2014
DOI: 10.1016/j.earscirev.2014.09.001
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Effects of wildfire on soil nutrients in Mediterranean ecosystems

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Cited by 188 publications
(149 citation statements)
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“…However, the past three decades have been characterized by an overall decrease in area burned, and also a decrease in the number of fires from mid-2000 (figure 2) [37,38]. This is often not recognized even within the scientific community, with some authors continuing to underpin the importance of their fire-related research with an increase of fire in this region [16,39].…”
Section: Has Fire Increased In Many Regions Around the Globe?mentioning
confidence: 99%
“…However, the past three decades have been characterized by an overall decrease in area burned, and also a decrease in the number of fires from mid-2000 (figure 2) [37,38]. This is often not recognized even within the scientific community, with some authors continuing to underpin the importance of their fire-related research with an increase of fire in this region [16,39].…”
Section: Has Fire Increased In Many Regions Around the Globe?mentioning
confidence: 99%
“…In the case of Mediterranean ecosystems, Caon et al (2014) stated that, as a general pattern, the forest floor carbon stock was reduced after wildfire and the mineral soil carbon stock declined in the short-term as well as long-term. The severe impact of fire on the forest floor is clearly the result of almost all the fresh litterfall material being burned.…”
Section: Wildfiresmentioning
confidence: 99%
“…In Mediterranean areas, carbon loss from mineral soil could be severe in the post-fire period due to soil erosion as the tree layer and forest floor could be greatly reduced (Novara et al, 2011;Caon et al, 2014).…”
Section: Wildfiresmentioning
confidence: 99%
“…Organic and mineral surface soils often display similar post-fire changes in geochemistry. These include a reduction in soil organic carbon (SOC) and total nitrogen (N) through the partial to complete removal of overlying organic matter [17,21,22]; the production of inorganic nitrogen including ammonium (NH 4 + ), a product of combustion, and nitrate (NO 3 − ), a subsequent product of nitrification, that occurs in the days to months following a wildfire [23,24]; and the concentration of non-volatized base cations (e.g., Mg 2+ , Ca 2+ , K + ) into ash lost via post-fire leaching and surface runoff [25,26]. The extent of post-fire changes in soil geochemistry reflects ecosystem type, burn severity, and fire frequency [27][28][29], all of which are influenced by topography [30].…”
Section: Introductionmentioning
confidence: 99%
“…Wildfire disturbance in forested systems alters vegetation communities and soil biogeochemical cycling as a function of fire duration, frequency, and intensity [17]-factors that are directly or indirectly shaped by topography [18][19][20]. Hillslope-scale topography exerts important control on fire severity and burn frequency in Western U.S. landscapes: more frequent, low intensity wildfires occur on drier south-facing slopes in moderate drought years compared to densely vegetated north-facing slopes that experience fewer yet more severe fires during extreme drought years [20].…”
Section: Introductionmentioning
confidence: 99%