Estimating evolution of δ13CH4 during methanization of cellulosic waste based on stoichiometric chemical reactions, microbial dynamics and stable carbon isotope fractionation.
A change in δ(13)CH(4) during mesophilic methanization of cellulosic waste (paper and cardboard) was described using a mathematical model based on stoichiometric chemical reactions, microbial dynamics and the equation for the (13)C isotope accumulation in products including isotope fractionation. In this study, experimental data, previously obtained by Qu et al. (2009), was used to model metabolic pathways of cellulose transformation. A significant change in δ(13)CH(4) occurred in time during cellulosic waste methanization which was in accordance with the model. It was explained by the change in input of acetoclastic and hydrogenotrophic methanogenesis as well as by fractionation of stable carbon isotopes (13)C and (12)C which was much higher for hydrogenotrophic methanogenesis when compared to acetoclastic methanogenesis.
Ecological Department of Water Problems Institute, Russian Academy of Sciences, 3 Gubkina Str., Moscow 119333, Russian Federation. vavilin@aqua.laser.ru
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D002247:Carbon Isotopes / Q000737:chemistry*; D002482:Cellulose / Q000737:chemistry* / Q000378:metabolism; D008697:Methane / Q000737:chemistry*; D008962:Models, Theoretical
D002247:Carbon Isotopes; D002482:Cellulose; D008697:Methane