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Molecular distributions of dicarboxylic acids, ketocarboxylic acids and α-dicarbonyls in biomass burning aerosols: implications for photochemical production and degradation in smoke layers

机译:生物质燃烧气溶胶中二羧酸,酮羧酸和α-二羰基分子的分子分布:对光化学产生和烟气层降解的影响

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Aerosols in the size class <2.5 μm (6 daytime and9 nighttime samples) were collected at a pasture site in Rond?nia,Brazil, during the intensive biomass burning period of 16–26 September 2002as part of the Large-Scale Biosphere-Atmosphere Experiment in Amazonia –Smoke, Aerosols, Clouds, Rainfall and Climate (LBA-SMOCC). Homologousseries of dicarboxylic acids (C2–C11) and related compounds(ketocarboxylic acids and α-dicarbonyls) were identified using gaschromatography (GC) and GC/mass spectrometry (GC/MS). Among the speciesdetected, oxalic acid was found to be the most abundant, followed bysuccinic, malonic and glyoxylic acids. Average concentrations of totaldicarboxylic acids, ketocarboxylic acids and α-dicarbonyls in theaerosol samples were 2180, 167 and 56 ng m−3, respectively. These are2–8, 3–11 and 2–16 times higher, respectively, than those reported in urbanaerosols, such as in 14 Chinese megacities. Higher ratios of dicarboxylicacids and related compounds to biomass burning tracers (levoglucosan andK+) were found in the daytime than in the nighttime, suggesting theimportance of photochemical production. On the other hand, higher ratios ofoxalic acid to other dicarboxylic acids and related compounds normalized tobiomass burning tracers (levoglucosan and K+) in the daytime provideevidence for the possible degradation of dicarboxylic acids (≥C3)in this smoke-polluted environment. Assuming that these and relatedcompounds are photo-chemically oxidized to oxalic acid in the daytime, andgiven their linear relationship, they could account for, on average, 77%of the formation of oxalic acid. The remaining portion of oxalic acid mayhave been directly emitted from biomass burning as suggested by a goodcorrelation with the biomass burning tracers (K+, CO and ECa) andorganic carbon (OC). However, photochemical production from other precursorscould not be excluded.
机译:作为大规模生物圈大气实验的一部分,在2002年9月16日至26日密集的生物量密集燃烧期间,在巴西隆德尼亚的牧场上收集了尺寸小于<2.5μm的气溶胶(6个白天和9个夜间样本)在亚马逊地区-烟,气溶胶,云,降雨和气候(LBA-SMOCC)。使用气相色谱法(GC)和气相色谱/质谱法(GC)鉴定了二羧酸(C 2 –C 11 )的同源系列以及相关化合物/多发性硬化症)。在检测到的物种中,草酸含量最高,其次是琥珀酸,丙二酸和乙醛酸。气溶胶样品中总二羧酸,酮羧酸和α-二羰基的平均浓度分别为2180、167和56 ng m -3 。这些分别比城市气溶胶(如中国14个特大城市)中报道的高2-8倍,3-11和2-16倍。与白天相比,白天发现的二羧酸和相关化合物与生物质燃烧示踪剂(左旋葡聚糖和K + )的比率更高,这表明光化学生产的重要性。另一方面,白天草酸与其他二元羧酸和相关化合物的比例较高,已标准化为生物量燃烧示踪剂(左旋葡聚糖和K + ),提供了二元羧酸可能降解的证据(≥C 3 )在这种烟雾污染的环境中。假设这些化合物和相关化合物在白天被光化学氧化为草酸,并保持线性关系,则它们平均可占草酸形成的77%。草酸的其余部分可能已经从生物质燃烧中直接释放出来,这与生物质燃烧示踪剂(K + ,CO和EC a )和有机碳(OC )。但是,不应排除其他前体的光化学生产。

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