A Self-Consistent Model of the Circumstellar Debris Created by a Giant Hypervelocity Impact in the HD172555 System
B.C. Johnson, C.M. Lisse, C.H. Chen, H. J. Melosh, M.C. Wyatt, P., Thebault, W.G. Henning, E. Gaidos, L.T. Elkins-Tanton, J.C. Bridges, A., Morlok

TL;DR
This paper models the debris disk around HD 172555 as resulting from a giant hypervelocity impact, explaining the stable infrared excess despite rapid dust removal by radiation pressure.
Contribution
It presents a self-consistent model linking impact-generated debris with observed spectral features and dust stability in HD 172555.
Findings
Infrared excess is consistent with impact-created debris disk at 6 AU.
Radiation pressure should clear submicron dust in less than a year.
Solid SiO emission is a plausible explanation for the 8 um spectral feature.
Abstract
Spectral modeling of the large infrared excess in the Spitzer IRS spectra of HD 172555 suggests that there is more than 10^19 kg of sub-micron dust in the system. Using physical arguments and constraints from observations, we rule out the possibility of the infrared excess being created by a magma ocean planet or a circumplanetary disk or torus. We show that the infrared excess is consistent with a circumstellar debris disk or torus, located at approximately 6 AU, that was created by a planetary scale hypervelocity impact. We find that radiation pressure should remove submicron dust from the debris disk in less than one year. However, the system's mid-infrared photometric flux, dominated by submicron grains, has been stable within 4 percent over the last 27 years, from IRAS (1983) to WISE (2010). Our new spectral modeling work and calculations of the radiation pressure on fine dust in…
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