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Imaging of the Vega Debris System using JWST/MIRI (2410.23636v1)

Published 31 Oct 2024 in astro-ph.EP

Abstract: We present images of the Vega planetary debris disk obtained at 15.5, 23, and 25.5 microns with the Mid-Infrared Instrument (MIRI) on JWST. The debris system is remarkably symmetric and smooth, and centered accurately on the star. There is a broad Kuiper-belt-analog ring at 80 to 170 au that coincides with the planetesimal belt detected with ALMA at 1.34 mm. The interior of the broad belt is filled with warm debris that shines most efficiently at mid-infrared along with a shallow flux dip/gap at 60 au from the star. These qualitative characteristics argue against any Saturn-mass planets orbiting the star outside of about 10 au assuming the unseen planet would be embedded in the very broad planetesimal disk from a few to hundred au. We find that the distribution of dust detected interior to the broad outer belt is consistent with grains being dragged inward by the Poynting-Robertson effect. Tighter constraints can be derived for planets in specific locations, for example any planet shepherding the inner edge of the outer belt is likely to be less than 6 Earth masses. The disk surface brightness profile along with the available infrared photometry suggest a disk inner edge near 3-5 au, disconnected from the sub-au region that gives rise to the hot near-infrared excess. The gap between the hot, sub-au zone and the inner edge of the warm debris might be shepherded by a modest mass, Neptune-size planet.

Summary

  • The paper presents detailed JWST/MIRI imaging of Vega, revealing a symmetric debris disk with a broad ring spanning 80–170 au.
  • The analysis constrains planetary influences by showing a lack of disk asymmetry, limiting the presence of Saturn-mass planets beyond 10 au.
  • The study identifies warm debris signatures and a shallow flux gap near 60 au, suggesting temperature and grain-size effects rather than strong gravitational disturbances.

Imaging of the Vega Debris System Using JWST/MIRI

Kate Y. L. Su et al. have conducted an extensive examination of the Vega debris system leveraging the JWST/MIRI to produce images at wavelengths of 15.5, 23, and 25.5 micrometers. This paper presents an in-depth analysis of the debris disk around Vega, one of the seminal systems exhibiting planetary debris, with particular attention to the structural characteristics and implications for planetary formation and dynamics.

Overview of the Vega Debris Disk

The investigation of Vega's disk, accentuated by JWST's superior resolution and sensitivity, reveals a remarkably symmetric and smooth disposition centered on the star. Notably, the disk exhibits a broad Kuiper-belt-like ring ranging from 80 to 170 au, consistent with planetesimal detections by ALMA at 1.34 mm. Additionally, the presence of warm debris is highlighted by an efficient mid-infrared signature and a discernible dip or gap in the surface flux at approximately 60 au.

The absence of significant asymmetry in the disk structure suggests stringent constraints on the mass and presence of any Saturn-mass planets beyond 10 au from the star. This is due to the lack of perturbative evidence that such massive bodies typically induce within debris disks.

Results and Implications

The data illuminate several crucial disk characteristics:

  • Temperature and Optical Depth: The paper extrapolates a distribution of dust temperatures and optical depth, indicating a possibly PR (Poynting-Robertson) drag-dominated nature for the inner disk. The researchers argue that the shallow gap detected might originate from the temperature and size effects rather than significant gravitational disturbances.
  • Constraining Inner Planetary Bodies: With the inner edge of the warm debris disk estimated to be around 3-5 au from the star, there remains a gap between this and the hot excess emission zone. This spacing could potentially be regulated by a Neptune-sized planet, though direct detection methods have not confirmed such bodies.
  • Disk Similarities and Differences: Comparing Vega's system with other well-studied debris disks like Fomalhaut reveals an intriguing contrast. While both systems exhibit mid-infrared emissions from dust interior to their cold belts, the Vega disk is smooth and centered, whereas Fomalhaut shows offset and asymmetrical features.

Conclusions and Future Work

The research emphasizes the constraints on planetary masses that the Vega system can elucidate, fostering deeper astronomical inquiries into disk-planet interactions. These findings offer a paradigm for comparison against less symmetric systems, such as Fomalhaut, and emphasize the need for further investigation into the infrared attributes of debris disks to uncover implicit planetary influences.

Future developments may involve more comprehensive simulations incorporating collisional behaviors and a broader spectrum of grain compositions to refine theories about planet-disk interactions and dust transport mechanisms in less massive debris environments. JWST/MIRI's capabilities thus not only enable a refined understanding of established debris systems but also set a benchmark for examining uncharted circumstellar environments where analogous dynamics may occur.

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