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Constraining the Planetary System of Fomalhaut Using High-Resolution
                                                                        ALMA Observations

                                                        A. C. Boley12 , M. J. Payne1 , S. Corder3 , W. Dent4 , E. B. Ford1 , and M. Shabram1
arXiv:1204.0007v1 [astro-ph.EP] 30 Mar 2012




                                                                                               ABSTRACT


                                                           The dynamical evolution of planetary systems leaves observable signatures in
                                                       debris disks. Optical images trace micron-sized grains, which are strongly affected
                                                       by stellar radiation and need not coincide with their parent body population. Ob-
                                                       servations of mm-size grains accurately trace parent bodies, but previous images
                                                       lack the resolution and sensitivity needed to characterize the ringā€™s morphology.
                                                       Here we present ALMA 350 GHz observations of the Fomalhaut debris ring. These
                                                       observations demonstrate that the parent body population is 13-19 AU wide with
                                                       a sharp inner and outer boundary. We discuss three possible origins for the ring,
                                                       and suggest that debris conļ¬ned by shepherd planets is the most consistent with the
                                                       ringā€™s morphology.

                                                       Subject headings: Planet-disk interactions ā€” planetary systems ā€” Submillimeter:
                                                       planetary systems



                                                                                            1. Introduction

                                                   The Fomalhaut debris system is a natural laboratory for testing planet formation theories.
                                              The nearby (7.69 pc, Perryman et al. 1997) A3V star (Di Folco et al. 2004) is surrounded by
                                              an eccentric debris ring with a peak brightness in scattered optical light at a semi-major axis
                                              a āˆ¼ 140 AU (Kalas et al. 2005, henceforth K05). The inner edge is sharply truncated, which,
                                              along with the ringā€™s eccentricity, suggests that a planet is shaping the ringā€™s morphology (Wyatt

                                                 1
                                                     Department of Astronomy, University of Florida, 211 Bryant Space Science Center, Gainesville, FL, 32611
                                                 2
                                                     Sagan Fellow
                                                 3
                                                   North American ALMA Science Center, National Radio Astronomy Observatory, 520 Edgemont Road, Char-
                                              lottesville, VA, 22903
                                                 4
                                                     ALMA, Alonso de Cordova 3107, Vitacura, Santiago, Chile
ā€“2ā€“


et al. 1999; Quillen 2006; Chiang et al. 2009). A candidate for the reputed planet (Fom b) has
been discovered in the optical (Kalas et al. 2008). The observations are consistent with a super-
Earth mass planet embedded in a planetesimal swarm (Kennedy & Wyatt 2011).
      Independent of direct detection of any planet, observations of the ringā€™s morphology can
constrain the dynamical history of the Fomalhaut system, including properties of any planets
near the ring. The effect of radiation pressure on a dust grainā€™s orbital eccentricity, assuming
an initially circular orbit, is e = (2Ļs s/(Ļāˆž sāˆž ) āˆ’ 1)āˆ’1 , where Ļs is the grainā€™s internal density
and s the grain radius. Here, āˆž represents grains that are unbound by radiation pressure. For
Fomalhaut, sāˆž āˆ¼ 8Āµm for Ļāˆž āˆ¼ 1 g/cc. Most of the scattered optical light should be from
the smallest bound grains (between āˆ¼ 8 and 16Āµm, see Chiang et al. 2009). The expected free
eccentricity of a 16Āµm grain due to radiation pressure is āˆ¼ 0.3 (for Ļs = Ļāˆž ), while grain sizes
near 1 mm will have free eccentricities e < 0.01, making mm grains excellent tracers of parent
bodies. While previous observations of mm grain emission do detect large grains, they lack
the resolution needed to characterize the parent body morphology (Holland et al. 1998; Ricci
et al. 2012). Here, we present high-resolution 850 Āµm ALMA images that resolve the northern
section of Fomalhautā€™s ring.



                               2. Observations and Reduction:

     Fomalhautā€™s ring was observed using ALMA cycle 0 in the compact conļ¬guration, measur-
ing projected baselines from 14 to 175m (Table 1). Observations were centered on the expected
position of Fom b at RA = 22h:57m:38.65s and Ī“ = -29d:37ā€™:12.6ā€ (J2000, proper motion in-
cluded). The total on-source integration time was 140 min. The observations were taken at 357
and 345 GHz (in the upper and lower sidebands) using the Frequency Domain Mode in dual
polarization with 4Ɨ1875 MHz bandpasses (2 in each of the sidebands). Neptune was used
as an absolute ļ¬‚ux calibrator, and J1924-292 for bandpass calibration. Atmospheric variations
at each antenna were monitored continuously using Water Vapor Radiometers (WVR), as well
as regular hot/ambient load measurements. For time-dependent gain calibration, the nearby
quasar J2258-279 was observed every 8 minutes. Data were reduced using CASA 3.4 (Mc-
Mullin et al. 2007): calibration involved removing the effects of rapid atmospheric variations
at each antenna using the WVR data, correcting the time- and frequency-dependence of system
temperature, and correcting for the complex antenna-based bandpass and time-dependent gain.
Amplitude calibration used the CASA Butler-JPL-Horizons 2010 model for Neptune, which
gives an estimated systematic ļ¬‚ux uncertainty of Ā±10%. The calibrated measurement set was
spectrally binned to a channel spacing of 49MHz, and then CLEANed using the Cotton-Schwab
algorithm, combining all channels to give the ļ¬nal continuum image. The primary beam cor-
ā€“3ā€“


rection (PBC) was performed using the voltage pattern for an Airy function in with an effective
dish diameter of 10.7 m, a blockage diameter of 0.75 m, a maximum radius of 1.784ā—¦ , and a
reference frequency of 1 GHz (see CASA functions vp.setpbairy and sm.setvp).



                                                   3. Results

     In Figure 1 we present the cleaned and primary beam-corrected images. We refer to these
as the uncorrected and corrected images, respectively. In the uncorrected image, the peak bright-
ness is āˆ¼ 0.84 mJy beamāˆ’1 , the total ļ¬‚ux density of the image is 20.5 mJy, and the RMS is
āˆ¼ 60 ĀµJy beamāˆ’1 (0.32 mK)1 . The synthesized beam is āˆ¼ 1.5 Ɨ 1.2 with position angle 77ā—¦ .
      The corrected image shows all emission to 7% power, which includes the ring and all
apparent emission related to the star. The total ļ¬‚ux in the corrected image is 45.5 mJy. The
projected image accounts for approximately half of the ring, so assuming equal brightness for
the second half and accounting for the expected contribution from the star (3 mJy), we ļ¬nd a
total ļ¬‚ux density of āˆ¼ 85 mJy, reasonably consistent with previous measurements (81 Ā± 7.2 and
97 Ā± 5 mJy Holland et al. 1998, 2003). Almost all of the emission is conļ¬ned to a thin ring.
      The ringā€™s surface brightness reaches a maximum of 1.54 mJy beamāˆ’1 near the ansa2 and
remains bright through the inferred apocenter. There also appears to be a reduction in the ring
brightness to the SW. We will discuss the signiļ¬cance of these azimuthal variations below. The
starā€™s peak brightness is 3.4 mJy beamāˆ’1 and has a ļ¬‚ux density āˆ¼ 4.4 mJy (3 mJy expected
for a blackbody photosphere), which suggests possible excess emission. We caution that the
measurement of total stellar ļ¬‚ux is strongly dependent on the PBC. Nonetheless, a detection of
excess emission is consistent with the results of (Stapelfeldt et al. 2004). The PBC error would
need to be 47% at the 10% power point to account for the excess, more than 4 times the ALMA
beam speciļ¬cation which has yet to be completely veriļ¬ed.
     Without the second ansa, we cannot reliably determine the ellipse. We show in Figure 1
two ellipse segments that are based on ļ¬ts to optical images (K05).The center for both ellipses,
denoted by the plus sign, is 0.29ā€ W and 1.7ā€ N of the star. The ellipses have a semi-major axis
a = 18.31ā€ and a position angle (PA = 336ā—¦ ). Assuming the ellipses represent sky-projected
circles, the red ellipse has an inclination of i = 66ā—¦ (K05) and the blue 67ā—¦ , which more closely

   1
    Unless otherwise stated, relative errors are assumed to be equal to the RMS value of 60ĀµJy beamāˆ’1 . Flux
densities are only expected to be good to about 10%.
   2
     Ansa refers to the sky-projected section of an astrophysical ring that is farthest from its central body, tradia-
tionally referring to planetary rings.
ā€“4ā€“


corresponds to our best-ļ¬t sky models (below).
     Surface brightness proļ¬les of the ring (Fig. 2) are taken along the 7 slices shown in Figure
1 using bilinear interpolation. Each slice can be ļ¬t by a single Gaussian except slice 4, which
requires a double Gaussian due to elongated emission. Altogether the slices, excluding slice 4,
have a combined FWHM āˆ¼ 2.19ā€, corresponding to a projected parent body width āˆ¼ 17 AU,
well-resolved by the synthesized beam.
     Deprojected slices through the corrected and uncorrected images at the ringā€™s ansa are
shown in Figure 2, which includes all points within Ā±2ā—¦ of the PA. The FWHM = 1.87 Ā± 0.03
and 1.85 Ā± 0.03 for the corrected and uncorrected proļ¬les, respectively. The surface brightness
in the corrected image peaks at āˆ¼ 18.4 (141.5 AU). The peak is similar to that found for the
small grains seen in the optical light radial brightness proļ¬le (K05), but the mm grains are much
more tightly conļ¬ned, consistent with radiation pressure effects.
      We estimate the mm grain mass by assuming the ring is optically thin and comprised of
grains with s āˆ¼ 1 mm and Ļs āˆ¼ 2.5 g/cc. The grain temperature Tg ā‰ˆ 0.7Tstar (Rstar /D)1/2 ,
where Tstar = 8750 K and Rstar = 1.82R are the stellar temperature and radius (Di Folco
et al. 2004), respectively. At D = 140 AU, Tg ā‰ˆ 48 K. The ringā€™s total ļ¬‚ux density of 82 mJy
(excluding the expected 3 mJy from the star), so Mmm āˆ¼ 0.017 MāŠ• .
     If collisions are the main removal mechanism of mm grains, then a lower limit can be
placed on the parent body mass Mpbdy /tage āˆ¼ Mmm /tcoll for ring age tage and mm-grain colli-
sion timescale tcoll āˆ¼ (Ļ„ ā„¦)āˆ’1 . The vertical optical depth through the ring can be estimated by
Ļ„ āˆ¼ (surface brightness/ļ¬‚ux density per grain)(Ļ€s2 ). The peak of the ringā€™s surface bright-
ness is āˆ¼ 1 mJy beamāˆ’1 . The synthesized beam effective area is āˆ¼ 2 AU2 at 7.69 pc. For
s āˆ¼ 1 mm and Tg āˆ¼ 48K, Ļ„ āˆ¼ 10āˆ’4 . At 140 AU, tcoll āˆ¼ 2 Myr. Combined with the above
                                                              Ė™
mass estimate, the ring should be losing mass at a rate of M āˆ¼ 0.01MEarth Myrāˆ’1 , requiring
Mpbdy > 1.7MEarth (for tage = 200 Myr), consistent with (Chiang et al. 2009).
     Best-ļ¬t models for the spatial distribution of mm grains are selected by minimizing the
difference between model and ALMA visibilities, where the u-v plane sampling from the ob-
servations is used in CASA to observe each model (tool sm.predict). Ring models are produced
using the following assumptions: (1) The ring is circular and has an offset relative to the star
that is in agreement with the deprojected ellipse models (see Fig. 1), approximating a grain
orbital eccentricity āˆ¼ 0.1. (2) The ring is uniform in azimuth. (3) The radial proļ¬le for mm
grains is described by either a Gaussian distribution in semi-major axes or a power law in sur-
face density. For the Gaussian, the FWHM is varied from 9.4 to 21 AU, and the inner radial
half-maximum point from 131 to 140 AU. For power law surface density proļ¬les, the annular
width is varied from 10 to 30 AU, the inner edge from 133 to 138 AU, and the power law index
ā€“5ā€“


from -9.5 to -1.5. (4) The vertical distribution for grains follows an exponential decay with a
scale height given by a constant angle above the midplane between 0 and 2.5ā—¦ . In each model,
the emission from grains at a given distance from the star is calculated from the Planck function
with the grain temperature Tg determined as described above. The total ļ¬‚ux density for the ring
at 850Āµm is normalized to either 80, 90, or 100 mJy. The starā€™s ļ¬‚ux is set to 3 mJy. Each model
is projected onto the sky with PA = 336ā—¦ and i = 66 to 67.5ā—¦ . The model ringā€™s apocenter is
set to the inferred apocenter of Fomalhautā€™s ring. It should be noted that models of a uniform
ring can become brighter near the ansae due to projection effects. Smooth, symmetric models
cannot, however, account for the excess brightness near apocenter. Such brightening could be
explained by variations in the mass distribution of grains or by variations in ringā€™s radial thick-
ness. Collisions between parent bodies could also produce asymmetries (Wyatt & Dent 2002).


     The best-ļ¬t models with a Gaussian semi-major axis distribution have a scale height cor-
responding to an opening angle of 1.0ā—¦ Ā± 0.25, a FWHM = 16 Ā± 3 AU, and an inner radial
half-maximum at 135+0.5 AU. The 1-Ļƒ errors for model parameters are estimated by including
                       āˆ’1
models for which āˆ†Ļ‡2 < 1. Models with i = 66.75ā—¦ and a total ļ¬‚ux density of 80 mJy are
preferred. Most of the dimming in the SW is consistent with a loss of sensitivity (Fig. 1). The
appearance of a hole may be due to brightening in the southern-most part of the ring, which
may be due to noise. The NE is not subtracted in the residual image (Fig. 1, bottom-right) and
contains contiguous excess surface brightness. The star is also not well-subtracted, suggesting
possible excess. Some of the extended surface brightness noted in slice 4 of Fig. 1 remains, but
is consistent with a high-noise peak.
     Some select, steep power law surface density proļ¬les are also consistent with the data.
These are limited to a surface density āˆ rāˆ’8.5 , an inner edge of 135+1 AU, an opening angle
                                                                     āˆ’1.5
   ā—¦                                 ā—¦
1.0 Ā± 0.5, and a preferred i = 67.25 . For these power laws, the half-maximum width is about
11.4 AU.



                                         4. Discussion

     Any formation mechanism for Fomalhautā€™s ring must address the following constraints:
(a) The ring has an eccentricity āˆ¼ 0.1. (b) The vertical scale height of the parent bodies is
consistent with an opening angle of āˆ¼ 1.0ā—¦ from the midplane. (c) The FWHM of the parent
bodies for the Gaussian model is āˆ¼ 16 AU, giving a width-to-height aspect ratio āˆ¼ 7. (d) The
outer edge of the parent bodies is consistent with being as sharply truncated as the inner edge.
(e) The micron grains are more radially extended than the parent bodies, but this is satisļ¬ed for
ā€“6ā€“


a variety of models due to radiation pressure. We consider three formation models. One is that
the ring is sculpted by a single interior planet (Wyatt et al. 1999; Kalas et al. 2005; Quillen 2006;
Kalas et al. 2008; Chiang et al. 2009). To account for requirement (d), this solution requires an
abrupt truncation of the outer disk through, for example, a stellar ļ¬‚yby (Ida et al. 2000). We
will return to this scenario below.
      Another possible model is that the ring is a remnant from a collision between two plan-
ets (Mamajek & Meyer 2007). Unless constrained, the radial width of the ring will slowly
spread due to collisions between ring particles with different semi-major axes. Take the ver-
tical velocity dispersion Ī“vz āˆ¼ vK sin i for Keplerian orbital speed vK . If the radial velocity
dispersion is of the same order, then the typical a difference between two colliding particles is
Ī“a āˆ¼ aĪ“e to factors of order unity, which for free eccentricity Ī“e āˆ¼ sin i is the scale height of
the disk, h. The effective collisional viscosity of the ring Ī½c āˆ¼ h2 /tcoll . Using a scale height
of 2.5 AU and a collisional time between mm grains of 2 Myr, Ī½c āˆ¼ 2.2 Ɨ 1013 cm2 /s, which
means the ring is diffusing on timescales āˆ¼ 90 Myr. If the ring is younger than the star, no
planetary inļ¬‚uence is necessary apart from the dynamics that led to the collision. However,
shattering gravitationally bound objects requires impact speeds several times the mutual escape
         2
speed (vesc = 2G(M1 + M2 )/(R1 + R2 ), for bodies with masses M1 and M2 and radii R1 and
R2 ). (Asphaug 2010; Leinhardt & Stewart 2012). For two 1MEarth planets (Mpbdy 1MEarth
for tage āˆ¼ 90 Myr), vesc āˆ¼ 11 km/s. The orbital escape speed at 140 AU from Fomalhaut is only
about 5 km/s. The impact speeds necessary to destroy Earths are not attainable.
      Finally, we propose a third formation model in which the ringā€™s morphology is dominated
by shepherd planets, analogous to the shepherd moons Cordelia and Ophelia of Uranusā€™s
ring (Goldreich & Tremaine 1979; Smith et al. 1986). Here, the ring is conļ¬ned by angular
momentum exchange between ring particles and the planets. We explore this possibility with
N-body simulations, using the Bulirsch-Stoer algorithm in Mercury (Chambers 1999). In each
simulation, two planets of mass Minner and Mouter are placed at ainner and aouter relative to
the 2.3 M star. Their relative inclinations are set to zero. Planet eccentricities are set to force
the planetesimals (see method in Chiang et al. 2009) at āˆ¼ 143 AU to have the eccentricity
observed for the ring (āˆ¼ 0.11). For each run, 105 massless particles are placed between rinner
and router with a surface density proļ¬le āˆ rāˆ’1 , where rinner = max(125 AU, ainner +1 AU) and
router = min(160 AU, aouter āˆ’ 1 AU). The integrations run for 108 years. Massless particles
are removed from simulations if the particle collides with a planet or if its radius from the star
exceeds 105 AU.
    The masses of the planets set the steepness and skew of the ringā€™s radial proļ¬le (Fig. 3).
Mutual perturbations will cause the system to evolve, which narrows parameter space by de-
manding that interactions between the planets do not destroy the ring. In the massless ring-
ā€“7ā€“


particle limit, either both planets must be < 3MEarth , or they must have an extreme mass ratio.
The planets do not need to be in resonance. A super-Earth and a Mars-mass planet produce
the most narrowly-peaked Gaussian for the radial parent body distribution among the simula-
tions presented here. As the masses for shepherd candidates are comparable to the minimum
estimated parent body mass in the ring, self-gravity of the ring may play a role in the systemā€™s
evolution. If the scattered optical light observations have detected Fom b, then the candidate
could be the innermost shepherd, although there is a discrepancy of āˆ¼ 10 AU between Fom bā€™s
proposed a and the inner shepherd in our models.
      Fomalhautā€™s debris has some similarities to the Kuiper belt. Both systems are thin rings,
āˆ†r/a āˆ¼ 0.1, which seem to owe their morphologies, at least in part, to the presence of planets.
There are nonetheless substantial differences. The outer edge of the Kuiper belt is near the 2:1
resonance with Neptune (Trujillo & Brown 2001). For the outer edge of Fomalhautā€™s ring to
be at the 2:1 resonance with an interior planet, the planet would need to have an a āˆ¼ 95 AU.
To truncate the ring at this location, the planet would need to be     3MJ (Chiang et al. 2009)
and could have been decected by Spitzer (Janson et al. 2012). If the ring had formed due to
outward migration of an interior planet, we would expect particles to be trapped in resonances,
like the Plutinos in the 3:2 resonance with Neptune. We detect only a single ring. The Kuiper
belt has a vertical thickness given by a dynamically hot and cold population with Gaussian
widths Ļƒ = 17ā—¦ Ā± 3 and Ļƒ = 2.2ā—¦ +0.2 , respectively (Brown 2001). While the Kuiper belt object
                                    āˆ’0.6
inclination distribution seems to be consistent with truncation due to a stellar ļ¬‚yby (Ida et al.
2000), Fomalhautā€™s parent body population may be too cold to be explained by this mechanism.
This leads us to favor shepherd planets as the explanation for the ringā€™s morphology.


     We thank Paul Kalas and the referee for helpful comments and ALMA NAASC for techni-
cal support. A.C.Bā€™s support was provided under contract with the California Institute of Tech-
nology funded by NASA through the Sagan Fellowship Program. M.J.P.ā€™s and E.C.B.ā€™s con-
tributions are supported by the National Science Foundation (NSF) under grant no. 0707203.
M.S.ā€™s support was provided in part by the National Radio Astronomy Observatory (NRAO)
through award SOSPA0-007. The NRAO is a facility of the NSF operated under cooperative
agreement by Associated Universities, Inc. This paper makes use of the following data from the
Atacama Large Millimeter/submillimeter Array (ALMA): ADS/JAO.ALMA#2011.0.00191.S.
The Joint ALMA Observatory is a partnership of the European Organization for Astronom-
ical Research in the Southern Hemisphere, the National Astronomical Observatory of Japan
(on behalf of the National Institutes of Natural Sciences and Academia Sinica), and the NRAO
(managed by Associated Universities, Inc. on behalf of the NSF and the National Research
Council of Canada) in cooperation with the Republic of Chile.
ā€“8ā€“


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   This preprint was prepared with the AAS L TEX macros v5.2.
                                            A
ā€“ 10 ā€“




Table 1: Observing Log: Target Fomalhautā€™s Ring and Fomalhaut b.   The precipitable water
vapor (PWV) is given in mm.
                 Date         Time        On-Source Antennas       PWV
                 dd/mm/yyyy (UTC)            (min)
                 22/09/2011   23:45:00.0      25         13        0.63
                 23/09/2011   00:49:30.0      25         13        0.48
                 23/09/2011   02:08:15.3      25         13        0.80
                 18/10/2011   03:31:00.9      25         15        0.62
                 18/10/2011   04:42:55.6      20         15        0.63
                 18/10/2011   05:44:40.4      20         15        0.57
ā€“ 11 ā€“




Fig. 1.ā€” Top-left: 350 GHz ALMA image of Fomalhautā€™s ring. The RMS noise is
āˆ¼ 60 ĀµJy beamāˆ’1 , and the contours represent 0.24, 0.33, 0.47, 0.66, 0.92, and 1.4 mJy beamāˆ’1 .
The circles are centered on the pointing center, and their diameters show the beamā€™s half and
7% power. Ellipses with PA = 336ā—¦ , and i = 66ā—¦ (red) and 67ā—¦ (blue) are shown, with the
ellipse centers given by the plus sign. The slices labeled 1-7 are used to show surface brightness
proļ¬les in Figure 2. The coordinate axis is centered on the star, which has a peak brightness of
0.49 mJy beamāˆ’1 (uncorrected). Top-right: The primary beam corrected image. The ring be-
comes bright near the ansa, and remains bright through the inferred apocenter. The contours are
the same as in the top-left, but begin at 0.47 mJy beamāˆ’1 . Bottom-left: The best-ļ¬t skymodel
is compared with the dirty ALMA image. The grayscale and contours show mJy beamāˆ’1 , with
the contour levels labeled on the colorbar. Bottom-right: The residual of the data minus the
model. The model subtracts the emission well, but there remains excess emission in the NE and
around the star.
ā€“ 12 ā€“




                                                     AU From Gaussian Peak                                                                AU From Ellipse Center
                                       -20   -15   -10  -5    0     5     10     15      20                              100   110       120 130 140 150 160                170   180
                                                                                1
                             1                                                  2                            1.5
                                                                                3                                             PB Corr
 Peak-Normalized Emission




                                                                                4                                         No PB Corr
                            0.8                                                                                      Normalized Slices
                                                                                5
                                                                                6
                                                                                                               1
                                                                                                                                                                      K05
                                                                                                  mJy/beam


                            0.6                                                 7
                                                                               Fit
                                                                                                             0.5
                            0.4
                                                                                                                         2 X RMS
                            0.2                                                                                0

                             0
                                                                                                             -0.5
                                  -3         -2       -1       0         1           2        3                     12         14          16       18        20            22      24
                                                    Arsec From Gaussian Peak                                                             Arcsec From Ellipse Center



Fig. 2.ā€” Left: Normalized surface brightness proļ¬les for slices 1-7 in Fig. 1. All proļ¬les
except slice 4 can be ļ¬t by a single Gaussian. A ļ¬t through all slices, excluding slice 4, is
shown with the dot-dot curve. Right: The deprojected radial surface brightness proļ¬le through
the ansa for the corrected and uncorrected data. Black curves show corresponding Gaussian
ļ¬ts. The heavy-dashed curve shows the scaled scattered optical light proļ¬le (K05). The dot-
dot curve shows the scaled Gaussian ļ¬t for the combined slices in the left panel.
ā€“ 13 ā€“




Fig. 3.ā€” Radial proļ¬les for a ring of parent bodies between two planets. Left-to-right:
Minner = 6MEarth and Minner = 3MEarth . Top-to-bottom: Mouter = Minner , Mouter =
Minner /3, and Mouter = Minner /10. Each color represents a proļ¬le-planet pair. The gray
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Eso1216

  • 1. Constraining the Planetary System of Fomalhaut Using High-Resolution ALMA Observations A. C. Boley12 , M. J. Payne1 , S. Corder3 , W. Dent4 , E. B. Ford1 , and M. Shabram1 arXiv:1204.0007v1 [astro-ph.EP] 30 Mar 2012 ABSTRACT The dynamical evolution of planetary systems leaves observable signatures in debris disks. Optical images trace micron-sized grains, which are strongly affected by stellar radiation and need not coincide with their parent body population. Ob- servations of mm-size grains accurately trace parent bodies, but previous images lack the resolution and sensitivity needed to characterize the ringā€™s morphology. Here we present ALMA 350 GHz observations of the Fomalhaut debris ring. These observations demonstrate that the parent body population is 13-19 AU wide with a sharp inner and outer boundary. We discuss three possible origins for the ring, and suggest that debris conļ¬ned by shepherd planets is the most consistent with the ringā€™s morphology. Subject headings: Planet-disk interactions ā€” planetary systems ā€” Submillimeter: planetary systems 1. Introduction The Fomalhaut debris system is a natural laboratory for testing planet formation theories. The nearby (7.69 pc, Perryman et al. 1997) A3V star (Di Folco et al. 2004) is surrounded by an eccentric debris ring with a peak brightness in scattered optical light at a semi-major axis a āˆ¼ 140 AU (Kalas et al. 2005, henceforth K05). The inner edge is sharply truncated, which, along with the ringā€™s eccentricity, suggests that a planet is shaping the ringā€™s morphology (Wyatt 1 Department of Astronomy, University of Florida, 211 Bryant Space Science Center, Gainesville, FL, 32611 2 Sagan Fellow 3 North American ALMA Science Center, National Radio Astronomy Observatory, 520 Edgemont Road, Char- lottesville, VA, 22903 4 ALMA, Alonso de Cordova 3107, Vitacura, Santiago, Chile
  • 2. ā€“2ā€“ et al. 1999; Quillen 2006; Chiang et al. 2009). A candidate for the reputed planet (Fom b) has been discovered in the optical (Kalas et al. 2008). The observations are consistent with a super- Earth mass planet embedded in a planetesimal swarm (Kennedy & Wyatt 2011). Independent of direct detection of any planet, observations of the ringā€™s morphology can constrain the dynamical history of the Fomalhaut system, including properties of any planets near the ring. The effect of radiation pressure on a dust grainā€™s orbital eccentricity, assuming an initially circular orbit, is e = (2Ļs s/(Ļāˆž sāˆž ) āˆ’ 1)āˆ’1 , where Ļs is the grainā€™s internal density and s the grain radius. Here, āˆž represents grains that are unbound by radiation pressure. For Fomalhaut, sāˆž āˆ¼ 8Āµm for Ļāˆž āˆ¼ 1 g/cc. Most of the scattered optical light should be from the smallest bound grains (between āˆ¼ 8 and 16Āµm, see Chiang et al. 2009). The expected free eccentricity of a 16Āµm grain due to radiation pressure is āˆ¼ 0.3 (for Ļs = Ļāˆž ), while grain sizes near 1 mm will have free eccentricities e < 0.01, making mm grains excellent tracers of parent bodies. While previous observations of mm grain emission do detect large grains, they lack the resolution needed to characterize the parent body morphology (Holland et al. 1998; Ricci et al. 2012). Here, we present high-resolution 850 Āµm ALMA images that resolve the northern section of Fomalhautā€™s ring. 2. Observations and Reduction: Fomalhautā€™s ring was observed using ALMA cycle 0 in the compact conļ¬guration, measur- ing projected baselines from 14 to 175m (Table 1). Observations were centered on the expected position of Fom b at RA = 22h:57m:38.65s and Ī“ = -29d:37ā€™:12.6ā€ (J2000, proper motion in- cluded). The total on-source integration time was 140 min. The observations were taken at 357 and 345 GHz (in the upper and lower sidebands) using the Frequency Domain Mode in dual polarization with 4Ɨ1875 MHz bandpasses (2 in each of the sidebands). Neptune was used as an absolute ļ¬‚ux calibrator, and J1924-292 for bandpass calibration. Atmospheric variations at each antenna were monitored continuously using Water Vapor Radiometers (WVR), as well as regular hot/ambient load measurements. For time-dependent gain calibration, the nearby quasar J2258-279 was observed every 8 minutes. Data were reduced using CASA 3.4 (Mc- Mullin et al. 2007): calibration involved removing the effects of rapid atmospheric variations at each antenna using the WVR data, correcting the time- and frequency-dependence of system temperature, and correcting for the complex antenna-based bandpass and time-dependent gain. Amplitude calibration used the CASA Butler-JPL-Horizons 2010 model for Neptune, which gives an estimated systematic ļ¬‚ux uncertainty of Ā±10%. The calibrated measurement set was spectrally binned to a channel spacing of 49MHz, and then CLEANed using the Cotton-Schwab algorithm, combining all channels to give the ļ¬nal continuum image. The primary beam cor-
  • 3. ā€“3ā€“ rection (PBC) was performed using the voltage pattern for an Airy function in with an effective dish diameter of 10.7 m, a blockage diameter of 0.75 m, a maximum radius of 1.784ā—¦ , and a reference frequency of 1 GHz (see CASA functions vp.setpbairy and sm.setvp). 3. Results In Figure 1 we present the cleaned and primary beam-corrected images. We refer to these as the uncorrected and corrected images, respectively. In the uncorrected image, the peak bright- ness is āˆ¼ 0.84 mJy beamāˆ’1 , the total ļ¬‚ux density of the image is 20.5 mJy, and the RMS is āˆ¼ 60 ĀµJy beamāˆ’1 (0.32 mK)1 . The synthesized beam is āˆ¼ 1.5 Ɨ 1.2 with position angle 77ā—¦ . The corrected image shows all emission to 7% power, which includes the ring and all apparent emission related to the star. The total ļ¬‚ux in the corrected image is 45.5 mJy. The projected image accounts for approximately half of the ring, so assuming equal brightness for the second half and accounting for the expected contribution from the star (3 mJy), we ļ¬nd a total ļ¬‚ux density of āˆ¼ 85 mJy, reasonably consistent with previous measurements (81 Ā± 7.2 and 97 Ā± 5 mJy Holland et al. 1998, 2003). Almost all of the emission is conļ¬ned to a thin ring. The ringā€™s surface brightness reaches a maximum of 1.54 mJy beamāˆ’1 near the ansa2 and remains bright through the inferred apocenter. There also appears to be a reduction in the ring brightness to the SW. We will discuss the signiļ¬cance of these azimuthal variations below. The starā€™s peak brightness is 3.4 mJy beamāˆ’1 and has a ļ¬‚ux density āˆ¼ 4.4 mJy (3 mJy expected for a blackbody photosphere), which suggests possible excess emission. We caution that the measurement of total stellar ļ¬‚ux is strongly dependent on the PBC. Nonetheless, a detection of excess emission is consistent with the results of (Stapelfeldt et al. 2004). The PBC error would need to be 47% at the 10% power point to account for the excess, more than 4 times the ALMA beam speciļ¬cation which has yet to be completely veriļ¬ed. Without the second ansa, we cannot reliably determine the ellipse. We show in Figure 1 two ellipse segments that are based on ļ¬ts to optical images (K05).The center for both ellipses, denoted by the plus sign, is 0.29ā€ W and 1.7ā€ N of the star. The ellipses have a semi-major axis a = 18.31ā€ and a position angle (PA = 336ā—¦ ). Assuming the ellipses represent sky-projected circles, the red ellipse has an inclination of i = 66ā—¦ (K05) and the blue 67ā—¦ , which more closely 1 Unless otherwise stated, relative errors are assumed to be equal to the RMS value of 60ĀµJy beamāˆ’1 . Flux densities are only expected to be good to about 10%. 2 Ansa refers to the sky-projected section of an astrophysical ring that is farthest from its central body, tradia- tionally referring to planetary rings.
  • 4. ā€“4ā€“ corresponds to our best-ļ¬t sky models (below). Surface brightness proļ¬les of the ring (Fig. 2) are taken along the 7 slices shown in Figure 1 using bilinear interpolation. Each slice can be ļ¬t by a single Gaussian except slice 4, which requires a double Gaussian due to elongated emission. Altogether the slices, excluding slice 4, have a combined FWHM āˆ¼ 2.19ā€, corresponding to a projected parent body width āˆ¼ 17 AU, well-resolved by the synthesized beam. Deprojected slices through the corrected and uncorrected images at the ringā€™s ansa are shown in Figure 2, which includes all points within Ā±2ā—¦ of the PA. The FWHM = 1.87 Ā± 0.03 and 1.85 Ā± 0.03 for the corrected and uncorrected proļ¬les, respectively. The surface brightness in the corrected image peaks at āˆ¼ 18.4 (141.5 AU). The peak is similar to that found for the small grains seen in the optical light radial brightness proļ¬le (K05), but the mm grains are much more tightly conļ¬ned, consistent with radiation pressure effects. We estimate the mm grain mass by assuming the ring is optically thin and comprised of grains with s āˆ¼ 1 mm and Ļs āˆ¼ 2.5 g/cc. The grain temperature Tg ā‰ˆ 0.7Tstar (Rstar /D)1/2 , where Tstar = 8750 K and Rstar = 1.82R are the stellar temperature and radius (Di Folco et al. 2004), respectively. At D = 140 AU, Tg ā‰ˆ 48 K. The ringā€™s total ļ¬‚ux density of 82 mJy (excluding the expected 3 mJy from the star), so Mmm āˆ¼ 0.017 MāŠ• . If collisions are the main removal mechanism of mm grains, then a lower limit can be placed on the parent body mass Mpbdy /tage āˆ¼ Mmm /tcoll for ring age tage and mm-grain colli- sion timescale tcoll āˆ¼ (Ļ„ ā„¦)āˆ’1 . The vertical optical depth through the ring can be estimated by Ļ„ āˆ¼ (surface brightness/ļ¬‚ux density per grain)(Ļ€s2 ). The peak of the ringā€™s surface bright- ness is āˆ¼ 1 mJy beamāˆ’1 . The synthesized beam effective area is āˆ¼ 2 AU2 at 7.69 pc. For s āˆ¼ 1 mm and Tg āˆ¼ 48K, Ļ„ āˆ¼ 10āˆ’4 . At 140 AU, tcoll āˆ¼ 2 Myr. Combined with the above Ė™ mass estimate, the ring should be losing mass at a rate of M āˆ¼ 0.01MEarth Myrāˆ’1 , requiring Mpbdy > 1.7MEarth (for tage = 200 Myr), consistent with (Chiang et al. 2009). Best-ļ¬t models for the spatial distribution of mm grains are selected by minimizing the difference between model and ALMA visibilities, where the u-v plane sampling from the ob- servations is used in CASA to observe each model (tool sm.predict). Ring models are produced using the following assumptions: (1) The ring is circular and has an offset relative to the star that is in agreement with the deprojected ellipse models (see Fig. 1), approximating a grain orbital eccentricity āˆ¼ 0.1. (2) The ring is uniform in azimuth. (3) The radial proļ¬le for mm grains is described by either a Gaussian distribution in semi-major axes or a power law in sur- face density. For the Gaussian, the FWHM is varied from 9.4 to 21 AU, and the inner radial half-maximum point from 131 to 140 AU. For power law surface density proļ¬les, the annular width is varied from 10 to 30 AU, the inner edge from 133 to 138 AU, and the power law index
  • 5. ā€“5ā€“ from -9.5 to -1.5. (4) The vertical distribution for grains follows an exponential decay with a scale height given by a constant angle above the midplane between 0 and 2.5ā—¦ . In each model, the emission from grains at a given distance from the star is calculated from the Planck function with the grain temperature Tg determined as described above. The total ļ¬‚ux density for the ring at 850Āµm is normalized to either 80, 90, or 100 mJy. The starā€™s ļ¬‚ux is set to 3 mJy. Each model is projected onto the sky with PA = 336ā—¦ and i = 66 to 67.5ā—¦ . The model ringā€™s apocenter is set to the inferred apocenter of Fomalhautā€™s ring. It should be noted that models of a uniform ring can become brighter near the ansae due to projection effects. Smooth, symmetric models cannot, however, account for the excess brightness near apocenter. Such brightening could be explained by variations in the mass distribution of grains or by variations in ringā€™s radial thick- ness. Collisions between parent bodies could also produce asymmetries (Wyatt & Dent 2002). The best-ļ¬t models with a Gaussian semi-major axis distribution have a scale height cor- responding to an opening angle of 1.0ā—¦ Ā± 0.25, a FWHM = 16 Ā± 3 AU, and an inner radial half-maximum at 135+0.5 AU. The 1-Ļƒ errors for model parameters are estimated by including āˆ’1 models for which āˆ†Ļ‡2 < 1. Models with i = 66.75ā—¦ and a total ļ¬‚ux density of 80 mJy are preferred. Most of the dimming in the SW is consistent with a loss of sensitivity (Fig. 1). The appearance of a hole may be due to brightening in the southern-most part of the ring, which may be due to noise. The NE is not subtracted in the residual image (Fig. 1, bottom-right) and contains contiguous excess surface brightness. The star is also not well-subtracted, suggesting possible excess. Some of the extended surface brightness noted in slice 4 of Fig. 1 remains, but is consistent with a high-noise peak. Some select, steep power law surface density proļ¬les are also consistent with the data. These are limited to a surface density āˆ rāˆ’8.5 , an inner edge of 135+1 AU, an opening angle āˆ’1.5 ā—¦ ā—¦ 1.0 Ā± 0.5, and a preferred i = 67.25 . For these power laws, the half-maximum width is about 11.4 AU. 4. Discussion Any formation mechanism for Fomalhautā€™s ring must address the following constraints: (a) The ring has an eccentricity āˆ¼ 0.1. (b) The vertical scale height of the parent bodies is consistent with an opening angle of āˆ¼ 1.0ā—¦ from the midplane. (c) The FWHM of the parent bodies for the Gaussian model is āˆ¼ 16 AU, giving a width-to-height aspect ratio āˆ¼ 7. (d) The outer edge of the parent bodies is consistent with being as sharply truncated as the inner edge. (e) The micron grains are more radially extended than the parent bodies, but this is satisļ¬ed for
  • 6. ā€“6ā€“ a variety of models due to radiation pressure. We consider three formation models. One is that the ring is sculpted by a single interior planet (Wyatt et al. 1999; Kalas et al. 2005; Quillen 2006; Kalas et al. 2008; Chiang et al. 2009). To account for requirement (d), this solution requires an abrupt truncation of the outer disk through, for example, a stellar ļ¬‚yby (Ida et al. 2000). We will return to this scenario below. Another possible model is that the ring is a remnant from a collision between two plan- ets (Mamajek & Meyer 2007). Unless constrained, the radial width of the ring will slowly spread due to collisions between ring particles with different semi-major axes. Take the ver- tical velocity dispersion Ī“vz āˆ¼ vK sin i for Keplerian orbital speed vK . If the radial velocity dispersion is of the same order, then the typical a difference between two colliding particles is Ī“a āˆ¼ aĪ“e to factors of order unity, which for free eccentricity Ī“e āˆ¼ sin i is the scale height of the disk, h. The effective collisional viscosity of the ring Ī½c āˆ¼ h2 /tcoll . Using a scale height of 2.5 AU and a collisional time between mm grains of 2 Myr, Ī½c āˆ¼ 2.2 Ɨ 1013 cm2 /s, which means the ring is diffusing on timescales āˆ¼ 90 Myr. If the ring is younger than the star, no planetary inļ¬‚uence is necessary apart from the dynamics that led to the collision. However, shattering gravitationally bound objects requires impact speeds several times the mutual escape 2 speed (vesc = 2G(M1 + M2 )/(R1 + R2 ), for bodies with masses M1 and M2 and radii R1 and R2 ). (Asphaug 2010; Leinhardt & Stewart 2012). For two 1MEarth planets (Mpbdy 1MEarth for tage āˆ¼ 90 Myr), vesc āˆ¼ 11 km/s. The orbital escape speed at 140 AU from Fomalhaut is only about 5 km/s. The impact speeds necessary to destroy Earths are not attainable. Finally, we propose a third formation model in which the ringā€™s morphology is dominated by shepherd planets, analogous to the shepherd moons Cordelia and Ophelia of Uranusā€™s ring (Goldreich & Tremaine 1979; Smith et al. 1986). Here, the ring is conļ¬ned by angular momentum exchange between ring particles and the planets. We explore this possibility with N-body simulations, using the Bulirsch-Stoer algorithm in Mercury (Chambers 1999). In each simulation, two planets of mass Minner and Mouter are placed at ainner and aouter relative to the 2.3 M star. Their relative inclinations are set to zero. Planet eccentricities are set to force the planetesimals (see method in Chiang et al. 2009) at āˆ¼ 143 AU to have the eccentricity observed for the ring (āˆ¼ 0.11). For each run, 105 massless particles are placed between rinner and router with a surface density proļ¬le āˆ rāˆ’1 , where rinner = max(125 AU, ainner +1 AU) and router = min(160 AU, aouter āˆ’ 1 AU). The integrations run for 108 years. Massless particles are removed from simulations if the particle collides with a planet or if its radius from the star exceeds 105 AU. The masses of the planets set the steepness and skew of the ringā€™s radial proļ¬le (Fig. 3). Mutual perturbations will cause the system to evolve, which narrows parameter space by de- manding that interactions between the planets do not destroy the ring. In the massless ring-
  • 7. ā€“7ā€“ particle limit, either both planets must be < 3MEarth , or they must have an extreme mass ratio. The planets do not need to be in resonance. A super-Earth and a Mars-mass planet produce the most narrowly-peaked Gaussian for the radial parent body distribution among the simula- tions presented here. As the masses for shepherd candidates are comparable to the minimum estimated parent body mass in the ring, self-gravity of the ring may play a role in the systemā€™s evolution. If the scattered optical light observations have detected Fom b, then the candidate could be the innermost shepherd, although there is a discrepancy of āˆ¼ 10 AU between Fom bā€™s proposed a and the inner shepherd in our models. Fomalhautā€™s debris has some similarities to the Kuiper belt. Both systems are thin rings, āˆ†r/a āˆ¼ 0.1, which seem to owe their morphologies, at least in part, to the presence of planets. There are nonetheless substantial differences. The outer edge of the Kuiper belt is near the 2:1 resonance with Neptune (Trujillo & Brown 2001). For the outer edge of Fomalhautā€™s ring to be at the 2:1 resonance with an interior planet, the planet would need to have an a āˆ¼ 95 AU. To truncate the ring at this location, the planet would need to be 3MJ (Chiang et al. 2009) and could have been decected by Spitzer (Janson et al. 2012). If the ring had formed due to outward migration of an interior planet, we would expect particles to be trapped in resonances, like the Plutinos in the 3:2 resonance with Neptune. We detect only a single ring. The Kuiper belt has a vertical thickness given by a dynamically hot and cold population with Gaussian widths Ļƒ = 17ā—¦ Ā± 3 and Ļƒ = 2.2ā—¦ +0.2 , respectively (Brown 2001). While the Kuiper belt object āˆ’0.6 inclination distribution seems to be consistent with truncation due to a stellar ļ¬‚yby (Ida et al. 2000), Fomalhautā€™s parent body population may be too cold to be explained by this mechanism. This leads us to favor shepherd planets as the explanation for the ringā€™s morphology. We thank Paul Kalas and the referee for helpful comments and ALMA NAASC for techni- cal support. A.C.Bā€™s support was provided under contract with the California Institute of Tech- nology funded by NASA through the Sagan Fellowship Program. M.J.P.ā€™s and E.C.B.ā€™s con- tributions are supported by the National Science Foundation (NSF) under grant no. 0707203. M.S.ā€™s support was provided in part by the National Radio Astronomy Observatory (NRAO) through award SOSPA0-007. The NRAO is a facility of the NSF operated under cooperative agreement by Associated Universities, Inc. This paper makes use of the following data from the Atacama Large Millimeter/submillimeter Array (ALMA): ADS/JAO.ALMA#2011.0.00191.S. The Joint ALMA Observatory is a partnership of the European Organization for Astronom- ical Research in the Southern Hemisphere, the National Astronomical Observatory of Japan (on behalf of the National Institutes of Natural Sciences and Academia Sinica), and the NRAO (managed by Associated Universities, Inc. on behalf of the NSF and the National Research Council of Canada) in cooperation with the Republic of Chile.
  • 8. ā€“8ā€“ REFERENCES Asphaug, E. 2010, Chemie der Erde / Geochemistry, 70, 199 Brown, M. E. 2001, AJ, 121, 2804 Chambers, J. E. 1999, MNRAS, 304, 793 Chiang, E., Kite, E., Kalas, P., Graham, J. R., & Clampin, M. 2009, ApJ, 693, 734 Di Folco, E., ThĀ“ venin, F., Kervella, P., et al. 2004, A&A, 426, 601 e Goldreich, P., & Tremaine, S. 1979, Nature, 277, 97 Holland, W. S., Greaves, J. S., Zuckerman, B., et al. 1998, Nature, 392, 788 Holland, W. S., Greaves, J. S., Dent, W. R. F., et al. 2003, ApJ, 582, 1141 Ida, S., Larwood, J., & Burkert, A. 2000, ApJ, 528, 351 Janson, M., Carson, J., Lafreniere, D., et al. 2012, ArXiv e-prints Kalas, P., Graham, J. R., & Clampin, M. 2005, Nature, 435, 1067 Kalas, P., Graham, J. R., Chiang, E., et al. 2008, Science, 322, 1345 Kennedy, G. M., & Wyatt, M. C. 2011, MNRAS, 412, 2137 Leinhardt, Z. M., & Stewart, S. T. 2012, ApJ, 745, 79 Mamajek, E. E., & Meyer, M. R. 2007, ApJ, 668, L175 McMullin, J. P., Waters, B., Schiebel, D., Young, W., & Golap, K. 2007, in Astronomical So- ciety of the Paciļ¬c Conference Series, Vol. 376, Astronomical Data Analysis Software and Systems XVI, ed. R. A. Shaw, F. Hill, & D. J. Bell, 127 Perryman, M. A. C., Lindegren, L., Kovalevsky, J., et al. 1997, A&A, 323, L49 Quillen, A. C. 2006, MNRAS, 372, L14 Ricci, L., Testi, L., Maddison, S. T., & Wilner, D. J. 2012, ArXiv e-prints Smith, B. A., Soderblom, L. A., Beebe, R., et al. 1986, Science, 233, 43 Stapelfeldt, K. R., Holmes, E. K., Chen, C., et al. 2004, ApJS, 154, 458
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  • 10. ā€“ 10 ā€“ Table 1: Observing Log: Target Fomalhautā€™s Ring and Fomalhaut b. The precipitable water vapor (PWV) is given in mm. Date Time On-Source Antennas PWV dd/mm/yyyy (UTC) (min) 22/09/2011 23:45:00.0 25 13 0.63 23/09/2011 00:49:30.0 25 13 0.48 23/09/2011 02:08:15.3 25 13 0.80 18/10/2011 03:31:00.9 25 15 0.62 18/10/2011 04:42:55.6 20 15 0.63 18/10/2011 05:44:40.4 20 15 0.57
  • 11. ā€“ 11 ā€“ Fig. 1.ā€” Top-left: 350 GHz ALMA image of Fomalhautā€™s ring. The RMS noise is āˆ¼ 60 ĀµJy beamāˆ’1 , and the contours represent 0.24, 0.33, 0.47, 0.66, 0.92, and 1.4 mJy beamāˆ’1 . The circles are centered on the pointing center, and their diameters show the beamā€™s half and 7% power. Ellipses with PA = 336ā—¦ , and i = 66ā—¦ (red) and 67ā—¦ (blue) are shown, with the ellipse centers given by the plus sign. The slices labeled 1-7 are used to show surface brightness proļ¬les in Figure 2. The coordinate axis is centered on the star, which has a peak brightness of 0.49 mJy beamāˆ’1 (uncorrected). Top-right: The primary beam corrected image. The ring be- comes bright near the ansa, and remains bright through the inferred apocenter. The contours are the same as in the top-left, but begin at 0.47 mJy beamāˆ’1 . Bottom-left: The best-ļ¬t skymodel is compared with the dirty ALMA image. The grayscale and contours show mJy beamāˆ’1 , with the contour levels labeled on the colorbar. Bottom-right: The residual of the data minus the model. The model subtracts the emission well, but there remains excess emission in the NE and around the star.
  • 12. ā€“ 12 ā€“ AU From Gaussian Peak AU From Ellipse Center -20 -15 -10 -5 0 5 10 15 20 100 110 120 130 140 150 160 170 180 1 1 2 1.5 3 PB Corr Peak-Normalized Emission 4 No PB Corr 0.8 Normalized Slices 5 6 1 K05 mJy/beam 0.6 7 Fit 0.5 0.4 2 X RMS 0.2 0 0 -0.5 -3 -2 -1 0 1 2 3 12 14 16 18 20 22 24 Arsec From Gaussian Peak Arcsec From Ellipse Center Fig. 2.ā€” Left: Normalized surface brightness proļ¬les for slices 1-7 in Fig. 1. All proļ¬les except slice 4 can be ļ¬t by a single Gaussian. A ļ¬t through all slices, excluding slice 4, is shown with the dot-dot curve. Right: The deprojected radial surface brightness proļ¬le through the ansa for the corrected and uncorrected data. Black curves show corresponding Gaussian ļ¬ts. The heavy-dashed curve shows the scaled scattered optical light proļ¬le (K05). The dot- dot curve shows the scaled Gaussian ļ¬t for the combined slices in the left panel.
  • 13. ā€“ 13 ā€“ Fig. 3.ā€” Radial proļ¬les for a ring of parent bodies between two planets. Left-to-right: Minner = 6MEarth and Minner = 3MEarth . Top-to-bottom: Mouter = Minner , Mouter = Minner /3, and Mouter = Minner /10. Each color represents a proļ¬le-planet pair. The gray dot-dashed line represents the best ļ¬t to the observed radial proļ¬le. The left y-axis shows the eccentricities of the planets, and the right shows the number surface density of particles, with each curveā€™s peak normalized to unity. The range of eccentricities occupied by the planets is indicated by the vertical error bars. The x-axis shows the semi-major axes for the planet and the radial distance of the planetesimals from the ellipse center.