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LibraryM. Matsuura (Cardiff Univ.), K. Volk (STScI), P. Kavanagh (Maynooth Univ.), B. Balick (Univ. of Washington), R. Wesson (Cardiff Univ., Univ. Coll. London), A.A. Zijlstra (Univ. of Manchester, Macquarie Unif.) H.L. Dinerstein (Univ. of Texas), E. Peeters (Univ. of Western Ontario, SETI), N.C. Sterling (Univ. of W. Georgia), J. Cami (Univ. of Western Ontario, SETI), M.J. Barlow (Univ. Coll. London), J. Kastner (RIT), J.R. Walsh (ESO), L.B.F.M. Waters (Radbound Univ., SRON Netherlands Inst. for Space Res.), N. Hirano (ASIAA), and 22 others, including G.C. Sloan (STScI, UNC)
2025, MNRAS, in press
NGC 6302 is a spectacular bipolar planetary nebula (PN) whose spectrum exhibits fast outflows and highly ionized emission lines, indicating the presence of a very hot central star (~220,000 K). Its infrared spectrum reveals a mixed oxygen and carbon dust chemistry, displaying both silicate and polycyclic aromatic hydrocarbon (PAH) features. Using the JWST Mid-Infrared Instrument (MIRI) and Medium Resolution Spectrometer, a mosaic map was obtained over the core of NGC 6302, covering the wavelength range of 5-28 µm and spanning an area of ~18.5" x 15". The spatially resolved spectrum reveals ~200 molecular and ionized lines from species requiring ionisation potentials of up to 205 eV. The spatial distributions highlight a complex structure at the nebula's centre. Highly ionized species such as [Mg VII] and [Si VII] show compact structures, while lower-ionization species such as H+ extend much farther outwards, forming filament-defined rims that delineate a bubble. Within the bubble, the H+ and H2 emission coincide, while the PAH emission appears farther out, indicating an ionization structure distinct from typical photodissociation regions, such as the Orion Bar. This may be the first identification of a PAH formation site in a PN. This PN appears to be shaped not by a steady, continuous outflow, but by a series of dynamic, impulsive bubble ejections, creating local conditions conducive to PAH formation. A dusty torus surrounds the core, primarily composed of large (µm-sized) silicate grains with crystalline components. The long-lived torus contains a substantial mass of material, which could support an equilibrium chemistry and a slow dust-formation process.
Last modified 16 July, 2025. © Gregory C. Sloan and others.