2011
DOI: 10.1016/j.geoderma.2011.09.011
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Short-term effects of experimental fire for a soil under eucalyptus forest (SE Australia)

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Cited by 116 publications
(85 citation statements)
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References 104 publications
(135 reference statements)
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“…This behavior supports observations by several authors, who have reported an increase in soil pH following forest burning and for the effect to last for one to several years [29,52]. Arocena and Opio [10] also reported that soil pH increased by 2 or 3 pH units for two or three years after fires, and Rhoades et al [53] found that soil pH was higher in logged burnout areas for more than three years after combustion of downed logs compared with adjacent soil.…”
Section: Soil Phsupporting
confidence: 84%
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“…This behavior supports observations by several authors, who have reported an increase in soil pH following forest burning and for the effect to last for one to several years [29,52]. Arocena and Opio [10] also reported that soil pH increased by 2 or 3 pH units for two or three years after fires, and Rhoades et al [53] found that soil pH was higher in logged burnout areas for more than three years after combustion of downed logs compared with adjacent soil.…”
Section: Soil Phsupporting
confidence: 84%
“…Burns are presumed to cause losses of un-dissociated organic acids in the litter and soil by combustion, removing them from the system [10]. In addition, the leaching of alkaline metals from the ash into the soil complex and the associated consumption of hydrogen ions in the formation of water could result in an increase in pH after fires [17,52]. The pH increase from the one-year post-burn soil may be related to losses of organic acids by heating [10].…”
Section: Soil Phmentioning
confidence: 99%
“…It is, in fact, considered a major disturbance in many ecosystems which leads to important shifts in soil properties and vegetation (Certini, 2005;Granged et al, 2011a). One of the most common effects of fire is the alteration in the composition and amount of soil organic matter (Knicker, 2007;Terefe et al, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…o valor de k s diminuiu de 15.36 mm h -1 (amostra B) até (Granged et al, 2011;Shalkesby e Doerr, 2006;Zavala et al, 2010). Segundo , em solos onde a matéria orgânica é responsável pela agregação, a combustão contribui para a perda de estabilidade dos agregados e à libertação de partículas finas provenientes quer dos agregados quer das cinzas (Zavala et al, 2009).…”
Section: Fig 6 -Cumulative Infiltration I In Function Of Time T unclassified