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dc.contributor.authorMcCall, David Samuel
dc.date.accessioned2011-09-06T08:13:13Z
dc.date.available2011-09-06T08:13:13Z
dc.date.issued2011-09-06
dc.identifier.urihttp://hdl.handle.net/2299/6374
dc.description.abstractAn investigation into the light scattering properties of Saharan dust grains is presented. An electrodynamic trap has been used to levitate single dust particles. By adjusting the trap parameters, partial randomisation of the particle orientation has been introduced. While levitated, the particles were illuminated by a laser, and a rotating half-wave retarder enabled selection of vertically or horizontally polarized incident light. A laser diffractometer and linear photodiode array have been used to measure intensity at scattering angles between 0.5° and 177°. Combining these measurements with Fraunhofer diffraction as calculated for a range of appropriately-sized apertures allows the calculation of the phase function and degree of linear polarization. The phase functions and degree of linear polarisation for four case study particles are presented - the phase functions are found to be featureless across most of the scattering region, with none of the halo features or rainbow peaks associated with regularly shaped particles such as hexagonal columns or spheres. Particle models comprised of large numbers of facets have been constructed to resemble the levitated particles. Utilizing Gaussian random sphere methods, increasing levels of roughness have been added to the surfaces of these models. A Geometric Optics model and a related model, Ray Tracing with Diffraction on Facets, have been modified to calculate scattering on these particle reconstructions. Scattering calculations were performed on each of these reconstructions using a range of refractive indices and two rotation regimes – one where the orientations of the reconstructed particle were limited to match those observed when the particle was levitated, and one where the orientation was not limited. Qualitative comparisons are performed on the phase functions and degree of linear polarization, where it is observed that the addition of roughness to the modelled spheroids causes the computed phase functions to increasingly resemble those from the levitated particles. Limiting the orientation of the particles does not affect the scattering noticeably. The addition of a very small absorption coefficient does not change the comparisons considerably. As the absorption coefficient is increased, however, the quality of the comparisons decreases rapidly in all cases but one. The phase functions are quantitatively compared using RMS errors, and further comparison is performed using the asymmetry parameter.en_US
dc.language.isoenen_US
dc.subjectLight scatteringen_US
dc.subjectRay Tracingen_US
dc.subjectGeometric opticsen_US
dc.subjectRTDFen_US
dc.subjectLaseren_US
dc.subjectDiffractionen_US
dc.subjectModellingen_US
dc.subjectDust particlesen_US
dc.subjectRadiative forcingen_US
dc.subjectPhase functionen_US
dc.subjectSpatial subdivisionen_US
dc.subjectMineral dusten_US
dc.subjectSaharanen_US
dc.subjectRough surfaceen_US
dc.titleMeasurement and Modelling of Light Scattering by Small to Medium Size Parameter Airborne Particlesen_US
dc.typeThesisen_US
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