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• W2071453721 abstract "Black carbon (BC) is ubiquitous in terrestrial environments and its unique physical and chemical properties suggest that it may play an important role in the global carbon budget (GCB). A critical issue is whether the global production of BC results in significant amounts of carbon (C) being removed from the short-term bio-atmospheric carbon cycle and transferred to the long-term geological carbon cycle. Several dozen field and laboratory based studies of BC formation during the burning of biomass have been documented. Findings are difficult to interpret because they have been expressed in an inconsistent manner, and because different physical and chemical methods have been used to derive them. High error terms documented in many of these studies also highlight the problems associated with the quantification of the amount of biomass C consumed in fire, the amount of residue produced and the constituents of that residue. To be able to estimate the potential for BC as a carbon sink, issues regarding its definition, the methods used in its identification and measurement, and the way it is expressed in relation to other components of the carbon cycle need to be addressed. This paper presents BC data in a standard way; BC production as a percentage of the amount of C consumed by fire (BC/CC), which can be readily integrated into a larger carbon budget. Results from previous studies and new data from Australian ecosystems were recalculated in this way. As part of this process, several BC estimates derived solely from physical methods were discarded, based on their inability to accurately identify and quantify the BC component of the post-fire residue. Instead, more focus was placed on BC estimates obtained by chemical methods. This recalculated data lowered the estimate for BC formation in forest fires from 4% to 5% to < 3% BC/CC. For savannah and grassland fires a value of < 3% is consistent with reported data, but considerable variation among estimates remains. An updated flow-chart linking the sources, fluxes and pools of BC formed in the terrestrial environment with the aquatic and marine environments, and estimates of mean residence times for BC are also presented." @default.
• W2071453721 created "2016-06-24" @default.
• W2071453721 creator A5022731672 @default.
• W2071453721 creator A5069258377 @default.
• W2071453721 creator A5086137194 @default.
• W2071453721 date "2006-10-01" @default.
• W2071453721 modified "2023-10-18" @default.
• W2071453721 title "Formation, transformation and transport of black carbon (charcoal) in terrestrial and aquatic ecosystems" @default.
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• W2071453721 cites W1586510012 @default.
• W2071453721 cites W1644402576 @default.
• W2071453721 cites W1644875771 @default.
• W2071453721 cites W1670565333 @default.
• W2071453721 cites W1968661986 @default.
• W2071453721 cites W1969649637 @default.
• W2071453721 cites W1971890674 @default.
• W2071453721 cites W1972260204 @default.
• W2071453721 cites W1975652300 @default.
• W2071453721 cites W1976796865 @default.
• W2071453721 cites W1977945389 @default.
• W2071453721 cites W1978716013 @default.
• W2071453721 cites W1980256263 @default.
• W2071453721 cites W1981173072 @default.
• W2071453721 cites W1984243241 @default.
• W2071453721 cites W1994639090 @default.
• W2071453721 cites W1994704198 @default.
• W2071453721 cites W1998368784 @default.
• W2071453721 cites W2002239606 @default.
• W2071453721 cites W2003410555 @default.
• W2071453721 cites W2011352468 @default.
• W2071453721 cites W2012609184 @default.
• W2071453721 cites W2014446516 @default.
• W2071453721 cites W2022150275 @default.
• W2071453721 cites W2023353983 @default.
• W2071453721 cites W2024655281 @default.
• W2071453721 cites W2035189842 @default.
• W2071453721 cites W2038287838 @default.
• W2071453721 cites W2040396208 @default.
• W2071453721 cites W2041679960 @default.
• W2071453721 cites W2045294223 @default.
• W2071453721 cites W2046828512 @default.
• W2071453721 cites W2047423094 @default.
• W2071453721 cites W2048265977 @default.
• W2071453721 cites W2049669797 @default.
• W2071453721 cites W2050609448 @default.
• W2071453721 cites W2051516225 @default.
• W2071453721 cites W2053740257 @default.
• W2071453721 cites W2055120425 @default.
• W2071453721 cites W2058339431 @default.
• W2071453721 cites W2059148395 @default.
• W2071453721 cites W2065730795 @default.
• W2071453721 cites W2067527596 @default.
• W2071453721 cites W2069540163 @default.
• W2071453721 cites W2075673711 @default.
• W2071453721 cites W2076458865 @default.
• W2071453721 cites W2077213975 @default.
• W2071453721 cites W2085601671 @default.
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• W2071453721 cites W2090155269 @default.
• W2071453721 cites W2092222764 @default.
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• W2071453721 cites W2118722194 @default.
• W2071453721 cites W2120350572 @default.
• W2071453721 cites W2121198834 @default.
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• W2071453721 cites W2135586608 @default.
• W2071453721 cites W2151165192 @default.
• W2071453721 cites W2155592285 @default.
• W2071453721 cites W2160106930 @default.
• W2071453721 cites W2160278136 @default.
• W2071453721 cites W2162312823 @default.
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• W2071453721 doi "https://doi.org/10.1016/j.scitotenv.2006.06.007" @default.
• W2071453721 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/16860374" @default.
• W2071453721 hasPublicationYear "2006" @default.
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