Multi-Epoch Observations of HD69830: High Resolution Spectroscopy and Limits to Variability

TL;DR

This study conducted multi-epoch high-resolution spectroscopy and photometry of HD69830, finding no significant variability in its dust and gas, and suggesting the dust originates outside the planets with a composition similar to C-type asteroids.

Contribution

First multi-epoch spectroscopic and photometric analysis of HD69830's debris system, constraining its variability, composition, and spatial distribution with high precision.

Findings

No significant variability in dust spectrum over 1 year.

Dust located outside the orbits of the three planets.

Dust composition similar to C-type asteroids.

Abstract

The main-sequence solar-type star HD69830 has an unusually large amount of dusty debris orbiting close to three planets found via the radial velocity technique. In order to explore the dynamical interaction between the dust and planets, we have performed multi-epoch photometry and spectroscopy of the system over several orbits of the outer dust. We find no evidence for changes in either the dust amount or its composition, with upper limits of 5-7% (1 $\sigma$ per spectral element) on the variability of the {\it dust spectrum} over 1 year, 3.3% (1 $\sigma$) on the broad-band disk emission over 4 years, and 33% (1 $\sigma$) on the broad-band disk emission over 24 years. Detailed modeling of the spectrum of the emitting dust indicates that the dust is located outside of the orbits of the three planets and has a composition similar to main-belt, C-type asteroids asteroids in our solar system. Additionally, we find no evidence for a wide variety of gas species associated with the dust. Our new higher SNR spectra do not confirm our previously claimed detection of H$_2$O ice leading to a firm conclusion that the debris can be associated with the break-up of one or more C-type asteroids formed in the dry, inner regions of the protoplanetary disk of the HD69830 system. The modeling of the spectral energy distribution and high spatial resolution observations in the mid-infrared are consistent with a $\sim$ 1 AU location for the emitting material.