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VLT spectropolarimetry of the fast expanding type Ia SN 2006X

机译:VLT spectropolarimetry of the fast expanding type Ia SN 2006X

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Aims. The main goal of this study is to probe the ejecta geometry and to get otherwise unobtainable information about the explosionmechanism of type Ia Supernovae (SNe).Methods. Using VLT-FORS1 we performed optical spectropolarimetric observations of the type Ia SN 2006X on 7 pre-maximumepochs (day 10 to day 1) and one post-maximum epoch (+39 days).Results. The SN shows strong continuum interstellar polarization reaching about 8 at 4000 A, characterized by a wavelengthdependency that is substantially different from that of the Milky-Way dust mixture. Several SN features, like Si II 6355 A and theCa II IR triplet, present a marked evolution. The Ca II near-IR triplet shows a pronounced polarization (1.4) already on day 10in correspondence with a strong high-velocity feature (HVF). The Si II polarization peaks on day 6 at about 1.1 and decreasesto 0.8 on day 1. By day +39 no polarization signal is detected for the Si II line, while the Ca II IR triplet shows a marked repolarizationat the level of 1.2. As in the case of another strongly polarized SN (2004dt), no polarization was detected across theO I 7774 A absorption.Conclusions. The fast-expanding SN 2006X lies on the upper edge of the relation between peak polarization and decline rate, andit confirms previous speculations about a correlation between degree of polarization, expansion velocity, and HVF strength. Thepolarization of Ca II detected in our last epoch, the most advanced ever obtained for a type Ia SN, coincides in velocity with theouter boundary of the Ca synthesized during the explosion (15 000–17 000 km s1) in delayed-detonation models. This suggests alarge scale chemical inhomogeneity as produced by off-center detonations, a rather small amount of mixing, or a combination ofboth effects. In contrast, the absence of polarization at the inner edge of the Ca-rich layer (8000–10 000 km s1) implies a substantialamount of mixing in these deeper regions.

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