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The contribution of biogas residues to soil organic matter formation and CO2 emissions in an arable soil

机译:耕地土壤中沼气残余物对土壤有机质形成和CO2排放的贡献

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The biogas production process generates as side-products biogas residues containing microbial biomass which could contribute to soil organic matter formation or induce CO2 emissions when applied to arable soil as fertilizer. Using an isotope labelling approach, we labelled the microbial biomass in biogas residues, mainly G(+) bacteria and methanogenic archaea via (KHCO3)-C-13, and traced the fate of microbial biomass carbon in soil with an incubation experiment lasting 378 days. Within the first seven days, 40% of the carbon was rapidly mineralized and after that point mineralization continued, reaching 65% by the end of the experiment Carbon mineralization data with 93% recovery could be fitted to a two-pool degradation model which estimated proportions and degradation rate constants of readily and slowly degrading pools. About 49% of the carbon was in the slowly degrading pool with a half-life of 1.9 years, suggesting mid-term contribution to living and non-living soil organic matter formation. Biogas residues caused a priming effect at the beginning, thus their intensive application should be avoided. (C) 2015 Elsevier Ltd. All rights reserved.
机译:沼气生产过程中会产生副产物沼气残留物,其中含有微生物生物质,当将其作为肥料施用到可耕种土壤中时,可能有助于土壤有机质的形成或引起CO2排放。使用同位素标记方法,我们通过(KHCO3)-C-13标记了沼气残余物中的微生物生物量,主要是G(+)细菌和产甲烷古菌,并通过持续378天的培养实验追踪了土壤中微生物生物量碳的命运。 。在开始的7天内,有40%的碳迅速矿化,此后矿化继续进行,到实验结束时达到65%。可将碳回收率93%的碳矿化数据拟合到两池降解模型中,该模型可估算出比例和缓慢降解池的降解速率常数。大约49%的碳在缓慢降解的库中,半衰期为1.9年,这表明中期对生物和非生物土壤有机物的形成有贡献。沼气残留物从一开始就引起启动效应,因此应避免大量使用。 (C)2015 Elsevier Ltd.保留所有权利。

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