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K2-287 b: An Eccentric Warm Saturn Transiting a G-dwarf

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Published 2019 February 6 © 2019. The American Astronomical Society. All rights reserved.
, , Citation Andrés Jordán et al 2019 AJ 157 100 DOI 10.3847/1538-3881/aafa79

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1538-3881/157/3/100

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 ${M}_{{\rm{P}}}=0.317\pm 0.026\,{M}_{{\rm{J}}}$, radius ${R}_{{\rm{P}}}=0.833\pm 0.013\,{R}_{{\rm{J}}}$, period $P=14.893291\pm 0.000025$ days, and eccentricity $e=0.476\pm 0.026$. The host star is a metal-rich V = 11.410 ± 0.129 mag G-dwarf for which we estimate a mass ${M}_{\star }={1.056}_{-0.021}^{+0.022}$ ${M}_{\odot }$, radius ${R}_{\star }=1.070\pm 0.010$ ${R}_{\odot }$, metallicity [Fe/H] = 0.20 ±0.05, and ${T}_{\mathrm{eff}}=5673\pm 75$ K. This warm eccentric planet with a time-averaged equilibrium temperature of ${T}_{\mathrm{eq}}\approx 800$ 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 (${T}_{\mathrm{eq}}$ < 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.

Figure 1.

Figure 1. Detrended K2 photometry of K2-287. Black points are individual 30 minute cadence K2 data The transits of K2-287b are clearly seen.

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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).

Figure 2.

Figure 2. Radial velocity (RV) curve for K2-287 obtained with FEROS (red) and HARPS (black). The black line corresponds to the Keplerian model with the posterior parameters found in Section 3.2.

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Figure 3.

Figure 3. Radial velocity (RV) vs. bisector span (BIS) scatter plot using data from our spectroscopic observations of K2-287. We find that the data is consistent with no correlation.

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Table 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

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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

Equation (1)

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 epsilon 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

Equation (2)

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.

Figure 4.

Figure 4. Ground-based light curves for the 2018 July 14 transit of K2-287b obtained with CHAT (left panel) and a LCOGT 1 m telescope at CTIO (right panel). The red lines represent the posterior Gaussian process models for remaining systematics after subtracting the transit and weighted comparison stars and obtained as described in Section 2.3.

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2.4. 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 ${T}_{\mathrm{eff}}=4994\pm 80$ K and a radius of ${R}_{\star }\,=1.18\pm 0.04\,{R}_{\odot }$. We used the observed parallax for K2-287 measured by GAIA for estimating a more precise value of ${R}_{\star }$ 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 ($\approx 12^{\prime\prime} $). 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 $v\sin i$, 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: ${T}_{\mathrm{eff}}$ = 5695 ± 58 K, $\mathrm{log}g$ = 4.4 ±0.15 dex, $[\mathrm{Fe}/{\rm{H}}]$ = 0.20 ± 0.04 dex, and $v\sin i$ = 3.2 ±0.2 km s−1. The ${T}_{\mathrm{eff}}$ 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 ${R}_{\star }$. 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 ${R}_{\star }$ 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 ${R}_{\star }=1.07\pm 0.01$ ${R}_{\odot }$ 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) 15h32m17fs84 EPIC
Decl. (J2000) −22d21m29fs74 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
${T}_{\mathrm{eff}}$ (K) 5695 ± 58 zaspe
$\mathrm{log}g$ (dex) 4.398 ± 0.015 zaspe
$[\mathrm{Fe}/{\rm{H}}]$ (dex) +0.20 ± 0.04 zaspe
$v\sin i$ (km s−1) 3.2 ± 0.2 zaspe
${M}_{\star }$ (${M}_{\odot }$) 1.056 ± 0.022 YY + GAIA
${R}_{\star }$ (${R}_{\odot }$) 1.07 ± 0.01 GAIA + this work
Age (Gyr) 4.5 ± 1 YY + GAIA
${\rho }_{\star }$ (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 ${R}_{\star }$ and the spectroscopic ${T}_{\mathrm{eff}}$ 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 ${M}_{\star }$, age, and $[\mathrm{Fe}/{\rm{H}}]$, where $[\mathrm{Fe}/{\rm{H}}]$ is fixed to the value found in the spectroscopic analysis. We explore the parameter space for ${M}_{\star }$ and stellar age using the emcee package, using uniform priors in both parameters. We find that the mass and age of K2-287 are ${M}_{\star }=1.036\pm 0.033$ ${M}_{\odot }$ 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.

Figure 5.

Figure 5. Yonsei-Yale isochrones for the metallicity of K2-287 in the ${T}_{\mathrm{eff}}$R plane. From left to right the isochrones correspond to 1, 3, 5, 7, and 9 Gyr. The position of K2-287 is at the center of the blue shaded region, which marks the 3σ confidence region for ${T}_{\mathrm{eff}}$ and ${R}_{\star }$.

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3.2. 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 ${\sigma }_{{\rho }_{* }}$ 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.

Figure 6.

Figure 6. Top panels show, from left to right, the phase folded Kepler K2 photometry (Kp band), the CHAT follow-up photometry (i band), and the LCO follow-up photometry (i band) for K2-287. For the three cases, the model generated with the derived parameters of EXONAILER is plotted with a blue line. The bottom panels show the corresponding residuals.

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Figure 7.

Figure 7. Top panel presents the radial velocities for K2-287 (filled circles) obtained with FEROS and HARPS as a function of the orbital phase. The RV model with the derived orbital parameters for K2-287b corresponds to the blue solid line. The bottom panel shows the residuals obtained for these radial velocity measurements.

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Table 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${}_{\star }$ U(1,300) ${23.87}_{-0.31}^{+0.30}$
${R}_{{\rm{P}}}$/${R}_{\star }$ U(0.001,0.5) ${0.08014}_{-0.00098}^{+0.00086}$
${\sigma }_{w}^{K2}$ (ppm) J(10, 50000) ${47.7}_{0.54}^{+0.54}$
${q}_{1}^{K2}$ U(0, 1) ${0.32}_{-0.05}^{+0.06}$
${q}_{2}^{K2}$ U(0, 1) ${0.57}_{-0.11}^{+0.13}$
${q}_{1}^{\mathrm{CHAT}}$ U(0, 1) ${0.83}_{-0.17}^{+0.12}$
${q}_{2}^{\mathrm{CHAT}}$ U(0, 1) ${0.15}_{-0.11}^{+0.16}$
${q}_{1}^{\mathrm{LCO}}$ U(0, 1) ${0.62}_{-0.19}^{+0.20}$
${q}_{2}^{\mathrm{LCO}}$ U(0, 1) ${0.08}_{-0.06}^{+0.11}$
K (m s−1) N(0, 100) ${28.8}_{-2.2}^{+2.3}$
e U(0, 1) ${0.478}_{-0.026}^{+0.025}$
i (deg) U(0, 90) ${88.13}_{-0.08}^{+0.1}$
ω(deg) U(0, 360) ${10.1}_{-4.2}^{+4.6}$
γFEROS (m s−1) N(32963.2, 0.1) ${32930.41}_{-0.10}^{+0.10}$
γHARPS (m s−1) N(32930.4, 0.1) ${32963.19}_{-0.10}^{+0.10}$
σFEROS (m s−1) J(0.1, 100) ${16.0}_{-1.8}^{+2.1}$
σHARPS (m s−1) J(0.1, 100) ${4.8}_{-1.6}^{+1.8}$
${M}_{{\rm{P}}}$ ( ${M}_{{\rm{J}}}$)   0.315 ± 0.027
${R}_{{\rm{P}}}$ (${R}_{{\rm{J}}}$)   0.847 ± 0.013
a (au)   ${0.1206}_{-0.0008}^{+0.0008}$
${T}_{\mathrm{eq}}$ a (K)   ${804}_{-7}^{+8}$

Note. For the priors, $N(\mu ,\sigma )$ 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).

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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 (${M}_{{\rm{P}}}$ = $0.317\pm 0.026$ ${M}_{{\rm{J}}}$, ${R}_{{\rm{P}}}$ = $0.833\pm 0.013$ ${R}_{{\rm{J}}}$) are consistent to those of Saturn. The noninflated structure of K2-287b is expected given its relatively low time-averaged equilibrium temperature of ${T}_{\mathrm{eq}}$ = 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 ${T}_{\mathrm{eq}}\approx 1000$ 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 ${M}_{c}=31\pm 4\,{M}_{\oplus }$. 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).

Figure 8.

Figure 8. Mass–radius diagram for the full population of transiting planets with both parameters measured to at least 20% precision. The points are color-coded by equilibrium temperature. K2-287b is the object in the plot that has error bars and is indicated by the arrow. The dashed gray lines correspond to isodensity curves of 0.3, 3, and 30 g cm−3, while the solid line represents the prediction of the Fortney et al. (2007) structural model with a central core mass of 10 M. Due to its relatively low equilibrium temperature, K2-287b lies in a sparsely populated region of the parameter space of moderately compact giant planets.

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The 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 ${R}_{{\rm{P}}}\gt 4\,{R}_{\oplus }$ and an incident flux $F\lt 150\,{F}_{\oplus }$, where ${F}_{\oplus }$ 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.

Figure 9.

Figure 9. Population of well characterized giant planets having ${R}_{{\rm{P}}}$ > 0.4 ${R}_{{\rm{J}}}$ in the orbital period—J magnitude plane. K2-287b is inside a black square. The size of the points represents the eccentricity of the orbit, while the color indicates the discovery method/mission (blue: ground-based photometry, yellow: RV planets, orange: CoRoT, red: Kepler, green: Kepler K2). The Kepler K2 mission has been the most effective source for discovering transiting bright (J < 11) warm (P > 10 days) giant planets.

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A.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).

Footnotes

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10.3847/1538-3881/aafa79