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COSUB2/SUB emissions from biomass combustion for bioenergy: atmospheric decay and contribution to global warming

机译:生物化学生物量燃烧的CO 2 排放:大气衰减和全球变暖的贡献

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Carbon dioxide (COSUB2/SUB) emissions from biomass combustion are traditionally assumed climate neutral if the bioenergy system is carbon (C) flux neutral, i.e. the COSUB2/SUB released from biofuel combustion approximately equals the amount of COSUB2/SUB sequestered in biomass. This convention, widely adopted in life cycle assessment (LCA) studies of bioenergy systems, underestimates the climate impact of bioenergy. Besides COSUB2/SUB emissions from permanent C losses, COSUB2/SUB emissions from C flux neutral systems (that is from temporary C losses) also contribute to climate change: before being captured by biomass regrowth, COSUB2/SUB molecules spend time in the atmosphere and contribute to global warming. In this paper, a method to estimate the climate impact of COSUB2/SUB emissions from biomass combustion is proposed. Our method uses COSUB2/SUB impulse response functions (IRF) from C cycle models in the elaboration of atmospheric decay functions for biomass-derived COSUB2/SUB emissions. Their contributions to global warming are then quantified with a unit-based index, the GWPSUBbio/SUB. Since this index is expressed as a function of the rotation period of the biomass, our results can be applied to COSUB2/SUB emissions from combustion of all the different biomass species, from annual row crops to slower growing boreal forest.
机译:来自生物量燃烧的二氧化碳(CO 2 )排放,如果生物能量系统是碳(c)焊剂中性,即释放生物燃料燃烧的CO 2 ,则传统地假设气候中性。等于在生物质中螯合的CO 2 的量。本公约在生物能源系统的生命周期评估(LCA)研究中广泛采用,低估了生物能源的气候影响。除了CO 2 排放中,C磁通中性系统(即来自临时C损失)的CO 2 排放也有助于气候变化:在被生物量捕获之前再生,CO 2 分子在大气中花费时间并有助于全球变暖。在本文中,提出了一种估计CO 2 排放对生物质燃烧的气候影响的方法。我们的方法使用C循环模型的CO 2 脉冲响应函数(IRF)在制定生物量衍生的CO 2 排放的大气衰减函数中。然后通过基于单位的指数来量化它们对全局变暖的贡献,GWP Bio 。由于该指标被表示为生物质的旋转时段的函数,因此我们的结果可以应用于来自所有不同生物量物种的燃烧的Co 2 排放,从年度排作弊越来越慢地生长北欧森林。

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