THE DEBRIS DISK AROUND HR 8799

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Published 2009 October 9 © 2009. The American Astronomical Society. All rights reserved.
, , Citation K. Y. L. Su et al 2009 ApJ 705 314 DOI 10.1088/0004-637X/705/1/314

0004-637X/705/1/314

ABSTRACT

We have obtained a full suite of Spitzer observations to characterize the debris disk around HR 8799 and to explore how its properties are related to the recently discovered set of three massive planets orbiting the star. We distinguish three components to the debris system: (1) warm dust (T ∼ 150 K) orbiting within the innermost planet; (2) a broad zone of cold dust (T ∼ 45 K) with a sharp inner edge orbiting just outside the outermost planet and presumably sculpted by it; and (3) a dramatic halo of small grains originating in the cold dust component. The high level of dynamical activity implied by this halo may arise due to enhanced gravitational stirring by the massive planets. The relatively young age of HR 8799 places it in an important early stage of development and may provide some help in understanding the interaction of planets and planetary debris, an important process in the evolution of our own solar system.

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1. INTRODUCTION

Rapid progress has been made in the past decade in discovering other planetary systems and in building theories for their formation and evolution. More than 300 extrasolar planets have been found through measuring stellar radial velocities and about 60 planets have been observed to transit their stars (Extrasolar Planets Encyclopaedia, http://exoplanet.eu/). However, these techniques are optimal in finding systems dramatically different from the solar system, with giant planets in orbits very close to their stars. There are two primary avenues for probing systems with planets that might have structures more analogous to that of the solar system. First, giant planets have recently been imaged around Fomalhaut (Kalas et al. 2008) and HR 8799 (Marois et al. 2008) in orbits with radii of tens of AU. Second, the Spitzer Space Telescope (Werner et al. 2004) has observed more than 200 debris disks, which represent dust production from colliding planetesimals, typically in zones analogous to the asteroid and Kuiper belts in the solar system. It is expected that these debris disks are sculpted by giant planets through gravitational interactions (Wyatt 2008 and references therein). Observations and models of well-studied examples show a wide variety of structures and behavior, possibly related to the individual quirks of their (unseen) planetary systems and their evolutionary states (e.g., Stapelfeldt et al. 2004; Su et al. 2005, 2008; Beichman et al. 2005; Song et al. 2005; Rhee et al. 2008; Hillenbrand et al. 2008; Backman et al. 2009).

HR 8799 has been known to have a prominent debris system presumably sculpted by unseen planets (Zuckerman & Song 2004). The recent detection of three giant planets orbiting this star, along with estimates of their masses and orbits, provides a new opportunity to understand in more detail the forces that shape debris disks. This paper reports new measurements with Spitzer that fully characterize the debris disk around HR 8799. We show that the debris system includes at least three components: warm dust interior to the three planets; cold dust exterior to them; and a halo of small grains surrounding the cold dust zone. The placement of the first two disk components appears to be, as expected, from the orbits of the planets. The dynamics of the three massive planets (Fabrycky & Murray-Clay 2008; Reidemeister et al. 2009; Goździewski & Migaszewski 2009) suggests substantial dynamical excitation in the overall planetary system. The elevated level of dynamical activity in the cold dust zone, which is the source of the large halo, is possibly a result of the unstable state of the system. The 20–160 Myr age of the system (Moór et al. 2006; Marois et al. 2008) corresponds to a critical phase in the history of our own solar system when planet formation processes were near completion and the solar system's dynamical configuration was being established. The HR 8799 debris system offers an exciting view of this phase of planetary system formation and evolution.

We present the new observations in Section 2, describe the general observational results in Section 3, build the detailed models in Section 4, and discuss the implications of this work in Section 5.

2. OBSERVATIONS AND DATA REDUCTION

The observations presented here are from the Spitzer Director's Discretionary Time (DDT) program 530 and Guaranteed Time Observations (GTO) program 50175 that utilize all of the major observation modes of both the InfraRed Spectrograph (IRS; Houck et al. 2004) and the Multiband Imaging Photometer for Spitzer (MIPS; Rieke et al. 2004). The observational setting and depth for each of the modes are summarized in Table 1. A short (6 s × 1 cycle) integration IRS spectrum of HR 8799 was previously published by Chen et al. (2006, 2009). Here, we present an IRS spectrum that is 4–60 times deeper along with newly obtained MIPS images. Observations at 24 μm were obtained in standard small-field photometry mode, for a total integration of 210 s. The observation at 70 μm provides a total integration of ∼320 s on source. The 160 μm observation was obtained using the enhanced mode at four subpixel-offset positions, for a total integration of ∼150 s. The MIPS spectral energy distribution (SED)-mode observation provides a low-resolution (R = 15–25) spectrum from 55 to 95 μm with 600 s of integration on source.

Table 1. Spitzer Observations of HR 8799

AOR Key Instrument Module Integration
28889856 IRS Staring SL2 6 s × 4 cycles
    SL1 14 s × 4 cycles
    LL2 120 s × 3 cycles
    LL1 120 s × 3 cycles
28889088 MIPS Photometry 24 μm, 5 cluster pos. 3 s × 1 cycle
28889344 MIPS Photometry 70 μm, default scale 10 s × 4 cycles
28889600 MIPS Photometry 160 μm, 4 cluster pos. 10 s × 1 cycle
    (enhanced mode)  
25711872 MIPS SED-mode 1' chop     10 s × 10 cycles

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All of the MIPS data were processed using the Data Analysis Tool (Gordon et al. 2005) for basic reduction (e.g., dark subtraction, flat fielding/illumination corrections), with additional processing to minimize instrumental artifacts (Engelbracht et al. 2007; Gordon et al. 2007). After correcting these artifacts in individual exposures, the final mosaics were combined with pixels half the size of the physical pixel scale; the resulting images are shown in Figure 1. The calibration factors used to transfer the instrumental units to the physical unit (mJy) are adopted from the MIPS calibration papers (Engelbracht et al. 2007; Gordon et al. 2007; Stansberry et al. 2007; Lu et al. 2008).

Figure 1.

Figure 1. MIPS images of HR 8799 with the orientation and beam sizes (FWHMs; black circles) indicated and the surface brightness scale on the side of each panel. (a) 24 μm image before photospheric subtraction. (b) 24 μm image after subtraction of the model stellar photosphere. (c) and (d) are the 70 and 160 μm images that are dominated by emission from the disk. The faint 24 μm background source located ∼21'' from HR 8799 is marked by a black arrow. The bright 24 μm source located ∼60'' away is a field G-type star, BD+20 5278p.

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To ensure the best flat field result at 24 μm, a second flat field made from a median stack of the data with all bright sources masked out was also applied in addition to the regular scan-mirror-dependent flat fielding (for details see Engelbracht et al. 2007). The flux density of the source at 24 μm was estimated using aperture photometry with both small and large apertures (the same photometry parameters7 as used in Su et al. 2006). The large aperture gives a flux density of 83.0 ± 0.5 mJy, while the small aperture gives a flux density of 80.8 ± 0.7 mJy (∼2.7% lower), implying the source profile is more extended than a true point source. Therefore, to capture all the flux from the extended component, we conducted photometry with a very large (radius of 35'') aperture on an image with the DC offset and all background sources subtracted without a sky annulus (i.e., the aperture photometry was relative to the median pixel value for the entire frame; therefore, an aperture correction of 1.06 was applied; see Engelbracht et al. 2007). The final measured flux we adopted was 86.4 mJy (before color correction).

The center of the source at 24 μm was determined using a 2D Gaussian fitting routine, and it coincides with the expected stellar position within the pointing error (<1''). This is consistent with the fact that the flux contribution in the 24 μm band is mostly from the stellar photosphere (58 mJy; see Section 3.1). The stellar photosphere was then subtracted by scaling an observed blue point spread function (PSF). After photospheric subtraction (see Figure 1(b)), the source has FWHMs of 5farcs78 × 5farcs67 at a position angle (P.A.) of 17°,8 slightly broader than an observed red PSF (5farcs61 × 5farcs55 for the ζ Lep disk; see Su et al. 2008). There is a faint (∼0.8 mJy) source located ∼21'' from HR 8799 at P.A. of −36°, presumably a background object.

The 70 μm data reduction follows the steps recommended by Gordon et al. (2007) and uses time filtering with the source region masked out. Several region sizes were tried. A masked radius of 55'' yields the minimum value for the background variation (1σ70 = 1.14 × 10−2 mJy arcsec−2 per subpixel). The source at 70 μm (see Figure 1(c)) is clearly extended with FWHMs of 24farcs6 × 24farcs4 at a P.A. of 77°,9 compared to the nominal resolution of 18''. The source has an azimuthally symmetric morphology in the image. The outer boundary of the source (though masked by the instrumental PSF) can be traced out to 42'' or 34'' in radius at 1σ70 or 3σ70 levels, respectively. Aperture photometry was used to estimate the flux density for the source since it is extended. An aperture of 42'' in radius (1σ boundary) was used with a sky annulus of 44''–54''. After correcting for lost light based on the same aperture settings applied to a theoretical PSF, the final integrated 70 μm flux density was 545 mJy (before color correction).

The 160 μm data were taken in the "enhanced" Astronomical Observation Template to allow them to be time filtered, as was also done for the 70 μm data (for details see Stansberry et al. 2007). No additional 160 μm PSF was obtained for the purpose of leak subtraction as it has been shown that the ghost image produced by the 160 μm filter leakage is less than ∼15 times of the photospheric flux density at 160 μm. The disk is ∼400 times brighter than the photosphere in this channel (see Table 2). This is also confirmed by careful inspection of the data where the expected ghost image lies. The final 160 μm mosaic shows some large-scale extended cirrus structures surrounding the source (see discussion in Section 5.3). The source is clearly detected at 160 μm (see Figure 1(d)), and is consistent with being azimuthally symmetric above the 5σ160 level at the expected star position. The source at 160 μm is surrounded by a low level of asymmetric background cirrus. The FWHMs are 47'' × 41'' (based on an image with a field of view of 88''), slightly broader than a nominal observed PSF (∼38''; Stansberry et al. 2007), possibly influenced by the background cirrus. Aperture photometry is used to determine the integrated flux. To minimize the influence of the background cirrus, we used small aperture sizes (16'' and 24''), sky annuli (64''–128''), and aperture corrections (4.683 and 2.613 for a red point source of 50 K; Stansberry et al. 2007). The resultant integrated 160 μm flux density is 539 mJy (before color correction). The centroid of the disk seen in the MIPS 70 and 160 μm images coincides with the expected position of the star.

Table 2. Observed Flux Densities

λc (μm) Flux Density (mJy)
  Totala Starb Disk MIR Corec FIR Cored Extendede
23.68 86.6 58 29 21 <5 7.5
71.42 610 6.5 605  ⋅⋅⋅ 285–387 319–217
155.89 555 1.4 554  ⋅⋅⋅ 554  ⋅⋅⋅

Notes. aIntegrated in a large aperture including the star after color correction. bFrom best-fit Kurucz model. cCentral unresolved source for the inner warm component at 24 μm. dCentral unresolved source for the outer cold component at 70 μm. eExtended emission for the cold component.

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The MIPS SED-mode data were reduced and calibrated as described by Lu et al. (2008) with an extraction aperture of five native pixels (∼50'') in the spatial direction. Since the source size (see below) is smaller than the extraction aperture, the slit loss was corrected based on a point source. This procedure would under-correct for the slightly extended source and may explain why there is a small offset (∼17% at the fiducial wavelength of the 70 μm band) between the 70 μm photometry and the MIPS–SED spectrum. The final MIPS SED-mode spectrum is smoothed to match the resolution at the long-wavelength portion of the spectrum (R = 15).

The basic reduction and extraction of the IRS spectral data were provided by the Spitzer Science Center IRS pipeline S18.5. We first trimmed a few endpoints from each module and manually removed large outliers by visually inspecting each of the co-added, background-subtracted spectra (differencing the two nod positions). The spectra were then averaged with sigma clipping (S/N = 3). All of the final photometry measurements (color corrected; see details in Section 3.2), MIPS SED-mode data, IRS combined spectrum, along with previously published data are shown in the SED (Figure 2).

Figure 2.

Figure 2. Spectral energy distribution (SED) of HR 8799. The best-fit Kurucz model (Teff = 7750 K with log g of 4.5, shown as a gray thin line) was determined using ground-based photometry for wavelengths shorter than 6 μm compiled from the Simbad database (including the 2MASS photometry shown as purple filled diamonds, Strömgen photometry shown as red filled triangles, Hipparcos BV photometry as blue filled circles, and various Johnson photometry shown as open squares). The ISO 60 and 90 μm measurements are from Moór et al. (2006), while the 850 μm datum is from Williams & Andrews (2006) and the 1.1 and 1.2 mm observations are from Sylvester et al. (1996). The MIPS broadband measurements are color corrected.

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3. ANALYSIS

3.1. Stellar Properties of HR 8799

HR 8799 (HD 218396, HIP114189), located at 39.4 pc (van Leeuwen 2007), is classified as an A5 V (Cowley et al. 1969), γ Doradus variable. It has λ Bootis type characteristics (Gray & Kaye 1999) with low abundances of the heavier elements (e.g., [Fe/H] = −0.55), but near-solar abundances of C and O (Sadakane 2006). A high-resolution optical spectrum of the star indicates Teff = 7250 K and log g = 4.30 (Sadakane 2006). The galactic space motion (UVW) of the star resembles those of young clusters and associations in the solar neighborhood with ages of 20–160 Myr (Moór et al. 2006; Marois et al. 2008). The stellar rotation velocity (vsin i) is 49 km s−1 (Royer et al. 2007), consistent with the star being viewed close to pole-on.

To determine the stellar SED, we fit all available optical to near-infrared photometry (Johnson UBV, Strömgen uvby photometry, Hipparcos Tycho BV photometry, and Two Micron All Sky Survey (2MASS) JHKs photometry) with the synthetic Kurucz model (Castelli & Kurucz 2003) based on a χ2 goodness-of-fit test. A value of Teff = 7500 K with R* = 1.4 R and log g = 4.5 and subsolar abundances give the best match, in good agreement with the results from spectroscopy (Sadakane 2006). The resulting stellar luminosity is 5.7 L, placing the star near the zero-age main sequence consistent with a young age. Based on the best-fit Kurucz model, we then estimate the stellar photospheric flux densities at 23.6, 71.42, and 155.9 μm for the MIPS 24, 70, and 160 μm bands, respectively. These values are listed in Table 2.

3.2. Disk Components

Figure 3 shows the excess SED after stellar photospheric subtraction. It is evident that there are at least two disk components in the system: one with a characteristic temperature of ∼150 K (warm) and the other with a characteristic temperature of ∼45 K (cold). Similar disk components have been suggested by Reidemeister et al. (2009) as well. For blackbody radiators that are in thermal equilibrium with the stellar radiation field, the warm (150 K) and cold (45 K) components correspond to radii of ∼9 AU (0farcs2) and ∼95 AU (2farcs4) from the star. Interestingly, HR 8799 d, c, and b are at projected separations of 24, 38, and 68 AU from the star, respectively (Marois et al. 2008). They all lie between the two dust reservoirs. In general, the location of the dust that is at a specific thermal equilibrium temperature depends on the grain properties (through the absorption efficiency Qabs, which is size dependent). The equilibrium dust temperature is computed by balancing the absorption and the emission energy, and ultimately it depends on cross sections (Qabsπa2, where a is the grain radius); therefore, the temperature of large grains is generally lower than that of small grains at the same distance from the heating source. We adopt the optical constants for astronomical silicates (Laor & Draine 1993) and compute the grain properties (Q values for the absorption and scattering efficiency for grain radii of 0.1–1000 μm in size) using Mie theory with additional modifications for large sizes (a≳10 μm). The resultant thermal equilibrium dust temperatures as a function of radius from the star are shown in Figure 4. Due to the nature of an optically thin debris system, any dust in a continuous spatial distribution between the two distinct temperature components will have intermediate temperatures, resulting in a smoother excess SED between 20 and 55 μm (see Figure 2 in Reidemeister et al. 2009). The SED shape and the distinct characteristic dust temperatures strongly suggest that very little dust resides between the two components.

Figure 3.

Figure 3. SED of the HR 8799 disk (after stellar photospheric subtraction). The symbols used are the same as in Figure 2. The short dashed blue line shows the blackbody emission at 150 K that matches the excess shortward 30 μm well, while the excess longward 30 μm is well fitted with modified blackbody emission (λ−0.95Bλ) at 45 K (long dashed red line). The MIPS 24 and 70 μm photometry points include the extended component; therefore, they are slightly higher than the spectra.

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Figure 4.

Figure 4. Thermal equilibrium dust temperature in the HR 8799 system computed based on the various grain sizes of astronomical silicates. The two horizontal dotted lines mark the dust temperatures (150 and 45 K) derived from the excess emission for blackbody radiators. For illustration, the projected distances of the three planets are marked as vertical dashed lines. The three disk components are marked in different filled patterns (see Section 3.2 for details).

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Based on Figure 4, the emitting zone for the warm component is between ∼5 and ∼15 AU, with an angular diameter of < 1''. This component, which dominates the emission detected in the IRS spectrum and the MIPS 24 μm band, should be unresolved at 24 μm (inside planet d). A similar calculation indicates that the cold component, if it has a size of ∼100 AU in radius, should be at best only barely resolved at 24 μm; however, the excess SED (Figure 3) shows that the cold component would contribute only a small (≲ 9%) portion of the total signal in the MIPS 24 μm band. Thus, the flux well outside the PSF at 24 μm suggests the detection of an extended component at this wavelength.

We estimate the flux of the unresolved point source in the 24 μm image (star + disk) by scaling a PSF to match the peak flux of the source. The scaling suggests that the central unresolved component is ∼78 mJy at maximum (assuming the extended component contributes no flux at the position of the star). The stellar photosphere is expected to be 58 mJy in the 24 μm band, so the central unresolved disk component is ∼20 mJy before color correction. Due to the large temperature differences between the warm and cold components, different color corrections must be applied to each of the components at 24 μm. Applying a color-correction factor of 1.055 for a blackbody of 150 K (see the MIPS Data Handbook, http://ssc.spitzer.caltech.edu/mips/dh/, for the detailed color corrections for the MIPS bands), the total flux density of the central unresolved (warm) disk component is ∼21 mJy, which agrees well with the photosphere-subtracted IRS spectrum (22.4 ± 1.4 mJy). Therefore, the extended disk component is ∼7.5 mJy (after applying a color correction of 0.894 for a blackbody of 50 K). Adding these measurements, the final total flux density for the entire system (star + two disk components after color corrections for the two different temperatures) is 86.6 ± 1.7 mJy (assuming 2% error based on the nominal calibration uncertainty; Engelbracht et al. 2007).

The expected stellar photosphere is 6.5 mJy in the 70 μm band, suggesting the disk is ∼603 mJy after a color-correction factor of 1.12 for a 50 K blackbody. Therefore, the total (star + disk) flux density at 70 μm is 610 ± 31 mJy (assuming 5% error based on the nominal calibration uncertainty; Gordon et al. 2007). At 160 μm, the stellar photosphere is 1.4 mJy; therefore, the total disk flux density is ∼554 mJy after a color correction of 1.03 for a blackbody of 50 K, resulting in a total (star+disk) flux of 555 ± 66 mJy (assuming 12% error based on the nominal calibration uncertainty; Stansberry et al. 2007).

The 70 μm image is essentially only from the disk since the star is ≲1% of the total flux in the far-infrared. An observed radial surface brightness profile of the disk at 70 μm is shown in Figure 5. As was indicated by the FWHM measurements, the disk is clearly resolved. The structure of the disk at 70 μm is similar to the one at 24 μm, a bright core and an extended disk; however, the bright core at 70 μm cannot originate from the warm component seen at 24 μm (because the temperature is too cold). This bright core is most likely to originate from a dust belt (hereafter, the planetesimal disk) outside planet b, where emission by dust is also detected at submillimeter wavelengths (Williams & Andrews 2006; Sylvester et al. 1996). Consistent with this possibility, the emission at 850 μm is mostly confined within 20'' (diameter) based on the JCMT/SCUBA measurements (Williams & Andrews 2006). However, if the dust emitting at 70 μm all originated from the same location as in the submillimeter, the disk could not be resolved by MIPS at 70 μm. In addition, Reidemeister et al. (2009) also estimate the outer edge of the cold dust component is between 125 and 170 AU (a narrow ring) based on simple SED fitting and assumed grain properties. Given the nominal resolution of 18'' in the MIPS 70 μm band, any disk structure that is smaller than 360 AU in radius is not resolvable at a distance of 40 pc. The large measured FWHMs at 70 μm suggest that the extended emission at 70 μm must originate from a component outside the planetesimal disk.

Figure 5.

Figure 5. Radial surface brightness profile of the HR 8799 disk at 70 μm. Data are shown in open black circles with error bars compared to the profile of a PSF (red solid line) scaled to match the peak of the disk flux. An extended (outer radius of 46'') model surface brightness profile is also shown as a dashed blue line for comparison (for details, see Section 4.1). The profile at radii of 75''–90'' is where the second bright Airy ring of the instrumental PSF falls, and the match in the profiles between the observed point sources and the theoretical PSF is poor in this range.

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Limited by the large beam size at 70 μm, the current data cannot differentiate whether there is any gap between the planetesimal disk and the extended component. We can only estimate the bright core (presumably the planetesimal disk) flux by normalizing a PSF to match the peak of the observed flux (this procedure provides an upper limit) or to match the flux within a 10'' radius (to provide a lower limit). After color correction for 50 K, the unresolved core flux density is 285–387 mJy, suggesting that the extended component is roughly equal in integrated brightness to the unresolved core.

3.3. Disk Inclination

Based on ten years of astrometric data on planet b, Lafrenière et al. (2009) suggest an orbital inclination of 13°–23° off the plane of the sky. In addition, both Fabrycky & Murray-Clay (2008) and Reidemeister et al. (2009) suggest that the system is unlikely to be exactly face-on from stability analyses of the planetary configuration. The resolved image at 24 μm provides very little constraint because the emission at this wavelength is mostly dominated by the central unresolved disk. The resolved image at 70 μm appears to be relatively azimuthally symmetric. From the ∼100 MIPS observations of a routine calibrator, HD 180711 (G9 III, 447 mJy at 70 μm), the measured FWHM ratio is 1.044 ± 0.023 for a point source at 70 μm. The measured FWHM ratio (1.008) of the HR 8799 70 μm disk suggests a deviation of ∼1.5σ from a face-on symmetric disk. From model images (see discussion in Section 4.2) constructed for various inclination angles, we can rule out any angles that are larger than ∼25° because the resultant images give a ratio much larger than the measured value.

3.4. Summary

In summary, the resolved disks at 24 and 70 μm indicate that the disk around HR 8799 has at least three components: a warm belt inside planet d, a planetesimal disk outside of planet b with extension of ≲10'', and a surrounding large extended disk. The separation into these three components and their placement relative to the planets in the system appear to be largely independent of assumed grain sizes and optical properties. All of the observed flux densities, including those for the three disk components, are listed in Table 2.

4. MODELS

We now build on the observational results of the preceding section through more detailed models of the HR 8799 debris disk. Although these specific models are under-constrained and hence not unique, they are guided by models of other debris systems and fit the observations of HR 8799. Therefore, they give a plausible picture of the disk behavior. In Section 4.1, we constrain the disk extent by fitting the observed surface brightness profiles with assumed power-law profiles that are independent of grain properties. The main purpose of this exercise is to derive spatial information that can be used in a realistic thermal model. In Section 4.2, we then utilize the disk components that are inferred from the observations with the adopted grain properties to estimate the physical extent and masses required for the dust in each component.

4.1. Disk Surface Brightness Distributions

Because of our low angular resolution, it is convenient to characterize the disk using radially averaged surface brightness distributions, represented as a mean value at a given radius and the standard deviation of the mean. For simplicity, we assume that the disk is face-on, so an azimuthally averaged radial profile can be used for modeling. This approximation greatly reduces the noise by averaging the intensity at a given radius (a similar approach has been used on the disks around Vega (Su et al. 2005) and epsilon Eri (Backman et al. 2009)). The surface brightness radial profile of the disk (after PSF subtraction for the stellar photosphere and masking out all nearby sources) at 24 μm is shown in Figure 6(a). For comparison, we also show the azimuthally averaged radial profiles of the smoothed theoretical PSF (generated by the STinyTim program; Krist 2006) and the unresolved disk around ζ Lep10 (K. Y. L. Su et al. 2009, in preparation) scaled to match the peak flux of the HR 8799 disk. The radial profile of the unresolved ζ Lep disk agrees well with the theoretical PSF, while it is clear that the second dark and the third bright Airy rings of the HR 8799 disk (in the range of ∼20'' to ∼30'' from the center) are brighter than for a point source.

Figure 6.

Figure 6. (a) Radial profile cut of the HR 8799 disk at 24 μm (black open circles). For comparison, similar radial profiles (scaled to match the peak of the HR 8799 disk flux) are shown based on the theoretical STinyTim PSF (boxcar smoothed, 150 K) and the unresolved disk around HD 38678 (ζ Lep). The unresolved disk around HD 38678 has high signal-to-noise ratio and shows a dynamical range of 2 × 104 in the radial profile (K. Y. L. Su et al. 2009, in preparation). An extended disk filling the second and third dark Airy rings is evident in the profile for HR 8799. (b) Radial profile cut of this extended disk at 24 μm after subtracting the scaled ζ Lep disk (color corrected).

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By subtracting the scaled radial profile of the ζ Lep disk from the observed radial profile of HR 8799, a rough disk surface brightness distribution for the extended disk component is revealed (Figure 6(b)). This component is very faint, ∼1 × 10−3 mJy arcsec−2 at a distance of ∼1000 AU from the star, similar to the surface brightness level seen at 24 μm in the Vega disk.

As shown in Figures 5 and 6, the true disk structure is masked by the instrumental PSFs. One way to understand the structure of the disk is to construct a trial surface brightness distribution, convolve it with the beam, and then compare with the observed data. In particular, this approach is a practical way to constrain the true disk outer radius in the low-resolution images. Since our goal is to set constraints on the main planetesimal disk, the 24 μm profile in the following fits is for the extended disk only. The simplest model is to assume that the surface brightness profile follows a power law, S(r) ∼ r−α, between an inner break radius (rbr) and an outer cutoff radius (rout). In an optically thin debris disk where the only heating source is stellar radiation and the disk density is only a function of radius in a power-law form of ∼rp, the radial surface brightness is then proportional to rpBλ(Tr) where Bλ is the Planck function, and Tr is the radial-dependent dust temperature (generally, Trr−0.33 for small grains and Trr−0.5 for large grains). This simple power-law formula has been used to fit the well-resolved Vega disk at both 24 and 70 μm, and it was found that the power indices change from r−3 for the inner part of the disk to r−4 for the outer part of the disk (Su et al. 2005). An inner break point is needed in this simple power law for steep indices (α∼ 3 or 4); otherwise, the profile mimics a point source after convolution with the PSF. Because the outermost planet is at a radius of ∼2'', we also set the disk surface brightness to zero inside 2'', i.e., S(r) = 0 for rrh = 2'' (h stands for hole).

We have tried four different cases for the model surface brightness distribution: (1) a larger inner hole with α = 4; (2) a flat distribution between rh and rbr but with α = 4 outward; (3) a single power law with α = 2; and (4) two power laws with indices of α = 2 and α = 3. In all cases, we varied rbr and rout of the surface brightness distribution (two free parameters) and computed the reduced χ2ν value to determine the best fit. The reduced χ2ν value was computed for data points between 5'' and 40'', and between 5''and 75'' at 24 and 70 μm, respectively. Note that the bright hump seen in the 70 μm profile between 75'' and 90'' is located at the same position as the second bright Airy ring (see Figure 5). The match between an observed PSF derived from the calibration stars and theoretical PSF is poor in this range; therefore, we disregard the 70 μm data points outside 75'' in the modeling. The results are shown in Figure 7.

Figure 7.

Figure 7. Model and observed surface brightness distributions at 70 μm (red) and 24 μm (blue). Solid and dashed lines are the model before and after PSF convolution, respectively. For details about the model surface brightness parameters see Section 4.1. In all cases, S(r) = 0 for r⩽2''. (a) is for a large, empty inner hole: rh = rbr = 5farcs5, S(r) ∼ r−4, rout = 46''; (b) a flat inner distribution: rh = 2'', rbr = 9'', S(r) ∼ r−4, rout = 23''; (c) a single power law: rh = 2'', rbr = 10'', S(r) ∼ r−2, rout = 26''; (d) two power laws: rh = 2'', S1(r) ∼ r−2, rbr = 10'', S2(r) ∼ r−3, rout = 28''. The best fit (indicated by lowest χ2ν) is case (a) with rout = 46''.

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Due to Spitzer's large beam sizes in the far-infrared, the assumed surface brightness behavior and its number of free parameters needed to describe the model, there is no unique fit for the observed profiles. The best-fit outer radii range from 23'' to 46'', consistent with the previous finding of emission from outside of the submillimeter planetesimal ring (<10''). From the model surface brightness profiles, we can also derive the surface brightness ratio (S70/S24) in the extended disk. The ratios range from ∼170 to ∼250, which can be used to set constraints on the grain properties since the density-dependent term cancels out in the ratio. Figure 8 shows the expected ratio for a size distribution of a−3.5 with a maximum size cutoff of ∼10 μm and various minimum grain size cutoffs (amin,cutoff) using astronomical silicate grains. Based on the range of derived S70/S24 ratios (represented by the horizontal dashed line in Figure 8), the acceptable range of amin,cutoff is ≲2 μm ∼ abl, the blowout size assuming a stellar mass of 1.5 M, the stellar luminosity of 5.7 L, and a grain density of 2.5 g cm−3. Outside the main planetesimal disk (r > 10''), only grains with minimum sizes, ≲ the radiation blowout size, have flux ratios in the observed range. This supports the idea that the disk outside of the main planetesimal disk consists of small grains being pushed outward by radiation pressure, i.e., the HR 8799 disk has an extended halo similar to that seen around the Vega disk (Su et al. 2005).

Figure 8.

Figure 8. Radial-dependent surface brightness flux ratio (S70/S24) in the HR 8799 system for various sizes of minimum grain size cutoffs. As in Figure 4, the projected distances of the three planets are marked as dashed lines. The three disk components are marked in different filled patterns. The range of the flux ratios inferred from the models in Section 4.1 are marked as the long-dashed lines near the upper right corner.

Standard image High-resolution image

4.2. Specific Disk Models

From the preceding section, we can expand on the description of the three disk components summarized at the end of Section 3.2: (1) the warm belt inside the innermost planet d has a temperature of ∼150 K with parameters dubbed as "warm;" (2) the main planetesimal disk outside the outermost planet b has a temperature of ∼45 K with parameters dubbed as "pb" (parent bodies); and (3) the outermost component is small grains strongly affected by photon pressure with parameters dubbed as "halo." The basic equations for computing the SED and surface brightness of an optically thin debris disk can be found in Backman & Paresce (1993), Wolf & Hillenbrand (2003), and Su et al. (2005). To model these structures, we use grain properties for astronomical silicates with a density of 2.5 g cm−3 and an n(a) ∼ a−3.5 size distribution appropriate for a steady-state collisional cascade (Dohnanyi 1969). Using the SED of the excess and the resolved images as constraints, we fit the minimum and maximum grain sizes (amin and amax) in the size distribution and the inner and outer radii of each of the disk components (Rin and Rout) by assuming a constant surface density (Σ(r) ∼ r0) disk for the strongly bound disk and Σ(r) ∼ r−1 for the weakly bound or unbound disk (i.e., the grains affected by photon pressure).

From its characteristic temperature (∼150 K) and Figure 4, the inner radius of the warm component can be as close as ∼6 AU if the grains have a size of ∼10 μm. However, the spectral shape of the 10 to 20 μm excess emission is better fitted with grains of ∼μm sizes. In addition, the spectral shape suggests that sub-micron grains are absent, since their emission spectrum would result in higher contrast features at 10 and 20 μm. We fit the inner warm component as a bound disk with parameters used in Table 3. The dust mass only accounts for the small grains that dominate the mid-IR emission. We lack the constraints, such as the flux of this warm component at longer wavelengths, that would be required to estimate the mass of the population of large grains and parent bodies associated with the warm emission.

Table 3. Parameters in the Preferred Model

Parameters Inner Warm Disk (warm) Planetesimal Disk (pb) Halo (halo)
Σ(r) r0 r0 r−1
Rin (AU) 6 90 300
Rout (AU) 15 300 1000
amin (μm) 1.5 10 1
amax (μm) 4.5 1000 10
Md (M) 1.1 × 10−6 1.2 × 10−1 1.9 × 10−2
fd = LIR/L* 2.2 × 10−5 7.5 × 10−5 1.0 × 10−4

Download table as:  ASCIITypeset image

It is less straightforward to fit the other two disk components, due to the lack of strong constraints on the size of the planetesimal disk. We can, however, use the following information: (1) we know roughly how much flux comes from the unresolved component (presumably the planetesimal disk) at 70 μm; (2) the minimum inner radius of the planetesimal disk is ∼90 AU, from the characteristic temperature of the cold component in the SED; and (3) large grains (at least a few hundred microns) are required due to the collisional cascade nature of debris disks. Not only the model parameters have to provide satisfactory fits to the global SED, but also the model images after convolution with the beam sizes have to match the observed images. Our modeling strategy is similar to the one applied to the γ Oph disk (Su et al. 2008); we first tried many combinations of parameters that can provide good fits to the SED, then refined the parameters by matching the observed radial profiles. We started with constraining the parameters for the inner component using data shortward of 30 μm since they are most sensitive to this component, then used the constraints listed above for the parameters in the other two disk components.

For the planetesimal disk, we fixed amax and Rin,pb at 1000 μm and 90 AU, respectively. Additionally, we constrained amin to be greater than abl (∼2 μm). For the extended halo disk, Rout,halo was fixed at 1000 AU; Rin,halo and Rout,pb were required to be equal (there is no gap between the planetesimal and halo disks). Initially, we fit the planetesimal disk with a narrow ring (ΔR < R) so the actual density distribution has less effect on the output SED. A difficulty in this narrow-ring model is that grains smaller than abl have relatively high thermal equilibrium temperatures at the location where the extended disk starts, and the resultant emission from the inner edge of the halo component is too strong in the 25–35 μm range. The only way to make the narrow-ring model work is to have far less contribution from the extended disk as shown in the SED of Figure 9(a) (top panel). However, the resulting model yields insufficient flux from the extended component; and therefore, also shows a disk at 70 μm that is too small, as shown in the model radial profile (Figure 9(a)).

Figure 9.

Figure 9. Model SED (top panel) and surface brightness profiles (bottom panel) compared to the data. Two sets of models are shown having the same inner warm disk component (Rin,warm = 6 AU, Rout,warm = 15 AU, amin = 1.5 μm, and amax = 4.5 μm with total Md of 1.1 × 10−6 M) and (a) a narrow planetesimal disk model (Rin,pb = 90 AU, Rout,pb = 150 AU, amin = 10 μm, and amax = 1000 μm with Md = 5.5 × 10−2 M) plus a halo (Rin,halo = 150 AU, Rout,halo = 1000 AU, amin = 1 μm, and amax = 1 μm with Md = 1.2 × 10−3 M), or (b) a wide planetesimal disk model (Rin,pb = 90 AU, Rout,pb = 300 AU, amin = 10 μm, and amax = 1000 μm with Md = 1.2 × 10−1 M) plus a halo (Rin,halo = 300 AU, Rout,halo = 1000 AU, amin = 1 μm, and amax = 10 μm with Md = 1.9 × 10−2M). The narrow-ring planetesimal disk model gives a satisfactory fit to the SED, but fails to match the disk radial profiles in contrast to the fit of a wide planetesimal disk shown in (b). The model submillimeter flux appears to be too high compared to the observed data. However, because of the source extension, the "observed" model flux actually agrees with the measurements that were calibrated assuming an unresolved source. For details, see Section 5.1.2.

Standard image High-resolution image

To satisfy all the constraints listed above simultaneously, the outer radius of the planetesimal disk has to extend to ∼300 AU. Figure 9(b) shows one of the best-fit models in terms of SED and radial profiles. In this model, the planetesimal disk extends from Rin,pb = 90 AU to Rout,pb = 300 AU and consists of grains of amin = 10 μm to amax = 1000 μm with a total dust mass (Md) of 1.2 × 10−1 M. The halo disk extends from Rin,halo = 300 AU to Rout,halo = 1000 AU and consists of grains of amin = 1 μm to amax = 10 μm with a total Md = 1.9 × 10−2 M. Note that the reduced χ2ν values in the SED fitting are similar between the narrow-ring and broad-disk models; however, the model flux ratio at 70 μm between the extended component (halo) and the unresolved core (planetesimal disk) is too low compared to the observed ratio (∼1). This mismatch is best shown in the model surface brightness profile at 70 μm (the bottom panel of Figure 9(a)), where the narrow-ring model does not fit the 70 μm profile at all.

The parameters used and derived in our thermal model for the disk components are listed in Table 3. Because of the ambiguous nature of SED modeling with multiple components and low-resolution images, these model parameters are not unique but were built from the least number of components with simple assumptions that produced a good match to all the available data. One should not take the model grain sizes too literally since they depend greatly on the grain properties used. However, the total dust mass in each of the components remains similar among all of the acceptable models.

5. DISCUSSION

5.1. Debris Disk Structure

The architecture of the HR 8799 planetary system is complex: a warm inner asteroid belt analog located at a radius of 6–15 AU; a cold Kuiper belt analog planetesimal disk located from ∼90 AU up to ∼300 AU; three massive planets orbiting between the two disk components; and a prominent halo of small grains extending up to ∼1000 AU. Similar components (except for imaged planets) have been found in a number of other debris disk systems, indicating some underlying order within the diversity in debris disk structures.

5.1.1. Inner Warm Component

Assuming the grains in the inner belt are astronomical silicates, we can rule out grains of sub-micron size, due to the absence of strong silicate features at 10 and 20 μm. The shape of the IRS spectrum strongly favors micron sizes for the grains that dominate the emission. If we further assume that all the grains in this component are bound (amin = abl), then the outer radius of this warm component can be as small as ∼10 AU based on temperature arguments (see the 2 μm curve in Figure 4). We also find that the maximum inner radius of this component is around ∼6 AU, again from temperature arguments. There are few, if any, grains inside this radius. An upper limit on the dust mass inside this inner warm component can be estimated based on the observed IRS excess spectrum. A flux density of 1 mJy at 10 μm corresponds to a dust mass of 2.3 × 10−7 M assuming astronomical silicates of a = 10 μm at 3 AU (i.e., Td ∼ 200 K) and a grain density of 2.5 g cm−3. This inner hole can be maintained by ice sublimation if the grains are icy (Jura et al. 1998); a process that will occur at a dust temperature of ∼150 K. Alternatively, the lack of grains inside ∼6 AU suggests that either there is another (unseen) interior planet maintaining a dust-free zone, or the growth of the protoplanets in the terrestrial zone (3–20 AU for an A-type star) at an early stage initiated a collisional cascade that moved outward and created this inner hole (Kenyon & Bromley 2004). Since we lack constraints such as a measurement of the long wavelength emission from this inner component at higher spatial resolution, we cannot set limits on amax. Because the dust in this component is warm, very little mass is required—only about 1.1 × 10−6 M for dust with an infrared fractional luminosity (fd) of 2.2 × 10−5. These values are rough lower limits because it is difficult to place tighter constraints without knowing additional parameters such as amax.

We also fit the inner warm component with amorphous carbon grains (density of 1.85 g cm−3; Zubko et al. 1996). As expected from the discussion in Section 4, the model results for the placement of the disk are not very sensitive to the assumed grain composition (Rin,warm ∼ 6 AU and Rout,warm ∼ 15 AU), and we can also rule out a significant amount of sub-micron carbonaceous grains in this inner component because the equilibrium temperature of 150 K places them right at the location of planet c. A similar result of low sensitivity to grain properties is also found in Su et al. (2005), which analyzed the behavior of the Vega system for grains of silicate, carbonaceous, and mixed composition.

A similar inner warm component (Td∼ 150 K) that dominates the disk emission at the IRS and MIPS 24 μm wavelengths is seen relatively commonly among resolved debris systems. For example, HR 4796A, Fomalhault, and epsilon Eri disks all have such a component (Wahhaj et al. 2005; Stapelfeldt et al. 2004; Backman et al. 2009). In fact, all of their excess SEDs look very similar: a steep inflection between the IRS spectrum and MIPS SED-mode data, indicating a relatively sharp inward-facing edge to the structure dominating the far-infrared emission. This feature may arise from the action of massive planets, as appears to be the case for Fomalhaut (Kalas et al. 2008; Quillen 2006; Chiang et al. 2009). HD 32297 and η Tel are other systems that show similar characteristics revealed by recent ground-based imaging (Moerchen et al. 2007; Fitzgerald et al. 2007; Smith et al. 2009). In addition, a recent IRS spectroscopic study of unresolved debris disks shows that warm components are very common (∼50%) among A-type excess stars (Morales et al. 2009). In the case of HR 8799, there are strong indications that this warm component is physically separated from the cold, outer component and that there is little dust in the intervening region.

5.1.2. Outer Cold Planetesimal Disk

Our best-fit model appears to indicate too much flux in the submillimeter (Figure 9) for the cold planetesimal disk. However, the model 850 μm disk has a FWHM of 17farcs8 after being convolved with the nominal 850 μm beam size of 15''. This slight extension would not be resolved by the 850 μm observation because the data were taken in photometry mode and no mapping was done. The flux density reported in Williams & Andrews (2006) was calibrated assuming a point source. Therefore, the correct way to compare the model and observed fluxes is to integrate the total flux in a 15'' diameter aperture on the model image. The 850 μm model flux within a diameter of 15'' is 9.33 mJy, consistent with the SCUBA measurement of 10.3 ± 1.8 mJy. Similarly, the 1.2 mm flux is also underestimated for the source extension since it was obtained using the IRAM 30 m single dish telescope (FWHM = 9farcs5).

The dust mass in the planetesimal disk that is derived from our three-component model is 0.12 M, consistent with the mass derived from the 850 μm observation (0.1 M; Williams & Andrews 2006). This is only twice as large as the mass required by the narrow-ring model, even though the disk is much larger. The dust mass in this cold component is similar to values derived for disks in the 12-Myr-old β Pic moving group (β Pic and HD 15115; Holland et al. 1998; Williams & Andrews 2006). The amount of the excess emission in the HR 8799 disk (R24 = 1.5 and R70 = 94, compared to the stellar photosphere) is comparable with other debris disks around A stars of similar age (20–160 Myr; Su et al. 2006), at least within statistical expectations. The infrared fractional luminosity for this component is 7.5 × 10−5, suggesting a collision-dominated disk.

Since the cold component is the birth place for the second-generation debris from collisional cascades, the presence of large grains is required. The inner edge of the disk, although not directly resolved by imaging, has a minimum radius of ∼90 AU from temperature arguments. We lack high-spatial-resolution submillimeter data to put strong constraints on the outer edge of the planetesimal disk. The outer radius of ∼300 AU in our model is based on the fewest and most straightforward assumptions.

5.1.3. Halo

Finally, we consider the halo component of the system. The general appearance and extent of this component are similar to the halo around the Vega system. In that case, the Spitzer observations provided sufficient angular resolution to fit the surface brightness profile and show that it is consistent with expectations for grains being blown out by radiation pressure. While the details of this process are complex, it is generally parameterized by β, the ratio of radiation pressure force to gravitational force. When collisions produce grains with β > 1, they will be blown out of the system quickly. When the collisional cascade produces grains over a narrow range of β below unity, they will tend to go into elliptical orbits. The behavior of these barely bound grains has been suggested to explain the broken power laws seen in the scattered-light disk surface brightness profile around AU Mic (Strubbe & Chiang 2006) and β Pic (Augereau et al. 2001). However, these highly elliptical orbits will continue to cross the parent body zone; and eventually it is likely that these grains will collide again, will break into smaller ones with β>1, and will blow out of the system. Thus, the timescale for mass loss from the system depends on the details of the collisional fragmentation of the grains.

However, qualitatively, the halo around HR 8799 resembles the behavior of Vega closely and differs substantially from the observations of most other A stars, indicating that both systems are currently undergoing an enhanced level of dynamical stirring in their outer planetesimal disks that leads to an elevated production rate for small grains with β near unity. These grains will eventually be ground down to sizes that participate in a general outflow from the system. We therefore model the halo by making assumptions similar to those used for the Vega outflow (Su et al. 2005).

To fit the Vega outflow, grains extending up to about five times the nominal blowout size were required. This apparent discrepancy probably arises because, for simplicity, the models are based on solid, spherical grains, whereas real grains are likely to be non-spherical and complex in structure with a substantial volume of voids (e.g., Dominik et al. 2007 and references therein). The influence of photon pressure will be much larger for such grains than for solid spherical ones. We use amax = 10 μm in the extended halo component, about five times larger than the blowout size for HR 8799, and other parameters of the model are similar to those used for Vega (Su et al. 2005). The estimated dust mass in the halo is relatively large, 1.9 × 10−2 M that is ∼6 times greater than the mass in the Vega outflow. The terminal radial velocity is 2–4 km s−1 for grains having β ∼ 1 and that are being produced in the planetesimal disk, 100–300 AU from a 1.5 M star (Moro-Martín & Malhotra 2005). For a disk radius of 1000 AU, the residence time for such particles is ∼ 900–2400 yr. For a static collisionally dominated disk (Wyatt et al. 2007), the expected ratio of mass in blown out grains to that of grains in the bound disk is ∼1.2% in the HR 8799 system (i.e., a 1.5 M star with a fractional disk luminosity of 8 × 10−5 and r∼ 100 AU). The observed ratio for HR 8799 is 15 times higher, qualitatively similar to the Vega system, where the mass in blown out grains is about 30 times the predicted static level. Both systems have much more prominent halos than systems such as Fomalhaut (Stapelfeldt et al. 2004) and β Leo (N. Stock et al. 2009, in preparation). This comparison indicates that there is an elevated level of dynamical activity in the bound disks of Vega and HR 8799 that is enhancing the production of small grains.

Although we have proceeded by analogy with Vega, future work should address the role of weakly bound grains in more detail. The conclusion that the halo indicates more dynamical activity than in A stars without such halos should be robust, but more complete modeling should draw out other aspects of the HR 8799 system.

5.2. Interaction of Planets and Debris

Based on the "resonance overlap" condition in the planar circular restricted three-body problem, the width of the chaotic region, Δa, in the vicinity of a planet with mass of Mp and orbital semimajor axis of ap orbiting a star with mass of M* is given by Malhotra (1998),

Equation (1)

Adopting the nominal parameters from Marois et al. (2008), stellar mass 1.5 M, planet masses 7 MJ and 10 MJ, and semimajor axes 24 or 68 AU for planets d and b, respectively, the width of the unstable zone near each planet is ∼8 and ∼23 AU, respectively. Therefore, the locations of the outer edge of the inner dust belt (∼15 AU) and the inner edge of the outer belt (∼90 AU) are both consistent with gravitational sculpting by the innermost known planet d and the outermost known planet b, respectively. The nearly dust-free zone interior to ∼6 AU may indicate the presence of additional unseen inner planets. If so, then this leads to an estimate of the timescale of inner planet formation of <20–160 Myr given the age of HR 8799. This is in good agreement with theoretical calculations for terrestrial planet accretion (Wetherill 1992) as well as isotopic constraints on the age of the Earth (Podosek & Ozima 2000).

The existence of the halo indicates that the outer planetesimal disk is heavily stirred due to either: (1) the planets not being in a stable configuration (Fabrycky & Murray-Clay 2008; Reidemeister et al. 2009; Goździewski & Migaszewski 2009); (2) the planet migration and orbital resonance crossings that are causing extreme excitation in the planetesimal disk, as in models for the Kuiper belt (Malhotra 1995) and for the Late Heavy Bombardment (Gomes et al. 2005); or (3) processes in the planetesimal disk itself, such as ongoing formation of (unseen) ice giants or planetary embryos that stir the disk (Kenyon & Bromley 2008). The first two possibilities relate the dynamical activity in the planetesimal disk to issues associated with the stability of the configuration of the three known planets, while the third hypothesis would be independent of the planets. Although no specific conclusions can be drawn, the outcomes of any of these scenarios are a heavily stirred planetesimal disk that produces an era of enhanced collisional activity. The resulting collisional cascades and avalanches will feed an outflow of small grains (Grigorieva et al. 2007).

5.3. The Background Cloud near HR 8799 and the λ Bootis Phenomenon

The cirrus seen at 160 μm resembles some of the large-scale structure in the CO (3–2) cloud detected by Williams & Andrews (2006). Figure 10 shows a new, 7' × 7' CO (3–2) map at 15'' resolution around HR 8799, taken with the HARP heterodyne array on the JCMT, overlaid on the Spitzer 160 μm map. The CO emission is integrated in the local standard of rest (LSR) velocity from −4 to −6 km s−1. The radial velocity of the star, −12.4 ± 0.5 km s−1, from Moór et al. 2006 is however in the heliocentric velocity frame, and converts to −4.6 km s−1 LSR. Thus, contrary to the conclusion in Williams & Andrews (2006), we cannot say that the cloud is not associated with HR 8799 and cannot place any limits on the gas content of the disk from these observations. This is also further confirmed by the new IRAM 30 m observation that found strong CO (2–1) line emission due to the cloud at the heliocentric radial velocity of HR 8799 (P. Hily-Blant et al. 2009, in preparation).

Figure 10.

Figure 10. CO J = 3–2 contours (green) overlaid on the 160 μm data (pseudocolor with blue contours). The field of view is 7' × 5farcm9 with N up and E toward the left. The contours of the 160 μm data range from 1σ, 2σ, 3σ, 5σ, and 8σ detection level, while the green CO contours show five linear levels of integrated intensity from 0.94 (2σ) to 2.7 (7σ) K km s−1. The stellar position is marked as a star-shaped symbol and the blue arrow shows the proper motion direction of HR 8799 with a length indicating 40''.

Standard image High-resolution image

Our new JCMT CO (3–2) map is larger and of higher quality than the map presented in Williams & Andrews (2006) and shows the extended, low level molecular emission in more detail. It appears to be associated with the extended arc of high latitude clouds, MBM 53–55, detected in CO (1–0) by Magnani et al. (2000). The distance of these objects and their relation to one another is not well known. If the association with the star is physical then, at 40 pc, this would be the closest known molecular cloud.

Whether physically associated or not, it is likely that the low flux levels (1σ–3σ) of the 160 μm emission come from the molecular cloud. The asymmetry in the outer part of the observed source at this wavelength may also be due to cloud contamination. Nevertheless, the detected source (with the peak flux > 8σ) is coincident with the expected stellar position, which is offset (∼20'') from the central emission of the nearby clump in the cloud. The cloud therefore contributes only a very small amount of flux that cannot be completely removed from our aperture photometry. At 70 μm, there is neither any resemblance to the large-scale background structure in the data nor an asymmetry seen in the source morphology; therefore, we can rule out any significant contribution from this extended background cloud to the 70 μm disk emission.

The arrow in Figure 10 shows the direction of proper motion of HR 8799 (δR.A. = 107.93 mas yr−1 and δdecl. = −49.63 mas yr−1; van Leeuwen 2007). Given the coincidence in space and velocity, it is plausible that accretion from the cloud might explain the abundance anomalies leading to the λ Bootis designation (Kamp & Paunzen 2002). Using Equation (16) from Martínez-Galarza et al. (2009) for Bondi–Hoyle accretion implies a mass accretion rate of ∼3 × 10−14 M yr−1 with an assumed density of 100 cm−3, just above the threshold to produce λ Bootis behavior (Turcotte & Charbonneau 1993). However, this calculation assumes a fluid model for the ISM, which is not strictly applicable at the expected density (Martínez-Galarza et al. 2009). Therefore, the accretion rates may be significantly lower than indicated (Alcock & Illarionov 1980). The accretion hypothesis rests on the untested assumption that the rate can be increased through such means as small scale high-density structures in the ISM and/or increases in density in the wake of the star.

6. CONCLUSIONS

We have obtained deep infrared images and spectra of the debris system around HR 8799. To our surprise at the distance of ∼40 pc, the HR 8799 disk is clearly resolved at both 24 and 70 μm; the outer boundary of the disk can be traced further than 1000 AU. From general, model-independent considerations, the star appears to have one zone of warm dust within the orbit of its innermost known planet, another broad zone of cold dust outside the orbit of its outermost known planet, and an extended halo of small grains from this outer zone.

We have constructed detailed models of the system, guided by models of other debris systems as well as the observations of HR 8799. Although the models are not unique, because we draw on experience from modeling many debris systems, they should give a reasonably accurate picture of conditions in the HR 8799 system. The models indicate that the inner zone lies between 6 and 15 AU with a total dust mass of 1.1 × 10−6 M and the outer zone is between 90 and 300 AU with a dust mass of 1.2 × 10−1 M. There is little dust inside the inner zone (r ≲ 6 AU) and in between the inner and outer cold zones where the three planets reside. The halo extends to at least 1000 AU and has a dust mass of 1.9 × 10−2 M, about 15 times the level expected for a static, quiescent debris system. The implied high level of dynamical activity in the HR 8799 debris system may be related to perturbations imposed by its system of three massive planets or may be signaling ongoing planet formation in the outer parts of this system.

HR 8799 is at an age similar to that of the solar system when the terrestrial planets formed, along the way to settling into the final configuration. The planetary system of HR 8799 (both planets and debris disk) provides an intriguing snapshot of processes occurring at this stage and may help us understand the formation and evolution of our own planetary system.

This work is based on observations made with the Spitzer Space Telescope, which is operated by the Jet Propulsion Laboratory, California Institute of Technology. Support for this work was provided by NASA through contract 1255094 and 1256424 issued by JPL/Caltech to the University of Arizona. We thank Chian-Chou Chen for assistance with the JCMT CO data; David Wilner, and Eric Mamajek for discussion of the background cloud; and Ben Zuckerman for pointing out the error in the velocity comparison of the star and the cloud. K.S. also thanks Glenn Schneider and Mike Meyer for the useful discussion. This research has made use of the SIMBAD database, operated at CDS, Strasbourg, France.

Footnotes

  • Small aperture: a radius of 6farcs23 with sky annulus from 19farcs92 to 29farcs88 and an aperture correction of 1.699; large aperture: a radius of 14farcs94 with sky annulus from 29farcs88 to 42farcs33 and an aperture correction of 1.142.

  • The disk brightness in the 24 μm band is dominated by the bright unresolved component (for details see Section 3.2). Therefore, the P.A. given here only reflects the angle of the instrumental PSF, not the extended disk.

  • Note that source appears to be azimuthally symmetric; therefore, the P.A. quoted here does not necessarily reflects the true P.A. of the source.

  • 10 

    Most of the available 24 μm PSF calibrators are stars and thus have very blue colors compared to the HR 8799 disk. We use the profile of the ζ Lep disk to demonstrate the accuracy of our data reduction and the stability of the Spitzer PSF, by matching the theoretical radial profile over a range in brightness of over more than 4 orders of magnitude.

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10.1088/0004-637X/705/1/314