INTERSTELLAR MEDIUM SCULPTING OF THE HD 32297 DEBRIS DISK

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Published 2009 August 10 © 2009. The American Astronomical Society. All rights reserved.
, , Citation John H. Debes et al 2009 ApJ 702 318 DOI 10.1088/0004-637X/702/1/318

0004-637X/702/1/318

ABSTRACT

We detect the HD 32297 debris disk in scattered light at 1.6 and 2.05 μm. We use these new observations together with a previous scattered light image of the disk at 1.1 μm to examine the structure and scattering efficiency of the disk as a function of wavelength. In addition to surface brightness asymmetries and a warped morphology beyond ∼1farcs5 for one lobe of the disk, we find that there exists an asymmetry in the spectral features of the grains between the northeastern and southwestern lobes. The mostly neutral color of the disk lobes implies roughly 1 μm-sized grains are responsible for the scattering. We find that the asymmetries in color and morphology can plausibly be explained by HD 32297's motion into a dense interstellar medium cloud at a relative velocity of 15 km s−1. We model the interaction of dust grains with H i gas in the cloud. We argue that supersonic ballistic drag can explain the morphology of the debris disks of HD 32297, HD 15115, and HD 61005.

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1. INTRODUCTION

Debris disks are created by the outgassing and collisions of planetesimals that may resemble analogs to the comets, asteroids, and dwarf planets in our solar system. Debris disks show us the conditions and environments of planet building for stars different than the Sun through their structure and mineralogy.

As more disks are resolved at multiple wavelengths, they reveal their intrinsic complexity. Both the morphology and spectra of disks change in ways that are not fully understood. In order to probe the intrinsic properties of a disk, effects that are due to the surrounding environment of a star must be accounted for.

HD 32297, an A5 star at 112 ± 11 pc with a recently discovered edge-on debris disk, appears to be a promising object of study. First noted as a star with an IRAS excess (Silverstone 2000), Schneider et al. (2005, hereafter S05) discovered an edge-on disk structure in scattered light at 1.1 μm. The disk extended out to ∼400 AU and showed surface brightness asymmetries between the two lobes of the disk. This morphology appears to be common among known edge-on disks like β-Pictoris and HD 15115, which both show similar asymmetries (Kalas & Jewitt 1995; Golimowski et al. 2006; Kalas et al. 2007; Debes et al. 2008a). The total LIR/L = 0.27% makes the disk optically thin S05.

Observations of HD 32297's outer disk in the R band revealed that it may be interacting with the surrounding interstellar medium (ISM). The disk appeared significantly warped at larger separations from the star (Kalas 2005, hereafter K05). The NE half of the disk appeared to bow away from the midplane of the disk. An extrapolated surface brightness profile implied blue colors for the disk which K05 interpreted as resulting from submicron silicate dust grains. K05 suggested that the bowed structure results from an ISM–disk interaction.

The disk was also spatially resolved at 12 and 18 μm in ground based observations with Gemini (Moerchen et al. 2007; Fitzgerald et al. 2007b). There is a suggestion that at distances >0farcs75 the disk is brighter on the NE side, i.e., reversed from the asymmetry seen in scattered light images (Moerchen et al. 2007). Models of the thermal emission and brightness temperature curves as a function of distance based on the 12 μm/18 μm colors suggest that the disk has a ring-like structure with an interior clearing out to ∼60–80 AU (Fitzgerald et al. 2007b; Moerchen et al. 2007).

Finally, HD 32297's disk has been resolved with the Combined Array for Research in Millimeter-wave Astronomy (CARMA) at 1.3 mm. The CARMA image shows a marginally resolved asymmetry in the disk that appears to match asymmetries seen in scattered light (Maness et al. 2008). Furthermore, the emission at 1.3 mm is well in excess of that inferred by shorter wavelength thermal emission. Models of the disk so far rely on analytic models of dust grain optical behavior representative of "dirty ice" mixtures, but there are few constraints on the true composition of the dust grains in the disk; the presumption of water ice is premature (Fitzgerald et al. 2007b; Maness et al. 2008).

In addition to dust, a small amount of gas is present in the HD 32297 system. Based on the detection of narrow circumstellar Na i absorption in the spectrum of HD 32297, Redfield (2007) determined that at most 0.3 M of gas resides within the disk. The CARMA observations also provided an upper limit of 95 M of gas (Maness et al. 2008).

In this paper, we present two new Near-Infrared and Multi-Object Spectrometer (NICMOS) coronagraphic scattered light images of the disk at 1.6 and 2.05 μm. We examine how the morphology of the disk changes with wavelength and how that might lead to new constraints on the composition of the dust in the disk. The properties of the disk suggest that it is interacting with the surrounding ISM. We model this interaction and explore how it affects the observed properties of the disk. In Section 2, we present the observations of HD 32297, in Section 3 we measure the morphology, surface brightness, and scattering efficiency of the dust as a function of wavelength. Finally, we present models of the interaction between the ISM and HD 32297, HD 15115, and HD 61005 in Section 4.

2. OBSERVATIONS

We observed HD 32297 with the Hubble Space Telescope's (HST) NICMOS (Thompson et al. 1998) using the coronagraph in Camera 2. We used the F160W and F205W filters with central wavelengths of 1.6 and 2.05 μm. Additionally, we re-analyzed archival data of HD 32297 in the F110W filter taken by S05. All new observations were taken on 2007 October 3 for HD 32297.

In between visits to HD 32297 we observed HD 31489, the point-spread function (PSF) reference. Accurate disk photometry requires a well-constrained scaling ratio between the target star and its PSF reference. To achieve the most accurate scaling, over the three visits we obtained three short 0.6 s exposures of both the target and PSF reference star without the coronagraph in both filters.

In F160W, the reference saturated in each 0.6 s exposure. To determine the proper scaling factor for F160W, we used an annulus centered on each star with a radius between 6 and 21 pixels to determine the total counts s−1 measured. In F205W, this was not an issue for either star, and so we used a simple circular aperture with a width of 21 pixels. In F160W, we found the ratio of flux densities for HD 32297 to HD 31489 to be 0.54 ± 0.02. In F205W, we found a ratio of 0.53 ± 0.01.

We also used the archival observations of HD 32297 and HD 83870. HD 83870 was reported in S05 to yield the best PSF subtraction using pixel offsets of [+0.304, +0.143] and a ratio of HD 32297 to HD 83870 of 0.440 ± 0.005. Short exposures of both stars were also available, though both were saturated at their cores. We re-determined the scaling using the same procedure as we used for the F160W filter and obtained a ratio of 0.441 ± 0.005, in excellent agreement with that determined by S05.

In order to determine the best subtraction, we minimized a chi-squared metric on a region of the target image dominated by the star's diffraction spikes. We assumed that good subtraction of the diffraction spikes corresponded to the best subtraction of the PSF within the region of interest (Schneider et al. 2001). We iteratively created subtractions for combinations of scaling and pixel offsets until we found an image that produced the lowest chi-squared measure. We searched within 1σ of the scaling ratios we determined above and within ±1 pixel to find the best x and y pixel offsets.

To quantify the systematic effects on the photometry, we repeated the subtractions varying the PSF scalings and offsets by ±1σ from the minimum chi-square solution found above. Using a rectangular photometric aperture matched to the size of the disk, we found the standard deviation in the disk flux densities from this suite of subtractions. We then propagated this uncertainty into the total uncertainty in the flux density of the disk per pixel.

We observed HD 32297 at two telescope orientations differing by 24°. This is essentially an azimuthal dither that allows astronomical objects that rotate with the field of view to be distinguished from rotationally invariant instrumental artifacts. The two differentially oriented PSF-subtracted images in each filter band were geometrically rectified and corrected for the linear optical distortion (Xscale = 75.95 mas pixel−1, Yscale = 75.42 mas pixel−1) at the Camera 2 coronagraphic focus. The geometrically corrected image pairs were rotated about the location of the occulted target (as determined through the target acquisition process) and averaged together. The final, combined images are shown in Figure 1.

Figure 1.

Figure 1. Logarithmically scaled, final combined NICMOS coronagraphic images of the HD 32297 debris disk at F110W (1.1 μm, upper left), F160W (1.6 μm, upper right), and F205W (2.05 μm, lower left). In the lower right corner of the figure is a logarithmically scaled color combined image of the disk, where blue is F110W, green is F160W, and red is F205W.

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In practice, instrument artifacts are rarely constant in time, so subtraction residuals remain and can contaminate photometric measurements of a disk. We therefore checked that the total disk flux measurement at each telescope orientation was consistent to the above quoted uncertainties.

3. RESULTS

3.1. Disk Geometry

To measure any warping of the HD 32297 disk system, we calculated the disk position angle (P.A.) as a function of radial distance. To calculate the P.A., we performed the following analysis. First, we separated the images at each spacecraft orientation for all three filters to create six independent images of the disk. In each image, we highlighted the midplane of the disk by performing an unsharp mask; we subtracted a Gaussian-smoothed disk image from the original image. Then, we used a rectangular aperture of width 3 pixels in the radial direction and height 8 pixels in the direction perpendicular to the midplane of the disk over the disk image. We centered the aperture on the disk midplane at radial distances of 6–40 pixels. In each aperture, we summed the surface brightness along the 3 pixels in the radial direction and found the center of the disk by fitting the resulting cross section with a Gaussian. For each radial distance, we took a median of the six independent measures of the P.A. from each image and calculated an uncertainty based on the standard deviation of the measures. The NE lobe has a median P.A. of 46.3 ± 1.3 (i.e., 226° ± 1° and the SW lobe has a median P.A. of 229° ± 2°. Our P.A. measurement differs from that reported in S05. However, the F110W PA was corrected to 47fdg6 ± 1 (i.e., 227fdg6 ± 1) in K05 (G. Schneider 2009, private communication).

The P.A. as a function of radial distance as measured from the stellar center is shown in Figure 2. The SW lobe of the disk shows a significant non-zero slope to the P.A. as a function of distance from the star, i.e., the disk midplane is curved. The NE lobe shows that the P.A. is uniform to within the uncertainties. However, visual inspection of the outer edge isophotes of the NE lobe with respect to the average P.A. measurements suggests that there might be some slight warping.

Figure 2.

Figure 2. Median measure of the position angle (P.A.) of each lobe of the HD 32297 debris disk as a function of distance from the star. A significant linear trend in the southwest lobe is seen.

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To determine the extent to the warping of the SW lobe, we performed a least-squares linear fit to the P.A. as a function of radial distance from the star. We found a slope of 2.1 ± 0fdg4/''. K05 found significantly different P.A.s for both lobes compared to S05; they reported a P.A. of 245° ± 2° for the SW lobe but they did not specify at what distance this was measured. However, if we extrapolate the curvature we see out to 8'', the radial midpoint of where the disk was detected in R, we would expect the P.A. to be 246fdg1 ± 3fdg4, consistent with what was reported in K05.

3.2. Surface Brightness Profiles

To study the surface brightness profiles of the HD 32297 disk we placed 3 × 3 pixel apertures on the images centered on the disk midplane. We measured the surface brightness of the disk in each aperture as a function of distance from the star and wavelength for both disk lobes. We used background apertures placed just beyond the disk to estimate the level of any systematic uncertainties. These background apertures were located at similar distances from the star as the photometric apertures.

Figure 3 shows the profiles in each filter. Overall, the profiles have a qualitatively similar shape. Of particular interest is the amount of asymmetry between the lobe surface brightnesses; S05 noted that the NE lobe of the disk was dimmer than the SW lobe beyond 1farcs7. This asymmetry is confirmed at new wavelengths by our data. We find that the asymmetry is more prominent at F160W and F205W, extending from about 1''–2farcs5.

Figure 3.

Figure 3. Surface brightness profiles of the northeast and southwest lobes of the HD 32297 debris disk in the F110W, F160W, and F205W filters. The F160W filters are scaled by a factor of 0.5, while the F205W filters are scaled by a factor of 0.125 for clarity. The surface brightnesses were measured in 3 × 3 pixel apertures. A surface brightness asymmetry exists between roughly 1farcs5 and 3'' in all three filters, with the asymmetry becoming more pronounced at longer wavelengths.

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The surface brightness profiles in both lobes and at all wavelengths cannot be described by a single power law, rather they are best fitted with broken power laws. We tabulate the best-fitting parameters for the power laws in Table 1 along with the radius of the break (Rbreak), the power-law index before Rbreak α, and the power-law index exterior to Rbreak. The radius at which the break occurs is slightly different between the two lobes, occurring closer to 90 AU on the NE lobe and 110 AU on the SE lobe of the disk, though this is at the limit of our spatial resolution and may not be significant. Both lobes are characterized by a slope less than r−2 in the interior of the disk indicating a rise in the optical depth of scatterers, followed by a drop-off in surface brightness of ∼r−3 beyond the break corresponding to a slow drop-off in optical depth beyond the break.

Table 1. Power-Law Indices to the Surface Brightness Profiles

Filter Rbreak (AU) Inner Index (α) Outer Index (β)
Southwest lobe
F110W 104 ± 6 −1.4 ± 0.2 −3.33 ± 0.03
F160W 111 ± 3 −1.0 ± 0.2 −3.57 ± 0.03
F205W 115 ± 4 −0.4 ± 0.2 −3.9 ± 0.1
Northeast lobe
F110W 80 ± 10 −1 ± 0.7 −3.00 ± 0.05
F160W 90 ± 10 −1.8 ± 0.3 −3.33 ± 0.05
F205W 97 ± 6 −1.6 ± 0.4 −3.8 ± 0.06

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3.3. Scattering Efficiency Versus Wavelength

The next step in our analysis is to infer some scattering properties for the dust grains in orbit around HD 32297. While resolved thermal images of the disk exist, it is not clear if any of the observations to date constrain the composition of the material in the disk (Silverstone 2000; Moerchen et al. 2007; Fitzgerald et al. 2007b; Maness et al. 2008). The spectral energy distribution (SED) at 12 μm shows no indication of emission around the strong 10 μm silicate line, typical of colder debris disks, or debris disks with larger particles (Moerchen et al. 2007; Fitzgerald et al. 2007b). In HD 32297's case, the temperature of the dust is estimated to be ∼170–180 K, hot enough to produce a silicate line if small silicate grains are present (Moerchen et al. 2007; Fitzgerald et al. 2007b). For these types of debris disks in particular, scattered light images provide one of the few avenues with which to infer dust composition.

Translating observed surface brightness profiles into information about the dust grains present requires removing the spectral contribution from the star itself to reveal the spectral character of the disk. In practical terms, the scattering efficiency of dust grains, Qsca, is proportional to the ratio of the surface brightness of the disk (SBν) to the flux density of the central star (Fν). We will measure Qsca by dividing our images (SBν) by the Fν.

For HD 32297, the direct imaging in each filter allows us to accurately estimate the flux density of HD 32297 for the different wavelengths observed. Since HD 32297 was not saturated in the F160W and F205W filters for our 0.6 s exposures, we found that Fν = 0.93 ± 0.02 Jy and 0.61 ± 0.01 Jy for F160W and F205W, respectively.

The F110W images pose a slight problem for estimating Fν since HD 32297 saturated the detector for the 0.6 s exposures. However, we can use the wings of the PSF to infer the total flux density of the star. We modeled the HD 32297 PSF with the tinytim software package (V6.2),4 assuming an A5 star. We used the same annulus described in Section for determining our PSF scalings to calculate an aperture correction in our synthetic images between the flux in the wings and the total flux in the PSF. We assumed a 5% error in the multiplicative correction term, or 9.6 ± 0.5. Our resulting flux density in F110W is 1.55 ± 0.08 Jy. S05 estimated the F110W flux density of HD 32297 using SYNPHOT. They estimated a flux density of 1.46 ± 0.04 Jy, consistent with our measurement uncertainties.

We used our 3 × 3 pixel apertures as described in Section 3.2 to convert our surface brightness measurements into scattering efficiencies for distances from the star ranging from 0farcs6 (67 AU) to 3'' (337 AU). Figures 4 and 5 show the scattering efficiency as a function of wavelength for 76, 127, and 313 AU, showing a representative range of colors for the disk as a function of distance. In particular, both lobes of the disk are roughly neutral in the interior of the disk and blue at the outer edges. The SW lobe has a red zone between 127 AU and 313 AU.

Figure 4.

Figure 4. Scattering efficiencies at three different distances in the HD 32297 disk for the northeastern lobe.

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Figure 5.

Figure 5. Same as Figure 4 but for the southwestern lobe.

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The surface brightness asymmetries appear to be the result of a color difference between the lobes. The color change begins at ∼127 AU, corresponding roughly to where the warp in the southwestern lobe becomes noticeable. The mostly neutral colors in the near-IR favor grains in the disk that are close in size to (or larger than) the wavelength of light observed, or ∼1 μm. Both silicates and water ice would be primary candidates to produce the observed efficiencies.

4. ASYMMETRIES AND WARPS DUE TO INTERACTION WITH THE ISM

The discovery of δ-Velorum's high-velocity interaction with the ISM in the Local Bubble (Gáspár et al. 2008) and the peculiar morphology of the debris disk HD 61005 demonstrate the need to also consider the interaction of ISM gas with circumstellar material (Hines et al. 2007, hereafter H07). A general picture of how the ISM may affect circumstellar disks is nicely summarized in Artymowicz & Clampin (1997, hereafter AC97) as well as in H07 and references therein. We argue that the simplest explanation for the color and brightness asymmetries, as well as the perturbed morphology of the outer disk, is the interaction of HD 32297 with a cloud of ISM material as first suggested by K05.

The behavior of HD 32297's surface brightness profiles is similar in behavior to the disks of AU Microscopii and β-Pictoris, both of which show breaks in their radial brightness profiles (Heap et al. 2000; Golimowski et al. 2006; Liu 2004; Kalas et al. 2004; Metchev et al. 2005; Graham et al. 2007; Fitzgerald et al. 2007a). These breaks are interpreted as arising from the "birth-ring" of large planetesimals that feed both the inner dust population through Poynting–Robertson or wind drag and the outer dust population through radiation pressure and mutual collisions (Strubbe & Chiang 2006). The outer disk is then composed of increasingly weakly bound dust grains, or grains that are unbound and leaving the system (the so-called β meteoroids).

There are two components to an ISM cloud that dust grains both bound and unbound in a disk will interact with. First is the hydrogen gas which makes up the bulk of the mass in a cloud, and thus is the dominant perturbation on the dynamics of the grains through supersonic ballistic gas drag. The second component is the small ISM grains in the cloud which will primarily affect the composition and grain size distribution of the disk grains through collisions with dust in the disk. ISM grains are repelled by radiation pressure of the central star at some radius, so this effect is primarily in the outer regions of a debris disk (AC97). Both of these components can have an observable effect on the morphology of the disk. In this section, we develop for the first time a simple model for a disk interacting with the gaseous part of the ISM. We apply it to HD 32297 and two other disks that have peculiar morphologies, HD 15115 and HD 61005.

4.1. The Interaction of Dust Grains with ISM Gas

We consider the situation where a collisional cascade has resulted in a steady flux of unbound β meteoroids traveling at escape speed from the system and encountering the ISM gas. Since the relative velocity of the dust grains is on the order or greater than the sound speed of the gas up to a gas temperature of ∼8000 K (the maximum temperature for a neutral cloud), the interaction of a single dust grain with the H i gas in the neutral ISM is akin to supersonic gas drag felt by meteorites entering the Earth's atmosphere with a drag coefficient Dg (Pecina & Ceplecha 1983; Hoppe 1937). In this model, the acceleration ($\mathbf {\vec{a}}$) a single dust grain feels from the gravity of the central star, the radiation pressure from the central star, and the drag from the ISM gas at a distance r is (e.g., Nakagawa et al. 1986)

Equation (1)

where the drag coefficient is (Hoppe 1937; Pecina & Ceplecha 1983)

Equation (2)

Here, A is a shape parameter and Γ is the drag coefficient for a supersonic spherical particle (AΓ ∼  1), ρgas and ρdust are the densities of the ISM gas and the disk dust grains, respectively, and $\mathbf {\vec{v}_{\mathrm{dust}}}$ and $\mathbf {\vec{v}_{\mathrm{gas}}}$ are the velocities of a dust grain and the ISM flow, respectively. We define β as the ratio of the force of radiation pressure to the gravitational force exerted by the star.

An order of magnitude estimate for the radial distance at which the dust grains are significantly perturbed from their original trajectories can be obtained by setting $\mathbf {\vec{a}}$ = 0 and assuming weakly bound grains, i.e., β ∼ 0.5, in Equation (1).

Equation (3)

where vrel is the relative velocity between the disk and the ISM. The assumption of β ∼ 0.5 implies a particular grain mass and density for a given dust grain composition. β for a perfectly absorbing spherical dust grain with radius rdust is (Burns et al. 1979)

Equation (4)

We can investigate Rdeflect as a function of ρgas, vrel, and L for a star moving through a typical ISM cloud. If we combine Equations (3) and (4) for β = 0.5, we remove the dependence on both dust grain size and density and create a scaling law for Rdeflect

Equation (5)

To synthesize model debris disk images to compare to our data, we integrated Equation (1) for various dust and cloud parameters using a modified N-body integrator. We released thousands of particles with initial velocities determined by the birth-ring orbital parameters: with an initial semimajor axis, uniformly distributed inclinations from 0° to 5°, uniformly distributed eccentricities <0.1, uniformly distributed longitudes of ascending node, uniformly distributed longitudes of pericenter, and true longitudes uniformly distributed between 0 and 2π. We assumed the dust grains have β = 0.51, that is, they are about the blow-out size for the star. A more thorough model could self-consistently calculate β for a given composition and grain size. This approach is unjustified for most debris disks as there are currently few compositional constraints.

We calculated each particle's trajectory with a Bulirsh–Stoer integrator (Press et al. 1992) with an initial time step of five years, for a total of 5000 years. We recorded particle positions every five years and accumulated them in a two-dimensional histogram of projected particle density

We constructed a final disk image by calculating the surface brightnesses of the columns of particles in each pixel. We then Gaussian smoothed the resulting image to model convolution with the PSF of a telescope. For example, a simulation of a NICMOS image of HD 32297 at F160W has a pixel size of 75 mas (corresponding to 8.5 AU at HD 32297's distance) and the image uses a Gaussian-smoothing kernel with a FWHM of ∼137 mas. This method of using histograms to represent the steady-state distribution of dust clouds has been used by several other authors (Wilner et al. 2002; Moro-Martín & Malhotra 2003; Moran et al. 2004; Stark & Kuchner 2008).

4.1.1. An ISM Gas Interaction Model for HD 32297

Modeling the structure of the HD 32297 disk ab initio would require knowing the mass, Teff, and luminosity of the star, the relative motion of the cloud compared to the disk, the composition of the disk grains, and the density of the gas cloud, all of which are poorly constrained or unknown. Therefore, we have simply chosen initial conditions to qualitatively match the observed morphology. With this approach we can (1) demonstrate that this scenario can plausibly explain many features within the disk using reasonable initial conditions and (2) back out some weak constraints on the disk grains and cloud parameters that appear to fit the data.

Before we experimented with the dynamical models, we re-examined the stellar parameters of HD 32297. Literature values for the spectral type to HD 32297 range from A0 (Perryman et al. 1997) to A5 (Fitzgerald et al. 2007b, and references therein). We conducted a least-squares fit of Kurucz models to HD 32297's BVJHKs photometry to determine both Teff and luminosity. The model that best fits the photometry has Teff = 7750 K and luminosity = 5.7 L.

However, these values place HD 32297 below the zero-age main sequence (ZAMS) on the tracks of both Siess et al. (2000) and D'Antona (1987), i.e., in an unphysical regime. The 1σ uncertainty on the distance to the star in the new Hipparcos reduction of van Leeuwen (2007) is 12 pc. Keeping the star at 7750 K and moving it farther away by 1σ, i.e., from 112 pc to 133 pc, would increase the inferred luminosity to 8.1 L; this is the luminosity on the ZAMS for a star of 1.7 M on the Siess tracks. We take these values to be the most likely stellar luminosity and mass.

One caveat to the above analysis is the possibility of extinction from the intervening ISM or circumstellar material. If the intrinsic Teff of the star is closer to ∼10,000 K, as would be appropriate for its earliest literature spectral type of A0, then considerable extinction would be necessary to fit the photometry. An ISM-like Av = 0.72 also provides a good fit to the observed BVJHKs photometry for Teff = 10,000 K and log g = 4.5 Kurucz models. In this case, the luminosity at the nominal distance is 13.8 L, which is also well below the ZAMS at that Teff. At Teff = 10,000 K, the ZAMS has luminosity ∼30 L for an M ∼ 2.3 M. That would require moving the star out to 165 AU, or 4.4σ on its Hipparcos distance. Given the low ISM Na column density toward the star (Redfield 2007), Fitzgerald et al. (2007b) dismissed the possibility of high Av, but other possible Av, Teff combinations could result in an allowed luminosity.

Alternatively, the star could experience gray extinction from circumstellar material to explain the discrepancy between the inferred luminosity and the ZAMS luminosity. This, however, would imply an optically thick circumstellar disk comprised of fairly large dust grains. This situation seems unlikely given the low LIR/L measured which is more in line with optically thin dust disks (Fitzgerald et al. 2007b). Also, the inferred amount of circumstellar gas is small, arguing for a late stage of evolution for the disk where relatively little primordial gas and dust remain (Redfield 2007).

In addition to the stellar parameters, we must consider the relative velocity vector between the disk and the ISM flow, β, and Dg to fully determine the initial conditions for our simulations. The relative velocity vector can be weakly constrained by the local dispersion of ISM cloud velocities and HD 32297's proper motion. The other parameters are more difficult to constrain.

In order to determine a vrel consistent with both the observed proper motion and radial velocity of HD 32297 as well as the morphology of the warped disk, one must make some assumptions about the impacting cloud's velocity vector relative to that of the star. From observations of the circumstellar and interstellar Na lines in HD 32297's spectrum, the radial velocity of HD 32297 is roughly 20 km s−1 while the ISM's radial velocity is ∼24 km s−1 (Redfield 2007). HD 32297's proper motion is primarily to the south at a speed of 15 km s−1 (assuming a distance closer to 133 pc). If the cloud only moves in the radial direction, the magnitude of the relative velocity between the cloud and HD 32297 would be 16 km s−1. The cloud may have additional proper motion relative to HD 32297. If we assume that the cloud's velocity vector is parallel to HD 32297's motion on the sky that would produce a minimum relative velocity, while if it was moving antiparallel it would produce the maximum relative velocity. Based on the dispersion in velocity of nearby ISM clouds, we assume the magnitude of the cloud's velocity relative to that of HD 32297 is ∼14 km s−1 (Redfield & Linsky 2008), the minimum and maximum relative velocities between the cloud and HD 32297 would be 4 km s−1 and 29 km s−1.

We varied the relative velocity vector and Dg until we found qualitatively similar morphologies between our models and HD 32297. The best morphological match came from a relative velocity vector with a magnitude of 15 km s−1 at an inclination of 55° with respect to the yz plane in coordinates where the x-axis is aligned with the disk midplane and the z-axis is perpendicular to the midplane. This represents parameters in the middle of our estimates above.

For this model, Dg = 1.2 × 10−18 cm−1. Given the above parameters, one would expect Rdeflect ∼ 438 AU, about where the southwestern lobe of the disk shows a warp of ∼7°.

We show a comparison between the F160W image of HD 32297 and our synthetic image in Figure 6, arbitrarily scaled to similar maximum brightnesses and using the same stretch. We also show a comparison between two contour maps of the surface brightness, using the same scaling. The model and the data agree qualitatively.

Figure 6.

Figure 6. Left: comparison between an F160W image of HD 32297's disk and a model of a disk interacting with a cloud of ISM gas with the parameters mentioned in Section 4.1.1. Right: a comparison of surface brightness contours between HD 32297 (black lines) and our model (red lines). Our model has been arbitrarily scaled to match the maximum observed surface brightness.

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4.1.2. An ISM Gas Interaction Model for HD 15115

HD 15115 is an F2 star at 45 pc that has a disk with a highly asymmetric edge-on morphology; the eastern lobe of the disk appears truncated relative to the western lobe (Kalas et al. 2007; Debes et al. 2008a). The proper-motion vector of HD 15115 is southeast, with its eastern component almost twice as large as its southern component. In this case, we do not have a measure of the ISM cloud's radial velocity, so we strictly consider the relative transverse motion in the sky between the cloud and HD 15115. We can convert this transverse motion to determine the relative velocity constraints between the disk and the hypothesized ISM. The disk midplane is oriented with a P.A. of 279°. The transverse velocity vector of HD 15115 on the sky is at roughly the same P.A. as the disk. If we again assume a cloud with velocity of 14 km s−1 on the sky, the minimum and maximum possible relative transverse velocity is between 7 and 35 km s−1 if the cloud's velocity vector is parallel or antiparallel to HD 15115's proper motion. The morphology of the disk is consistent with the midplane plowing headlong into an ISM flow.

We assumed that HD 15115 had a stellar mass of 1.5 M and that grains were launched from 35 AU, the rough inner radius of HD 15115's disk as inferred from its IR excess (Zuckerman & Song 2004; Williams & Andrews 2006). Experimenting with different models showed that Dg = 1.3 × 10−18 cm−1 and a relative velocity vector with equal components along the midplane and along the observer's line of sight with a magnitude of 30 km s−1 best matched the observed data.

Figure 7 shows a comparison of the F110W image of HD 15115 with our disk model on the same size scale. The eastern lobe (left side of Figure 7) is contaminated by a strong residual that points roughly northeast in the figure (see Debes et al. 2008a). Otherwise, the figure shows that the morphology of the model matches the observation of HD 15115 showing a significant truncation of one lobe of the disk. Additionally, the figure shows that our models predict that the FWHM of the disk midplane should be wider on the truncated side. This aspect of the disk morphology is not significantly probed by current observations (Debes et al. 2008a). Another proposed scenario for this morphology is the close flyby of HD 15115 by another star (Kalas et al. 2007). However, no definitive candidates for a flyby have currently been detected (Debes et al. 2008a).

Figure 7.

Figure 7. Comparison between an F110W image of HD 15117's disk from Debes et al. (2008b) and a model of a disk interacting with a cloud of ISM gas with the parameters mentioned in Section 4.1.2.

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4.1.3. An ISM Gas Interaction Model for HD 61005

The disk observed around HD 61005, the "Moth," shows a peculiar disk morphology reminiscent of material being pushed up out of the disk midplane (H07). This shape might indicate disk interaction with the gas component of the ISM. The star itself is a late G8 dwarf at a distance of 34 pc, and H07 found that the surface brightness of the dust is consistent with dust grains roughly the size of the blow-out radius, 0.3 μm. H07 also determined from HD 61005's disk SED that the grains originate from radii ∼10 AU from the star.

The proper motion of HD 61005 is −56.09 mas in R.A., and 74.53 mas in declination (van Leeuwen 2007). If we rotate these velocities to a frame where the x-axis is parallel to the presumed major axis of the disk and convert to relative velocities under the same assumptions we used above as for HD 15115, the relative velocities will range in magnitude from 2 km s−1 to 30 km s−1, with a vector primarily along the xz plane at an inclination of 68° relative to the x-axis. If icy 0.3 μm grains are the population we observe around HD 61005, we can derive Dg under the assumption of an ISM gas density N(H i) = 100 cm−3. These two assumptions result in Dg = 3.3 × 10−18 cm−1.

We experimented with various relative velocity vectors until we found a qualitative match to the data. A velocity vector that is nearly perpendicular to the disk midplane with a magnitude of 25 km s−1 matches the data best, along with an inclination between the observer and the disk of 20°. Figure 8 shows a comparison of the model and the data, at the same size scale and stretch. We also see good qualitative agreement with the morphology of this disk as well.

Figure 8.

Figure 8. Comparison between an F110W image of HD 61005's disk (kindly provided by G. Schneider) and a model of a disk interacting with a cloud of ISM gas with the parameters mentioned in Section 4.1.3.

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5. DISCUSSION

In this section, we discuss some details that our ISM interaction model presently lacks.

5.1. ISM Dust Grains

For a disk interacting with an atomic ISM cloud with small grains, AC97 calculated an "avoidance radius," rav, where the radiation pressure of the central star was strong enough to scatter small grains away from a circumstellar disk. The distance rav depends on β, v, the initial velocity of a grain at large distances, and the stellar mass M.

Equation (6)

Incoming ISM dust grains pile up at this radius and scatter away from the star, leaving a paraboloidal region with minimum radius rav that is free from sandblasting from small ISM grains. This boundary marks the separation between where grains from the ISM could have a significant effect and where the ISM dust does not impact the evolution of dust in a circumstellar disk.

The color asymmetries observed for HD 32297 could potentially be explained by this ISM grain sandblasting. With some assumptions about the ISM grains as well as the cloud that may be impacting HD 32297's disk, we can estimate what rav is for HD 32297. AC97 calculated expected β's for ISM dust for an A5 star such as HD 32297. They calculated a maximum β for β-Pictoris assuming silicate+carbonaceous grains of 19.2. HD 32297 has a similar luminosity to β-Pictoris, so rav for HD 32297 would then be on order of between 133 AU and 1061 AU. The relative velocity of 15 km s−1 that we used for our gas interaction model of HD 32297 would correspond to an rav = 245 AU. This is slightly larger than expected from the observations, and could be accounted for by a combination of the gas interaction and sandblasting by ISM grains.

AC97 calculated how ISM grain sandblasting would affect dust erosion rates in a disk. They found that there should be larger dust removal rates in the part of the disk directly impacting the ISM, which in turn causes a large asymmetry in dust production/erosion between regions that suffer direct sandblasting and those that avoid it. Additionally, there is an asymmetry between dust grains that are moving antiparallel with the ISM flow and those that move away from the ISM flow, especially for grains in orbit around the star. Detailed modeling of the interaction with self-consistent grains of a particular composition and between the dusty ISM grains as well as the H i gas contained in the ISM cloud is left for a future paper (J. H. Debes et al. 2009, in preparation).

5.2. Other Uncertainties in the ISM Interaction Model

While the interaction of dust with the surrounding ISM provides an attractive explanation for the above disks, our models contain several uncertainties. For example, we have followed only a single size of dust grain in our interaction models, when clearly a size distribution of grains will be present in the disk. Furthermore, we have assumed a steady bulk flow to the ISM, even though one would expect turbulence on moderate size scales which could create further substructure.

While we found specific values of Dg, β, and vrel that fit the observed morphology, any of these can be varied to balance out a change in the other; we cannot derive unique fits to the data without further constraints on composition and vrel. Choosing a specific composition and grain type, such as spherical or fluffy particles would fix β and constrain Dg. Modeling the morphology and surface brightness of a disk at multiple wavelengths may provide further constraint on a particular gas interaction model. In some cases, this effect should help to further constrain dust grain particles, since the exact morphology of an interaction depends on the dust properties.

Physical processes, such as the presence of a stellar wind, can work to frustrate the interaction between the ISM and the circumstellar disk. For young solar-type stars, such as HD 61005, this may be important, while this may be less so for earlier type stars that have less magnetic activity. Regardless, models of interactions between a dense ISM cloud and the solar wind can guide us to the order of magnitude of this effect. Yeghikyan & Fahr (2003) modeled the interaction between an ISM cloud with N(H i) = 100 cm−3 and a solar-type wind. They found that when the Sun was placed in such a dense cloud the heliopause shrunk to ∼1 AU, well interior to the circumstellar region we observe for HD 61005. However, younger stars have stronger winds, which shield their debris disks out to hundreds of AU.

Finally, there are large uncertainties in the velocities and densities of the modeled ISM clouds. Background stars near each of the above stars could provide a possible probe of the clouds and constrain their density/radial velocity by providing lines of sight spatially coincident with the debris disks. Measurement of the transverse motions of the clouds would require a way of detecting the clouds directly at high spatial resolution, a difficult endeavor.

6. CONCLUSIONS

We have detected the HD 32297 debris disk at two additional wavelengths, bringing to four the total number of wavelengths in which this disk has been observed in scattered light. Both the morphology and the surface brightness of the disk as a function of wavelength hold useful clues to the nature of the dust in orbit around the star. The addition of more resolved near-IR scattering images of the HD 32297 disk provides measures of the morphology, surface brightness profiles, and scattering efficiency of the dust at three separate wavelengths.

We find that the morphology and asymmetries of the HD 32297 disk can qualitatively be explained by the interaction of the disk's dust with a moderately dense ISM cloud. We developed a numerical model for the interaction of a debris disk with ISM gas, and applied it to this system. We have also applied our ISM interaction model to two other disks, HD 15115 and HD 61005 and demonstrated that some warps and asymmetries in the outer regions of these disks can plausibly be explained by this mechanism.

Future coronagraphic observations of HD 32297' debris disk, especially with Space Telescope Imaging Spectrograph (STIS), will precisely measure the scattering efficiency of the inner disk in visible wavelengths. More work needs to be done to understand precisely the effect of a debris disk's environment on how it appears.

The authors thank Dean Hines and Glenn Schneider for kindly providing an image of HD 61005 and useful discussions on both HD 61005 and HD 32297. We also thank Carey Lisse for pointing out that stellar winds can affect dust/gas interactions and Chris Stark for a careful reading of the manuscript. This research is based on observations with the NASA/ESA Hubble Space Telescope which is operated by the AURA, under NASA contract NAS 5-26555. These observations are associated with programs GO No. 10177, No. 10527, and No. 10857. Support for program No. 10857 was provided by NASA through a grant from STScI. This research was supported by an appointment of JD to the NASA Postdoctoral Program at the Goddard Space Flight Center, administered by Oak Ridge Associated Universities through a contract with NASA. A.J.W. and M.J.K. also acknowledge support from the NASA Astrobiology Institute.

Footnotes

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10.1088/0004-637X/702/1/318