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Astron. Astrophys. 331, 581-595 (1998)
1. Introduction
Surface rotation is a key observational parameter for stellar
evolution, as a diagnostic of the mechanisms responsible for stellar
angular momentum loss and internal angular momentum transport. The
latter are responsible for chemical mixing and they modify the stellar
thermal structure (e.g. Martin & Claret 1996), and hence affect
the overall evolution. Rotation is also the driving force behind
stellar activity (coronae, chromospheres, spots, flares), through
dynamo production of magnetic fields.
Pre-main-sequence rotational evolution of low mass stars is
generaly presumed to be dominated by magnetic coupling with the parent
protostellar disk (Cameron & Campbell 1993, Shu et al. 1994): as
long as a star is surrounded by a substantial accretion disk, its
equatorial velocity remains approximately constant at
20 (e.g.
Bouvier et al. 1993). Once accretion stops, disk braking disappears,
and angular momentum conservation then becomes the dominant factor.
Stars therefore spin up during their contraction along an Hayashi
track, as their moment of inertia decreases. Since the time at which
this happens depends on details of their circumstellar environment,
stars arrive on the ZAMS with a broad distribution of rotational
velocities (e.g. Bouvier et al. 1997). Once on the main sequence the
moment of inertia no longer changes significantly. As first suggested
by Schatzman (1962), magnetic winds then brake down the stars to low
final equatorial velocities, approximately with a
Skumanich (1972) law. The time scale for this
angular momentum dissipation is mass-dependent: rapid rotators are
found at all spectral types (G-M) at the age of the
Persei cluster ( 50 Myr)
(Prosser 1991), in the Pleiades ( 70 Myr) only
later than mid-K (Stauffer & Hartmann, 1987), and in the Hyades
( 600 Myr) only within the M dwarfs (Stauffer et
al. 1987; Stauffer et al. 1997). The situation in the field is
slightly less clear, since several age groups are represented, but all
G dwarfs rotate slowly, and there are good spectroscopic or dynamic
arguments to attribute a (very) young age to all K-early M rapid
rotators.
Over the years, a large observational effort has established this
picture of rotation along low mass stellar tracks, and models
incorporating the above general elements (e.g. Bouvier & Forestini
1995, Krishnamurthi et al. 1997) successfully reproduce the rotational
velocity distribution of solar mass dwarfs at all ages:
pre-main-sequence T Tauri and post-T Tauri star, young main
sequence stars in open clusters, and field stars.
Some aspects of the models however remain largely phenomenological,
mostly because the complex physics of accretion and stellar dynamos is
only partly understood. A number of competing models therefore exist,
that differ on, for instance, radiative core/convective envelope
decoupling, or parameterisation of the angular momentum loss law. The
uncertain physical mechanisms are expected to have a strong mass
dependence, and it is therefore useful to extend the observational
database to the lower mass M dwarfs (e.g. Krishnamurthi et al. 1997).
The [M0V,M6V] range is also interesting because it contains the mass
( , M2.5V) below which main sequence stars no
longer develop a radiative core. The radiative/convective boundary
layer is essential (e.g. Spiegel & Weiss 1980; Spruit & van
Ballegooijen 1982) to the operation of the standard
shell dynamo which is generally believed to
generate the large scale solar magnetic field, and a break in both the
activity level and the rotation properties could, at least naively, be
expected at this spectral type.
A number of authors have discussed the rotation behaviour of M
dwarfs in young open clusters (most recently Stauffer et al. (1997)
for the Hyades, Stauffer et al. (1994) for the Pleiades, Patten &
Simon (1996) for IC 2391), but there are fewer studies for field M
dwarfs. Stauffer & Hartmann (1986) measured v sin i for
approximately 200 field M dwarfs with a 10 km.s -1
sensitivity. Only 11 have significant broadening, a few of which may
actually be unrecognized double-lined spectroscopic binaries. Marcy
& Chen (1992) observed 47 field M dwarfs with v sin i
sensitivity of 3 km.s -1, only five
of which have detectable rotation, all with v sin i
km.s -1. Both surveys have
relatively bright limiting magnitudes (V=12 and V=11, respectively)
and as a consequence preferentially sample early M dwarfs. More
recently, two papers have examined the rotation of very low mass field
stars (M6 or later). Martin et al. (1996) have determined rotational
periods for a set of very late (M6-M9) dwarfs, and all 6 field stars
in their sample have very short rotational periods
8 hours ( ). Basri &
Marcy (1995) have measured v sin i for 5 extreme cool field
dwarfs, of which 3 rotate, including the brown dwarf candidate
BRI 0021-0214 (M9.5+, v sin i =40 km.s -1).
Surprisingly, BRI 0021-0214 is a rapid rotator but has very weak
(Basri & Marcy 1995) though detectable (Tinney et al. 1997)
chromospheric activity, as measured by
emission. This suggests a possible change in the rotation/activity
relation for the latest M dwarfs, and it is therefore important to
examine slightly earlier M dwarfs.
In the course of a radial velocity survey for low mass companions
and planets around nearby M dwarfs (Delfosse et al. 1997), we have
obtained high resolution optical spectra for a volume-limited sample
of 118 K5 to M6.5 dwarfs. Here we analyse the accurate
v sin i measurements (or significant upper limits,
2 ) that
we derive from those data, using digital correlation techniques. They
fill the spectral type gap between the generally earlier slow rotators
measured by Marcy & Chen (1992) and the later than M6 very low
mass rapid rotators observed by Basri & Marcy (1995) and Martin et
al. (1996). This brings important new constraints on angular momentum
dissipation in mid-M dwarfs at a few Gyr.
© European Southern Observatory (ESO) 1998
Online publication: February 16, 1998
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