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Laboratory measurements of the optical properties of sea salt aerosol

机译:海盐气溶胶光学特性的实验室测量

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The extinction spectra of laboratory generated sea salt aerosols have beenmeasured from 1 μm to 20 μm using a Bruker 66v/S FTIR spectrometer.Concomitant measurements include temperature, pressure, relative humidity andthe aerosol size distribution. The refractive indices of the sea salt aerosolhave been determined using a simple harmonic oscillator band model(Thomas et al., 2004) for aerosol with relative humidities at eight different valuesbetween 0.4% to 86%. The resulting refractive index spectra showsignificant discrepancies when compared to existing sea salt refractiveindices calculated using volume mixing rules (Shettleand Fenn, 1979). Specifically, anadditional band is found in the refractive indices of dry sea salt aerosoland the new data shows increased values of refractive index at almost allwavelengths. This implies that the volume mixing rules, currently used tocalculate the refractive indices of wet sea salt aerosols, are inadequate.Furthermore, the existing data for the real and imaginary parts of therefractive indices of dry sea salt aerosol are found not to display theKramers-Kronig relationship. This implies that the original data used for thevolume mixing calculations is also inaccurate.
机译:使用Bruker 66v / S FTIR光谱仪测量了实验室产生的海盐气溶胶的消光光谱,范围为1μm至20μm,同时测量的温度,压力,相对湿度和气溶胶粒径分布。海盐气溶胶的折射率已经使用简单的谐波振荡器带模型(Thomas等人,2004)确定了气溶胶的相对湿度,其八个相对值在0.4%到86%之间。与使用体积混合法则计算出的现有海盐折射率相比,所得的折射率光谱显示出明显的差异(Shettleand Fenn,1979)。具体而言,在干海盐气溶胶层的折射率中发现了一个附加谱带,新数据显示几乎所有波长的折射率值都增加了。这意味着目前用于计算湿海盐气溶胶的折射率的体积混合规则是不充分的。此外,发现干海盐气溶胶的折射率的实部和虚部的现有数据没有显示出Kramers-Kronig关系。这意味着用于体积混合计算的原始数据也不准确。

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