کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
5429761 | 1397370 | 2011 | 13 صفحه PDF | دانلود رایگان |
![عکس صفحه اول مقاله: Model of light scattering by dust particles in the solar system: Applications to cometary comae and planetary regoliths Model of light scattering by dust particles in the solar system: Applications to cometary comae and planetary regoliths](/preview/png/5429761.png)
We analyze both the intensity and linear polarization of cosmic dust particles by using the physically exact superposition T-matrix method in a fixed orientation for various aggregates of spheres and DDA for the aggregates of Gaussian random spheres. We study both the spherical geometry (in cometary comae) and cylindrical slabs (for regoliths) up to 2000 monomers with size parameters less than â¼3. It is straightforward to produce the observed linear polarization in both geometries while the typically convex and strong opposition spike seems to require wide regolith geometries. The dependence of various parameters on light scattering has also been studied in a rather detailed form. In applications to the cometary polarization we can fit the data in six colors from UV to the J band at a very good accuracy. We, however, emphasize that we do not claim our model to be unique. The most important parameters here are the refractive index and the size distribution of submicron particles. Rest of the parameters has only a minor role. We also found that it is critically important to use several realizations from any assumed particle geometry model because corresponding scattering characteristics can vary quite a lot.
Research highlights⺠Fixed orientation superposition T-matrix method can handle larger geometries faster. ⺠Optimal cubature on the sphere-method performs well in orientation averaging. ⺠Two-parameter model was able to produce the linear polarization of the high-Pmax comets.
Journal: Journal of Quantitative Spectroscopy and Radiative Transfer - Volume 112, Issue 11, July 2011, Pages 1658-1670