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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Experimental determination of scattering matrices of randomly oriented fly ash and clay particles at 442 and 633 nm
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Experimental determination of scattering matrices of randomly oriented fly ash and clay particles at 442 and 633 nm

机译:实验确定随机取向的粉煤灰和粘土颗粒在442和633 nm处的散射矩阵

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We present measurements of the scattering angle distribution of the whole scattering matrix for randomly oriented particles of three mineral samples: fly ash, green clay, and red clay at 442 and 633 nm. Fly ash consists of aggregates of nearly spherical particles while green clay and red clay particles represent irregular compact particles. We compare the measured results for fly ash with an experiment ally determined average scattering matrix which is based on measurements for a broad selection of irregular mineral aerosol particles. We find that the scattering matrix of our polydisperse sample of aggregates of nearly spherical particles differs considerably from that of compact particles. In addition, the angular distribution of the elements of the scattering matrix (except F-22(theta)/F-11(theta)) for fly ash particles seem to be dominated by the single monomers. The effects of small differences in composition on the scattering behavior have also been studied by comparing our experimental results for green clay particles with those obtained by Volten et at. [2001] for red clay particles at the same wavelengths. [References: 49]
机译:我们介绍了三种矿物样品(粉煤灰,绿色粘土和红色粘土)在442和633 nm处随机取向的颗粒的整个散射矩阵的散射角分布测量。粉煤灰由近球形颗​​粒的聚集体组成,而绿色粘土和红色粘土颗粒则代表不规则的致密颗粒。我们将飞灰的测量结果与实验确定的平均散射矩阵进行比较,该矩阵基于对不规则矿物气溶胶颗粒的广泛选择的测量结果。我们发现,我们的接近球形颗粒聚集体的多分散样品的散射矩阵与紧密颗粒的散射矩阵有很大不同。另外,飞灰颗粒的散射矩阵的元素的角分布(F-22θ/F-11θ除外)似乎由单一单体决定。通过比较我们的绿色粘土颗粒实验结果与Volten等人获得的实验结果,也研究了成分上的微小差异对散射行为的影响。 [2001]对于相同波长的红粘土颗粒。 [参考:49]

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