首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Optical scattering patterns from single urban aerosol particles at Adelphi, Maryland, USA: A classification relating to particle morphologies
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Optical scattering patterns from single urban aerosol particles at Adelphi, Maryland, USA: A classification relating to particle morphologies

机译:美国马里兰州阿德菲的单个城市气溶胶颗粒的光学散射图:与颗粒形态有关的分类

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Angularly resolved elastic light scattering patterns from individual atmospheric aerosol particles (diameter 0.5–12 micrometers) sampled during fall (October 2004) at an urban site in the Baltimore-Washington metroplex are reported. These two-dimensional angular optical scattering (TAOS) patterns were collected for polar scattering angles varying from approximately 75° to 135° and azimuthal angles varying from 0° to 360°. Approximately 6000 scattering patterns were sampled over a span of 18 hours from an inlet located above our laboratory roof at Adelphi, Maryland. Our instrument recorded light scattering patterns of higher resolution and accuracy than have previously been achievable. The patterns suggest that background aerosol particles have diverse morphologies ranging from single spheres to complex structures. The frequency of occurrence of particle morphologies inferred from the TAOS patterns is strongly dependent on size. For nominally 1-μm particles, 65% appear spherical (or perturbed sphere) and only about 9% have complex structure (as suggested by their complex scattering features); whereas for nominally 5-μm particles, only 5% appear spherical (or perturbed sphere) and 71% appear to have complex structure. The patterns are quantitatively characterized using a degree of symmetry (Dsym) factor, calculated by examining both mirror and rotational symmetries in each pattern. In our measurements, atmospheric particles have two distinct populations: mostly micron-sized particles with Dsym values close to that of spheres and a population of mostly supermicron particles having a low but broad range of Dsym values. These observations are consistent with the commonly accepted notion that most micron-sized particles (in the accumulation mode) appear to be nearly spherical and are probably formed in the atmosphere through gas-particle reactions; whereas most supermicron particles appear to be nonspherical and are likely directly injected into the atmosphere. Our observations suggest that Lorenz-Mie theory may be adequate for most micron-sized particles but not for supermicron particles.
机译:据报道,在秋季(2004年10月)在巴尔的摩-华盛顿都市圈的一个城市地点采样到的单个大气气溶胶颗粒(直径0.5-12微米)的角度分辨的弹性光散射图案。收集这些二维角光学散射(TAOS)模式,以获取大约75°至135°的极性散射角和0°至360°的方位角。在我们位于马里兰州阿德菲(Adelphi)实验室屋顶上方的进样口中,在18小时的时间内采样了大约6000种散射图案。我们的仪器记录的光散射图案具有比以前可实现的更高的分辨率和精度。这些图案表明背景气溶胶颗粒具有从单个球体到复杂结构的多种形态。从TAOS模式推断出的颗粒形态的发生频率在很大程度上取决于尺寸。对于名义上为1μm的颗粒,有65%的颗粒呈球形(或扰动的球体),只有约9%的颗粒具有复杂的结构(复杂的散射特征表明);而对于名义上为5μm的颗粒,只有5%出现球形(或扰动的球形),而71%出现复杂的结构。使用对称度(Dsym)因子对图案进行定量表征,该系数通过检查每个图案中的镜像对称性和旋转对称性来计算。在我们的测量中,大气粒子有两个不同的种群:Dsym值接近球形的大多数微米级粒子,以及Dsym值范围很低但范围很广的多数超微粒子。这些观察结果与普遍接受的观点一致,即大多数微米级的粒子(在累积模式下)似乎接近球形,并且很可能是通过气体粒子反应在大气中形成的。而大多数超微粒似乎是非球形的,很可能直接注入大气中。我们的观察结果表明,Lorenz-Mie理论可能适用于大多数微米尺寸的颗粒,但不适用于超微米颗粒。

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