A&A 469, L43-L47 (2007)
DOI: 10.1051/0004-6361:20077612
LETTER TO THE EDITOR
S. Udry1 - X. Bonfils2 - X. Delfosse3 - T. Forveille3 - M. Mayor1 - C. Perrier3 - F. Bouchy4 - C. Lovis1 - F. Pepe1 - D. Queloz1 - J.-L. Bertaux5
1 - Observatoire de Genève, Université de Genève, 51 Ch.
des Maillettes, 1290 Sauverny, Switzerland
2 - Centro de Astronomia e Astrofísica da Universidade de
Lisboa, Tapada da Ajuda, 1349-018 Lisboa, Portugal
3 - Laboratoire d'Astrophysique, Observatoire de Grenoble,
Université J. Fourier, BP 53,
38041 Grenoble, Cedex 9, France
4 - Institut d'Astrophysique de Paris, CNRS, Université Pierre et
Marie Curie, 98bis Bd Arago, 75014 Paris, France
5 - Service d'Aéronomie du CNRS/IPSL, Université de Versailles
Saint-Quentin, BP 3, 91371 Verrières-le-Buisson, France
Received 4 April 2007 / Accepted 9 May 2007
Abstract
This Letter reports on the detection of two super-Earth
planets in the Gl 581 system, which is already known to
harbour a hot Neptune. One of the planets has a mass of
5
and resides at the "warm'' edge of the habitable
zone of the star. It is thus the known exoplanet that most resembles
our own Earth. The other planet has a 7.7
mass and
orbits at 0.25 AU from the star, close to the "cold'' edge of the
habitable zone. These two new light planets around an M3 dwarf
further confirm the formerly tentative statistical trend toward (i)
many more very low-mass planets being found around M dwarfs than
around solar-type stars and (ii) low-mass planets outnumbering
Jovian planets around M dwarfs.
Key words: stars: individual: Gl 581 - stars: planetary systems - techniques: radial velocities - methods: observational
M dwarfs are of prime interest in planet-search programmes. First of
all, they extend the domain of stellar parameters that are probed for
planets. For high-precision radial-velocity planet searches, M dwarfs
are excellent targets as well, because the lower primary mass makes
the detection of very light planets easier than it would be around
solar-type stars. In particular, Earth-mass planets around M dwarfs
are within reach of current high-precision planet-search programmes.
Furthermore, the habitable zones of M dwarfs reside much closer to
these stars (around 0.1 AU, Scalo et al. 2007) than for Sun-like
stars (Kasting et al. 1993). Habitable terrestrial planets are thus
detectable today. Such detections will provide targets for future
space missions looking for life tracers on other planets, like the ESA
Darwin and NASA TPF-C/I projects. To find these very light planets in
the habitable zone of M dwarfs, our consortium (Mayor et al. 2003)
dedicates
10% of the Guaranteed Time Observations on HARPS to
the precise radial-velocity monitoring of some 100 nearby M dwarfs.
In this Letter we present the detection of two additional planets
orbiting Gl 581, where we previously found a 1st
close-in Neptune-mass planet. The minimum mass of the 2nd new
planet is 5.03 terrestrial mass, the lowest for any exoplanet to date,
close to the 5.5
of the microlensing candidate
OGLE-2005-BLG-390Lb (Beaulieu et al. 2006) found at a large
separation from another M dwarf. It resides on the inner edge of the
habitable zone of Gl 581. The 3
planet, at 0.25 AU
from the star, is also in the super-Earth category (7.7
)
and is situated close to the outer edge of the habitable zone of the
system. Section 2 briefly recalls some relevant properties of the
parent star. Section 3 describes the precise HARPS velocities and
characterises the new planets. We also examine the possibility that
the long-period low-mass planet is actually an artefact of dark spots
modulated by rotation of the star and conclude that this is unlikely.
The Letter ends with our conclusions.
The paper reporting the first Neptune-mass planet on a 5.36-d orbit around Gl 581 (Bonfils et al. 2005) describes the properties of the star. We highlight here just those characteristics that are most relevant for this paper:
The 20 high-resolution HARPS spectra available when we detected
Gl 581 b (Bonfils et al. 2005) have typical S/N per pixel of
40, and at that time the typical radial-velocity uncertainty was
1.3 m s-1 per measurement, when taking calibration uncertainties
into account.
The periodogram of their residuals from the 1-planet Keplerian
solution showed a tentative 2
signal at a frequency of
1/13 d-1. With this limited number of observations, the low
amplitude of the 13-day velocity variation only had modest
significance, but it prompted us to gather 30 additional
high-precision observations with HARPS (uncertainty
<1.5 m s-1). We also took advantage of a concerted effort to
improve the reduction pipeline with a special emphasis on wavelength
calibration (Lovis & Pepe 2007). These improvements are directly
visible on the new set of barycentric radial velocities (available in
electronic form at the CDS): their average uncertainty is
0.9 m s-1 (including photon noise, calibration uncertainty, and
spectrograph-drift uncertainty). The 50 high-precision HARPS radial
velocities confirm the 5.36-d period planet, and we now clearly see
the 13-day signal in the periodogram of the residuals around the
1-planet solution (Fig. 1). Some power is also visible
around 80 days. The false-alarm probability of the 13-day peak is
only 0.0025.
| |
Figure 1: Lomb-Scargle periodogram of the radial-velocity residuals around the 1-planet solution, clearly showing a peak close to 13 days and some extra-power between 70 and 90 days. |
| Open with DEXTER | |
| |
Figure 2: Periodogram of the radial-velocity residuals around the 2-planet Keplerian model for Gl 581 showing power at P = 84 d. |
| Open with DEXTER | |
Table 1: Orbital and physical parameters derived from 3-planet Keplerian models of Gl 581 for the free-eccentricity and circular cases, with uncertainties directly derived from the covariance matrix.
Although the new radial-velocity measurements strongly confirm the
5.36-day planet, their modeling by a single Keplerian orbit is poor:
the residuals around the 1-planet solution are very high
(3.2 m s-1 standard deviation) compared with the typical
measurement errors (0.9 m s-1), and the reduced
per
degree of freedom is
= 17.3. This, and the 13-day
peak in the periodogram, motivates investigating a 2-planet model. For
the first planet, that solution gives orbital parameters consistent
with the Bonfils et al. (2005) orbit. The 2nd planet moves on a
slightly eccentric orbit (e
0.28
0.06), with a
period of 12.895 days.
The measured radial-velocity semi-amplitude is only 3.5 m s-1, or 4 times our typical noise on individual measurements. At this
small-amplitude radial-velocity variation, this solution represents a
highly significant improvement in the system modeling:
decreases from 17.3 to 9.2, and the weighted rms of the residuals
around the solution is now 2.2 m s-1. We can note here that a
circular orbit for the 2nd planet provides a solution of equal
quality with a
= 9.0. The observed dispersion of the
residuals is, however, still larger than the internal errors, and the
periodogram of the residuals from this 2-planet fit
(Fig. 2) shows clear power at 84 days (the false-alarm
probability of this signal is only 0.0028). In the next section we
examine this 3rd signal in terms of an additional planet, and
discuss whether it could instead be caused by magnetic activity.
![]() |
Figure 3: 3-planet Keplerian model of the Gl 581 radial-velocity variations. The upper panels display the phase-folded curve of each of the planets, with points representing the observed radial velocities, after removing the effect of the other planets. The bottom panel presents the periodogram of the residuals. |
| Open with DEXTER | |
![]() |
Figure 4: Temporal display of the 3-planet Keplerian model of Gl 581, on time intervals with dense observational sampling. |
| Open with DEXTER | |
For the 0.31
mass of Gl 581
(Bonfils et al. 2005), the derived orbital parameters for the 2nd
planet lead to an
5.6
minimum
mass and a separation a = 0.073 AU. From the 0.013
stellar luminosity (Bonfils et al. 2005), we compute an equilibrium
temperature for the planet of
C (for a Venus-like albedo
of 0.64) to
C (for an Earth-like albedo of 0.35). With
a planetary radius of
1.5
(in the case of
Earth-type composition, Valencia et al. 2006) and a temperature that would
be
C for a 0.5 albedo, Gl 581 c is probably
the most Earth-like of all known exoplanets. It is obvious, however,
that the actual surface temperature of the planet strongly depends on
the highly uncertain composition and thickness of its atmosphere,
which govern both the planetary albedo and the strength of the
greenhouse effect. It is probable that the planet is located towards
the "warm'' edge of the habitable zone around the star
(Kasting et al. 1993). A detailed study will also need to consider the
possible tidal locking of the planetary rotation to the orbital
period.
Since the periodogram has significant power around 84 days, we
examined a 3-planet model. That solution only slightly changes the orbital
parameters of the inner two planets from the 2-planet
solution (lower eccentricities). The mass of the 2nd planet is
now 5.03
.
Adjusting their eccentricities finds that they
are not constrained according to a Lucy & Sweeney (1971) test. We thus
provide the orbital parameters in Table 1 for both cases
(free and fixed-to-zero eccentricities). The 3rd planet has an
83.6-day period and a slightly eccentric orbit (e = 0.2). The
inferred planet mass is 7.7
(8.3
in the
circular case) and the mean star-planet separation is 0.25 AU,
putting the planet close to the outer edge of the habitable zone
(Kasting et al. 1993). Aside from being most prominent in the
frequency analysis, the 84-day period naturally comes out in global
solution searches based on the genetic-algorithm approach. This makes
a misidentified alias unlikely. An ongoing stability study of the
system (Beust et al. in prep.) shows that the system is stable over
millions of years, even in the more eccentric case (
).
Figure 3 displays the 3-planet Keplerian solution, together
with the phase-folded radial velocities, and Fig. 4 plots
time sequences for densely sampled measurement intervals.
Introducing a 3rd planet adds 5 free parameters and will thus
always lower residuals, but here the quality of the solution improves
impressively and, statistically, very significantly: its
drops from 9.2 to 3.45, and the 1.2 m s-1 rms residual is now
closer to the typical internal error of 0.9 m s-1. A modeling of the
system including planet-planet gravitational interactions gives the
same results and shows that for those low masses the mentioned
interactions are negligible.
Can the 84-day radial-velocity variation have another source? Among
the very low-mass planets around M dwarfs, the recent
Gl 674 b detection provides a particularly illustrative
comparison: the radial-velocity measurements of Gl 674 show
two superimposed small-amplitude variations with 4.7 and 35 days, but
monitoring of chromospheric indices and photometric observations
demonstrate that the 35-day variation reflects rotational modulation
of stellar activity, leaving only one 11
planet with a
4.7-d period (Bonfils et al. 2007). This recent example emphasises that
the interpretation of small-amplitude radial-velocity variations of M dwarfs needs care, since most of them are expected to be at least
moderately active. It also illustrates the value of chromospheric
diagnostics and photometric followups for these stars.
Since a comparison with Gl 674 (Fig. 1
of Bonfils et al. 2007) shows that Gl 581 is significantly less
active, its rotational period is most likely longer than
40 days, and it could potentially coincide with the 84-day
signal. One therefore needs a serious look at the possibility that the
84-day signal reflects a spot on the stellar surface. At such a low
rotation rate, one would need a huge spot, however, to affect the
radial velocities at the several m s-1 level. Scaling from
Saar & Donahue (1997), a spot responsible for the observed variation needs
to cover 2.6% of the stellar surface
. Such a large spot
would only be expected in a fairly active star, which Gl 581
is not. Planned spectroscopic (radial velocities and activity index)
and photometric monitoring of the star will settle that issue, but we
are already confident that the 3rd planet is real.
We report the detection of two new, very light planets orbiting the
low-metallicity M dwarf Gl 581, already known to harbour a
15.7
closer-in planet (Bonfils et al. 2005). The high
radial-velocity precision reached with the HARPS spectrograph on the
ESO 3.6-m telescope enabled these discoveries.
The first planet, Gl 581 c, is a 5.03
super-Earth at a distance of 0.073 AU from the star. Its mass is the
lowest found so far for an exoplanet. After its separation from an M3 dwarf, the planet resides at the inner edge of the habitable zone of
this low-luminosity star. With a radius close to 1.5
(for an Earth-type composition), the planet is the closest Earth twin
to date. The HARPS radial velocities also reveal a longer-period
planetary companion of mass 7.7
on a 83.6-day period
orbit, close to the outer edge of the star's habitable zone.
Considering uncertainties on the determination of the edges of the
habitable zone, mainly due to the lack of realistic cloud models,
these two planets are promising targets for future observatories. The
spectral characterisation of their atmosphere would provide a crucial
constraint on the actual limits of the habitable zone.
The two new, very low-mass planets further support statistical trends already outlined in the literature:
From both our observational programmes and planet formation simulations, very low-mass planets seem more frequent than the previously found giant worlds. They will thus provide preferential targets for photometric transit-search missions in space like COROT and Kepler and for projects like Darwin or TPF-I/C looking for biotracers in the atmospheres of habitable planets.
Acknowledgements
The authors thank the different observers from the other HARPS GTO sub-programmes who have also measured Gl 581. We especially thank Franck Selsis and Lisa Kaltenegger for thoughtful discussions during the reviewing process, on the location of the habitable zone around Gl581. We would like to thank the Swiss National Science Foundation (FNRS) for its continuing support of this project. X.B. acknowledges support from the Fundação para a Ciência e a Tecnologia (Portugal) in the form of a fellowship (references SFRH/BPD/21710/2005).