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Determining particle index of refraction with measurements of scattering at two angles.

机译:通过测量两个角度的散射来确定粒子的折射率。

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摘要

A new Twin Angle optical particle counter (TAOPC), that measures forward scattering at 40° and 74° was developed to determine index of refraction of polar stratospheric cloud (PSC). The counter response function at the two angles, along with realistic measurement uncertainties were used to estimate the effective size range of the instrument. A method to analyze the data to determine index of refraction was developed. The error analysis indicates that measurement uncertainties at 40° are between 4 and 10% for particles >1.5 mum and between 5 and 15% at 74°. For the index of refraction determination the measurement uncertainties lead to index of refraction uncertainties between 1 and 2.5%. The lower size limitation for index of refraction determination of single particles with the TAOPC was found to be ∼1.5 mum. The instrument was tested in the laboratory with monodisperse spherical particles of known composition and size. The majority of the estimated indices of refraction were within +/- 1% of the expected indices and size determination was within acceptable error. Tests of polydisperse aerosol were less conclusive. The measurement uncertainties were used to evaluate possible index of refraction determination of PSC particles. Concentration of solid non-spherical particles >1.5 mum in a PSC can be large enough for the index of refraction determination; however, the assumption of spherical solid particles instead of non-spherical particles introduces large uncertainties in index of refraction and size determination, and may preclude a useful measurement.; The complex index of refraction of mineral dust particles was measured in Laramie, Wyoming, February 2006, with the TAOPC. The index of refraction was determined with the particle number ratio approach (Hu et al. , 2006) and was estimated to be in the range of 1.64-1.67 for the real part and 0.009-0.0104 for the imaginary part. Simultaneously with TAOPC measurements, particles were collected on polycarbonated filters for computer-controlled scanning electron microscopy (CCSEM) analysis. Index of refraction calculated from this analysis was in the range of 1.607-1.656 for the real part and 0.008-0.012 for the imaginary part. Particles were also collected on two different filter pack systems in July 2005 and February 2006. Estimates of index of refraction from these measurements compared well with the CCSEM analysis. The TAOPC scattering measurements were also modeled using an independent measurement of size with an Aerodynamic Particle Sizer, and assuming particle refractive index of 1.67-0.009i. The modeled scattering compares with the TAOPC measurements only if the uncertainties on size are increased. The larger uncertainties in scattering probably result from sampling of non-spherical particles and/or a polydisperse index of refraction distribution.; A T-matrix database, developed in collaboration between Danish Meteorological Institute, the ETH Zurich, the CNR-ISAC and the University of Wyoming is used to determine scattering by randomly oriented non-spherical axially symmetric particles with a range of real indices of refraction, size and shape. It is shown that use of the T-matrix database requires caution when calculating scattering by spherical particles due to low size resolution in the T-matrix database and since spherical particles are independent of particle orientation; however, the low size resolution calculations are acceptable for non-spherical particles due to the averaging over particle orientation.
机译:开发了一种新的双角度光学粒子计数器(TAOPC),用于测量40°和74°处的前向散射,以确定极地平流层云(PSC)的折射率。使用两个角度的计数器响应函数以及实际的测量不确定性来估算仪器的有效尺寸范围。提出了一种分析数据以确定折射率的方法。误差分析表明,> 1.5 mum的颗粒在40°时的测量不确定度在4%至10%之间,而在74°时的测量不确定度在5%至15%之间。对于折射率的确定,测量不确定度导致折射率不确定度在1%到2.5%之间。用TAOPC测定单个颗粒的折射率的下限为〜1.5μm。该仪器在实验室中用已知成分和大小的单分散球形颗粒进行测试。大部分估计的折射率在预期折射率的+/- 1%之内,并且尺寸确定在可接受的误差范围内。多分散气雾剂的测试尚无定论。测量不确定度用于评估PSC颗粒的可能的折射率测定。在PSC中,固体非球形颗粒> 1.5 mum的浓度足以确定折射率。但是,假设使用球形固体颗粒而不是非球形颗粒会在折射率和尺寸确定方面带来很大的不确定性,并且可能无法进行有用的测量。矿物粉尘颗粒的复合折射率是在TAOPC于2006年2月在怀俄明州的拉勒米(Laramie)上测量的。折射率是通过粒子数比法确定的(Hu等人,2006),实部估计在1.64-1.67范围内,虚部估计在0.009-0.0104范围内。与TAOPC测量同时,将颗粒收集在聚碳酸酯滤膜上,以进行计算机控制的扫描电子显微镜(CCSEM)分析。由该分析计算出的折射率的实部在1.607-1.656的范围内,而虚部在0.008-0.012的范围内。还分别在2005年7月和2006年2月在两个不同的滤嘴包装系统上收集了颗粒。根据这些测量结果得出的折射率估计值与CCSEM分析结果相符。还使用空气动力学粒度仪对尺寸进行独立测量,并假设颗粒折射率为1.67-0.009i,从而对TAOPC散射测量结果进行建模。仅当尺寸的不确定性增加时,模型化的散射才与TAOPC测量进行比较。散射的较大不确定性可能是由于对非球形颗粒的采样和/或折射率分布的多分散指数造成的。由丹麦气象研究所,苏黎世联邦理工学院,CNR-ISAC和怀俄明大学合作开发的T矩阵数据库用于确定具有一定范围的实际折射率的随机取向的非球形轴对称粒子的散射,尺寸和形状。结果表明,由于T矩阵数据库中的尺寸分辨率较低,并且球形粒子与粒子方向无关,因此在计算球形粒子的散射时,应谨慎使用T矩阵数据库。但是,由于对整个粒子方向进行平均,因此对于非球形粒子,低尺寸分辨率的计算是可以接受的。

著录项

  • 作者

    Eidhammer, Trude.;

  • 作者单位

    University of Wyoming.;

  • 授予单位 University of Wyoming.;
  • 学科 Physics Atmospheric Science.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 136 p.
  • 总页数 136
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
  • 关键词

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