对庭园垃圾条垛堆肥过程中温室气体排放的量化。
Quantification of greenhouse gas emissions from windrow composting of garden waste.
机构信息
Department of Environmental Engineering, Technical University of Denmark, DK-2800 Kongens Lyngby, Denmark.
出版信息
J Environ Qual. 2010 Feb 19;39(2):713-24. doi: 10.2134/jeq2009.0329. Print 2010 Mar-Apr.
Microbial degradation of organic wastes entails the production of various gases such as carbon dioxide (CO(2)), methane (CH(4)), nitrous oxide (N(2)O), and carbon monoxide (CO). Some of these gases are classified as greenhouse gases (GHGs), thus contributing to climate change. A study was performed to evaluate three methods for quantifying GHG emissions from central composting of garden waste. Two small-scale methods were used at a windrow composting facility: a static flux chamber method and a funnel method. Mass balance calculations based on measurements of the C content in the in- and out-going material showed that 91 to 94% of the C could not be accounted for using the small-scale methods, thereby indicating that these methods significantly underestimate GHG emissions. A dynamic plume method (total emission method) employing Fourier Transform Infra Red (FTIR) absorption spectroscopy was found to give a more accurate estimate of the GHG emissions, with CO(2) emissions measured to be 127 +/- 15% of the degraded C. Additionally, with this method, 2.7 +/- 0.6% and 0.34 +/- 0.16% of the degraded C was determined to be emitted as CH(4) and CO. In this study, the dynamic plume method was a more effective tool for accounting for C losses and, therefore, we believe that the method is suitable for measuring GHG emissions from composting facilities. The total emissions were found to be 2.4 +/- 0.5 kg CH(4)-C Mg(-1) wet waste (ww) and 0.06 +/- 0.03 kg N(2)O-N Mg(-1) ww from a facility treating 15,540 Mg of garden waste yr(-1), or 111 +/- 30 kg CO(2)-equivalents Mg(-1) ww.
微生物降解有机废物会产生各种气体,如二氧化碳 (CO2)、甲烷 (CH4)、氧化亚氮 (N2O) 和一氧化碳 (CO)。其中一些气体被归类为温室气体 (GHGs),从而导致气候变化。本研究旨在评估三种方法来量化花园废物集中堆肥的温室气体排放。两种小规模方法用于堆肥设施:静态通量室法和漏斗法。基于进出物料中 C 含量的测量进行的质量平衡计算表明,91%至 94%的 C 无法用小规模方法来解释,这表明这些方法严重低估了温室气体排放。采用傅里叶变换红外 (FTIR) 吸收光谱的动态羽流方法 (总排放方法) 被发现能够更准确地估计温室气体排放,测得的 CO2 排放量为降解 C 的 127 +/- 15%。此外,用这种方法,确定有 2.7 +/- 0.6%和 0.34 +/- 0.16%的降解 C 以 CH4 和 CO 的形式排放。在本研究中,动态羽流方法是一种更有效的工具,可以用来计算 C 的损失,因此,我们认为该方法适用于测量堆肥设施的温室气体排放。从处理 15540 Mg 花园废物 yr(-1) 的设施中发现,总排放量为 2.4 +/- 0.5 kg CH4-C Mg(-1)湿废物 (ww) 和 0.06 +/- 0.03 kg N2O-N Mg(-1) ww,或 111 +/- 30 kg CO2-当量 Mg(-1) ww。