The Mineralogy and Structure of the Inner Debris Disk of {\beta} Pictoris
Dan Li, Charles M. Telesco, and Christopher M. Wright

TL;DR
This study uses mid-infrared spectroscopy and imaging to analyze the mineralogy and spatial distribution of dust in the inner debris disk of {eta} Pictoris, revealing detailed dust compositions and potential orbital motion of a dusty clump.
Contribution
It provides new spatially resolved spectral data on dust components and confirms the motion of a dusty clump, offering insights into disk structure and dynamics.
Findings
The 2.0-micron glassy olivine peaks at the disk center.
The 0.1-micron glassy olivine shows a double-peaked distribution.
A dusty clump at 52 AU exhibits potential Keplerian motion.
Abstract
We observed the edge-on, planet-bearing disk of {\beta} Pictoris using T-ReCS at Gemini to clarify and extend previous observations and conclusions about this unique system. Our spectroscopy and spectral modeling of the 10-micron silicate feature constrain the spatial distributions of three representative dust components (0.1-micron/2.0-micron glassy olivine and crystalline forsterite) across the inner 20-AU of the disk. We confirm that the 2.0-micron glassy olivine is strongly peaked in the disk center and that the 0.1-micron glassy olivine does not show this concentration, but rather is double peaked, with the peaks on either side of the star. However, we do not see the strong difference in brightness between those two peaks reported in a previous study. Although the spatial distribution of the 0.1-micron dust is consistent with the scenario of a dust-replenishing planetesimal belt…
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