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首页> 外文期刊>Atmospheric chemistry and physics >Quantifying black carbon from biomass burning by means of levoglucosan – a one-year time series at the Arctic observatory Zeppelin
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Quantifying black carbon from biomass burning by means of levoglucosan – a one-year time series at the Arctic observatory Zeppelin

机译:通过左旋葡聚糖量化生物质燃烧产生的黑碳–北极天文望远镜齐柏林飞艇的一年时间序列

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Levoglucosan, a highly specific tracer of particulate matter from biomassburning, has been used to study the influence of residential wood burning,agricultural waste burning and Boreal forest fire emissions on the Arcticatmosphere black carbon (BC) concentration. A one-year time series fromMarch 2008 to March 2009 of levoglucosan has been established at the Zeppelinobservatory in the European Arctic. Elevated concentrations of levoglucosanin winter (mean: 1.02 ng m?3) compared to summer (mean:0.13 ng m?3) were observed, resembling the seasonal variation seen for e.g.sulfate and BC. The mean concentration in the winter period was 2–3orders of magnitude lower than typical values reported for Europeanurban areas in winter, and 1–2 orders of magnitude lower thanEuropean rural background concentrations. Episodes of elevated levoglucosanconcentration lasting from 1 to 6 days were more frequent in winter than insummer and peak values were higher, exceeding 10 ng m?3 at the most.Concentrations of elemental carbon from biomass burning (ECbb) wereobtained by combining measured concentrations of levoglucosan and emissionratios of levoglucosan and EC for wildfires/agricultural fires and forresidential wood burning. Neglecting chemical degradation by OH providesminimum levoglucosan concentrations, corresponding to a mean ECbbconcentration of 3.7 ± 1.2 ng m?3 in winter (October–April) and0.8 ± 0.3 ng m?3 in summer (May–September), or8.8 ± 4.5% of the measured equivalent black carbon (EBC) concentration inwinter and 6.1 ± 3.4% in summer. When accounting for chemicaldegradation of levoglucosan by OH, an upper estimate of 31–45% of EBCcould be attributed to ECbb* (ECbb adjusted for chemicaldegradation) in winter, whereas no reliable (<100%) upperestimate could be provided for summer for the degradation rates applied.Hence, fossil fuel sources appear to dominate the European Arctic BCconcentrations in winter, whereas the very wide range obtained for summerdoes not allow us to conclude upon this for the warm season.Calculations using the Lagrangian particle dispersion model FLEXPART showthat the seasonal variation of the modeled ECbb (ECbb,m)concentration compared relatively well with observationally derivedECbb from agricultural fires/wildfires during summer, and residential woodburning in winter. The model overestimates by a factor of 2.2 in winter and4.4 in summer when compared to the observationally derived mean ECbbconcentration, which provides the minimum estimate, whereas itunderestimates by a factor of 2.3–3.3 in winter and a factor of 4.5 insummer when compared to ECbb*, which provides the upperestimate. There are indications of too-low emissions of residential woodburning in northern Russia, a region of great importance with respect toobserved concentrations of BC in the European Arctic.
机译:左旋葡聚糖是生物质燃烧产生的颗粒物的高特异性示踪剂,已用于研究住宅木材燃烧,农业废弃物燃烧和北方森林火灾排放对北极大气黑碳(BC)浓度的影响。从2008年3月到2009年3月,为期一年的左旋葡聚糖的时间序列已在欧洲北极地区的Zeppelino天文台建立。观察到冬季(平均:1.02 ng m ?3 )的左葡糖苷浓度升高(夏季:平均:0.13 ng m ?3 ),类似于季节性变化,例如硫酸盐和BC。冬季的平均浓度比欧洲城市地区冬季报告的典型值低2-3个数量级,比欧洲农村的背景浓度低1-2个数量级。冬季左旋葡聚糖浓度升高持续1至6天的发作比夏季更频繁,且峰值更高,最高超过10 ng m ?3 。 元素碳的浓度通过结合实测浓度的左旋葡聚糖和左旋葡聚糖和EC的排放浓度,可得自生物质燃烧(EC bb ),用于野火/农业大火和住宅木材燃烧。忽略OH引起的化学降解可提供最低的左旋葡聚糖浓度,相当于冬季(10月至4月)的EC bb 平均浓度为3.7±1.2 ng m ?3 和0.8±0.3夏季(5月至9月)为ng m ?3 ,即冬季测得的当量黑碳(EBC)浓度的8.8±4.5%,夏季为6.1±3.4%。当考虑到OH对左旋葡聚糖的化学降解时,EBC的31%至45%的较高估计值可以归因于EC bb * (经调整的EC bb 冬季的化学降解),而夏季无法提供可靠的(<100%)高估。因此,化石燃料来源似乎在冬季占据了欧洲北极BC浓度的主导地位,而夏季获得的范围却很广让我们可以得出一个温暖季节的结论。 使用拉格朗日粒子色散模型FLEXPART进行的计算表明,建模的EC bb (EC bb,m < / sub>)浓度与夏季从农业火灾/野火和冬季住宅燃烧得到的EC bb 的观测值相比相对较好。与观察得出的平均EC bb 浓度相比,该模型在冬季高估了2.2倍,在夏季高估了4.4倍,提供了最小的估计值,而在冬季低估了2.3-3.3倍与EC bb * 相比,夏季因子是4.5,后者提供了最高估计值。有迹象表明,俄罗斯北部的居民区燃木排放量过低,这是一个相对于欧洲北极地区观察到的BC浓度而言极为重要的地区。

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