Clinging dust grains – Planetesimal belts are not only traced at long wavelengths
Nicole Pawellek
Max Planck Institute for Astronomy, Heidelberg, Germany


Debris discs are dusty belts of planetesimals around main-sequence stars, similar to comets and asteroids in the solar system. The planetesimals themselves cannot be observed directly, yet they produce detectable dust in mutual collisions. Observing this debris dust, we can try to infer properties of invisible planetesimals. Here we address the question of what is the best way to measure the location and extent of outer planetesimal belts, i.e., "Kuiper belts" that encompass extrasolar planetary systems. A standard method is using resolved images at millimetre wavelengths, which reveal dust grains of comparable sizes. This is because smaller dust particles seen in the infrared or optical are subject to a large array of non-gravitational forces that drag them away from their birth places, and so may not closely trace the parent bodies. In this study, we examine whether imaging of debris discs at shorter, far- or even mid-infrared, wavelengths with future facilities such as the James Webb Space Telescope, which offer high resolution, would allow one to determine the spatial location of the exo-Kuiper belts with sufficient accuracy. We find that around A-type stars, where the majority of debris discs is found, and even around G-type stars discs are brightest at the location of the birth ring in both the millimetre and the mid-infrared wavelength bands. Thus, we are able to trace planetesimal belts even at shorter wavelengths.