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Particulate matter and black carbon optical properties and emission factors from prescribed fires in the southeastern United States

机译:美国东南部规定的大火产生的颗粒物和黑碳光学性质及排放因子

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Aerosol optical properties of biomass burning emissions are critical parameters determining how these emissions impact the Earth's climate. Despite their importance, field measurements of aerosol optical properties fromfires remain scarce. Aerosol emissions from prescribed fires of forested and grass plots in the southeastern United States were measured and compared to emissions from laboratory simulations. Fine particulatematter (PM_(2.5)), black carbon (BC), and aerosol light scattering and absorption were characterized for all fires. Refractory BC emission factors (EFs)measured at ground level (~2m) were 0.76 ± 0.15 g/kg, comparable to the 0.93 ± 0.32 g/kg measured aloft (~100–600m). However, PM EFs measured by aircraft were only 18% (5.4 ± 2.0 g/kg) of thosemeasured on the ground (28.8 ± 9.8 g/kg). Such large differences in PMEFs for the same fire have not been previously reported and may plausibly be due to the differing particle measurement methodologies being applied but also likely related to partitioning of organic compounds to the gas phase as the plume dilutes aloft. Higher PM EFs on the ground may also be related to a higher contribution from smoldering combustion. The absorption ?ngstr?m exponents (α_a) for the high intensity South Carolina fires were 3.92 ± 0.6, which was larger than prescribed forest fire in Florida (2.84) and the grass fire in Florida (2.71), implying a larger absorption contribution from brown carbon from higher-intensity fires. Aerosol optical properties from laboratory simulations did not represent field measurements.
机译:生物质燃烧排放物的气溶胶光学特性是决定这些排放物如何影响地球气候的关键参数。尽管具有重要意义,但对火灾起火气溶胶光学特性的现场测量仍然很少。测量了美国东南部森林和草地的指定火灾造成的气溶胶排放,并将其与实验室模拟的排放进行了比较。对所有火灾都进行了细颗粒物(PM_(2.5)),黑碳(BC)以及气溶胶光散射和吸收的表征。在地面(〜2m)处测得的难治性BC排放因子(EFs)为0.76±0.15 g / kg,与在高处(〜100–600m)测得的0.93±0.32 g / kg相当。但是,飞机测量的PM EF仅为地面测量的PM EF(28.8±9.8 g / kg)的18%(5.4±2.0 g / kg)。之前尚未报道过同一起火的PMEF如此大的差异,这可能是由于采用了不同的颗粒测量方法,但也可能是由于烟羽稀薄而导致有机化合物在气相中的分配。地面上较高的PM EF也可能与闷燃燃烧的较高贡献有关。高强度南卡罗来纳州大火的吸收指数(α_a)为3.92±0.6,大于佛罗里达州规定的森林火灾(2.84)和佛罗里达州的草地火灾(2.71),表明来自高强度火灾产生的棕色碳。实验室模拟得出的气溶胶光学特性不代表现场测量。

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