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International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Soil heating during the complete combustion of mega-logs and broadcast burning in central Oregon USA pumice soils

Jane E. Smith A C , Ariel D. Cowan B and Stephen A. Fitzgerald B
+ Author Affiliations
- Author Affiliations

A USDA Forest Service, Pacific Northwest Research Station, 3200 SW Jefferson Way, Corvallis, OR 97331, USA.

B Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR 97331, USA.

C Corresponding author. Email: jsmith01@fs.fed.us

International Journal of Wildland Fire 25(11) 1202-1207 https://doi.org/10.1071/WF16016
Submitted: 27 January 2016  Accepted: 26 July 2016   Published: 12 September 2016

Abstract

The environmental effect of extreme soil heating, such as occurs with the complete combustion of large downed wood during wildfires, is a post-fire management concern to forest managers. To address this knowledge gap, we stacked logs to create ‘mega-log’ burning conditions and compared the temperature, duration and penetration of the soil heat pulse in nine high intensity burned (HB) plots paired with adjacent masticated and broadcast burned low intensity burned (LB) plots at different soil depths (0, 5, 10 and 30 cm) in a Pinus ponderosa stand with volcanic pumice soils. Maximum soil surface temperatures ranges were 424–1168°C with a mean and standard error of 759 ± 9°C in the HB treatment and 42–360°C (107 ± 43°C) in the LB treatment. In the HB treatment, temperatures causing fine root and soil organism mortality (>60°C) penetrated the soil to at least 10 cm, but were not recorded at 30 cm. In the HB treatment, mean duration above 60°C at 0–10 cm persisted for 4–13 h (7.61 ± 1.02 h). Soils in the LB treatment experienced lethal temperatures at the surface for about an hour (1.19 ± 0.70 h) and at 5 cm were mostly well below lethal temperatures with the exception of one at 57°C and another at 100°C that remained above 60°C for 1.4 h. Large areas of high burn severity may affect long-term forest productivity. Our quantification of soil heating establishes conditions for ongoing studies investigating the effects of soil burn severity on tree seedling growth, soil fungi and nutrients.

Additional keywords: fire intensity, fire severity, fuel reduction, post-fire impacts.


References

Agee JK (1993) Fire ecology of Pacific northwest forests. (Island Press: Washington, DC.)

Aznar JM, González-Pérez JA, Badía D, Martí C (2013) At what depth are the properties of gypseous forest soil affected by fire? Land Degradation & Development 27, 1344–1353.
At what depth are the properties of gypseous forest soil affected by fire?Crossref | GoogleScholarGoogle Scholar |

Badía D, Martí C (2003a) Effect of simulated fire on organic matter and selected microbiological properties of two contrasting soils. Arid Land Research and Management 17, 55–69.
Effect of simulated fire on organic matter and selected microbiological properties of two contrasting soils.Crossref | GoogleScholarGoogle Scholar |

Badía D, Martí C (2003b) Plant ash and heat intensity effects on chemical and physical properties of two contrasting soils. Arid Land Research and Management 17, 23–41.
Plant ash and heat intensity effects on chemical and physical properties of two contrasting soils.Crossref | GoogleScholarGoogle Scholar |

Badía-Villas D, González-Pérez JA, Aznar JM, Arjona-Gracia B, Martí-Dalmau C (2014) Changes in water repellency, aggregation and organic matter of a mollic horizon burned in laboratory: soil depth affected by fire. Geoderma 213, 400–407.
Changes in water repellency, aggregation and organic matter of a mollic horizon burned in laboratory: soil depth affected by fire.Crossref | GoogleScholarGoogle Scholar |

Bormann BT, Homann PS, Darbyshire RL, Morrissette BA (2008) Intense forest wildfire sharply reduces mineral soil C and N: the first direct evidence. Canadian Journal of Forest Research 38, 2771–2783.
Intense forest wildfire sharply reduces mineral soil C and N: the first direct evidence.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BD1cXhtlentb7P&md5=05d1cff7e1c478c8f6fe5a32096594c3CAS |

Brown JK, Oberheu RD, Johnston CM (1982) Handbook for inventorying surface fuels and biomass in the interior west. USDA Forest Service, Fort Collins Research Station, General Technical Report INT-129. (Fort Collins: CO)

Brown JK, Reinhardt ED, Kramer KA (2003) Coarse woody debris: managing benefits and fire hazard in the recovering forest. USDA Forest Service, Rocky Mountain Research Station, General Technical Report RMRS-GTR-105. (Ogden, UT)

Busse MD, Hubbert KR, Fiddler GO, Shestak CJ, Powers RF (2005) Lethal soil temperatures during burning of masticated forest residues. International Journal of Wildland Fire 14, 267–276.
Lethal soil temperatures during burning of masticated forest residues.Crossref | GoogleScholarGoogle Scholar |

Busse MD, Shestak CJ, Hubbert KR, Knapp EE (2010) Soil physical properties regulate lethal heating during burning of woody residues. Soil Science Society of America Journal 74, 947–955.
Soil physical properties regulate lethal heating during burning of woody residues.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DC%2BC3cXmtVWmsLo%3D&md5=6ba1198846cea5f3c6c946bea2d7ad72CAS |

Busse MD, Shestak CJ, Hubbert KR (2013) Soil heating during burning of forest slash piles and wood piles. International Journal of Wildland Fire 22, 786–796.
Soil heating during burning of forest slash piles and wood piles.Crossref | GoogleScholarGoogle Scholar |

Busse MD, Hubbert KR, Moghaddas EEY (2014) Fuel reduction practices and their effects on soil quality. USDA Forest Service, Pacific Southwest Research Station, General Technical Report PSW-GTR-241. (Albany, CA)

Chambers DP, Attiwill PM (1994) The ash-bed effect in Eucalyptus regnans forest: chemical physical, and microbiological changes in soil after heating or partial sterilization. Australian Journal of Botany 42, 739–749.
The ash-bed effect in Eucalyptus regnans forest: chemical physical, and microbiological changes in soil after heating or partial sterilization.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaK2MXktFKntbc%3D&md5=21fe3faaa94561b1591206ddec2a6022CAS |

Cochran PH (1965) Heat and moisture transfer in a pumice soil. PhD Thesis, Oregon State University.

Cooper CF (1960) Changes in vegetation, structure, and growth of southwestern pine forests since white settlement. Ecological Monographs 30, 129–164.
Changes in vegetation, structure, and growth of southwestern pine forests since white settlement.Crossref | GoogleScholarGoogle Scholar |

Cooper CF (1961) Pattern in ponderosa pine forests. Ecology 42, 493–499.
Pattern in ponderosa pine forests.Crossref | GoogleScholarGoogle Scholar |

Cowan AD, Smith JE, Fitzgerald SA (2016) Recovering lost ground: effects of soil burn intensity on nutrients and ectomycorrhiza communities of ponderosa pine seedlings. Forest Ecology and Management 378, 160–172.
Recovering lost ground: effects of soil burn intensity on nutrients and ectomycorrhiza communities of ponderosa pine seedlings.Crossref | GoogleScholarGoogle Scholar |

DeVries DA (1963) Thermal properties of soil. In ‘Physics of plant environment’. (Ed. WR van Wijk) pp. 210–235. (North-Holland: Amsterdam)

Dunn CJ, Bailey JD (2015) Temporal fuel dynamics following high-severity fire in dry mixed conifer forests of the eastern Cascades, Oregon, USA. International Journal of Wildland Fire 24, 470–483.
Temporal fuel dynamics following high-severity fire in dry mixed conifer forests of the eastern Cascades, Oregon, USA.Crossref | GoogleScholarGoogle Scholar |

Goforth BR, Graham RC, Hubbert KR, Zanner CW, Minnich RA (2005) Spatial distribution and properties of ash and thermally altered soils after high-severity forest fire, southern California. International Journal of Wildland Fire 14, 343–354.
Spatial distribution and properties of ash and thermally altered soils after high-severity forest fire, southern California.Crossref | GoogleScholarGoogle Scholar |

Hebel CL, Smith JE, Cromack K (2009) Invasive plant species and soil microbial response to wildfire burn severity in the Cascade Range of Oregon. Applied Soil Ecology 42, 150–159.
Invasive plant species and soil microbial response to wildfire burn severity in the Cascade Range of Oregon.Crossref | GoogleScholarGoogle Scholar |

Holden ZA, Morgan P, Hudak AT (2010) Burn severity of areas reburned by wildfires in the Gila National Forest, New Mexico, USA. Fire Ecology 6, 77–85.
Burn severity of areas reburned by wildfires in the Gila National Forest, New Mexico, USA.Crossref | GoogleScholarGoogle Scholar |

Hungerford RD, Harrington MG, Frandsen WH, Ryan KC, Niehoff GJ (1991) Influence of fire on factors that affect site productivity. In ‘Proceedings – management and productivity of Western-montane forest soils’, 10–12 April 1990 Boise, ID. (eds AE Harvey, LF Neuenschwander) USDA Forest Service, Intermountain Research Station, INT-GTR 280, pp. 32–50. (Ogden, UT)

Jiménez Esquilín AE, Stromberger ME, Massman WJ, Frank JM, Shepperd WD (2007) Microbial community structure and activity in a Colorado Rocky Mountain forest soil scarred by slash pile burning. Soil Biology & Biochemistry 39, 1111–1120.
Microbial community structure and activity in a Colorado Rocky Mountain forest soil scarred by slash pile burning.Crossref | GoogleScholarGoogle Scholar |

Korb JE, Johnson NC, Covington WW (2004) Slash pile burning effects on soil biotic and chemical properties and plant establishment: recommendations for amelioration. Restoration Ecology 12, 52–62.
Slash pile burning effects on soil biotic and chemical properties and plant establishment: recommendations for amelioration.Crossref | GoogleScholarGoogle Scholar |

Massman WJ, Frank JM (2004) Effect of a controlled burn on the thermophysical properties of a dry soil using a new model of soil heat flow and a new high temperature heat flux sensor. International Journal of Wildland Fire 13, 427–442.
Effect of a controlled burn on the thermophysical properties of a dry soil using a new model of soil heat flow and a new high temperature heat flux sensor.Crossref | GoogleScholarGoogle Scholar |

Massman WJ, Frank JM, Reisch NB (2008) Long-term impacts of prescribed burns on soil thermal conductivity and soil heating at a Colorado Rocky Mountain site: a data/model fusion study. International Journal of Wildland Fire 17, 131–146.
Long-term impacts of prescribed burns on soil thermal conductivity and soil heating at a Colorado Rocky Mountain site: a data/model fusion study.Crossref | GoogleScholarGoogle Scholar |

Monsanto PG, Agee JK (2008) Long-term post-wildfire dynamics of coarse woody debris after salvage logging and implications for soil heating in dry forests of the eastern Cascades, Washington. Forest Ecology and Management 255, 3952–3961.
Long-term post-wildfire dynamics of coarse woody debris after salvage logging and implications for soil heating in dry forests of the eastern Cascades, Washington.Crossref | GoogleScholarGoogle Scholar |

Neary DG, Klopatek CC, DeBano LF, Ffolliott PF (1999) Fire effects on belowground sustainability: a review and synthesis. Forest Ecology and Management 122, 51–71.
Fire effects on belowground sustainability: a review and synthesis.Crossref | GoogleScholarGoogle Scholar |

Poff R (1989) Compatibility of timber salvage operations with watershed values. In ‘Proceedings of the symposium on fire and watershed management’, 26–28 October 1988, Berg, NH. USDA Forest Service, Pacific Southwest Forest and Range Experiment Station, pp. 137–140. (Berkeley, CA)

Powers HA, Wilcox RE (1964) Volcanic ash from Mount Mazama (Crater Lake) and from Glacier Peak. Science 144, 1334–1336.
Volcanic ash from Mount Mazama (Crater Lake) and from Glacier Peak.Crossref | GoogleScholarGoogle Scholar | 1:CAS:528:DyaF2cXktl2gsbo%3D&md5=ac8973ae51865bb49263aba37138e819CAS | 17808195PubMed |

Reazin C, Morris S, Smith JE, Cowan AD, Jumpponen A (2016) Fires of differing intensities rapidly select distinct soil fungal communities in a Northwest US ponderosa pine forest ecosystem. Forest Ecology and Management 377, 118–127.
Fires of differing intensities rapidly select distinct soil fungal communities in a Northwest US ponderosa pine forest ecosystem.Crossref | GoogleScholarGoogle Scholar |

Rhoades CC, Fornwalt PJ (2015) Pile burning creates a fifty-year legacy of openings in regenerating lodgepole pine forests in Colorado. Forest Ecology and Management 336, 203–209.

Rhoades CC, Fornwalt PJ, Paschke MW, Shanklin A, Jonas JL (2015) Recovery of small pile burn scars in conifer forests of the Colorado Front Range. Forest Ecology and Management 347, 180–187.

Schoennagel T, Smithwick EAH, Turner MG (2008) Landscape heterogeneity following large fires: insights from Yellowstone National Park, USA. International Journal of Wildland Fire 17, 742–753.
Landscape heterogeneity following large fires: insights from Yellowstone National Park, USA.Crossref | GoogleScholarGoogle Scholar |

Shakesby RA, Doerr SH, Walsh RPD (2000) The erosional impact of soil hydrophobicity: current problems and future research directions. Journal of Hydrology 231–232, 178–191.
The erosional impact of soil hydrophobicity: current problems and future research directions.Crossref | GoogleScholarGoogle Scholar |

White AS (1985) Presettlement regeneration patterns in a southwestern ponderosa pine stand. Ecology 66, 589–594.
Presettlement regeneration patterns in a southwestern ponderosa pine stand.Crossref | GoogleScholarGoogle Scholar |

Wright CS, Balog CS, Kelly JW (2010) Estimating volume, biomass, and potential emissions of hand-piled fuels. USDA Forest Service, Pacific Northwest Research Station, General Technical Report PNW-GTR 805. (Portland, OR)

Youngblood A (2009) Pringle Falls Lookout Mountain Study Plan: forest dynamics after thinning and fuel reduction in dry forests. USDA Forest Service, Pacific Northwest Research Station. (Portland, OR)

Youngblood A, Johnson K, Schlaich J, Wickman B (2004) Silvicultural activities in Pringle Falls Experimental Forest, central Oregon. In ‘Silviculture in special places: proceedings of the 2003 National Silviculture Workshop’, 8–11 September 2003, Granby, CO. (Eds Sheppard WD, Eskew LG) USDA Forest Service, Rocky Mountain Research Station, Proceedings RMRS-P-34, pp. 31–48. (Ogden, UT)