Abstract
We report the discovery of K2-287b, a Saturn mass planet orbiting a G-dwarf with a period of P ≈ 15 days. First uncovered as a candidate using K2 campaign 15 data, follow-up photometry and spectroscopy were used to determine a mass , radius , period days, and eccentricity . The host star is a metal-rich V = 11.410 ± 0.129 mag G-dwarf for which we estimate a mass , radius , metallicity [Fe/H] = 0.20 ±0.05, and K. This warm eccentric planet with a time-averaged equilibrium temperature of K adds to the small sample of giant planets orbiting nearby stars whose structure is not expected to be affected by stellar irradiation. Follow-up studies on the K2-287 system could help constrain theories of planet migration in close-in orbits.
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1. Introduction
Giant extrasolar planets that orbit their host stars at distances shorter than ≈1 au but farther away than the hot-Jupiter pile-up at ≈0.1 au, are termed "warm" giants. They have been efficiently discovered by radial velocity (RV) surveys (e.g., Hébrard et al. 2016; Jenkins et al. 2017), and have a wide distribution for their eccentricities, with a median of ≈0.25. The origin for these eccentricities is a topic of active research because the migration of planets through interactions with the protoplanetary disk predicts circular orbits (Dunhill et al. 2013), while planet–planet scattering after disk dispersal at typical warm giant orbital distances should usually generate planet collisions rather than high-eccentricity excitations (Petrovich et al. 2014).
Transiting giants are key for constraining theories of orbital evolution of exoplanets. Besides providing the true mass of the planet, follow-up observations can be carried out to constrain the sky-projected spin–orbit angle (obliquity) of the system, which is a tracer of the migration history of the planet (e.g., Zhou et al. 2015; Esposito et al. 2017; Mancini et al. 2018). While the obliquity for hot giant (P < 10 days) systems can be affected by strong tidal interactions (Triaud et al. 2013; Dawson 2014), the periastra of warm giants are large enough that significant changes in the spin of the outer layers of the star are avoided, and thus the primordial obliquity produced by the migration mechanism should be conserved.
Unfortunately, the number of known transiting warm giants around nearby stars is still very low. In addition to the scaling of the transit probability as a−1, the photometric detection of planets with P > 10 days requires a high duty cycle, which puts strong limitations on the ability of ground-based wide-angle photometric surveys (e.g., Bakos et al. 2004, 2013; Pollacco et al. 2006) to discover warm giants. From the total of ≈250 transiting giant planets detected from the ground, only 5 have orbital periods longer than 10 days (Kovács et al. 2010; Howard et al. 2012; Lendl et al. 2014; Brahm et al. 2016b; Hellier et al. 2017). On the other hand, the Kepler and CoRoT space missions found dozens of warm giants (e.g., Bonomo et al. 2010; Deeg et al. 2010; Dawson et al. 2012; Borsato et al. 2014), but orbiting mostly faint stars, for which detailed follow-up observations are very challenging.
Due to their relatively low equilibrium temperatures ( < 1000 K), transiting warm giants are important objects for characterizing the internal structure of extrasolar giant planets because their atmospheres are not subject to the yet unknown mechanisms that inflate the radii of typical hot Jupiters (for a review, see Fortney & Nettelmann 2010). For warm giants, standard models of planetary structure can be used to infer their internal composition from mass and radii measurements (e.g., Thorngren et al. 2016).
In this work we present the discovery of an eccentric warm giant planet orbiting a bright star, having physical parameters similar to those of Saturn. This discovery was made in the context of the K2CL collaboration, which has discovered a number of planetary systems using K2 data (Brahm et al. 2016a, 2018, 2019; Espinoza et al. 2017; Jones et al. 2018; Giles et al. 2018; Soto et al. 2018).
2. Observations
2.1. K2
Observations of campaign 15 (field centered at R.A. =15:34:28 and decl. = −20:04:44) of the K2 mission (Howell et al. 2014) took place between 2017 August 23 and November 20. The data of K2 campaign 15 was released on 2018 March. We followed the steps described in previous K2CL discoveries to process the light curves and identify transiting planet candidates. Briefly, the K2 light curves for Campaign 15 were detrended using our implementation of the EVEREST algorithm (Luger et al. 2016), and a Box-Least-Squares (Kovács et al. 2002) algorithm was used to find candidate box-shaped signals. The candidates that showed power above the noise level were then visually inspected to reject evident eclipsing binary systems and/or variable stars. We identified 23 candidates in this field. Among those candidates, K2-287 (EPIC 24945186) stood out as a high priority candidate for follow-up due to its relatively long period, deep flat-bottomed transits, and bright host star (V = 11.4 mag). The detrended light curves of the six transits observed for K2-287 by K2 are displayed in Figure 1.
2.2. Spectroscopy
We obtained 52 R = 48,000 spectra between March and July of 2018 using the FEROS spectrograph (Kaufer et al. 1999) mounted on the 2.2 MPG telescope in the La Silla observatory. Each spectrum achieved a signal-to-noise ratio of ≈90 per spectral resolution element. The instrumental drift was determined via comparison with a simultaneous fiber illuminated with a ThAr+Ne lamp. We additionally obtained 25 R = 115,000 spectra between March and August of 2018 using the HARPS spectrograph (Mayor et al. 2003). Typical signal-to-noise ratio for these spectra ranged between 30 and 50 per spectral resolution element. Both FEROS and HARPS data were processed with the CERES suite of echelle pipelines (Brahm et al. 2017a), which produce radial velocities and bisector spans in addition to reduced spectra.
Radial velocities and bisector spans are presented in Table 1 with their corresponding uncertainties, and the radial velocities are displayed as a function of time in Figure 2. No large amplitude variations were identified, which could be associated with eclipsing binary scenarios for the K2-287 system, and no additional stellar components were evident in the spectra. The radial velocities present a time correlated variation in phase with the photometric ephemeris, with an amplitude consistent with the one expected to be produced by a giant planet. We find no correlation between the radial velocities and the bisector spans (95% confidence intervals for the Pearson coefficient are [−0.19, 0.21], see Figure 3).
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Standard image High-resolution imageTable 1 . Relative Radial Velocities and Bisector Spans for K2-287
BJD | RV | σRV | BIS | σBIS | Instrument | |
---|---|---|---|---|---|---|
(2,400,000+) | (m s−1) | (m s−1) | (m s−1) | (m s−1) | ||
58168.8957118 | 32.9339 | 0.0076 | −0.033 | 0.012 | FEROS | |
58170.9025854 | 32.9108 | 0.0074 | −0.002 | 0.011 | FEROS | |
58177.8140231 | 32.9778 | 0.0058 | −0.014 | 0.008 | HARPS | |
58178.8260537 | 32.9917 | 0.0063 | −0.014 | 0.008 | HARPS | |
58178.8381972 | 33.0086 | 0.0058 | −0.009 | 0.008 | HARPS | |
58179.8509201 | 32.9812 | 0.0055 | −0.009 | 0.008 | HARPS | |
58179.8616916 | 32.9802 | 0.0055 | −0.026 | 0.007 | HARPS | |
58207.7691953 | 32.9344 | 0.0070 | −0.051 | 0.011 | FEROS | |
58210.8120326 | 32.9501 | 0.0070 | −0.038 | 0.010 | FEROS | |
58211.8033524 | 32.9607 | 0.0045 | −0.014 | 0.006 | HARPS | |
58211.8839384 | 32.8921 | 0.0070 | −0.055 | 0.011 | FEROS | |
58211.8969659 | 32.8463 | 0.0083 | −0.100 | 0.012 | FEROS | |
58212.8162559 | 32.9528 | 0.0035 | −0.014 | 0.004 | HARPS | |
58213.8155843 | 32.9494 | 0.0042 | −0.005 | 0.005 | HARPS | |
58214.8225570 | 32.9416 | 0.0051 | 0.001 | 0.007 | HARPS | |
58235.7054437 | 32.9695 | 0.0045 | −0.004 | 0.006 | HARPS | |
58236.8070269 | 32.9719 | 0.0040 | −0.012 | 0.005 | HARPS | |
58239.7443848 | 32.9381 | 0.0081 | −0.024 | 0.010 | FEROS | |
58241.8009423 | 32.9284 | 0.0070 | −0.020 | 0.010 | FEROS | |
58241.8119744 | 32.9144 | 0.0070 | −0.026 | 0.010 | FEROS | |
58242.8136144 | 32.9167 | 0.0070 | −0.017 | 0.010 | FEROS | |
58242.8246191 | 32.9256 | 0.0070 | −0.023 | 0.010 | FEROS | |
58243.6877674 | 32.9314 | 0.0070 | −0.005 | 0.010 | FEROS | |
58243.8443690 | 32.9224 | 0.0070 | −0.017 | 0.010 | FEROS | |
58244.7006355 | 32.9125 | 0.0070 | −0.021 | 0.010 | FEROS | |
58244.8366538 | 32.9122 | 0.0070 | 0.008 | 0.011 | FEROS | |
58245.8250104 | 32.9202 | 0.0095 | −0.014 | 0.014 | FEROS | |
58245.8380679 | 32.9165 | 0.0085 | −0.018 | 0.013 | FEROS | |
58247.7318034 | 32.9308 | 0.0090 | −0.037 | 0.013 | FEROS | |
58247.8756418 | 32.9519 | 0.0079 | −0.055 | 0.012 | FEROS | |
58249.7532000 | 32.9432 | 0.0070 | −0.001 | 0.011 | FEROS | |
58250.7827423 | 32.9318 | 0.0070 | −0.013 | 0.010 | FEROS | |
58250.6025575 | 32.9402 | 0.0070 | −0.005 | 0.011 | FEROS | |
58251.6502971 | 32.9379 | 0.0070 | −0.030 | 0.010 | FEROS | |
58251.7959960 | 32.9500 | 0.0080 | −0.044 | 0.012 | FEROS | |
58253.5376199 | 33.0158 | 0.0072 | −0.022 | 0.011 | FEROS | |
58261.6566471 | 32.9088 | 0.0070 | −0.025 | 0.009 | FEROS | |
58261.6676712 | 32.9182 | 0.0070 | −0.025 | 0.009 | FEROS | |
58261.6786827 | 32.9222 | 0.0070 | −0.004 | 0.009 | FEROS | |
58262.6356569 | 32.9146 | 0.0070 | −0.034 | 0.009 | FEROS | |
58262.6501525 | 32.9193 | 0.0070 | −0.025 | 0.009 | FEROS | |
58262.6526217 | 32.9496 | 0.0045 | −0.007 | 0.006 | HARPS | |
58262.6646765 | 32.9165 | 0.0070 | −0.011 | 0.009 | FEROS | |
58263.6490366 | 32.9372 | 0.0070 | −0.022 | 0.009 | FEROS | |
58263.6600382 | 32.9246 | 0.0070 | −0.014 | 0.009 | FEROS | |
58263.6710446 | 32.9198 | 0.0070 | −0.024 | 0.009 | FEROS | |
58263.7327984 | 32.9479 | 0.0040 | −0.007 | 0.005 | HARPS | |
58264.6559473 | 32.9164 | 0.0070 | −0.024 | 0.011 | FEROS | |
58264.6629948 | 32.9538 | 0.0085 | −0.006 | 0.011 | HARPS | |
58264.6669743 | 32.9180 | 0.0070 | −0.006 | 0.010 | FEROS | |
58264.6779962 | 32.9157 | 0.0070 | −0.019 | 0.009 | FEROS | |
58264.6890058 | 32.9034 | 0.0070 | −0.016 | 0.010 | FEROS | |
58264.7000122 | 32.9152 | 0.0070 | −0.017 | 0.010 | FEROS | |
58265.6537546 | 32.9415 | 0.0070 | −0.010 | 0.010 | FEROS | |
58265.6647735 | 32.9370 | 0.0070 | 0.000 | 0.010 | FEROS | |
58265.6757786 | 32.9348 | 0.0070 | −0.018 | 0.010 | FEROS | |
58265.6867851 | 32.9425 | 0.0070 | −0.026 | 0.009 | FEROS | |
58265.7022013 | 32.9415 | 0.0070 | −0.011 | 0.009 | FEROS | |
58266.6252665 | 32.9718 | 0.0062 | −0.009 | 0.008 | HARPS | |
58266.6331695 | 32.9814 | 0.0082 | −0.029 | 0.011 | FEROS | |
58266.6441948 | 32.9417 | 0.0077 | −0.025 | 0.011 | FEROS | |
58266.6552239 | 32.9633 | 0.0079 | −0.009 | 0.011 | FEROS | |
58266.6662336 | 32.9449 | 0.0078 | −0.026 | 0.011 | FEROS | |
58266.6772400 | 32.9545 | 0.0079 | −0.010 | 0.011 | FEROS | |
58312.6234698 | 32.9979 | 0.0070 | −0.018 | 0.010 | FEROS | |
58313.6965328 | 32.9663 | 0.0070 | −0.022 | 0.010 | FEROS | |
58314.5467674 | 32.9861 | 0.0029 | −0.009 | 0.004 | HARPS | |
58314.5754726 | 32.9420 | 0.0070 | −0.033 | 0.010 | FEROS | |
58316.5526131 | 32.9562 | 0.0058 | −0.009 | 0.008 | HARPS | |
58320.5251962 | 32.9501 | 0.0051 | 0.025 | 0.015 | HARPS | |
58321.5156072 | 32.9413 | 0.0051 | −0.024 | 0.007 | HARPS | |
58322.6976017 | 32.9433 | 0.0073 | −0.021 | 0.007 | HARPS | |
58323.6016488 | 32.9468 | 0.0040 | −0.021 | 0.007 | HARPS | |
58332.5127365 | 32.9503 | 0.0040 | −0.020 | 0.009 | HARPS | |
58333.5353776 | 32.9433 | 0.0033 | −0.021 | 0.005 | HARPS | |
58332.5127365 | 32.9503 | 0.0040 | −0.007 | 0.005 | HARPS | |
58333.5353776 | 32.9433 | 0.0033 | −0.024 | 0.004 | HARPS |
2.3. Ground-based Photometry
On July 14 of 2018 we observed the primary transit of K2-287 with the Chilean-Hungarian Automated Telescope (CHAT), installed at Las Campanas Observatory, Chile. CHAT is a newly commissioned 0.7 m telescope, built by members of the HATSouth (Bakos et al. 2013) team, and dedicated to the follow-up of transiting exoplanets. A more detailed account of the CHAT facility will be published at a future date (A. Jordán et al. 2018, in preparation17 ). Observations were obtained in the Sloan i band and the adopted exposure time was of 53 s per image, resulting in a peak pixel flux for K2-287 of ≈45,000 ADU during the whole sequence. The observations covered a fraction of the bottom part of the transit and the egress (see Figure 6). The same event was also monitored by one telescope of the Las Cumbres Observatory 1 m network (Brown et al. 2013) at Cerro Tololo Inter-American Observatory, Chile. Observations were obtained with the Sinistro camera with 2 mm of defocus in the Sloan i band. The adopted exposure time for the 88 observations taken was 60 s, and reduced images were obtained with the standard Las Cumbres Observatory pipeline (BANZAI pipeline). The light curves for CHAT and the Las Cumbres 1 m telescope were produced from the reduced images using a dedicated pipeline (N. Espinoza et al. 2018, in preparation).
The light curves were detrended by describing the systematic trends as a Gaussian Process with an exponential squared kernel depending on time, airmass, and centroid position and whose parameters are estimated simultaneously with those of the transit. A photometric jitter term is also included; this parameter is passed on as a fixed parameter in the final global analysis that determines the planetary parameters (Section 3.2). In more detail, the magnitude time series is modeled as
where Z is a zero-point, c1 and c2 are comparison light curves, x1 and x2 are parameters weighting the light curves, δ is the transit model, and is a Gaussian Process to model the noise. The subscript i denotes evaluation at the time t = ti of the time series. For the Gaussian process, we assume a kernel given by
The variables xm are normalized time (m = 0), flux centroid in x (m = 1), and flux centroid in y (m = 2); δij is the Kronecker delta. The normalization is carried out by setting the mean to 0 and the variance to 1. The priors on the kernel hyper parameters were taken to be the same as the ones defined in Gibson (2014), the priors for the photometric jitter term σ and A were taken to be uniform in the logarithm between 0.01 and 100, with σ and A expressed in mmag. In Figure 4 we show the CHAT and LCOGT light curves with the weighted comparison stars subtracted along with the Gaussian process posterior model for the systematics.
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Standard image High-resolution image2.4. GAIA DR2
Observations of K2-287 by GAIA were reported in DR2 (Gaia Collaboration et al. 2016, 2018). From GAIA DR2, K2-287 has a parallax of 6.29 ± 0.05 mas, an effective temperature of K and a radius of . We used the observed parallax for K2-287 measured by GAIA for estimating a more precise value of by combining it with the atmospheric parameters obtained from the spectra as described in Section 3. We corrected the GAIA DR2 parallax for the systematic offset of −82 μas reported in Stassun & Torres (2018).
Two additional sources to K2-287 are identified by GAIA inside the adopted K2 aperture (). However, both stars are too faint (ΔG > 7.8 mag) to produce any significant effect on the planetary and stellar parameters found in Section 3. The RV variations in-phase with the transit signal, which are caused by K2-287, confirm that the transit is not caused by a blended stellar eclipsing binary on one of the companions.
3. Analysis
3.1. Stellar Parameters
As in previous K2CL discoveries we estimated the atmospheric parameters of the host star by comparing the coadded high resolution spectrum to a grid of synthetic models through the ZASPE code (Brahm et al. 2017b). In particular, for K2-287 we used the coadded FEROS spectra, because they provide the higher signal-to-noise ratio spectra, and because the synthetic grid of models used by ZASPE was empirically calibrated using FEROS spectra of standard stars. Briefly, ZASPE performs an iterative search of the optimal model through χ2 minimization on the spectral zones that are most sensitive to changes in the atmospheric parameters. The models with specific values of atmospheric parameters are generated via trilinear interpolation of a precomputed grid generated using the ATLAS9 models (Castelli & Kurucz 2004). The interpolated model is then degraded to match the spectrograph resolution by convolving it with a Gaussian kernel that includes the instrumental resolution of the observed spectrum and an assumed macroturbulence value given by the relation presented in Valenti & Fischer (2005). The spectrum is also convolved with a rotational kernel that depends on , which is considered as a free parameter. The uncertainties in the estimated parameters are obtained from Monte Carlo simulations that consider that the principal source of error comes from the systematic mismatch between the optimal model and the data, which in turn arises from poorly constrained parameters of the atomic transitions and possible deviations from solar abundances. We obtained the following stellar atmospheric parameters for K2-287: = 5695 ± 58 K, = 4.4 ±0.15 dex, = 0.20 ± 0.04 dex, and = 3.2 ±0.2 km s−1. The value obtained with ZASPE is significantly different to that reported by GAIA DR2, but is consistent that of the K2 input catalog (Huber et al. 2016).
The stellar radius is computed from the GAIA parallax measurement, the available photometry, and the atmospheric parameters. As in Brahm et al. (2019), we used a BT-Settl-CIFIST spectral energy distribution model (Baraffe et al. 2015) with the atmospheric parameters derived with ZASPE to generate a set of synthetic magnitudes at the distance computed from the GAIA parallax. These magnitudes are compared to those presented in Table 2 for a given value of . We also consider an extinction coefficient AV in our modeling that affects the synthetic magnitudes by using the prescription of Cardelli et al. (1989). We explore the parameter space for and AV using the emcee package Foreman-Mackey et al. (2013), using uniform priors in both parameters. We found that K2-287 has a radius of and has a reddening of AV = 0.56 ± 0.03 mag, which is consistent with what is reported by GAIA DR2.
Table 2 . Stellar Properties of K2-287
Parameter | Value | References |
---|---|---|
Names | EPIC 249451861 | EPIC |
2MASS J15321784-2221297 | 2MASS | |
TYC 6196-185-1 | TYCHO | |
WISE J153217.84-222129.9 | WISE | |
R.A. (J2000) | 15h32m1784 | EPIC |
Decl. (J2000) | −22d21m2974 | EPIC |
pmR.A. (mas yr−1) | −4.59 ± 0.11 | GAIA |
pmdecl. (mas yr−1) | −17.899 ± 0.074 | GAIA |
π (mas) | 6.288 ± 0.051 | GAIA |
Kp (mag) | 11.058 | EPIC |
B (mag) | 12.009 ± 0.169 | APASS |
g' (mag) | 11.727 ± 0.010 | APASS |
V (mag) | 11.410 ± 0.129 | APASS |
r' (mag) | 11.029 ± 0.010 | APASS |
i' (mag) | 10.772 ± 0.020 | APASS |
J (mag) | 9.677 ± 0.023 | 2MASS |
H (mag) | 9.283 ± 0.025 | 2MASS |
Ks (mag) | 9.188 ± 0.021 | 2MASS |
WISE1 (mag) | 9.114 ± 0.022 | WISE |
WISE2 (mag) | 9.148 ± 0.019 | WISE |
WISE3 (mag) | 9.089 ± 0.034 | WISE |
(K) | 5695 ± 58 | zaspe |
(dex) | 4.398 ± 0.015 | zaspe |
(dex) | +0.20 ± 0.04 | zaspe |
(km s−1) | 3.2 ± 0.2 | zaspe |
() | 1.056 ± 0.022 | YY + GAIA |
() | 1.07 ± 0.01 | GAIA + this work |
Age (Gyr) | 4.5 ± 1 | YY + GAIA |
(g cm−3) | 1.217 ± 0.045 | YY + GAIA |
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Finally, the stellar mass and evolutionary stage for K2-287 are obtained by comparing the estimation of and the spectroscopic with the predictions of the Yonsei-Yale evolutionary models (Yi et al. 2001). We use the interpolator provided with the isochrones to generate a model with specific values of , age, and , where is fixed to the value found in the spectroscopic analysis. We explore the parameter space for and stellar age using the emcee package, using uniform priors in both parameters. We find that the mass and age of K2-287 are and 5.6 ± 1.6 Gyr (see Figure 5), similar to those of the Sun. The stellar parameters we adopted for K2-287 are summarized in Table 2.
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Standard image High-resolution image3.2. Global Modeling
In order to determine the orbital and transit parameters of the K2-287b system we performed a joint analysis of the detrended K2 photometry, the follow-up photometry, and the radial velocities. As in previous planet discoveries of the K2CL collaboration, we used the exonailer code, which is described in detail in Espinoza et al. (2016). Briefly, we model the transit light curves using the batman package (Kreidberg 2015) by taking into account the effect on the transit shape produced by the long integration time of the long-cadence K2 data (Kipping 2010). To avoid systematic biases in the determination of the transit parameters we considered the limb-darkening coefficients as additional free parameters in the transit modeling (Espinoza & Jordán 2015), with the complexity of limb-darkening law chosen following the criteria presented in Espinoza & Jordán (2016). In our case, we select the quadratic limb-darkening law, whose coefficients were fit using the uninformative sampling technique of Kipping (2013). We also include a photometric jitter parameter for the K2 data, which allows us to have an estimation of the level of stellar noise in the light curve. The radial velocities are modeled with the radvel package (Fulton et al. 2018), where we considered systemic velocity and jitter factors for the data of each spectrograph. We use the stellar density estimated in our stellar modeling as an extra "data point" in our global fit as described in Brahm et al. (2018). Briefly, there is a term in the likelihood of the form
where
by Newton's version of Kepler's law, and ρ* and are the mean stellar density and its standard deviation, respectively, derived from our stellar analysis. In essence, because the period P is tightly constrained by the observed periodic transits, this extra term puts a strong constraint on a/R*, which in turn helps to extract information about the eccentricity e and argument of periastron ω from the duration of the transit. Resulting planet parameters are set out in Table 3, the best-fit light curves in Figure 6, and the best-fit orbit solutions in Figures 2 and 7.
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Standard image High-resolution imageTable 3 . Planetary Properties of the K2-287 System
Parameter | Prior | Value |
---|---|---|
P (days) | N(14.893, 0.01) | 14.893291 ± 0.000025 |
T0 (BJD) | N(2458001.722, 0.01) | 2458001.72138 ± 0.00016 |
a/R | U(1,300) | |
/ | U(0.001,0.5) | |
(ppm) | J(10, 50000) | |
U(0, 1) | ||
U(0, 1) | ||
U(0, 1) | ||
U(0, 1) | ||
U(0, 1) | ||
U(0, 1) | ||
K (m s−1) | N(0, 100) | |
e | U(0, 1) | |
i (deg) | U(0, 90) | |
ω(deg) | U(0, 360) | |
γFEROS (m s−1) | N(32963.2, 0.1) | |
γHARPS (m s−1) | N(32930.4, 0.1) | |
σFEROS (m s−1) | J(0.1, 100) | |
σHARPS (m s−1) | J(0.1, 100) | |
( ) | 0.315 ± 0.027 | |
() | 0.847 ± 0.013 | |
a (au) | ||
a (K) |
Note. For the priors, stands for a normal distribution with mean μ and standard deviation σ, U(a, b) stands for a uniform distribution between a and b, and J(a, b) stands for a Jeffrey's prior defined between a and b.
aTime-averaged equilibrium temperature computed according to Equation (16) of Méndez & Rivera-Valentín (2017).Download table as: ASCIITypeset image
4. Discussion
By combining data from the Kepler K2 mission and ground-based photometry and spectroscopy, we have confirmed the planetary nature of a P = 14.9 day candidate around the V = 11.4 mag G-type star K2-287. We found that the physical parameters of K2-287b ( = , = ) are consistent to those of Saturn. The noninflated structure of K2-287b is expected given its relatively low time-averaged equilibrium temperature of = 808 ±8 K. In Figure 8 the mass and radius of K2-287b are compared to those for the full population of transiting planets with parameters measured to a precision of 20% or better. Two other transiting planets, orbiting fainter stars, that share similar structural properties to K2-287b are HAT-P-38b (Sato et al. 2012) and HATS-20b (Bhatti et al. 2016), which have equilibrium temperatures that are higher but relatively close to the K limit below which the inflation mechanism of hot Jupiters does not play a significant role (Kovács et al. 2010; Demory & Seager 2011). By using the simple planet structural models of Fortney et al. (2007) we find that the observed properties of K2-287b are consistent with having a solid core of . However, models that consider the presence of solid material in the envelope of the planet are required to obtain a more reliable estimate for the heavy element content of K2-287b (e.g., Thorngren et al. 2016).
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Standard image High-resolution imageThe numerous RV measurements obtained for the K2-287 system allow us to constrain the eccentricity of the planet to be e = 0.478 ± 0.025. Even though K2-287b is among the most eccentric extrasolar planets to have a period shorter than 50 days, its periastron distance is not small enough to cause a significant migration by tidal interactions throughout the main-sequence lifetime of the host star. Specifically, by using the equations of Jackson et al. (2009), we find that in the absence of external sources of gravitational interaction, K2-287b should have possessed an eccentricity of e ≈ 0.65 and a semimajor axis of a ≈ 0.15 au when the system was 0.1 Gyr old. Under the same assumptions, we expect that K2-287b would be engulfed by its host star at an age of ≈12 Gyr before being able to reach full circularization at a distance of a ≈ 0.1 au. These orbital properties for K2-287b and those of the majority of eccentric warm giants are not easy to explain. If K2-287b was formed in situ (Huang et al. 2016) at 0.15 au or migrated to this position via interactions with the protoplanetary disk (Lin & Ida 1997), its eccentricity could have been excited by the influence of another massive object in the system after disk dispersal. However, planet–planet scattering (Ford & Rasio 2008) at these close-in orbits generally produces planet collisions rather than eccentricity excitation (Petrovich et al. 2014). An alternative proposition for the existence of these eccentric systems is that they are being subject to secular gravitational interactions produced by another distant planet or star in the system (Rasio & Ford 1996), with the planet experiencing long-term cyclic variations in its eccentricity and spin–orbit angle. In this scenario, the planet migrates by tidal interactions only during the high-eccentricity stages, but it is usually found with moderate eccentricities. Further observations on the K2-287 system could help support this mechanism as being responsible for its relatively high eccentricity, particularly given that Petrovich & Tremaine (2016) concludes that high-eccentricity migration excited by an outer planetary companion can account for most of the warm giants with e > 0.4. Specifically, long-term RV monitoring and the search for transit timing variations could be used to detect the relatively close companions to migrating warm Jupiters proposed by Dong et al. (2014). Future astrometric searches of companions with GAIA could also be used to find companions and infer the predicted mutual inclination between both orbits, which are predicted to be high (Anderson & Lai 2017).
Finally, it is worth noting that an important fraction of the transiting warm giants amenable for detailed characterization (J < 11 mag) have been discovered in the last couple of years thanks to the K2 mission (see Figure 9). The combination of relatively long observing campaigns per field, and the increased number of fields monitored, have allowed the discovery and dynamical characterization of several warm giant planets with data from the K2 mission (see Figure 9, Sinukoff et al. 2016; Barragán et al. 2018; Shporer et al. 2017; Smith et al. 2017; Brahm et al. 2018, 2019; Johnson et al. 2018; Yu et al. 2018). While not particularly designed to discover warm giants, the TESS mission (Ricker et al. 2015) is expected to discover ≈120 additional warm giants with and an incident flux , where is the incident flux at Earth, around J ≲ 11 mag stars (Barclay et al. 2018). With such a population at hand, it will be possible to compare the distributions of eccentricities and obliquities to predictions from different migration mechanisms (e.g., Petrovich & Tremaine 2016) in order to establish a clearer picture about how eccentric warm giant planets originate.
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Standard image High-resolution imageA.J. acknowledges support from FONDECYT project 1171208, CONICYT project BASAL AFB-170002, and by the Ministry for the Economy, Development, and Tourism's Programa Iniciativa Científica Milenio through grant IC 120009, awarded to the Millennium Institute of Astrophysics (MAS). R.B. acknowledges support from FONDECYT Post-doctoral Fellowship Project 3180246, and from the Millennium Institute of Astrophysics (MAS). M.R.D. acknowledges support by CONICYT-PFCHA/Doctorado Nacional 21140646, Chile. A.Z. acknowledges support by CONICYT-PFCHA/Doctorado Nacional 21170536, Chile. J.S.J. acknowledges support by FONDECYT project 1161218 and partial support by CONICYT project BASAL AFB-170002. This paper includes data collected by the K2 mission. Funding for the K2 mission is provided by the NASA Science Mission directorate. This work has made use of data from the European Space Agency (ESA) mission Gaia (https://www.cosmos.esa.int/gaia), processed by the Gaia Data Processing and Analysis Consortium (DPAC, https://www.cosmos.esa.int/web/gaia/dpac/consortium). Funding for the DPAC has been provided by national institutions, in particular, the institutions participating in the Gaia Multilateral Agreement. Based on observations collected at the European Organisation for Astronomical Research in the Southern Hemisphere under ESO programmes 0101.C-0497, 0101.C-0407, and 0101.C-0510.
Facilities: CHAT 0.7 m - , LCOGT 1 m - , MPG 2.2 m - , ESO 3.6 m - , Kepler - The Kepler Mission, GAIA - , APASS - , 2MASS - , WISE - Wide-field Infrared Survey Explorer.
Software: EXO-NAILER (Espinoza et al. 2016), CERES (Jordán et al. 2014; Brahm et al. 2017a), ZASPE (Brahm et al. 2015, 2017b), radvel (Fulton et al. 2018).