Issue |
A&A
Volume 519, September 2010
|
|
---|---|---|
Article Number | A105 | |
Number of page(s) | 7 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201015016 | |
Published online | 20 September 2010 |
A physically-motivated photometric calibration of M dwarf metallicity
K. C. Schlaufman - G. Laughlin
Astronomy and Astrophysics Department, University of California, Santa Cruz, CA 95064, USA
Received 18 May 2010 / Accepted 11 June 2010
Abstract
The location of M dwarfs in the
color-magnitude diagram (CMD) has been shown to correlate with
metallicity. We demonstrate that previous empirical photometric
calibrations of M dwarf metallicity exploiting this correlation
systematically underestimate or overestimate metallicity at the
extremes of their range. We improve upon previous calibrations in three
ways. First, we use both a volume-limited and kinematically-matched
sample
of F and G dwarfs from the Geneva-Copehnagen Survey (GCS) to infer
the mean metallicity of M dwarfs in the Solar Neighborhood.
Second, we use theoretical models of M dwarf interiors and
atmospheres to determine the effect of metallicity on M dwarfs in the
CMD.
Third, though we use the GCS to infer the mean metallicity of
M dwarfs in the Solar Neighborhood, our final calibration is based
purely on high-resolution spectroscopy of FGK primaries with
M dwarf companions as well as the trigonometric parallaxes and
apparent V- and
-band
magnitudes of those M dwarf companions. As a result, our
photometric calibration explains an order of magnitude more of the
variance in the calibration sample than previous photometric
calibrations. We use our calibration to non-parametrically quantify the
significance of the observation that M dwarfs that host exoplanets
are preferentially in a region of the
plane populated by metal-rich M dwarfs. We find that the probability p that planet-hosting M dwarfs are distributed across the
CMD in the same way as field M dwarfs is p = 0.06
0.008. Interestingly, the subsample of M dwarfs that host
Neptune and sub-Neptune mass planets may also be preferentially located
in the region of the
plane populated by high-metallicity M dwarfs. The probability of this occurrence by chance is p = 0.40
0.02, and this observation hints that low-mass planets may be more
likely to be found around metal-rich M dwarfs. The confirmation of
this hint would be in contrast to the result obtained for
FGK stars, where it appears that metal-rich and metal-poor stars
hosts Neptune-mass planets with approximately equal probability.
An increased rate of low-mass planet occurrence around metal-rich
M dwarfs would be a natural consequence of the core-accretion
model of planet formation.
Key words: planets and satellites: formation - stars: abundances - stars: low-mass - stars: statistics
1 Introduction
The determination of metallicity for M dwarfs is a very difficult problem (e.g. Gustafsson 1989). Their cool atmospheres permit the existence of many molecules for which molecular opacities are currently poorly constrained. As a result, the estimation of the continuum level of a spectrum is challenging, rendering line-based metallicity indicators unreliable. The poorly constrained molecular opacity data currently available makes the determination of metallicity through spectral synthesis difficult as well. For those reasons, alternative methods must be employed to estimate M dwarf metallicities.
Table 1: M dwarfs in binary systems with an FGK primary and those that host planets.
The main sequence lifetimes of M dwarfs are longer than the
Hubble time, so they have not yet departed much from the zero-age
main sequence. Consequently, M dwarfs might be expected to form a
two-parameter sequence in mass and metallicity, suggesting that a
two-color broad-band photometric calibration might constrain their
properties. There have been several attempts to obtain the metallicity
of M dwarfs using their photometric properties, including two
recent breakthroughs.
Bonfils et al. (2005a) - bon05a
hereafter - had the subtle insight to realize that M dwarfs
in binary or multiple systems should have metallicities commensurate
with the easily-measured metallicity of an FGK primary in the
system. In that way, bon05a identified a calibration sample of
M dwarfs with metallicities securely determined in one of two
ways: (1) high-resolution spectroscopy of an FGK companion
and (2) high-resolution spectroscopy of M dwarfs for
which
and
could
be fixed with photometric data. For the former,
the metallicity is very likely the same as the metallicity
inferred from high-resolution spectroscopy of its FGK companion.
For the latter, spectral synthesis after fixing
and
with photometric data eliminates some degeneracy and produces a reasonable metallicity
estimate. They noted that low-metallicity M dwarfs have blue
color at constant
-band absolute magnitude
,
and they fit a linear model to their calibration sample using
and
to predict [Fe/H]. Johnson & Apps (2009) -
joh09 hereafter - addressed the relative lack of high-metallicity
M dwarfs in the
calibration sample of bon05a and created an empirical model in which
the distance of an M dwarf above the field M dwarf main
sequence (MS) in the
color-magnitude diagram (CMD) indicated its metallicity. The great
insight of joh09 was that the mean metallicity of a population of
M dwarfs could be characterized by the easily-measured mean
metallicity of a similar population of FGK stars. Indeed, they
assumed that the field M dwarf MS was an isometallicity contour
with the same metallicity as a volume-limited sample of G and
K stars and fit a linear model using the distance above the field
M dwarf MS to predict [Fe/H].
M dwarfs are attractive targets around which to search for low-mass planets because they have large reflex velocities and transit depths even for low-mass and small-radius companions. Given that the metallicity of protoplanetary disks is a key parameter in models of planet formation (e.g. Laughlin et al. 2004; Ida & Lin 2004), the metallicity of M dwarfs that host planets will constrain the planet formation process in low-mass protoplanetary disks. Indeed, it is well-established that metal-rich FGK stars are more likely to host giant planets (e.g. Fischer & Valenti 2005; Santos et al. 2004), but there is also evidence to suggest that metal-rich FGK stars are not much more likely to host Neptune-mass planets than their low-metallicity counterparts (e.g. Sousa et al. 2008; Bouchy et al. 2009; Udry et al. 2006). Already, joh09 have used their model of M dwarf metallicity to suggest that the M dwarfs that host planets are preferentially metal-rich. However, joh09 did not address whether the apparent lack of a correlation between FGK host stellar metallicity and the presence of Neptune-mass planets extends to M dwarfs.
In this paper, we examine a calibration sample of M dwarfs
with securely estimated metallicities and we show that the models of
bon05a and joh09 systematically underestimate or overestimate
metallicity at the extremes of the range of this calibration sample. We
demonstrate that a volume-limited and kinematically-matched sample of
Sun-like stars produces a better estimate of the mean M dwarf
metallicity in the Solar Neighborhood, and we use M dwarf models
of different metallicities from Baraffe et al. (1998) to improve on the technique described in joh09. The position of an M dwarf in the
CMD
remains an indicator of its metallicity, and we use that fact to
non-parametrically quantify the significance of the observation that
planet-hosting M dwarfs are preferentially in a region of the
plane
populated by metal-rich M dwarfs. Moreover, we identify for the
first time a hint that the subsample of M dwarfs that host Neptune
and sub-Neptune mass planets may also be more likely to be in the
region of the
CMD
associated with metal-rich M dwarfs. We describe our analysis in
Sect. 2 and summarize our findings in Sect. 3.
2 Analysis
2.1 Testing previous calibrations
We first collect from bon05a and joh09 a calibration sample of M dwarfs in wide binary or multiple systems with an FGK primary. The metallicity of the FGK primary in the system is straightforward to measure from a high-resolution spectrum, and if the M dwarf secondary and the FGK primary formed in the same molecular core, then the expectation is that the two should have commensurate metallicities. We collect 13 examples from bon05a, selecting only those M dwarfs with precise V-band magnitudes from CCD photometry. We also collect six high-metallicity examples from joh09. We summarize this calibration sample of M dwarfs in the first 19 lines of Table 1.
We compute the metallicity predicted for this calibration sample from
both the bon05a and joh09 relations and compare it to the observed
values. Note that the bon05a relation was initially based on a
calibration sample that included M dwarfs in binary or multiple
systems with FGK primaries (some with V-band
magnitudes deduced from photographic plates) as well as low-metallicity
M dwarfs with metallicity inferred from spectroscopy after
fixing
and
with
photometric data. Meanwhile, the joh09
calibration sample included only the six metal-rich M dwarfs in
binary or multiple systems with FGK primaries listed in
rows 14 through 19 in Table 1.
For those reasons, we believe that the 19 M dwarfs with
metallicities inferred from high-resolution spectroscopy of
FGK primaries in Table 1
is the largest and most reliable set of M dwarf metallicities from
which to verify previous calibrations. We apply both the bon05a and
joh09 relations to this sample and compute the residual between each
model and observation. We plot the distribution of residuals for both
models in Fig. 1, and we find
that the bon05a relation systematically underestimates M dwarf
metallicity and that the joh09 relation systematically overestimates
M dwarf metallicity.
2.2 A physically-motivated empirical model of M dwarf metallicity
As discussed in Sect. 2.1 and Fig. 1, the models of bon05a and joh09 have non-negligible residuals when applied to the calibration sample in Table 1. Still, there is a correlation between the metallicity of an M dwarf and its
distance in the
plane
from the field M dwarf MS. We attempted to improve the joh09 model
by reassessing both the zero point of the model and the direction from
the M dwarf MS in the
plane best correlated with metallicity.
Recall that joh09 set the mean metallicity of the Solar Neighborhood
M dwarf sample equal to the mean metallicity of a volume-limited
sample of G0-K2 stars (
4.0 < MV < 6.5) from the SPOCS catalog of Valenti & Fischer (2005).
The SPOCS sample of joh09 was based on a catalog of stars selected
to have absorption lines deep enough to enable high-precision radial
velocity detection of exoplanets. As a result, the
SPOCS sample is biased against metal-poor stars and therefore
potentially unsuitable for the determination of the average metallicity
in the Solar Neighborhood (as noted in Valenti & Fischer 2005). Alternatively, the Geneva-Copenhagen Survey (GCS - Holmberg et al. 2009,2007; Nordström et al. 2004)
of Solar Neighborhood F and G dwarfs is magnitude-complete,
kinematically-unbiased, and free of the line depth bias inherent in the
SPOCS catalog. Though
the GCS metallicity estimates are based on Strömgren photometry
and not high-resolution spectroscopy, the precision of the
GCS metallicities are sufficient when combined with the reduced
bias of the sample to provide a better estimate of the mean Solar
Neighborhood
metallicity than the SPOCS sample.
![]() |
Figure 1: Optimally-smoothed residual distributions for Bonfils et al. (2005a) - bon05a hereafter - and Johnson & Apps (2009) - joh09 hereafter. In both cases the vertical dashed line indicates the mean of the distribution. The mean value of the bon05a residuals is 0.12 with standard deviation 0.16, while the mean value of the joh09 residuals is -0.12 with standard deviation 0.12. Note that the bon05a distribution has a heavy tail at large positive values (indicating systematically low [Fe/H] estimates) and the joh09 distribution has a heavy tail at large negative values (indicating systematically high [Fe/H] estimates). |
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In addition, the UVW kinematics of a volume-limited sample
of M dwarfs is not necessarily equivalent to the kinematics of a
volume-limited sample of FGK dwarfs. Since the mean of a sample is
sensitive to outliers, and because Sun-like stars with outlier
kinematics are also likely to be outliers in metallicity,
a kinematic-match is important to determine the mean metallicity
of Solar Neighborhood M dwarfs in this way. To address this
point, we use the M dwarf UVW distribution described by Hawley et al. (1996) to create a volume-limited and kinematically-matched sample of F and G dwarfs from Holmberg et al. (2009) from which we infer the average metallicity of the Solar Neighborhood
M dwarf population. In Fig. 2 we superimpose the UVW velocity-space distribution of local M dwarfs derived by Hawley et al. (1996) on top of the UVW
velocity-space distribution of F and G stars from the GCS with
parallax-based distance estimates that place them within 20 pc of
the Sun. We bootstrap resample from the subset of GCS stars within
20 pc and with kinematics consistent with the M dwarf
velocity ellipsoid as defined in Hawley et al. (1996). We ensure that 68% of the GCS stars in each bootstrap sample have UVW velocities that place them within the one-sigma contour of Hawley et al. (1996)
and that the rest of each bootstrap sample lies within the two-sigma
contour. In the end, we find that a volume-limited and
kinematically-matched sample of F and G dwarfs from the GCS survey
has a mean metallicity of [Fe/H] = -0.14
0.06. We obtain a similar result with a sample of GCS stars
volume-limited in the same way as the volume-limited SPOCS sample
of joh09, for which we find a mean Solar Neighborhood metallicity of
[Fe/H] = -0.15
0.02. In this case, the superior statistics of the larger
volume-limited sample is enough to formally achieve a higher precision
than the volume-limited and kinematically-matched sample, though the
volume-limited sample is subject to a greater degree of possible
systematic error. For that reason, we regard the volume-limited and
kinematically-matched result as likely more reliable.
![]() |
Figure 2:
Velocity ellipsoids inferred for a volume-limited sample of early M dwarfs from Hawley et al. (1996) superimposed on the UVW velocity distribution of a volume-limited sample (
|
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The mean metallicity of our volume-limited and kinematically-matched
GCS sample suggests that the field M dwarf MS defined by
joh09 is an isometallicity contour with [Fe/H]
-0.14. Note that if the isometallicity contour corresponded to [Fe/H] = -0.05 as in joh09, five stars from Table 1
with [Fe/H] < -0.05 would be to the right of the isometallicity
contour indicating [Fe/H] > -0.05. Alternatively, if we
assume that the isometallicity contour corresponds to [Fe/H]
-0.14, then only two of the 19 stars are on the wrong side of contour.
We now determine which direction in the
plane an isochrone moves as a function of metallicity. In Fig. 3 we plot the M dwarfs with securely determined metallicity from Table 1, along with the M dwarf MS from joh09 and
two different isochrones from Baraffe et al. (1998). We use the transformation of Carpenter (2001) to transform the
given in Baraffe et al. (1998) into
.
The left-most isochrone corresponds to a population with [Fe/H] = -0.5 and Y = 0.25 while the right-most isochrone corresponds to a population with [Fe/H] = 0 and Y = 0.275. Both isochrones use mixing-length parameter l = 1 for a 5 Gyr population (there is no detectable evolution in
CMD after 3 Gyr). The horizontal lines connect points of constant mass. With all other
parameters constant, metallicity should best correlate with horizontal shifts in the
plane.
For that reason, we compute the distance from the M dwarf MS
in the horizontal direction for each M dwarf with secure
metallicity from Table 1. We then fit a linear model using this distance as a predictor with [Fe/H] as the response. We find that
is the optimal model. In this case,





![]() |
Figure 3:
Position of M dwarfs with secure metallicities from Table 1 (blue points) in the
|
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![]() |
Figure 4:
Left: position of M dwarfs known to host Jupiter-mass planets
(dark blue triangles) and Neptune-mass (or below) planets (blue
squares) in relation to a control sample of field M dwarfs (gray
points) and the field M dwarf MS from joh09 (black line). Again,
like the high-metallicity M dwarfs, the M dwarfs that host
planets are concentrated to the right of the field M dwarf MS. Right: distribution of cumulative sample distances from the field M dwarf MS of joh09, which we assume to be a [Fe/H] |
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We use two of the model selection criteria given in Hocking (1976) to evaluate all three models. First, we compute the residual mean square (rms), defined as
where n is the number of data points, p is the number of predictors in the model, and





where yi and

Differing
scales have been well-noted as a source of metallicity discrepancies in metallicity studies of the Solar Neighborhood (e.g. Holmberg et al. 2007). The differing
calibrations
between the GCS and other surveys will not affect our results,
as our calibration (including the metallicity of the M dwarf
MS) is based on the horizontal distance in the
CMD
from the mean M dwarf MS of joh09 of M dwarfs with
metallicities known from high-resolution spectroscopy of
FGK primaries. We only used the GCS Strömgren-based metallicities
to establish the fact that the mean Solar Neighborhood metallicity is
closer to [Fe/H]
-0.15 than it is to [Fe/H]
-0.05 as argued by joh09.
For that reason, our calibration is based purely on
high-resolution spectroscopy of FGK primaries as well as the
trigonometric parallaxes and apparent V- and
-band magnitudes of their M dwarf companions.
The M dwarfs in binary systems with FGK primaries that we use to fix
our calibration are not a volume-limited or kinematically-matched
sample. The volume-limit and kinematic-match were only necessary to
verify the fact that the mean metallicity of the M dwarf
population in the Solar
Neighborhood is a well-defined quantity. That verification is a
necessary precondition that must be established before any joh09 style
calibration using distance from the field M dwarf MS in the
CMD can even be considered. Once the points along the field M dwarf MS in the
CMD are fixed to the mean metallicity of the Solar Neighborhood, the metallicity of an M dwarf with given
color and absolute magnitude
along the curve is specified regardless of its position or velocity.
Indeed, when we build our calibration using only the metallicities of
M dwarfs in binaries with FGK primaries, their V- and
-band
magnitudes, and trigonometric parallaxes, we find that the mean
metallicity of the Solar Neighborhood M dwarf MS based on the
calibration sample ([Fe/H] = -0.17
0.07)
is statistically indistinguishable from the mean metallicity inferred
from the volume-limited and kinematically-matched sample
([Fe/H] = -0.14
0.06).
2.3 The metallicity of M dwarfs that host planets
We plot the location of M dwarfs that host planets in the left-hand panel of Fig. 4. The M dwarf models of Baraffe et al. (1998) suggest that horizontal distance in the
CMD
best correlates with metallicity. To non-parametrically determine
the degree to which planet-hosting M dwarfs are preferentially
found to the right of the M dwarf MS, we need to quantify the
likelihood that the cumulative horizontal distance from the
isometallicity contour of a randomly selected sample of field
M dwarfs can be as large as that observed in the sample of
M dwarfs that host planets simply by chance.
To address this issue, we create a control sample of field M dwarfs selected from the Hipparcos (van Leeuwen 2007) and Yale Parallax Catalogs (van Altena et al. 1995). We include in the control sample those M dwarfs from the Hipparcos catalog that have parallaxes mas precise to better than 5% and those M dwarfs from the Yale catalog that have parallaxes
mas. We use V-band photometry from each catalog and we obtain
photometry for both samples from the 2MASS database (Skrutskie et al. 2006). For a sample of size n we can compute the statistic
:
To characterize the likelihood that an observed value of










2.4 Discussion
The apparent position of planet-hosting M dwarfs in the region of the
CMD
associated with known high-metallicity M dwarfs tentatively
suggests that metal-rich M dwarfs are more likely to host
Jupiter-mass and possibly Neptune-mass planets as well.
If this correlation is confirmed in the future, it can be
understood as a natural consequence of the core-accretion model of
planet formation (e.g. Laughlin et al. 2004; Ida & Lin 2004).
Indeed, a more metal-rich protoplanetary disk will almost
certainly have a higher surface density of solids, and that increased
surface density enables the rapid formation of the several Earth-mass
cores necessary to accrete gas from the protoplanetary disk before the
gaseous disk is dissipated. Moreover, it would be especially
interesting if the tentatively suggested correlation extends to the
hosts of Neptune-mass planets, as current evidence seems to suggest
that the probability that an FGK star hosts a Neptune-mass planet
is not a strong
function of metallicity (e.g. Sousa et al. 2008; Bouchy et al. 2009; Udry et al. 2006).
If the tentatively suggested correlation between the presence of
planets and the metallicity of their host M dwarfs is eventually
confirmed, it might indicate a lower-limit on the amount of solid
material necessary to form planets. To see why, recall that the
mass of a protoplanetary disk
scales roughly as
and that the fraction of solid material in a disk
scales roughly as
where
is the metal content of the host star. The total amount of solid material in a protoplanetary disk will then scale like
.
Minimum-mass Solar Nebula models (MMSN - Hayashi 1981)
and observations of T Tauri disks in star-forming regions
suggest that protoplanetary disks around young Solar-type stars are
about 1% the mass of their host stars, albeit with significant
scatter (e.g. Hartmann et al. 1998). Combined with the fact that the metal content of the Sun is
by mass, the total solid mass in the MMSN was about
.
This is a lower-limit, as more careful calculations suggest that the protoplanetary disk around the Sun had
(e.g. Lissauer 1993). In either case, this is a factor of a few to ten greater than the
of material necessary to form the core of a gas or ice giant planet in
the core-accretion model of planet formation. In the case of a
Solar-metallicity mid-M dwarf with
,
the total amount of solid material in the disk is 70% less, about
.
This is factor of order unity to a few times the mass necessary to form
the core of a gas or ice giant. Since planet formation likely does not
lock-up the entire solid component of a protoplanetary disk in planets,
reducing the total mass of solids in the disk - either by reducing
the metallicity or mass - will also reduce the chances of forming
a
core (and therefore a gas or ice giant) before the parent protoplanetary disk is dissipated.
The confirmation of the hint of a correlation between the presence of low-mass planets and M dwarf metallicity could be evidence of this threshold solid mass necessary to form Neptune-mass planets. Around FGK stars, the same threshold solid mass suggests that a correlation between the presence of low-mass planets and host star metallicity might occur at one-third Solar metallicity, or [Fe/H] = -0.5. This is just below the typical metallicity of stars observed at high radial velocity precision with HARPS (Sousa et al. 2008). This expected correlation might be verified as larger samples of low-metallicity stars are surveyed at high radial velocity precision or by transit surveys of nearby low-metallicity open clusters (e.g. NGC 752 or IC 4756).
The hint of a correlation between the presence of Neptune-mass
(and below) planets and M dwarf metallicity tentatively
suggests that searches for low-mass planets around M dwarfs like
the MEarth Project (Nutzman & Charbonneau 2008) could improve their yield by shading their target list toward M dwarfs that have red
colors at constant
-band absolute magnitude
.
Note that since the absolute magnitude
of an M dwarf depends only on the logarithm of its often poorly-known distance, while
depends linearly on its often poorly-known
V-band magnitude, the collection of high-quality CCD-based V-band
magnitudes for M dwarfs in the Solar Neighborhood could be the
first step towards maximizing the yield of planets around
M dwarfs.
3 Conclusion
We showed that previous empirical photometric calibrations of
M dwarf metallicity systematically underestimate or overestimate
metallicity at the extremes of their range. We derived a
physically-motivated model that explains an order of magnitude more of
the variance in the calibration sample than either the Bonfils et al. (2005a) or Johnson & Apps (2009) models. We used the correlation underlying our model to non-parametrically show that the probability p that there is no relationship between position of an M dwarf in the
CMD and the presence
or absence of planets is p = 0.06
0.008. For the subsample of M dwarfs that host Jupiter-mass planets, the probability that there is no correlation is p = 0.04
0.005. Meanwhile, for the subsample of M dwarfs that host
Neptune-mass (or below) planets, we find that the probability that
there is no correlation is p = 0.40
0.02. Since the models of Baraffe et al. (1998) suggest that the position of an M dwarf in the
CMD
is a qualitative indicator of metallicity, this observation tentatively
suggests that metal-rich M dwarfs are more likely to host planets
and hints that the correlation may extend to low-mass planets
as well. If this correlation is confirmed in the future,
it will be in contrast to planetary systems around FGK stars,
in which there appears to be only a weak connection between
metallicity
and the presence of Neptune-mass planets.
We thank Connie Rockosi for useful comments and conversation and the anonymous referee for many insightful suggestions that improved this paper significantly. This research has made use of NASA's Astrophysics Data System Bibliographic Services, the Exoplanet Orbit Database and the Exoplanet Data Explorer at exoplanets.org, and the NASA/IPAC Infrared Science Archive, which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration. This material is based upon work supported under a National Science Foundation Graduate Research Fellowship.
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All Tables
Table 1: M dwarfs in binary systems with an FGK primary and those that host planets.
All Figures
![]() |
Figure 1: Optimally-smoothed residual distributions for Bonfils et al. (2005a) - bon05a hereafter - and Johnson & Apps (2009) - joh09 hereafter. In both cases the vertical dashed line indicates the mean of the distribution. The mean value of the bon05a residuals is 0.12 with standard deviation 0.16, while the mean value of the joh09 residuals is -0.12 with standard deviation 0.12. Note that the bon05a distribution has a heavy tail at large positive values (indicating systematically low [Fe/H] estimates) and the joh09 distribution has a heavy tail at large negative values (indicating systematically high [Fe/H] estimates). |
Open with DEXTER | |
In the text |
![]() |
Figure 2:
Velocity ellipsoids inferred for a volume-limited sample of early M dwarfs from Hawley et al. (1996) superimposed on the UVW velocity distribution of a volume-limited sample (
|
Open with DEXTER | |
In the text |
![]() |
Figure 3:
Position of M dwarfs with secure metallicities from Table 1 (blue points) in the
|
Open with DEXTER | |
In the text |
![]() |
Figure 4:
Left: position of M dwarfs known to host Jupiter-mass planets
(dark blue triangles) and Neptune-mass (or below) planets (blue
squares) in relation to a control sample of field M dwarfs (gray
points) and the field M dwarf MS from joh09 (black line). Again,
like the high-metallicity M dwarfs, the M dwarfs that host
planets are concentrated to the right of the field M dwarf MS. Right: distribution of cumulative sample distances from the field M dwarf MS of joh09, which we assume to be a [Fe/H] |
Open with DEXTER | |
In the text |
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