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Organic composition of single and submicron particles in different regions of western North America and the eastern Pacific during INTEX-B 2006

机译:INTEX-B 2006期间北美西部和东部太平洋不同地区的单个和亚微米颗粒的有机组成

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摘要

Single particles were collected from an aircraft platform as part of theIntercontinental Chemical Transport Experiment – Phase B (INTEX-B) conductedover the eastern Pacific and western North America. Single particle spectrawere obtained using scanning transmission X-ray microscopy-near edge X-rayabsorption fine structure spectroscopy (STXM-NEXAFS). Bulk submicronparticles were also collected and organic functional group and elementalconcentrations were quantified with Fourier transform infrared (FTIR)spectroscopy and X-ray fluorescence (XRF). Single particle spectra wereclassified into metaclasses associated with different sources and atmosphericprocessing. Particles with spectra indicative of secondary organic aerosolproduction and combustion sources were found at several locations and a rangeof altitudes. At lower altitudes, particles with spectra resembling soil dustand biomass burning fingerprints were commonly observed. The types ofparticle spectra most commonly observed aloft were similar to those observedduring a previous study over the northwestern Pacific, indicating thatlong-range transport may have been an important particle source. Singleparticle spectra provided evidence that condensation and surface-limitedoxidation contributed to particle growth. Organic mass (OM) concentrationsranged from 1 to 7 μg m and averaged 2.4–4.1 μg m.Alkane functional groups were the largest fraction of OM, averaging1.9–2.1 μg m or 50–76% of OM, followed by alcoholfunctional groups (0.35–0.39 μg m, 9–14%). Organic andelemental concentrations are compared within and among geographical air massregions: "Pacific" free troposphere, "Continental" free troposphere,"Seattle" metropolitan region, and the California "Central Valley". OMconcentrations were highest and most variable in the Central Valley(3.5±2 μg m). Oxygen-to-carbon ratios were relativelyconstant in the Central Valley but variable for the Continental air masses.Overall, the OM concentrations showed greater variability within air masscategories as compared to averages among them, suggesting sampled air massregions included a variety of sources and processing of organic aerosol.
机译:在整个东太平洋和北美西部进行的洲际化学品运输实验-B期(INTEX-B)中,从飞机平台上收集了单个颗粒。使用扫描透射X射线显微镜-近边缘X射线吸收精细结构光谱法(STXM-NEXAFS)获得单粒子光谱。还收集了大块的亚微粒,并通过傅立叶变换红外(FTIR)光谱和X射线荧光(XRF)定量了有机官能团和元素浓度。单粒子光谱被分类为与不同来源和大气处理相关的亚类。在几个位置和一定高度范围内发现了具有指示第二有机气溶胶产生和燃烧源的光谱的粒子。在较低的高度,通常观察到具有类似于土壤粉尘和生物质燃烧指纹图谱的颗粒。高空最常观察到的粒子光谱类型与西北太平洋先前研究中观察到的相似,表明长距离传输可能是重要的粒子来源。单粒子光谱提供了凝结和表面受限氧化有助于粒子生长的证据。有机质(OM)浓度范围为1至7μgm,平均为2.4–4.1μgm。烷烃官能团是OM的最大部分,平均为1.9–2.1μgm或OM的50–76%,其次是醇官能团( 0.35–0.39μgm,9–14%)。比较了地理空气质量区域内和之间的有机和元素浓度:“太平洋”对流层,“大陆”对流层,“西雅图”大都市区和加利福尼亚“中谷”。在中央谷地,OM浓度最高,变化最大(3.5±2μgm)。中央谷地的氧碳比相对恒定,但随大陆气团的变化而变化。总体而言,OM浓度与平均水平相比,在气团类别中显示出更大的可变性,这表明采样的气团区域包括多种来源和有机气溶胶。

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