. Treatments are applied to 40 ha units and are each replicated five times. Interdisciplinary research is facilitated by a permanently monumented data reference system. Within each treatment unit, permanent reference points are established on a 100-meter grid with accuracy to 15 cm. In addition to monitoring vegetative changes over time, researchers are also monitoring response of passerine birds and small mammals to the treatments. Key words: interior ponderosa pine, white fir, thinning, prescribed fire

scholarly journals Short- and long-term effects of ponderosa pine fuel treatments intersected by the Egley Fire Complex, Oregon, USA

Fire Ecology ◽  
2019 ◽  
Vol 15 (1) ◽  
Author(s):  
Jessie M. Dodge ◽  
Eva K. Strand ◽  
Andrew T. Hudak ◽  
Benjamin C. Bright ◽  
Darcy H. Hammond ◽  
...  
Keyword(s):  
Prescribed Fire ◽  
Vegetation Cover ◽  
Tree Density ◽  
Tree Canopy ◽  
Fuel Treatments ◽  
Dead Tree ◽  
High Severity ◽  
Short And Long Term ◽  
One Year

Abstract Background Fuel treatments are widely used to alter fuels in forested ecosystems to mitigate wildfire behavior and effects. However, few studies have examined long-term ecological effects of interacting fuel treatments (commercial harvests, pre-commercial thinnings, pile and burning, and prescribed fire) and wildfire. Using annually fitted Landsat satellite-derived Normalized Burn Ratio (NBR) curves and paired pre-fire treated and untreated field sites, we tested changes in the differenced NBR (dNBR) and years since treatment as predictors of biophysical attributes one and nine years after the 2007 Egley Fire Complex in Oregon, USA. We also assessed short- and long-term fuel treatment impacts on field-measured attributes one and nine years post fire. Results One-year post-fire burn severity (dNBR) was lower in treated than in untreated sites across the Egley Fire Complex. Annual NBR trends showed that treated sites nearly recovered to pre-fire values four years post fire, while untreated sites had a slower recovery rate. Time since treatment and dNBR significantly predicted tree canopy and understory green vegetation cover in 2008, suggesting that tree canopy and understory vegetation cover increased in areas that were treated recently pre fire. Live tree density was more affected by severity than by pre-fire treatment in either year, as was dead tree density one year post fire. In 2008, neither treatment nor severity affected percent cover of functional groups (shrub, graminoid, forb, invasive, and moss–lichen–fungi); however, by 2016, shrub, graminoid, forb, and invasive cover were higher in high-severity burn sites than in low-severity burn sites. Total fuel loads nine years post fire were higher in untreated, high-severity burn sites than any other sites. Tree canopy cover and density of trees, saplings, and seedlings were lower nine years post fire than one year post fire across treatments and severity, whereas live and dead tree basal area, understory surface cover, and fuel loads increased. Conclusions Pre-fire fuel treatments effectively lowered the occurrence of high-severity wildfire, likely due to successful pre-fire tree and sapling density and surface fuels reduction. This study also quantified the changes in vegetation and fuels from one to nine years post fire. We suggest that low-severity wildfire can meet prescribed fire management objectives of lowering surface fuel accumulations while not increasing overstory tree mortality.

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