1997
DOI: 10.1097/00010694-199707000-00003
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Modifications Induced in Soil Physico-Chemical Parameters by Experimental Fires at Different Intensities

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Cited by 162 publications
(131 citation statements)
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“…Soil samples were heated for 30 minutes in a muffle furnace at temperatures of 25°, 150°, 250° and 500°C. These temperatures cover the range that is habitually reached in surface soils affected by fires (Chandler et al, 1983;Giovannini & Lucchesi, 1997;Walker et al, 1986). Soil sample treated at 250ºC was selected for adding black ashes, in a quantity related to plant biomass growing on each soil (Martí, 1998).…”
Section: Methodsmentioning
confidence: 91%
“…Soil samples were heated for 30 minutes in a muffle furnace at temperatures of 25°, 150°, 250° and 500°C. These temperatures cover the range that is habitually reached in surface soils affected by fires (Chandler et al, 1983;Giovannini & Lucchesi, 1997;Walker et al, 1986). Soil sample treated at 250ºC was selected for adding black ashes, in a quantity related to plant biomass growing on each soil (Martí, 1998).…”
Section: Methodsmentioning
confidence: 91%
“…Field experimentation, which could have provided a better understanding of fire behavior and effects in Italian ecosystems (e.g., Giovannini & Lucchesi 1997, Bovio et al 2001, Rutigliano et al 2007), have been limited for similar reasons (Mazzoleni & Esposito 1993).…”
Section: Legislationmentioning
confidence: 99%
“…Calabri (1981) and Leone et al (1999) argued that the absence of clear guidelines in PB regulations, especially concerning the attribution of responsibilities in the use of fire, has de facto prevented its implementation even when the interest was there. Field experimentation, which could have provided a better understanding of fire behavior and effects in Italian ecosystems (e.g., Giovannini & Lucchesi 1997, Bovio et al 2001, Rutigliano et al 2007), have been limited for similar reasons (Mazzoleni & Esposito 1993).…”
Section: Legislationmentioning
confidence: 99%
“…For example, when temperatures are between 200-450 ○ C, soil structure stability decreases within a few minutes [48] and the combustion of organics can change particle size distribution [90]. The laterization process (i.e., when weathering causes depletion of soluble substances in soils and rocks) begins when soils are exposed to temperatures exceeding 450 ○ C for at least one hour [90].…”
Section: Relating the Pfi To Post-fire Physical Soil Responsementioning
confidence: 99%
“…For example, when temperatures are between 200-450 ○ C, soil structure stability decreases within a few minutes [48] and the combustion of organics can change particle size distribution [90]. The laterization process (i.e., when weathering causes depletion of soluble substances in soils and rocks) begins when soils are exposed to temperatures exceeding 450 ○ C for at least one hour [90]. From the reported interaction between soil heating, char color, and mineral soil appearance, one could infer that areas with soil PFI categories 2.0 through 4.0 may experience changes in soil physical properties (e.g., laterization, structural stability, or mineralogical changes) [48,88,91].…”
Section: Relating the Pfi To Post-fire Physical Soil Responsementioning
confidence: 99%