Abstract
In this paper, we present visible-range light curves of the irregular Uranian satellites Sycorax, Caliban, Prospero, Ferdinand, and Setebos taken with the Kepler Space Telescope over the course of the K2 mission. Thermal emission measurements obtained with the Herschel/PACS and Spitzer/MIPS instruments of Sycorax and Caliban were also analyzed and used to determine size, albedo, and surface characteristics of these bodies. We compare these properties with the rotational and surface characteristics of irregular satellites in other giant planet systems and also with those of main belt and Trojan asteroids and trans-Neptunian objects. Our results indicate that the Uranian irregular satellite system likely went through a more intense collisional evolution than the irregular satellites of Jupiter and Saturn. Surface characteristics of Uranian irregular satellites seem to resemble the Centaurs and trans-Neptunian objects more than irregular satellites around other giant planets, suggesting the existence of a compositional discontinuity in the young solar system inside the orbit of Uranus.
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1. Introduction
Giant planets basically possess two distinct types of satellites concerning orbital dynamics. Regular satellites are characterized by orbits with small eccentricity that are very close to the planets' equatorial plane, and always have a prograde orbit within , where rH is the radius of the Hill sphere of host planet. In contrast, irregular satellites have moderate-to-high eccentricities and inclinations with prograde or retrograde orbits up to from their host planets. The existence of two classes of satellites reflects two different ways of evolution: regular satellites likely formed in the same subnebula as the host planet, while irregular satellites could not have formed at their present orbits. The most accepted scenario currently is that they have been captured from the inside of the planet's subnebula in the last phase of planet formation on temporary orbits, then settled through some kind of loss of angular momentum (see Nicholson et al. 2008 for a review).
There were several deep surveys of irregular satellites in the 2000s that established the basis of the currently known set of irregular satellites (Gladman et al. 1998, 2000, 2001; Holman et al. 2000, 2003, 2004; Kavelaars et al. 2004; Sheppard & Jewitt 2003; Sheppard et al. 2003, 2005, 2006). These surveys provided the main orbital characteristics of the satellites found and allowed for the identification of orbital grouping/families around the specific planets (Nicholson et al. 2008).
Unlike the members of other small body populations in the solar system, irregular satellites may have remained close to their formation locations and their compositions may be an intermediate one between that of the main-belt asteroids and the icy trans-Neptunian objects. The physical characterization of these satellites is, however, still a challenging task due to the large distance and the typical size below 100 km, even in the case of the closest Jovian system. Among these characteristics, light curves provide information on the shape and/or surface albedo variegations and may give hints of the internal structure and strength in the case of fast rotators; the distribution of rotational frequencies and amplitudes are important properties of a small body population (Pravec et al. 2002). A high-quality light curve is available for the largest Jovian irregular, Himalia (Pilcher et al. 2012), rotational properties are known for the Jovian satellites Lysithea, Ananke, Carme, and Sinope (Luu 1991) and the Cassini spacecraft provided rotation periods for many irregular satellites in the Saturnian system (Denk & Mottola 2013, 2014, 2015). In the Uranian system, Maris et al. (2001, 2007) performed the investigation of the light curves of irregular satellites and obtained rotational characteristics for Sycorax, Caliban, Prospero, and Setebos. However, in these latter cases, the results are based on sparsely sampled data due to the observing capabilities of the telescopes and the large distance (hence faintness) of these satellites.
Broadband colors are the most readily available tools that can be used to characterize the surface of the irregular satellites (see Nicholson et al. 2008, and references therein). In the Jovian system the colors are similar to those of carbonaceous asteroids and Jovian Trojans, while in the Saturnian system they show somewhat redder surfaces. However, in both systems the colors are still far from that of the red material typically found in the Kuiper Belt. In the Uranian system, the colors show a wide variety, but there are certainly satellites that show typical "Kuiper Belt" colors (Maris et al. 2001, 2007; Romon et al. 2001; Grav et al. 2004).
Well-established size and albedo values are available for a limited sample only, mainly from data of space probes—e.g., Himalia and Phoebe by Cassini (Porco et al. 2003, 2005), or Nereid by Voyager-2 (Thomas et al. 1991). Recently, thermal emission data obtained with the MIPS camera of the Spitzer Space Telescope (Rieke et al. 2004) and the PACS camera of the Herschel Space Observatory (Poglitsch et al. 2010) also provided independent size and albedo estimates for Sycorax (Lellouch et al. 2013) and Nereid (Kiss et al. 2016).
As we noted above, ground-based observations could not place strong constraints on the rotation of most of the irregular satellites observed earlier. However, it was demonstrated in recent works (Pál et al. 2015, 2016; Szabó et al. 2016, 2017) that data from the extended Kepler mission (Howell et al. 2014, K2) can be very effectively used to obtain rotational light curves of solar system bodies due to uninterrupted photometric time series of several tens of days in length, including main belt and Jovian Trojan asteroids, and trans-Neptunian objects, even at the brightness level of typical irregular satellites. Lately, a thorough light-curve analysis of the Neptunian irregular satellite Nereid was also performed (Kiss et al. 2016), showing the great capabilities of K2 measurements for this kind of application.
In this paper, we present the results of Uranian irregular satellite observations performed with the Kepler space telescope in Campaign 8 of the K2 mission. We provide light curves and derive rotational characteristics for Sycorax, Caliban, Prospero, Setebos, and Ferdinand (Section 4). In addition, we use thermal emission measurements of the Spitzer Space Telescope and the Herschel Space Observatory to derive more accurate size and albedo for Sycorax; we also give constraints on the size and albedo of Caliban, Trinculo, and Ferdinand (Section 3) based on Herschel/PACS observations. Our results are compared with the properties of other irregular satellites and other small body populations of our solar system (Sections 5 and 6).
2. Observations
2.1. Kepler/K2 Measurements
Continuous photometry from the Kepler space telescope may provide accurate and unbiased rotation rates and amplitudes for solar system targets. The telescope gathers light in a wide visual band spanning from 420 to 900 nm, and follows a step-and-stare scheme in the K2 mission, observing different fields for up to 80 days along the Ecliptic plane (Howell et al. 2014). Kepler observed Uranus and its vicinity during Campaign 8 of the mission for 78.73 days, between 2016 January 4.55 and March 23.28. Apart from the planet, four irregular satellites Caliban, Setebos, Sycorax, and Prospero, were also proposed and selected for observations (GO8039, PI: A. Pál).7
We applied the same pipeline for the reduction of the Kepler observations that we used in previous works, e.g., to determine the light variations and rotation rates of various Trans-Neptunian Objects, main-belt and Trojan asteroids, or of the moon Nereid (Pál et al. 2015, 2016; Kiss et al. 2016; Szabó et al. 2016, 2017). The method is based on the FITSH8 software package (Pál 2012): the processing steps are detailed in the previous papers and in the companion paper that describes the light curves of main-belt asteroids drifting though the same image mosaic (Molnár et al. 2017), also providing information on the limitations and capabilities. In short, we created mosaic images from the individual Target Pixel Files (TPFs), which contain the time-series photometric information (time, flux, flux error, and background) for each downloaded pixel around a given target, as opposed to light-curve files that contain a pipeline-extracted brightness summed in an aperture as a function of time. For more details, the reader is directed to Kepler Archive Manual.9 We then derived the astrometric solutions for the mosaic images, using the USNO-B1.0 catalog (Monet et al. 2003), where the K2 full-frame images from the campaign were exploited as initial hints for the source cross-matching. Then, we registered the images into the same reference system, and subtracted a median image from each image. This median image was created from a selection of individual images that did not include the obvious diffraction pattern contamination from Uranus. We then applied aperture photometry at the positions of the satellites. The sharp images of the stars that were shifted to compensate the attitude changes of the telescope create characteristic residuals in the differential images that may contaminate our photometry. Therefore we filtered out the epochs when the scatter of the background pixels in the photometric annulus was high. The per-cadence photometric uncertainty values were derived from the shot noise of Kepler and from the estimated background noise.
All observations were collected in long cadence mode, with a sampling of 29.4 minutes. Three of the proposed satellites fell into, or near, the large mosaic that also covered the apparent motion of Uranus (Figure 1). Other satellites were also present in the same mosaic, and we successfully detected the light variations of a fourth one, Ferdinand.
Prospero fell onto an adjacent CCD module, and its motion was covered with a narrow band of pixels. In that case, we collected the TPFs of nearby, unrelated targets into a small mosaic around the track of Prospero in order to have a good astrometric solution. The log of observations is summarized in Table 1. The duty cycle there shows the ratio of accepted photometric data points to the number of cadences when the satellites were present on the images. We note that Ferdinand was observed twice, at the beginning and at the end of the campaign: the two rows in the table refer to the entire length of the observation and the sections when Ferdinand was on the Kepler CCD array, respectively. The temporal distribution of data points we used for photometry is presented in Figure 2. We also checked other satellites that fell on the CCD array, e.g., Stephano (24.5 mag) or Trinculo (25.5 mag), but found no meaningful signals in their photometry.
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Standard image High-resolution imageTable 1. Log of the Kepler Observations
Name | Start | Length | Points | Duty | Kp |
---|---|---|---|---|---|
TBJD (d) | d | Cycle | (mag) | ||
Caliban | 7419.16 | 22.23 | 1019 | 0.93 | 21.99 |
Setebos | 7416.15 | 28.85 | 495 | 0.35 | 22.87 |
Sycorax | 7418.55 | 13.67 | 599 | 0.89 | 20.18 |
Prospero | 7416.48 | 28.89 | 793 | 0.56 | 22.94 |
Ferdinand | 7392.12 | 74.01 | 270 | 0.07 | 23.12 |
On Array | ⋯ | 16.14 | ⋯ | 0.32 | ⋯ |
Note. TBJD means truncated BJD, BJD-2450000. The last line shows the values for ferdinand if we ignore the 57.87-day-long period it spent off the detector array during the campaign. Duty cycle is 1.0 when all photometric points are retained and 0 when all had to be discarded. Kp is the mean brightness of the target in the Kepler photometric system.
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2.2. Infrared Data
2.2.1. Sycorax
Sycorax was observed with the MIPS camera of the Spitzer Space Telescope (Rieke et al. 2004) at two epochs, on 2008 December 27 and 29, both at 24 and 70 μm. The summary of these observations is given in Table 2 below. Sycorax was successfully detected at both epochs and at both wavelengths (see Figure 3). We used the same data reduction and photometry pipeline as in Mueller et al. (2012) and Stansberry et al. (2008, 2012). The MIPS instrument team data analysis tools (Gordon et al. 2005) were used to produce flux-calibrated images for each band, and the contribution of background objects were subtracted (see Stansberry et al. 2008). Aperture photometry was performed both on the original and final images and the final flux values were obtained using the aperture corrections by Gordon et al. (2007) and Engelbracht et al. (2007). Color correction of the in-band fluxes were done following Stansberry et al. (2007). The flux densities obtained are presented in Table 3.
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Standard image High-resolution imageTable 2. Summary of Thermal Infrared Observations
Instrument | AORKEY/ | Target | Band | Date | r | Δ | α |
---|---|---|---|---|---|---|---|
OBSID | (μm) | (JD) | (au) | (au) | (deg) | ||
Spitzer/MIPS | 28832512 | Sycorax | 24 | 2454827.702 | 20.081 | 19.672 | 2.68 |
28832512 | 70 | 2454827.718 | 20.081 | 19.672 | 2.68 | ||
28832768 | 24 | 2454829.672 | 20.081 | 19.704 | 2.71 | ||
28832768 | 70 | 2454829.688 | 20.081 | 19.704 | 2.71 | ||
Herschel/PACS | 1342221837–38 | Sycorax | 70 | 2455710.589 | 20.084 | 20.519 | 2.62 |
1342221875–76 | 70 | 2455710.939 | 20.084 | 20.514 | 2.62 | ||
1342221839–40 | 100 | 2455710.617 | 20.084 | 20.519 | 2.62 | ||
1342221877–78 | 100 | 2455710.966 | 20.084 | 20.513 | 2.63 | ||
1342221837–40 | 160 | 2455710.589 | 20.084 | 20.519 | 2.62 | ||
1342221875–78 | 160 | 2455710.939 | 20.084 | 20.514 | 2.62 | ||
Herschel/PACS | 1342236891–92 | Caliban | 70 | 2455933.979 | 20.119 | 20.359 | 2.73 |
1342237436–37 | 70 | 2455940.001 | 20.117 | 20.457 | 2.63 | ||
1342236891–92 | 160 | 2455933.979 | 20.119 | 20.359 | 2.73 | ||
1342237436–37 | 160 | 2455940.001 | 20.117 | 20.457 | 2.63 | ||
Herschel/PACS | 1342236891–92 | Trinculo | 70 | 2455933.979 | 20.051 | 20.293 | 2.73 |
1342237436–37 | 70 | 2455940.001 | 20.048 | 20.390 | 2.64 | ||
1342236891–92 | 160 | 2455933.979 | 20.051 | 20.293 | 2.73 | ||
1342237436–37 | 160 | 2455940.001 | 20.048 | 20.390 | 2.64 | ||
Herschel/PACS | 1342236891–92 | Ferdinand | 70 | 2455933.979 | 19.930 | 20.174 | 2.75 |
1342237436–37 | 70 | 2455940.001 | 19.929 | 20.173 | 2.65 | ||
1342236891–92 | 160 | 2455933.979 | 19.930 | 20.174 | 2.75 | ||
1342237436–37 | 160 | 2455940.001 | 19.929 | 20.173 | 2.65 |
Note. The columns are (1) telescope/instrument; (2) AORKEY (Spitzer/MIPS) or OBSID (Herschel/PACS); (3) target—in the case of Caliban the target was caught in a larger, off-Uranus field; (4) band (nominal wavelength in μm); (5) date of the observation (julian date); (6) heliocentric distance; (7) distance from observer; (8) phase angle.
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Table 3. Summary of Thermal Infrared Observations
Target | Detector/ | Fi | Fm | |||
---|---|---|---|---|---|---|
Filter | (μm) | (mJy) | (mJy) | (mag) | ||
Sycorax | MIPS 24 | 23.68 | 3.017 ± 0.045 | 0.96 ± 0.01 | 3.14 ± 0.16 | 7.50 ± 0.04 |
MIPS 70 | 71.42 | 14.68 ± 2.78 | 0.92 ± 0.01 | 16.07 ± 2.89 | (Grav et al. 2004) | |
MIPS 24 | 23.68 | 3.109 ± 0.046 | 0.96 ± 0.01 | 3.17 ± 0.17 | ⋯ | |
MIPS 70 | 71.42 | 19.12 ± 2.70 | 0.92 ± 0.01 | 20.78 ± 3.11 | ⋯ | |
PACS 70 | 70.0 | 16.7 ± 0.6 | 0.98 ± 0.01 | 17.0 ± 1.0 | ⋯ | |
PACS 100 | 100.0 | 15.3 ± 1.6 | 1.00 ± 0.01 | 15.3 ± 1.8 | ⋯ | |
PACS 160 | 160.0 | 5.3 ± 3.1 | 1.04 ± 0.01 | 5.5 ± 3.2 | ⋯ | |
Caliban | PACS 70 | 70.0 | 1.4 ± 0.8 | 0.98 ± 0.01 | 1.4 ± 0.8 | 9.16 ± 0.016 |
PACS 160 | 160.0 | <3 mJy | 1.04 ± 0.01 | <3 mJy | (Grav et al. 2004) | |
Trinculo | PACS 70 | 70.0 | <0.8 mJy | 0.98 ± 0.01 | <0.8 mJy | 11.92 ± 0.18 |
PACS 160 | 160.0 | <3 mJy | 1.04 ± 0.01 | <3 mJy | (Grav et al. 2004) | |
Ferdinand | PACS 70 | 70.0 | <0.8 mJy | 0.98 ± 0.01 | <0.8 mJy | 12.5 ± 0.1(R) |
PACS 160 | 160.0 | <3 mJy | 1.04 ± 0.01 | <3 mJy | (this work) |
Note. The columns are (1) target—in the case of Caliban the target was caught in a larger, off-Uranus field; (2) detector and filter combination; (3) effective wavelength of the band (); (4) in-band flux density (Fi); (5) color correction factor (); (6) monochromatic flux (); (7) absolute magnitude in V or R Band; Herschel/PACS flux densities of Sycorax are taken from Lellouch et al. (2013).
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Sycorax was also observed in dedicated observations with the PACS camera of the Herschel Space Observatory, in the framework of the "TNOs are Cool!" Herschel Open Time Key Program (Müller et al. 2009). The flux densities derived from these observations have already been presented in Lellouch et al. (2013).
We used both the Spitzer/MIPS and Herschel/PACS data for modeling of the thermal emission of the satellite (see Section 3.1).
2.2.2. Serendipitous Herschel/PACS Observations of Irregular Satellites
Caliban was identified as potentially present on some far-infrared maps taken with the PACS camera of the Herschel Space Observatory. Herschel/PACS observed the environment of Uranus at two epochs: on 2012 January 7 (OBSIDs: 1342236891/92/scan and cross-scan) and on 2012 January 13 (OBSIDs: 1342237436/37), under the proposal ID OT1_ddan01_1 in both cases. All measurements used the 70/160 μm filter combination in all four cases. The data reduction pipeline we used is the same as the one used in the 'TNOs are Cool! Herschel Open Time Key Programme (Müller et al. 2009), described in detail in Kiss et al. (2014), and identical to the one we used to reduce the Herschel/PACS maps of Nereid (Kiss et al. 2016). As our aim was to obtain photometry of a point source, we used the photProject() task with high-pass filtering to create maps from the time domain detector data. The photProject() task performs a simple coaddition of the frames using the drizzle method (Fruchter & Hook 2002), and the high-pass filtering applies a sliding median-filter on individual pixel timelines. More details on the procedure can be found in The PACS Data Reduction Guide.10
Maps were created from the detector scans in the co-moving frame of Uranus (see Figure 4), which was practically identical to that of the satellites due to the small relative velocities of Uranus and the satellites (<05 hr−1).
We identified a faint source at both epochs in the 70 μm band at the expected location of Caliban, obtained from the NASA Horizons System considering the Herschel-centric observing geometry (see Figure 5), and derived a combined flux of F70 = 1.4 ± 0.8 mJy. No obvious source could be identified on the 160 μm maps, and the general photometric accuracy obtained using the implanted source method (see Kiss et al. 2014) defined a 1σ upper limit of F160 < 3 mJy for the 160 μm brightness of Caliban.
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Standard image High-resolution imageWhile Trinculo and Ferdinand could potentially be present on the same set of Herschel/PACS images as Caliban, these were not detected either at 70 or at 160 μm, therefore we consider that their flux densities are below 0.8 mJy and 3 mJy at 70 and 160 μm, respectively.
2.3. Konkoly Observatory 1 m Telescope Observations of Sycorax
Sycorax was also observed on the night of 2015 November 05/06 with the 1 m Ritchey-Cretien Coude (RCC) telescope of the Konkoly Observatory, located at Piszkéstető Mountain Station. In total, 70 frames were acquired with an exposure time of 300 s each, using an Andor iXon-888 electron-multiplying CCD camera. Although it is not so relevant for such long exposures, we note here that the camera was operated in frame transfer readout mode in order to have an effectively zero dead time between the subsequent frames. The frames were taken in Sloan r' filters and used the SDSS-III DR9 catalog (Ahn et al. 2012) for reference magnitudes of the comparison stars. Standard calibration procedures and aperture photometry were performed using the various tasks of the FITSH package (Pál 2012). The resulted light curve is plotted in Figure 6.
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Standard image High-resolution image3. Thermal Emission Models
To model the thermal emission of some of our targets, infrared monochromatic flux densities were derived from the in-band flux densities applying the appropriate color corrections, based on the surface temperatures of the targets (see Colbert 2011; Müller et al. 2011, for the Herschel/PACS and Spitzer/MIPS color corrections, respectively), see also Table 3.
We used these monochromatic flux densities and the observing geometry parameters listed in Table 2 to constrain the thermal emission models of our targets by calculating the values of the modeled and observed monochromatic flux densities (see, e.g., Vilenius et al. 2014, for details). We applied either the Near-Earth Asteroid Thermal Model (NEATM, Harris 1998) or a thermophysical model (TPM Lagerros 1996, 1997, 1998; Müller & Lagerros 2002) to obtain the model flux densities. TPM was only chosen in the case of Sycorax, as in the case of the other satellites with limited amounts of thermal data (low degrees of freedom) it is not meaningful to run a complex TPM model over a more simple NEATM one. We used our own NEATM code written in IDL,11 and a TPM code developed by J.S.V. Lagerros and T.G. Müller (see the references above).
3.1. Sycorax
The thermal emission of Sycorax was modeled using the flux densities listed in Table 3, applying a NEATM model. Due to the notable difference in observing geometry at the PACS and MIPS epochs, for a specific model (given size and beaming parameter) the corresponding observation geometries were considered at the PACS and MIPS epochs separately, and the values were derived accordingly. The best-fit model is presented in Figure 7, where the flux densities of the MIPS and PACS epochs are shown individually. The NEATM model provided a best-fit effective diameter and albedo estimate of D = 165 ± 13 km, , with a beaming parameter of .
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Standard image High-resolution imageIn addition to the NEATM model, we also applied thermophysical modeling (TPM, see Müller & Lagerros 1998, 2002, and references therein) considering an absolute magnitude of HV = 750 ± 004 (Grav et al. 2004), a default slope parameter of G = 0.15 and a wavelength-dependent emissivity (Müller & Lagerros 2002). We used P = 6.9162 hr for the rotation period, as determined from the combination of K2 and Konkoly 1m-RCC measurements (see Section 4.1); possible thermal inertia values were considered in the Γ = 0.1–50 range and surface roughness values were allowed between ρ = 0.1 and 0.9. Because the spin-axis orientation of Sycorax is not known, we considered three possible scenarios, a pole-on (spin-axis orientation of λ = 356°, β ≈ 0° in ecliptic coordinates), an equator-on (λ = 0°, β = 90°), and an intermediate one (λ = 356°, β = 45°). The equator-on and intermediate solutions provide a low best-fit reduced of < 1, and give very similar best-fit values for the size. However, no acceptable solution with sufficiently low could be obtained for the pole-on case ( in all cases) and a non-pole-on configuration is also supported by the presence of a definite visible-range light curve. Our best estimates for the size and albedo are km and , associated with a likely intermediate surface roughness (ρ ≈ 0.5) and a close-to-equator-on spin-axis configuration. Based on this analysis, very low levels of thermal inertia () can be excluded for Sycorax.
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Standard image High-resolution imageThe diameter and geometric albedo obtained by our analysis is close to the best-fit values obtained by Lellouch et al. (2013) using Herschel/PACS data alone (, , see also Figure 8), but in our case with smaller error bars. However, the beaming parameter is much better constrained with the consideration of the Spitzer/MIPS fluxes, as the Herschel/PACS data could not restrict the models further due to the lack of short wavelength (≲40 μm) data ( in Lellouch et al. 2013). Our best-fit η = 1.20 is very close to the median values obtained for Centaurs and trans-Neptunian objects based on a large sample of Spitzer/MIPS and Herschel/PACS measurements (η ≈ 1.2, Stansberry et al. 2008; Lellouch et al. 2013). The thermal inertia value of Γ = 3–4 we obtained for Sycorax is also in agreement with the Γ = 5 ± 1 value found by Lellouch et al. (2013) for Centaurs at heliocentric distances <25 au.
3.2. Small Irregular Satellites on Herschel/PACS Images
For all potentially detectable satellites, we used a NEATM model with a constant emissivity of = 0.9 to estimate the expected flux densities in the 70 μm Herschel/PACS band for a range of diameters/geometric albedos and beaming parameters. The beaming parameter η was allowed to vary between 0.6 and 1.6, while the diameters were chosen to match a V-band geometric albedo range of . Phase integrals were calculated applying both the geometric albedo-dependent phase integral developed for the outer Solar system by Brucker et al. (2009) and the "standard" value using the canonical slope parameter of G = 0.15 (see, e.g., Muinonen et al. 2010). The difference between the 70 μm thermal emission flux densities obtained by the two methods were ≤4 μJy in all cases, and are negligible for our purposes.
As described above, Caliban was tentatively detected on Herschel/PACS 70 μm maps with a combined monochromatic flux density of F70 = 1.4 ± 0.8 mJy. A generally assumed dark surface of pV ≈ 0.04 and the corresponding diameter of ∼70 km would produce a 70 μm flux density of F70 > 2.4 mJy, easily detectable on our Herschel/PACS maps, over 3σ of the 0.8 mJy 70 μm flux uncertainty of the Herschel/PACS maps. The fact that the detected flux density of Caliban is smaller than that already indicates a brighter surface. We obtained km and as the best-fit NEATM solution using the single available 70 μm flux density, with no real constraint on the beaming parameter in our originally chosen 0.6 ≤ η ≤ 1.6 range, with our best-fit model having a corresponding η of 0.8. The 70 μm flux of Caliban can, however, be equally well fitted with D ≈ 50 km and ≈ 0.15, using a higher η value of ∼1.4. The uncertainties in the size and albedo due to the unconstrained beaming parameter are reflected in the errors of the best-fit values quoted above. The geometric albedo we obtained for Caliban may seem to be surprisingly high in the Uranian irregular satellite system, taking into account the low albedo of Sycorax. On the other hand, relatively bright surfaces exist among other irregular satellites, e.g., Nereid has a surface with > 20% (Kiss et al. 2016), but it is notably larger than Caliban, ∼350 km in effective diameter.
Trinculo and Ferdinand were not detected on the Herschel/PACS images. However, considering the 0.8 mJy 70 μm flux uncertainties as an upper limit for both targets, we can put some constraints on their geometric albedos and diameters. We note that for Ferdinand we calculated the R-band absolute magnitude using data in the Minor Planet Circular MPEC-2003-S105, assuming an R-band specific linear phase correction of (Belskaya et al. 2008) and obtained HR = 12.06 ± 0.15 mag. For Trinculo, we used the value provided by Grav et al. (2004; see also Table 3). The 0.8 mJy 1σ upper limit indicates a geometric albedo of > 0.03 for both satellites, and correspondingly their diameters are D < 50 km.
4. Rotational Characteristics from K2 Measurements
We searched for significant periodicities using the Fourier method as implemented in the Period04 program package (Lenz & Breger 2005) and also the Lomb–Scargle periodogram in the gatspy Python package.12 We got very similar results in several test cases, therefore we decided to stick to the Lomb–Scargle periods. We note that the errors of the individual photometric points are taken into account. Only those signals were considered that were significant on the 3σ level compared to the background local noise periodogram. We phase-folded the light curves with the best period and its double value, then decided which gave a better fit based on a visual inspection. As we have shown previously (Szabó et al. 2016) period determination of solar system object with K2 long cadence measurements is solid if the coverage exceeds five days and the duty cycle is above 60%. These conditions are fulfilled for three of our targets, as we have shown in Table 1 already. The other two, Setebos and Ferdinand, have lower duty cycles, but the long baseline of the observations compensates for them. Overall, we were able to derive reliable solutions for most Uranian irregular satellites in our sample. The results are presented in Figures 10 and 11 and in Table 4 below. Table 4 also lists the rotation periods obtained from previous investigations. We emphasize that we do not accept all formally significant periods, but simply choose the one with the highest amplitude.
Table 4. Summary of Previous and Present Light-curve Observations of the Uranian Irregular Satellites Sycorax, Caliban, Prospero, Setebos, and Ferdinand with the Most Likely Rotation Periods Identified
Previous Works | This Work | |||||||
---|---|---|---|---|---|---|---|---|
Satellite | P | Δm | References | f0 | P | Δm | Comm. | Ps |
(hr) | (mag) | (cycle day−1) | (hr) | (mag) | (hr) | |||
Sycorax | 4.12 ± 0.04 | 0.032 ± 0.008s | M01 | 6.9374 ± 0.0083 | 6.9190 ± 0.0082 | 0.121 ± 0.020 | K2,d | 67.3423 |
3.60 ± 0.02 | 0.067 ± 0.004s | M07 | 6.9402 ± 0.0013 | 6.9162 ± 0.0013 | 0.120 ± 0.019 | K2+1 m,d | ||
Caliban | 2.66 ± 0.04 | 0.13 ± 0.01s | M01 | 4.8249 ± 0.0092 | 9.948 ± 0.019 | 0.16 ± 0.03 | K2,d | 7.0026 |
Prospero | 4.55 ± 0.04 | 0.22 ± 0.03s | M07 | 3.359 ± 0.044 | 7.145 ± 0.092 | 0.41 ± 0.07 | K2,s | 16.5871 |
Setebos | 4.38 ± 0.05 | 0.189 ± 0.03s | M07 | 5.640 ± 0.022 | 4.255 ± 0.017 | 0.27 ± 0.06 | K2,s | 13.1705 |
Ferdinand | ⋯ | ⋯ | ⋯ | 2.027 ± 0.039 | 11.84 ± 0.22 | 0.54 ± 0.09 | K2,s | 82.715 |
Note. The light-curve amplitudes are peak-to-peak values, unless marked with an "s" upper index—in this case, they represent a sinusoidal amplitude. The references used in the table are M01—Maris et al. (2001) and M07—Maris et al. (2007). In the last column "K2" and "1 m" indicates data obtained from the K2 mission and with 1 m telescope of konkoly observatory, while "d" and "s" mark single-peak and double-peak rotation periods. The last column (Ps) lists the stroboscopic periods calculated from the single-peak periods.
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4.1. Sycorax
Maris et al. (2001) performed the first detailed study of the light curve in the R band using the 3.6 m ESO NTT telescope at La Silla, on 1999 October 8 and 9. The amplitude of light variation they found was A = 0032 ± 0008 with a P = 4.12 ± 0.04 hr period. Measurements taken with the VLT in 2005 (Maris et al. 2007) provided the most likely light-curve period and amplitude of P = 3.6 ± 0.02 hr and A = 0067 ± 0004.
Our K2 measurements revealed a well-defined rotational period with a frequency of f = 6.9374 ± 0.0083 cycle day−1 (P = 3.458 ± 0.001 hr, see Figure 10). We assume that the light curve of Sycorax is double-peaked, which is supported by the slight asymmetry of the light curve when it is folded with the half frequency/double rotation period (Figure 10). This gives a double-peaked rotation period of P = 6.9190 ± 0.0082 hr. The single-peaked period is very close to that obtained by Maris et al. (2007) using VLT measurements. The peak-to-peak light-curve amplitude obtained from K2 data is A = 012 ± 002, consistent with that obtained by Maris et al. (2007) as sinusoidal amplitude.
There is a second significant peak on the frequency diagram at 0.35 cycle day−1 (Figure 9, upmost panel). Such secondary periods are often explained by tumbling rotation or a companion. Although a companion around Sycorax (a moon of a moon) would be an intriguing possibility, we suggest that this second peak is a sampling artifact. The interaction of a strictly periodic sampling (such as that of Kepler) and a strictly periodic process (such as a rotation of the asteroid) results in periodic phase shifts in the sampling, and hence, an emergence of a stroboscopic period that can modulate timing, brightness, shape modulations, etc. In Szabó et al. (2013), we calculated the stroboscopic period as , where Ps is the stroboscopic period, P is the observed actual period, C is the cadence, and denotes the fractional part. Substituting the rotation period (6.9162 ± 0.0013 hr) and the cadence (1765.5 s) into the formula, the stroboscopic period is calculated to be 9.5–10.0-times the rotation period. Since the ratio of the two detected periods is 9.97, this is perfectly compatible with the stroboscopic origin of the long-period brightness variation. Stroboscopic periods were calculated from the single-peak periods of the other targets too (see below), as listed in Table 4. We note that a stroboscopic period is not accepted simply by an amplitude criterion as a possible rotation period, but should be rejected due to its stroboscopic nature.
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Standard image High-resolution imageSince the series of ground-based observations with the 1 m telescope of the Konkoly Observatory was roughly three months before the K2 measurements and the precision of K2 measurements are rather fine, one can extrapolate the rotation cycle numbers in an unambiguous manner for such a relatively short period. This allows us to combine the two series of measurements (K2 and 1 m RCC) to get an accurate rotational frequency, for which we obtained n = 3.47012 ± 0.00067 cycle day−1, i.e., P = 6.9162 ± 0.0013 hr.
4.2. Smaller Satellites
Caliban: Maris et al. (2001) determined a light-curve period of 2.66 hr that is not confirmed by our data (see Figure 10). Instead, we obtained a most likely frequency of f = 4.8249 ± 0.0092 cycle day−1 and the asymmetry of the folded light curve indicates that the real rotation period corresponds to the half frequency, i.e., P = 4.9742 ± 0.0095 hr. The single-peak period of Caliban is the only one apart from that of Sycorax for which the corresponding stroboscopic frequency (Ps = 7.0026 hr or fs = 3.4256 cycle day−1) is close to a significant peak in Figure 10.
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Standard image High-resolution imageProspero: In our analysis, the least unambiguous light-curve period was obtained for Prospero (see Figure 11). We identified the most likely period of 3.359 ± 0.044 cycle day−1 (P = 7.145 ± 0.092 hr), but a strong, secondary peak is also visible at f = 4.415 ± 0.045 cycle day−1 that corresponds to a single-peak rotation period of P = 5.346 ± 0.055 hr, very close to the light-curve period obtained by Maris et al. (2007).
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Standard image High-resolution imageSetebos: For this satellite, we confirm the light-curve period of 4.38 ± 0.05 hr obtained by Maris et al. (2007) as we derived a most likely rotation period of P = 4.255 ± 0.017 hr, very close to the previously mentioned value, without indication of a double-peak light curve.
Ferdinand: The light curve period of Ferdinand was not determined earlier. The most likely frequency of 2.027 ± 0.039 cycle day−1 corresponds to a rather long rotation period of 11.84 ± 0.22 hr, the longest one in our sample (assuming a single-peak light curve, see Figure 11). Such long rotation periods are, however, not rare and present e.g., in the Saturnian system where the rotation periods of 10 from 16 irregular satellites in a recently studied sample show rotation periods longer than that of Ferdinand (Denk & Mottola 2013a).
5. Comparison with the Rotational Characteristics of Other Irregular Satellites and Asteroids
Rotation of small body populations in the solar system is often characterized by the so-called spin barrier, a critical rotation period at which a rubble pile asteroid would fly apart due to its centripetal acceleration. This spin barrier is well established for main-belt asteroids, the critical rotation period is ∼2.2 hr (dashed horizontal line in Figure 12), resulting in a critical density estimate of ∼2.0 g cm−3, using the formula by Pravec & Harris (2000). In Figure 12, we plot the rotation period versus size for various small body populations as well as for irregular satellites of the giant planet systems.
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Standard image High-resolution imageConsidering our sample, the median rotational frequencies are notably higher in the Uranian system (≈3.4 cycle day−1) than in the other giant planet systems (≈2 cycle day−1 for Jupiter, Saturn, and Neptune). Also, assuming the double-peak rotation periods for Sycorax and Caliban provides us with critical densities ≤ 0.76 g cm−3. When the single-peak periods are considered for all Uranian irregular satellites still remains below 1 g cm−3. These values are below the upper limits of ∼2 g cm−3 of main-belt asteroids, but higher than the ∼0.5 g cm−3 obtained for e.g., Jovian Trojans (Szabó et al. 2017), the typical densities of cometary nuclei and trans-Neptunian objects (A'Hearn 2011; Brown 2013; Vilenius et al. 2014), and also those critical densities that can be estimated for the irregular satellites of the other giant planet systems, based on rotational light curves alone. However, e.g., the mass of the largest Jovian irregular Himalia has been estimated from its perturbations on other satellites (Emelyanov et al. 2005), and it gives an independent estimate on the density, ρ > 2.6 g cm−3, using the size obtained during the Cassini flyby (effective radius of ∼67 km Porco et al. 2003). This is significantly larger than the critical density of ∼0.2 g cm−3 that can be obtained from the rotation period of 7.78 hr and the light-curve amplitude of 020 ± 001 (Pilcher et al. 2012).
The Uranian irregular satellites in our sample are in the size range where Maxwellian distribution of rotational frequencies starts for main-belt asteroids (D ≳ 40 km, Pravec et al. 2002). While our sample is small and certainly not unbiased, the large median rotational frequency of the Uranian irregular satellites (3.4 cycle day−1) may indicate that this irregular satellite system had a collisional evolution different from those around Jupiter and Saturn and Uranian irregulars suffered from a higher number and/or more energetic collisions. The median rotation period of 7.1 hr in the Uranian system is close to that obtained for Centaurs (7.35 hr, Duffard et al. 2009) and somewhat smaller than that of trans-Neptunian objects (8.6 hr, Thirouin et al. 2014), however, these populations certainly went through a different collisional evolution than that of the Uranian irregular satellite system.
6. The Albedo-color Diversity of Irregular Satellites
In Figure 13, we plotted the colors (represented by spectral slopes, Luu & Jewitt 1990) versus the geometric albedos of those irregular satellites for which this information was available. The Jovian irregular satellites are typically found in the same albedo-color region as the Centaurs/trans-Neptunian objects with dark-neutral surfaces (pale blue dots in Figure 13). This is also the characteristic region for cometary nuclei and Jovian Trojan asteroids (see, e.g., Lacerda et al. 2014). Only two Jovian irregular satellites show red surfaces, both extremely red and dark, already outside the bright-red group of outer solar systems objects (pale red dots in Figure 13). Saturnian irregulars (red symbols) are obviously in the dark-neutral group. Here we included Hyperion, too (highest albedo Saturnian point in Figure 13), though this is strictly speaking not an irregular satellite, but shows characteristics different from the typical regular Saturnian satellites (elongated shape, highly cratered surface, likely porous interior). The Neptunian irregular, Nereid is also a likely dark-neutral object. Triton, however, is clearly distinct from all other irregulars, and, as it is expected due to its large size, resembles more the group of large dwarf planets than any other irregular satellites—in that case internal processes (cryovolcanism) may have significantly altered the original surface. The surface of Triton, as well as those of the large regular satellites are more similar to the largest dwarf planets (green symbols in Figure 13) and the members of the Haumea collisional family (yellow symbols).
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Standard image High-resolution imageThe two irregular Uranian satellites, Sycorax and Caliban, for which albedo and color data are available both seem to fall into the bright-red group, along with some regular Uranian satellites (Puck, Miranda, Ariel, Umbriel, Titania, and Oberon). Currently, no other irregular satellites in other giant planet systems can be assigned to this albedo-color group.
Although our sample is limited, the location of the irregular satellites on the albedo-color diagram may indicate that the surfaces of satellites in the Uranian system may resemble those of the bright-red trans-Neptunian objects. Irregular satellites in the Jovian and Saturnian systems, and also Nereid are generally darker and more neutral in color. If the surfaces of the Uranian irregular satellites and those in other giant planet systems are intrinsically different, and not a consequence of a different evolution of surfaces, this may be a further indication of a compositional discontinuity in the young solar system. This discontinuity should have existed close to the heliocentric distance of Uranus, caused by the same processes that induced the bimodality among Centaurs and trans-Neptunian objects (Lacerda et al. 2014).
The research leading to these results has received funding from the European Unions Horizon 2020 Research and Innovation Programme, under Grant Agreement No. 687378; from the K-115709, PD-116175, and GINOP-2.3.2-15-2016-00003 grants of the National Research, Development and Innovation Office (NKFIH, Hungary); and from the LP2012-31 grant of the Hungarian Academy of Sciences. L.M. was supported by the János Bolyai Research Scholarship of the Hungarian Academy of Sciences. Funding for the Kepler and K2 missions are provided by the NASA Science Mission Directorate. The data presented in this paper were obtained from the Mikulski Archive for Space Telescopes (MAST). STScI is operated by the Association of Universities for Research in Astronomy, Inc., under NASA contract NAS5-26555. Support for MAST for non-HST data is provided by the NASA Office of Space Science via grant NNX09AF08G and by other grants and contracts. This work is based in part on archival data obtained with the Spitzer Space Telescope, which is operated by the Jet Propulsion Laboratory, California Institute of Technology under a contract with NASA. The authors thank the hospitality the Veszprém Regional Centre of the Hungarian Academy of Sciences (MTA VEAB), where part of this project was carried out. We also thank our referee for the helpful comments and suggestions.
Software: FITSH (Pál 2012), Period04 (Lenz & Breger 2005), gatspy (https://github.com/astroML/gatspy/).
Footnotes
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See http://herschel.esac.esa.int/hcss-doc-14.0/ for version 14 documentation.
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Interactive Data Language, Harris Geospatial Solutions.
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