Inferring Magnetic Field Morphology and Dust Scattering Geometry from Mid-IR Polarimetry: the Extended Aitken Method
Frank Városi, Charles M. Telesco, Christopher M. Wright, Sergio José Fernández Acosta
TL;DR
The paper extends the Aitken method for mid-IR polarimetry by incorporating a graphite-scattering polarization template, enabling a three-component decomposition into absorptive, emissive, and scattering contributions. Applying this to CanariCam data for the Egg Nebula, W3 IRS5, and W51 IRS2 shows that scattering can dominate in some sightlines and that including it yields more accurate emissive/absorptive components and PA relations, particularly producing a PA difference between absorptive and emissive components that peaks near perpendicular, consistent with magnetic-field-aligned elongated grains. Where scattering is negligible, the extended method converges to the original Aitken results, underscoring its compatibility and robustness. The approach provides a practical framework for disentangling polarization mechanisms across at least three wavelengths bracketing the silicate feature, enabling improved magnetic field morphology inferences in diverse dust environments.
Abstract
The Aitken method is a useful approach for decomposing mid-IR polarimetry of silicates in astronomical sources into emissive and absorptive components. Here we extend this method to include the effects of polarization caused by scattering from graphite or similar particles along the same sightlines. To demonstrate the extended method, we apply it in the analysis of CanariCam multi-wavelength imaging polarimetry observations of the Egg Nebula, W3 IRS5, and W51 IRS2, and also spectropolarimetry of W3 IRS5. We compare these results with those obtained with the original Aitken method and show that the Egg Nebula observations are fit better when this third component is incorporated into the analysis. Polarimetry observations of W3 IRS5 are also fit better with the extended Aitken method, but the original method suffices to fit many sightlines. Observations of W51 IRS2 are fit well by either the original or extended Aitken method. Including scattering by dust in the decomposition of polarimetry observations of the Egg Nebula and W3 IRS5 produces better results for the emissive and absorptive components, and in particular for the position angle (PA) of those components. The distribution of the difference between absorptive and emissive PA is then found to be more peaked at a single angle, nearly perpendicular. This supports the theory that mid-IR polarization arises from elongated dust grains aligned along magnetic field lines, since then the PA of emissive and absorptive polarization would be perpendicular. When significant scattering is not present the extended method produces the same results as the original method.
