Protoplanetary disk A resolved circumstellar disk was first identified in 1997 with the
Owens Valley Radio Observatory. The semi-major axis was initially estimated to be 110
AU. Observations with STIS revealed that the disk is much larger, with a radius of 450 AU, has an inclination of about °, and has a cleared central zone. An outer ring was discovered in scattered light with the
Very Large Telescope (VLT) instrument NACO. The ring was initially seen as broken. Later, observations with the
Gemini Planet Imager showed the complete ring. Notably, an offset exists between the star's position and the ring's outline. This is likely due to the scattered light on the disk's surface. A flared, inclined disk will make the ring appear to be offset. The scattered light images trace small dust grains.
Atacama Large Millimeter Array (ALMA) dust observations showed multiple rings. The ALMA dust observations trace larger dust grains in the midplane of the disk. High-resolution ALMA dust and CO images were presented in 2018 by the DSHARP team. This new image showed the previously known rings, an inner ring with a gap, and a dust crescent near the B67 ring. The outer disk shows time-variable illumination between 2011 (
Subaru) and 2016 (VLT/SPHERE). This time-dependent change is likely driven by shadows cast from the inner disk. New observations with STIS found an outer ring at 330 AU and also found time-variable changes. The disk has a total (gas+dust) mass of less than 0.35 , or between 0.01 and 0.15 . The B67 ring has a dust mass of 81 ±13 , and the B100 ring has a dust mass of .
Disk composition In 1999, observations between 3 and 15 μm from the
NASA Infrared Telescope Facility were published. The spectrum showed
silicate emission, consistent with an
olivine and
pyroxene mixture. The study suggested that this is evidence of grains that will be incorporated into
exocomets later. Observations with the
Infrared Space Observatory were published in 2000. The team found
amorphous silicates,
water ice,
iron oxide and a small fraction of very large (
mm to
cm-sized)
crystalline silicates.
Herschel/PACS observations detected warm
water and the
hydroxyl molecule. Observations with the
Submillimeter Array showed that the
carbon monoxide ice-line begins at around 155 AU. Later, ALMA observed carbon monoxide (CO) and other molecules in higher resolution. The CO snowline was detected with the help of DCO+ (
deuterated aldehyde). Another analysis of ALMA data found that
N2H+ emission is a better tracer of the CO snowline, and this line is located at 90 AU (at 25
Kelvin).
Formaldehyde was detected throughout the disk, but was found to be enhanced in the outer disk. This could be due to
hydrogenation of CO ices on dust grains and sublimation of formaldehyde from
UV-radiation. Alternatively, formaldehyde is more efficiently produced in the gas phase.
Methanol was not detected in the disk around HD 163296. The abundance of methanol is lower when compared to
TW Hydrae, likely due to a difference in stellar radiation. The water snowline has an upper limit of 8-20 AU from ALMA observations.
Possible exoplanets The gaps in the disk around HD 163296 are thought to be carved by newly formed planets. As of 2023, four planets in the disk have been proposed. Below are the gaps and an explanation of candidate planets in those gaps: D10 gap: One work suggests that a planet carves the gap with a mass of 0.35-0.71 . D45 gap: The crescent at 55 AU can be re-created by a 0.15 planet at 54 AU. Another work estimated the mass to be 1.07-2.18 from the size of the gap. Hydrodynamic simulations suggest a mass of 0.46 . Later modelling found that a Jupiter-mass planet can explain the crescent-shaped asymmetry at 48 AU. The crescent represents dust with a mass between 10 and 15 , trapped at
Lagrange point L5 of the planet. Carbon emission localized at the position of the proposed planet at the D45 gap could represent protoplanet inflow/outflow or disk winds. Another work suggests that two sub-Saturn planets are inside the D45 gap and in a 4:3
orbital resonance. The crescent is seen as dust trapped in the L5 point of the outer planet. D86 gap: Perturbations of the CO gas could be explained by a Jupiter-mass planet at 83 AU. One work suggests this planet could have a mass of 0.07-0.14 . A point-like source at 67 AU was identified from
Keck observations as a potential protoplanet with a mass of 6-7 . It might be less massive if a
circumplanetary disk surround the planet. The point-like Keck source was not detected
SPHERE imaging, excluding it as a massive planet. It could still be a lower-mass planet if the spectrum is very red. A velocity kink in CO gas suggests the presence of a planet at 94 ±6 AU with a mass of 1 . D141 gap: Two
Saturn-mass
exoplanets were inferred from the gas and dust depletion of the middle and outer dust rings seen by ALMA. These planets would reside at 100 and 160 AU. It is, however, possible that no exoplanets are present and that other effects cause this observation. Perturbations of the CO gas could be explained by Jupiter-mass planets at 137 AU. Another work suggests a mass of 0.46 , a distance of 105 AU, and another planet at 160 AU with a mass of 0.58 . A point-like candidate was detected with
NIRCam at 111 AU outside the B100 ring. This candidate is however at a different position compared to the velocity kink. A mass of 2-4 is suggested. Follow-up observations are needed to confirm this candidate. D270 gap: Another candidate was proposed from perturbation of the disk's gas, suggesting a 2 planet at around 260 AU. This candidate was not detected with SPHERE, but could not be excluded. The spiral structure of the CO gas is explained by the planet, producing a planetary
wake generated by
Lindblad resonances. == References ==