Effects of charring on mass, organic carbon, and stable carbon isotope composition of wood

dc.contributor.authorCzimczik, C.I.
dc.contributor.authorPreston, C.M.
dc.contributor.authorSchmidt, M.W.I.
dc.contributor.authorWerner, R.A.
dc.contributor.authorSchulze, E.-D.
dc.date.accessioned2021-10-17T10:58:49Z
dc.date.available2021-10-17T10:58:49Z
dc.date.issued2002
dc.description.abstractTo aid in understanding black carbon (BC) formation during smoldering combustion in forest fires, we characterized charring of a softwood and hardwood. Charring (150, 340, 480°C) caused mass loss (7–84%), enrichment of organic carbon (OC) (0–32%), and 13C depletion (>150°C). As determined by 13C MASNMR, the OC composition of the woods was dominated by (di)-O-alkyl structures, and the chars by alkyl and aromatic structures. With increasing temperature, aromatic structures increased and the chars became more similar, although initial differences in OC concentration and d13C of woods persisted. The BC cluster sizes apparently remained small, pointing towards a low resistance against oxidation.ru_RU
dc.identifier.citationOrganic Geochemistry, 2002, 33, 1207–1223ru_RU
dc.identifier.doi10.1016/S0146-6380(02)00137-7
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/30809
dc.language.isoenru_RU
dc.titleEffects of charring on mass, organic carbon, and stable carbon isotope composition of woodru_RU
dc.typeArticleru_RU

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