Silicate Dust in the Environment of RS Ophiuchi following the 2006 Eruption

We present further Spitzer Space Telescope observations of the recurrent nova RS Ophiuchi, obtained over the period 208-430 days after the 2006 eruption. The later Spitzer IRS data show that the line emission and free-free continuum emission reported earlier is declining, revealing incontrovertible...

Full description

Saved in:
Bibliographic Details
Published in:The Astrophysical journal Vol. 671; no. 2; pp. L157 - L160
Main Authors: Evans, A, Woodward, C. E, Helton, L. A, van Loon, J. Th, Barry, R. K, Bode, M. F, Davis, R. J, Drake, J. J, Eyres, S. P. S, Geballe, T. R, Gehrz, R. D, Kerr, T, Krautter, J, Lynch, D. K, Ness, J.-U, O’Brien, T. J, Osborne, J. P, Page, K. L, Rudy, R. J, Russell, R. W, Schwarz, G, Starrfield, S, Tyne, V. H
Format: Journal Article
Language:English
Published: Chicago, IL IOP Publishing 20-12-2007
University of Chicago Press
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:We present further Spitzer Space Telescope observations of the recurrent nova RS Ophiuchi, obtained over the period 208-430 days after the 2006 eruption. The later Spitzer IRS data show that the line emission and free-free continuum emission reported earlier is declining, revealing incontrovertible evidence for the presence of silicate emission features at 9.7 and 18 mu m. We conclude that the silicate dust survives the hard radiation impulse and shock blast wave from the eruption. The existence of the extant dust may have significant implications for understanding the propagation of shocks through the red giant wind and likely wind geometry.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:1538-4357
0004-637X
1538-4357
DOI:10.1086/524944