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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Biomass burning - A review of organic tracers for smoke from incomplete combustion [Review]
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Biomass burning - A review of organic tracers for smoke from incomplete combustion [Review]

机译:生物质燃烧-不完全燃烧产生的烟气有机示踪剂综述[综述]

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Biomass combustion is an important primary source of particles with adsorbed biomarker compounds in the global atmosphere. The introduction of natural product organic compounds into smoke occurs primarily by direct volatilization/steam stripping and by thermal alteration based on combustion temperature. Although the molecular compositions of organic matter in smoke particles are highly variable, the molecular tracers are generally still source specific. Dehydroabietic acid is typically the major tracer for conifer smoke in the atmosphere. Degradation products from biopolymers (e.g. levoglucosan from cellulose, methoxyphenols from lignin) are also excellent tracers. Additional markers of thermally-altered and directly-emitted natural products in smoke have been defined which aids the assessment of the organic matter types and input from biomass combustion to aerosols. The precursor to product approach of compound characterization by organic geochemistry has also been applied successfully to provide source specific tracers for studying the chemistry and dispersion of ambient aerosols and the intermingling of natural with anthropogenic emissions and with smoke plumes. A brief review of the organic matter composition in aerosols derived from the major sources is also given, with emphasis on the detection of biomass burning components. These major sources are the natural background from biogenic detritus (e.g. plant wax, microbes, etc.) and anthropogenic particle emissions (e.g. oils, soot, synthetics, compounds, etc.). The emissions of organic constituents in coal smoke particulate matter are also reviewed and depend on combustion temperature, ventilation, burn time, and coal rank (geologic maturity). The components of peat and brown coal and to a lesser degree semi-bituminous coal consist mainly of hydrocarbons, biomarkers, and aromatic components, quite similar to burning of contemporary biomass. Dispersion from the source and long range transport of smoke particulate matter with the associated organic compounds is also discussed. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 292]
机译:生物质燃烧是全球大气中吸附有生物标志物的颗粒的重要主要来源。将天然产物有机化合物引入烟雾的过程主要是通过直接挥发/汽提和基于燃烧温度的热变化进行的。尽管烟雾颗粒中有机物的分子组成变化很大,但分子示踪剂通常仍然是特定于源的。脱氢松香酸通常是大气中针叶树烟雾的主要示踪剂。生物聚合物的降解产物(例如纤维素的左旋葡聚糖,木质素的甲氧基苯酚)也是很好的示踪剂。已经定义了烟雾中热改变和直接排放的天然产物的其他标记,这些标记有助于评估有机物质的类型以及从生物质燃烧到气溶胶的输入。通过有机地球化学表征化合物的产物方法的前体也已成功地用于为特定源提供示踪剂,以研究周围气溶胶的化学和分散性,以及自然与人为排放物和烟羽的混合。还简要回顾了主要来源的气溶胶中有机物的组成,重点是生物质燃烧成分的检测。这些主要来源是生物碎屑(例如植物蜡,微生物等)和人为颗粒排放物(例如油,烟灰,合成物,化合物等)的自然背景。还检查了煤烟颗粒物中有机成分的排放,并取决于燃烧温度,通风,燃烧时间和煤等级(地质成熟度)。泥炭和褐煤的成分,以及次要程度的半烟煤的成分主要由碳氢化合物,生物标志物和芳香族成分组成,与当代生物质的燃烧非常相似。还讨论了烟源颗粒物与相关有机化合物的来源扩散和远距离运输。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:292]

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