Infrared spectroscopy of the 2019 eruption of the recurrent nova V3890 Sgr: separation into equatorial and polar winds revealed
A. Evans (Keele University, UK), T. R. Geballe (Gemini, Observatory/NSF's NOIRLab), C. E. Woodward (Minnesota Institute for, Astrophysics), D. P. K. Banerjee (Physical Research Laboratory, Ahmedabad,, India), R. D. Gehrz (Minnesota Institute for Astrophysics), S. Starrfield

TL;DR
This study analyzes infrared spectra from the 2019 eruption of recurrent nova V3890 Sgr, revealing distinct equatorial and polar wind components, their evolution, and coronal line phases, providing insights into the eruption dynamics.
Contribution
It is the first detailed infrared spectroscopic analysis of V3890 Sgr's eruption, distinguishing between equatorial and polar winds and characterizing coronal line phases.
Findings
Broad components originate from fast ejecta perpendicular to the binary plane.
Narrow components arise from material interacting with circumstellar matter.
Coronal gas temperature estimated at 9.3×10^5 K with near-solar abundances.
Abstract
We present infrared spectroscopy of the 2019 eruption of the recurrent nova V3890 Sgr, obtained over the period 5.1-46.3 days after the eruption. The spectrum of the red giant became more prominent as the flux declined, and by day 46.3 dominated the spectrum. Hydrogen and helium emission lines consisted of a narrow component superposed on a broad pedestal. The full width at half maximum of the narrow components declined with time as the eruption progressed, as , whereas those of the broad components remained essentially constant. Conversely, the line fluxes of the narrow components of Pa, remained roughly constant, while those of the broad components declined by a factor over a period of ~days. The behaviour of the broad components is consistent with them arising in unencumbered fast-flowing ejecta perpendicular to the binary plane, in…
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Taxonomy
TopicsAstrophysical Phenomena and Observations · High-pressure geophysics and materials
