A&A 459, 955-963 (2006)
DOI: 10.1051/0004-6361:20054710
A.-M. Lagrange1 - H. Beust1 - S. Udry2 - G. Chauvin3 - M. Mayor2
1 - Laboratoire d'Astrophysique de Grenoble, Université
J. Fourier, BP 53, 38041 Grenoble Cedex 9, France
2 -
Observatoire de Genève, 51 Ch. des Maillettes, 1290 Sauverny, Switzerland
3 - ESO Casilla 19001, Santiago 19, Chile
Received 16 December 2005 / Accepted 1 March 2006
Abstract
Aims. We present the results of multi epoch imaging observations of the companion to the planetary host Gliese 86. Associated with radial velocity measurements, this study aimed at dynamically characterizing with the orbital properties and the mass of this companion (hereafter Gliese 86 B), but also at investigating the possible history of this particular system.
Methods. We used the adaptive optics instrument NACO at the ESO Very Large Telescope to obtain deep coronographic imaging to obtain new photometric and astrometric measurements of Gliese 86 B.
Results. Part of the orbit is resolved. The photometry of Gl 86 B indicates colors compatible with a 70 Jupiter mass brown dwarf or a white dwarf. Both types of objects fit the available, still limited astrometric data. If we attribute the long term radial velocity residual drift observed for Gl 86 A to B, then the mass of the latter object is
.
We analyse both astrometric and radial velocity data to propose first orbital parameters for Gl 86 B. Assuming Gl 86 B is a
white dwarf, we explore the constraints induced by this hypothesis and refine the parameters of the system.
Key words: stars: individual: Gliese 86 - stars: low mass, brown dwarfs - stars: planetary systems - instrumentation: adaptive optics
Gl 86 A is a K0V star with an estimated mass of
(Baraffe et al. 1998; Siess et al. 1997) and is located at 10.9 pc from the
Sun (Perryman et al. 1997). Through RV measurements, Queloz et al. (2000)
detected a 4
(minimum mass) planet Gl 86 b, orbiting Gl 86 A at
.
This star is also surrounded by a more distant
companion Gl 86 B, discovered at
using
coronagraphy coupled to adaptive optics imaging (Els et al. 2001). The
estimated photometry of Gl 86 B is compatible with that expected for a
40-
brown dwarf companion. Howewer, Mugrauer & Neuhäuser (2005)
showed recently that this was also compatible with a cool white dwarf,
and that the latter hypothesis was more likely regarding the K band
spectrum of the companion. The absence of near-IR molecular and atomic
lines as well as the steep K-band continuum are consistent with
what is expected for a high gravity object with an effective
temperature higher than 4000 K.
Apart from the RV wobble due to the hot Jupiter companion,
Gl 86 A also exhibits a long term RV drift measured with CORAVEL
and CORALIE over 20 years.
This drift indicates the possible presence of an additional more distant
companion, with a
substellar mass and a distance to star greater
than 20 AUs. Els et al. (2001) claimed that Gl 86 B cannot
account for this RV drift, due to its low mass.
They postulated instead that an additional
companion, located in 2000 "behind'' the star (i.e., under the coronographic
mask), could be responsible for the observed drift.
In the course of a deep search for faint outer companions to stars
hosting planets with NACO, we were able to make new images of Gl 86 A
and B in the near IR. We present the observational results in
Sect. 2. In Sect. 3, we report new photometric result of Gl 86 B and we
present an analysis of both astrometric and RV data, assuming that the
RV drift is due to Gl 86 B. In Sect. 4 we discuss the nature of
Gl 86 B, and we confirm that it is very probably a
white
dwarf. We discuss the implications of this hypothesis.
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Figure 1:
VLT/NACO
![]() ![]() |
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The calibrations of platescale and detector orientation were done
using the
Ori C astrometric field on November 12, 2003,
September 22, 2004 and July 29, 2005. On November 12, 2003 and July 29,
2005, the orientation of true north of the S27 camera was found
respectively at
and
east of the vertical with an
uncertainty of 0.20
and the platescale was
mas. On
September 22, 2004, the orientation of true north of the S13 camera was
found
east of the vertical with an uncertainty of
and the platescale was
mas.
Table 1 summarizes the new observations as well as archival
ones and Fig. 1 shows a
(
m,
m) image recorded in September 2004.
Table 1:
Observation log.
is a CONICA neutral
density filter with a transmission of 1.4%. S13 and S27 are two
CONICA cameras corresponding respectively to a platescale of 13.25 and
27.01 mas. WFS corresponds to the wave front sensor of the adaptive
optics system.
The reported photometry is significantly different from the ones given by Els et al. (2001) (see Table 1). This could be related to systematic photometric errors induced by an incorrect subtraction of the Gl 86 A PSF wings within the coronagraphic image. This effect is generally larger for shorter wavelengths where AO corrections are poorer. It often leads to an underestimation of the companion flux, as is the case in Table 1 when comparing ADONIS and NACO data. Thanks to the highest angular resolution and the enhanced detection capabilities provided by NACO at VLT, we can reasonably expect our data to be less sensitive to this PSF subtraction effect in deriving the Gl 86 B photometry.
The new NACO photometry is still compatible with the conclusions
of Els et al. (2001) that Gl86 B has a photometry similar to that
expected for a substellar companion with a mass of 40-
(spectral type L7-T5). However, this photometry can also correspond
to the one expected for a cool white dwarf and, as recently claimed by
Mugrauer & Neuhäuser (2005), this is more likely the case as the spectrum of Gl 86 B
does not exhibit the molecular absorption features in K band that are
characteristic of L or T dwarfs.
In the following, we reinvestigate this issue (brown or white dwarf) from a dynamical point of view.
It is tempting to try to attribute this regular decrease to Gl 86 B.
The temporal derivative of the radial velocity of the primary in a binary
system is easy to derive. One gets
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This result led Els et al. (2001) to conclude that the RV residuals
are not due to Gl 86 B, but rather to an unseen, additional body.
Conversely if we keep attributing the RV decrease to Gl 86 B,
this raises the question of the mass of Gl 86 B. The available photometry is
compatible with a
object (Els et al. 2001). But it can also
be compatible with a
object if this object is a white
dwarf.
Obviously, more data, in particular spectroscopic data
are needed to discriminate between these two possibilities.
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Table 2: Photometry of Gl86 A and B.
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Figure 2: Least square fits of the right ascension ( left) and of the declination ( right) of Gl 86 B relative to A. |
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Table 3: Offset positions of the Gl 86 B relative to A.
Depending on the free parameter set we choose, there is not necessarily an orbital solution compatible with the constraints. In particular, it turns out that there is no solution for ![]() |
Figure 3:
The semi-major axis a of the orbital solution for the
Gl 86 companion, as a function of the longitude of the ascending
node ![]() ![]() ![]() ![]() |
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Figure 4: Same as Fig. 3, but for the orbital eccentricty of the solution. |
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Figure 5: Same as Fig. 3, but for the present mean anomaly M. |
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Figure 6: A representation of the orbital solutions described by Eq. (3) (upper plot, brown dwarf case) and Eq. (4) (lower plot, white dwarf case), as projected onto the plane of the sky. In each case, the right plot represents a view of the full orbit and the left plot is an enlargement of the present day motion. The dotted line is the projection of the line of apsides of the orbit. |
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In order to better show the shape of the orbital solution, we display
one typical solution, marked as a bullet in
Figs. 3-5, and charaterized by
,
and
In Fig. 7, we show the Gl 86 radial velocity data set, superimposed on the theoretical curve that would be expected for the solutions we display in Fig. 6. Note that in those curves, we do not add the short period modulation due to the hot Jupiter companion, as this object produces a much smaller amplitude. We also add to the theoretical radial velocity curve an empirical offset, intended to correspond to the mean heliocentric velocity of the Gl 86 system, fixed in such a way that the radial velocity matches the mean observed value in 2003.126. The only relevant parameter we need to compare between the data and the theory is the mean temporal derivative of the radial velocity at in 2003.126, and also the general trend over 25 years.
In Fig. 7, the theoretical radial velocity
curve corresponding to Eq. (3) is represented as a dashed line.
We see that it does not match the data. In fact the decrease in 2003.126 is only
10% of the observed values (
).
As explained above, this was expected from our order of magnitude
estimate of the mass needed to account for the observe decrease rate.
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Figure 7:
Radial velocity data of Gl 86 A as monitored
over 25 years,
superimposed on the theoretical curves (in grey) corresponding
to the orbital solutions displayed in Fig. 6. The low
accuracy data up to 1998 are the CORAVEL data
(typical error ![]() ![]() ![]() ![]() |
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Figure 8:
The semi-major axis a of the orbital solution for
Gl 86 B that also fits the radial velocity data residuals,
as a function of the longitude of the ascending
node ![]() ![]() ![]() |
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Figure 9: Same as Fig. 8, but for the orbital eccentricty of the solution. |
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Figure 10: Same as Fig. 8, but for the present mean anomaly M. |
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Figure 11: Same as Fig. 8, but for the fitted mass of the Gl 86 B companion. |
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As in the previous section, we display one peculiar solution assumed to
represent a standard solution, charaterized by
and
In Fig. 6, we show the projection of this solution onto
the plane of the sky as for the orbit corresponding to
Eq. (3), and in Fig. 7 we show the
corresponding radial velocity curve as a solid grey curve.
The agreement with both the radial
velocity and the astrometric data is very good. Apart from small changes
in the orbital elements, the main difference to the orbit described in
Eq. (3) is the mass of the companion. With
,
it is obviously not a brown dwarf.
It seems thus more natural to attribute the RV residuals
to the sole Gl 86 B companion. In that case, it must be a
0.4-
object. As from its photometry it cannot be
a main sequence star of that mass, Gl 86 B is necessarily
a white dwarf. Our dynamical analysis finally leads to the same
conclusion that Mugrauer & Neuhäuser (2005) derived from independent spectrophotometric
arguments.
Based on the present constraint put on the mass of Gl 86 B and on the new NACO JHKs photometry, presented in Sect. 2.2, we can now re-investigate the physical properties of this white dwarf companion, using predictions of the evolutionary cooling sequences models of Bergeron et al. (2001) for hydrogen- and helium-rich white dwarfs.
The model predictions are reported in a color-magnitude diagram
(J-K vs. MK) for both cases: hydrogen-rich
(Fig. 12, left) and helium-rich
(Fig. 12, right) white dwarfs. We notice
the discrepancy between the model predictions and the previous
photometric data of Els et al. (2001) that Mugrauer & Neuhäuser (2005) used to derive an
effective temperature of
K for Gl 86 B.
Our new NACO photometric data are in very good agreement
with the model and with the dynamical constraints.
Then, if we add the fact that the mass of Gl 86 B is dynamically
constrained between (0.4-
), we can derive the
effective temperature, the gravity as well as the
cooling age of the
Gl 86 B companion based on model predictions. The derived physical
parameters for hydrogen- and helium-rich white dwarf model predictions
are reported in Table 4.
Table 4: Physical parameters of Gl 86 B based on predictions of the evolutionary cooling sequences models of Bergeron et al. (2001) for hydrogen- and helium-rich white dwarfs.
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Figure 12:
Color-magnitude diagram (J- K vs. MK) with
model predictions for different masses in two different cases: white
dwarfs with hydrogen-rich (Fig. 12, left) and
helium-rich (Fig. 12, right) atmospheres. The
predictions for a 0.4, 0.5 and
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For Gl 86, a first constraint is that Gl 86 B
must have been more massive than Gl 86 A in the past
(i.e.,
), in order to have more quickly evolved
to the post main-sequence state.
The IFMR is an increasing function of the initial mass. It is usually measured using white dwarfs that are members of open clusters of known ages. Weidemann (1987) gives a semi-empirical IFMR, but further measurements of white dwarfs in NGC 2516 (Jeffries 1997) have shown it was inaccurate. More relevant relations for various metallicities (Z) are given by Hurley et al. (2000). In the following, we will assume the IFMR given by Hurley et al. (2000) (Fig. 18) for Z=0.02.
Note that this IFMR is different from another one that is sometimes shown (Fagotto et al. 1994; Iben 1991; Bressan et al. 1993), which shows the mass of the white dwarf remnant as a function of that of the core at the beginning of the TP-AGB phase. We are interested in the full initial mass of Gl 86 B at Zero Age Main Sequence (ZAMS), so that the first IFMR is relevant here.
In the case of Gl 86, we are concerned by the slow mass loss case. The
equations defining the variation of the semi-major axis a and
of the eccentricity e are given by Hadjidemetriou (1963):
If the mass loss is a slow process, Eq. (5) can be averaged
over one orbital period. This gives
,
which means that the eccentricity is secularly constant
(Jeans 1928; Hadjidemetriou 1963). Subsequently, the evolution of the semi-major
axis obeys the simple rule
.
As Mdecreases, it is obvious that the orbit gets wider. If the total change
of M (only due to Gl 86 B) is known from the IFMR, it is then
possible to derive the initial semi-major axis.
If we apply this theory to the case of Gl 86 B, we are able to derive
the former characteristics of the Gl 86 system. The fit of
Sect. 3.3 allows to derive the present day orbital and mass
characteristics of Gl 86 B (a, e and m). For each solution,
using the IFMR of Hurley et al. (2000), we are able to derive the initial mass
,
and subsequently the initial
initial semi-major axis
of the orbit, using
.
All solutions that lead to
unreaslistic (negative) values for
are
then eliminated; we also eliminate all solutions for which
,
as Gl 86 B must have been initially more
massive than Gl 86 A. This can be done for each solution that fits the
radial velocity and the astrometric data. This constraint turns out
to be by far the strongest one.
The result is shown in Figs. 13-14.
In these figures, we plot the resulting values of
,
and
for all the solutions displayed
in Figs. 8-11. However, we only retain those
solutions that lead to compatible values for
,
and to
.
This is
the reason why the curves are often interrupted. In particular, all
solutions with
have been eliminated.
In all cases we have
(typically
),
showing that the orbit is more detached presently than it was in the past.
This is for instance the case for the solution described in
Eq. (4), for which we have
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Figure 13:
The initial ZAMS semi-major axis
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Figure 14: Same as Fig. 13, but for the initial main-sequence mass of the Gl 86 B progenitor, assuming Gl 86 B is presently a white dwarf. |
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Figure 15:
Same plot as Fig. 11, but all solutions
laeding to unphysical or unacceptable values for
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Another puzzling issue is the way the exoplanet formed. To what extent
was the initial circumstellar
disk of Gl 86 A that gave birth to its companion truncated by tidal
interaction with Gl 86 B?
According to Eggenberger et al. (2004), the minimum separation in a binary
that allows a large enough circumstellar disk for planet formation
to survive ranges between 10 and 50 AU. This could mean that we should
remove all solutions with
AU, which would
result in
.
The constraints on
and
help to eliminate some of the fitted solutions
in Figs. 8-11. This does not change the
basic constraints on a, e and M, but refines that on the present
mass m of Gl 86 B. In Fig. 15, we show the same plot as in
Fig. 11, but all solutions that do not fulfill the constraints
on
,
and
have been
removed. In order to explore all possilities, we performed the same
calculation for many inclination values (not only for
,
...). The resulting possibilities are summarized
as grey areas in Fig. 15. We see that m is fairly well
constrained. It is thus possible to state that
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The mass of Gl 86 B is severely constrained by the dynamics. We derive
.
The orbit
is eccentric (e>0.4) with a
semi-major axis of a few tens of AU. The associated orbital period is
several hundreds of years at least, and the stars have recently
(5-20 years ago) passed at periastron. The orbit is retrograde
with respect to the plane of the sky, but does not exactly lie in that
plane. We can say that
.
Based on new photometric results on Gl 86 B and the dynamical mass constrains, we also re-investigated the physical properties of this white dwarf companion. Using model predictions of Bergeron et al. (2001), we derived the effective temperature, the gravity and the cooling age of Gl 86 B for both hydrogen-rich and helium-rich atmospheres models of white dwarfs.
When Gl 86 B was a main sequence star, its mass probably ranged between
and
,
which implies a spectral type between
K2V and F7V. Its orbit was closer. The strong post-main sequence mass loss
caused the orbit to widen. If it had been
a more massive star, the initial semi-major axis would have been too
small to allow orbital stability for the exoplanet orbiting Gl 86 A.
However Saffe et al. (2005) recently used the chromospheric index and metallicity
measurements to estimate the age of all known stars harbouring
exoplanets. For Gl 86 A, they derived an age ranging between 2 Gyr
and 3 Gyr. Given the main sequencelifetimes and the white dwarf
cooling times (Table 4), assuming this age for Gl 86 B
would imply that its progenitor had
.
This seems to be incompatible with our dynamical constraints.
To solve this discrepancy, the dynamical evolution
of the whole system, including the exoplanet needs to be investigated
in more detail. There are many open questions associated
with this issue: the exoplanet must have survived all the late evolution stages
of Gl 86 B. If the system is not coplanar,
the exoplanet could have been subject to the Kozai resonance
in the past. Moreover, the planet must have formed in
a large enough circumstellar disk, which implies a minimum
initial separation of
AU.
All these issues need to be addressed,
and this will be the purpose of forthcoming work.
Acknowledgements
We would like to thank the ESO staff of Paranal-La Silla observatory for helping us in the preparation and the execution of our observations. We aknowledge the valuable contribution of Pierre Bergeron who significantly helped us in the use and the interpretation of the cooling models of white dwarfs. We are particularly grateful for his insightful remarks, as well as for the detailed comments of our anonymous referee. We also acknowledge partial financial support from the Programmes Nationaux de Planétologie et de Physique Stellaire (PNP & PNPS), in France.