Issue |
A&A
Volume 521, October 2010
|
|
---|---|---|
Article Number | A9 | |
Number of page(s) | 10 | |
Section | Stellar structure and evolution | |
DOI | https://doi.org/10.1051/0004-6361/201014305 | |
Published online | 14 October 2010 |
Thermohaline mixing in evolved low-mass stars
M. Cantiello - N. Langer
Argelander-Institut für Astronomie der Universität Bonn, Auf dem Hügel 71, 53121 Bonn, Germany
Received 23 February 2010 / Accepted 27 May 2010
Abstract
Context. Thermohaline mixing has recently been proposed to
occur in low-mass red giants, with large consequence for the chemical
yields of low-mass stars.
Aims. We investigate the role of thermohaline mixing during the evolution of stars between 1
and 3
,
in comparison with other mixing processes acting in these stars.
Methods. We use a stellar evolution code which includes rotational mixing, internal magnetic fields and thermohaline mixing.
Results. We confirm that during the red giant stage, thermohaline mixing has the potential to decrease the abundance of 3He,
which is produced earlier on the main sequence. In our models we find
that this process is working on the RGB only in stars with initial mass
.
Moreover we report that thermohaline mixing is also present during core
He-burning and beyond, and has the potential to change the surface
abundances of AGB stars. While we find rotational and magnetic
mixing to be negligible compared to the thermohaline mixing in the
relevant layers, the interaction of thermohaline motions with the
differential rotation may be essential to establish the timescale of
thermohaline mixing in red giants.
Conclusions. To explain the surface abundances observed at the
bump in the luminosity function, the speed of the mixing process needs
to be more than two orders of magnitude higher than in our models.
However it is not clear if thermohaline mixing is the only physical
process responsible for these surface-abundance anomalies. Therefore it
is not possible at this stage to calibrate the efficiency of
thermohaline mixing against the observations.
Key words: stars: abundances - stars: evolution - stars: magnetic field - nuclear reactions, nucleosynthesis, abundances - stars: AGB and post-AGB - stars: rotation
1 Introduction
Stars are rotating, self-gravitating balls of hot plasma. Due to thermonuclear reactions in the deep stellar interior, stars, which presumably start out chemically homogeneous, develop chemical inhomogeneities. At the densities typically achieved in stars, thermal diffusion, or Brownian motion, is not able to lead to chemical mixing. However, various turbulent mixing processes are thought to act inside stars, leading to transport of chemical species, heat, angular momentum, and magnetic fields (Heger et al. 2000; Pinsonneault 1997; Heger et al. 2005).
Thermohaline mixing is usually not considered to be an important mixing
process in single stars, because the ashes of thermonuclear fusion
consist of heavier nuclei than its fuel, and stars usually burn from
the inside out. The condition for thermohaline mixing, however, is
that the mean molecular weight ()
decreases inward. This can occur in accreting binaries, and the
importance of thermohaline mixing has long been recognized by the
binary community (e.g., de Greve & Cugier 1989; Sarna 1992; Wellstein et al. 2001). Recently Charbonnel & Zahn (2007b, CZ07)
identified thermohaline mixing as an important mixing process, which
significantly modifies the surface composition of red giants after the
first dredge-up. The work by CZ07 was initiated by the paper of Eggleton et al. (2006, EDL06), who found an mean molecular weight (
)
inversion - i.e.,
-
below the red giant convective envelope in a 1D-stellar evolution
calculation. While EDL06 then investigated the stability of the zone
containing the
-inversion
with a 3D hydro-code and found these layers to be
Rayleigh-Taylor-unstable, CZ07 could not confirm this, but found
the layers to be unstable due to thermohaline mixing.
Eggleton et al. (2006) found a -inversion in their
stellar evolution model, occurring
after the so-called luminosity bump on the red giant branch, which is
produced after the first dredge-up, when the H-burning shell source
enters the chemically homogeneous part of the envelope. The
-inversion is produced by the reaction 3He(3He, 2p)4He, as predicted by Ulrich (1972). It does not occur earlier, because the magnitude of the
-inversion is small and negligible compared to a stabilizing
-stratification.
Mixing processes below the convective envelope in models of low-mass
stars turn out to be essential for the prediction of their chemical
yield of 3He (EDL06), and are essential to understand the surface abundances of red giants - in particular the 12C/13C ratio, 7Li and
the carbon and nitrogen abundances (CZ07). This may also be
important for other occurrences of thermohaline mixing in stars,
i.e., in single stars when a -inversion is produced by off-center ignition in semi-degenerate cores (Siess 2009) or in stars which accrete chemically enriched matter from a companion in a close binary (e.g., Stancliffe et al. 2007).
Accreted metal-rich matter during the phases of planetary formation
also leads to thermohaline mixing, which can reconcile the
observed metallicity distribution of the central stars of planetary
systems (Vauclair 2004).
In the present paper we investigate the evolution of solar metallicity stars between
and
from the ZAMS up to the thermally-pulsing AGB stage, based on
models computed during the last years. We show for which initial mass
range and during which evolutionary phase thermohaline mixing occurs
and what consequences it has. Besides thermohaline mixing, our
models include
convection, rotation-induced mixing, and internal magnetic fields, and
we compare the significance of these processes in relation to the
thermohaline mixing.
2 The speed of thermohaline mixing
2.1 Thermohaline mixing VS Rayleigh-Taylor
As pointed out by CZ07, a -inversion
inside a star should give rise to thermohaline mixing,
which is a slow mixing process acting on the local thermal timescale.
Could a Rayleigh-Taylor instability be present in these layers? Indeed,
EDL06 interpret the origin of the instability which they find in their
3D models as due to the buoyancy
produced by the
-inversion, i.e. a dynamical effect. But a dynamical instability should only occur if the
-inversion
were to lead to a density inversion. However, this would only be
possible if the considered layers were convectively unstable in the
hydrostatic 1D stellar evolution models. As pointed out by
CZ07 and as confirmed by our models, the
-inversion produced by the 3He(3He, 2p)4He
reaction does not induce convection. We conclude that the
Rayleigh-Taylor instability may not be a likely explanation of the
hydrodynamic motions found by EDL06. A similar conclusion was also
reached by Denissenkov & Pinsonneault (2008), who studied in detail the instability driven by the
-inversion in both the adiabatic and the radiative limit.
Because smaller blobs have a smaller thermal timescale (Kippenhahn et al. 1980), could EDL06 have found the high wavenumber tale of the thermohaline instability? They found the instability to occur within 2000 s. The size of a blob with such a short thermal timescale above the H-burning shell of a red giant is on the order of 50 km. This is too small to be resolved in the 3D model shown by ELD06. Furthermore, an inspection of their Fig. 5 reveals that the length scale of the instability they found is on the order of 103...104 km, which corresponds to thermal timescales of about 1 yr. Therefore, it seems unlikely that EDL06 actually picked up the thermohaline instability in their 3D hydrodynamic model, unless its non-linear manifestation involves a timescale much shorter than the thermal timescale.
2.2 The efficiency of thermohaline mixing
In Sect. 3 we explain the
details of our implementation of thermohaline mixing in 1D stellar
evolution calculations. The diffusion coefficient for the mixing
process contains a parameter which depends on the geometrical
configuration of the fluid elements. This parameter (
)
is very important to understand the role of thermohaline mixing.
It determines the timescale of the mixing (the velocity of
the fingers/blobs) that we show in Sects. 4 and 5
plays a role not only in determining how fast the surface abundances of
redgiants can change, but also if thermohaline mixing is present in
stars of different mass and at different evolutionary phases.
Charbonnel & Zahn (2007b) showed that a high value of
is needed to match the surface abundances of field stars after the luminosity bump (Gratton et al. 2000). Similar to the value adopted by Ulrich (1972) they use an efficiency factor corresponding to
in
our diffusion coefficient. This value corresponds to the diffusion
process involving fingers with an aspect ratio (length/width)
of 5. Denissenkov & Pinsonneault (2008)
claim that to explain the observed mixing pattern in low-mass
RGB stars, fluid elements have to travel over length scales
exceeding their diameters by a factor of 10 or more.
On the other hand, the order of magnitude of our efficiency parameter
corresponds to the prescription of Kippenhahn et al. (1980),
where the diffusion process involves blobs of size L traveling a
mean free path L before dissolving. The same prescription has been
used by Stancliffe et al. (2007), who dealt
with the problem of thermohaline mixing in accreting binaries. The
sensitivity of thermohaline mixing to a change of the efficiency
parameter is shown in Fig. 1, where the change of the surface abundance of
at the luminosity bump is shown for different values of
.
That a prescription can reproduce the observed surface abundances may not be sufficient to prefer it over others. It is possible that other mixing processes are at work. The resulting observed abundances could still be mainly due to thermohaline mixing, as proposed by CZ07, but at this stage it is not possible to exclude that magnetic buoyancy (Nordhaus et al. 2008; Busso et al. 2007), or the interaction of different mixing processes (e.g., thermohaline mixing and magnetic buoyancy, Denissenkov et al. 2009), could play an even more important role.
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Figure 1:
Evolution of the surface abundance of 3He for
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To clarify the picture here we discuss the main differences between the
two physical prescriptions for thermohaline mixing. Experiments of
thermohaline mixing show slender fingers in the linear regime (e.g., Krishnamurti 2003), supporting the picture of Ulrich (1972).
On the other hand the physical conditions inside a star are quite
different from those in the laboratory. In particular the Prandtl
number ,
defined as the ratio of the kinematic viscosity
to the thermal diffusivity
,
is very small in stars (
).
This number is about 7 in water, where most of thermohaline mixing
experiments have been performed. The question arises if for such small
values of
a finger-like structure can be stable, especially in layers where shear
and horizontal turbulence is present. 2D hydrodynamic simulations of
double-diffusive phenomena, without external perturbations have been
performed in the past (e.g., Merryfield 1995; Bascoul 2007b,a).
While the resolution required by the physical conditions in stellar
interiors is computationally not accessible, lowering the Prandtl
number to values of about 10-2 always results in increasingly unstable structures (Merryfield 1995; Bascoul 2007a).
Therefore it might be dangerous to assume that the same configuration
of thermohaline mixing, as observed in water, is occurring
in stars.
As we show in Sect. 6, the radiative buffer between the H-burning shell and the convective envelope is a region of the star where the angular velocity is rapidly changing. Even if the order of magnitude of the rotationally-induced instabilities is much lower than the one from thermohaline mixing (cf. Fig. 9), it is possible that the interaction of the shear motions with the thermohaline diffusion prevents a relatively ordered flow to be stable, contrary to Ulrich's assumption. That shear can decrease the efficiency of thermohaline mixing was already pointed out by Canuto (1999). The effect of strong horizontal turbulence in stellar layers has also been discussed by Denissenkov & Pinsonneault (2008), and we conclude in Sect. 6.3 that this effect could work against the fingers and in favor of blobs.
The thermohaline mixing prescription proposed by Kippenhahn et al. (1980) has been used for the calculations presented here. It is clear from the discussion above that a better calibration of the mixing speed requires realistic hydrodynamic calculations of the instability.
3 Method
We use a 1D hydrodynamic stellar evolution code (Yoon et al. 2006, and references therein). Mixing is treated as a diffusive process and is implemented by solving the diffusion equation
where D is the diffusion coefficient constructed from the sum of individual mixing processes and Xn the mass fraction of species n. The second term on the right hand side accounts for nuclear reactions. The contributions to the diffusion coefficient are convection, semiconvection, thermohaline mixing, rotationally induced mixing, and magnetic diffusion. The code includes the effect of centrifugal force on the stellar structure, and the transport of angular momentum is also treated as a diffusive process (Pinsonneault et al. 1989; Endal & Sofia 1978).
The condition for the occurrence of thermohaline mixing is
i.e. the instability operates in regions that are stable against convection (according to the Ledoux criterion) and where an inversion in the mean molecular weight is present. Here





where





For rotational mixing, four different diffusion coefficients are calculated for dynamical shear, secular shear, Eddington-Sweet circulation and Goldreich-Schubert-Fricke instability. Details on the physics of these instabilities and their implementation in the code can be found in Heger et al. (2000).
Chemical mixing and transport of angular momentum due to magnetic fields (Spruit 2002) is included as in Heger et al. (2005). The contribution of magnetic fields to the mixing is also calculated as a diffusion coefficient (
), which is added to the total diffusion coefficient D that enters Eq. (1).
We compute evolutionary models of
,
,
and
at solar metallicity (Z=0.02). The initial equatorial velocities of these models were chosen to be 10, 45, 140 and 250
(Tassoul 2000);
we assume the stars to be rigidly rotating at the zero-age main
sequence. Throughout the evolution of all models, the mass-loss rate of
Reimers (1975) was used.
4 Thermohaline mixing on the giant branch
We compute the stellar models of 1.0, 1.5, 2.0 and 3.0
with solar metallicity. The evolutionary calculations presented are the same as in Suijs et al. (2008), to which we refer for the details of their main sequence evolution.
The surface composition of low-mass stars is substantially changed
during the first dredge-up: lithium and carbon abundances as well as
the carbon isotopic ratio decline, 3He and
nitrogen abundances increase. After the first dredge-up the H-burning
shell is advancing while the convective envelope retreats; the shell
source then enters the chemically homogeneous part of the envelope. Eggleton et al. (2006) and CZ07 have shown that in this situation an inversion of the molecular weight is created by the reaction 3He(3He, 2p)4He in the outer wing of the H-burning shell in models of 1.0 and 0.9 .
This inversion was already predicted by Ulrich (1972).
We confirm an inversion in the mean molecular weight in the outer wing
of the H-burning shell. This inversion occurs after the luminosity bump
on the red giant branch in the 1.0, 1.5 and 2.0
models. The size of the
-inversion depends on the local amount of 3He and in the studied mass range decreases with increasing initial mass
. According to Inequality 2
this inversion causes thermohaline mixing in the radiative buffer
layer, the radiative region between the H-burning shell and the
convective envelope. We emphasize that the extension of the region in
which the mixing process is active is not chosen arbitrarily, but is
calculated self-consistently by the code. This is done at each time
step of the evolutionary calculation by checking which grid points
fulfill condition 2. This
is a major difference between models including thermohaline mixing and
models where the extra mixing is provided by magnetic buoyancy (Denissenkov et al. 2009; Nordhaus et al. 2008; Busso et al. 2007).
Indeed for the latter a self-consistent implementation is still not
available in 1D stellar evolution codes, and the extension of the
extra mixing has to be set arbitrarily.
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Figure 2:
Evolution of the region between the H-burning shell source and the
convective envelope in the RGB phase after the onset of thermohaline mixing for a
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Figure 3:
Evolution of the surface abundance profiles of the 12C/13C ratio (dotted red line) and 3He (dashed green line), and of the luminosity (solid blue line) from the onset of thermohaline mixing up to the AGB for a
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In our 1
model thermohaline mixing develops at the luminosity bump and
transports chemical species between the H-burning shell and the
convective envelope (see Fig. 2). This results in a change of the stellar surface abundances. Figure 3 shows the evolution of the 3He surface-abundance and of the ratio
,
qualitatively confirming the result of EDL06 and CZ07, namely that thermohaline mixing is depleting 3He and lowering the ratio
on the giant branch. As already observed by CZ07, the surface abundance of 16O is not affected because thermohaline mixing does not transport chemical species deep enough the H-burning shell.
Unlike the 1.0
and the 1.5
model, in the 2.0
model thermohaline mixing starts but never connects the H-burning shell
to the convective envelope. This is a direct consequence of the lower 3He abundance, which results in smaller
-inversion and therefore in a slower
thermohaline mixing, according to Eq. (3).
It is surprising that thermohaline mixing, once started in the
outer wing of the H-burning shell, does not spread through the whole
radiative buffer layer. In fact the H-shell burns in a chemically
homogeneous region, meaning that no compositional barrier is expected
to stop the instability. The reason is that the region unstable to
thermohaline mixing moves too slowly in the mass coordinates and never
catches-up with the quicker receding envelope. This situation is shown
in Fig. 4.
As a result no change in the stellar surface composition due
to thermohaline mixing is observed during the RGB phase of the
2.0
model.
In our 3.0
model the H-burning shell never penetrates the homogeneous region left
by the 1DUP. Accordingly thermohaline mixing does not occur during
this phase.
In conclusion our models predict that before the He-core
burning thermohaline mixing is able to change surface abundances only
in stars with
.
During the RGB evolution the choice of
,
roughly corresponding to the prescription of Kippenhahn et al. (1980) for the thermohaline mixing, allows our stellar models to reach helium ignition without having depleted too much 3He in the envelope. The presence of leftover 3He allows thermohaline mixing to play a role also during a later evolutionary phase, as we show below.
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Figure 4:
Evolution of the region between the H-burning shell source and the
convective envelope in the RGB phase after the onset of thermohaline mixing for a
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Figure 5:
Evolution of the internal structure of a
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5 Thermohaline mixing on the horizontal branch and during the AGB stage
While CZ07 and EDL07 investigate thermohaline mixing only during the
RGB, we followed the evolution of our models until the
thermally-pulsing AGB stage (TP-AGB). Indeed a -inversion
is always created if a H-burning shell is active in a chemically
homogeneous layer, the size of the inversion depending on the
local abundance of 3He. This happens not only during the
RGB, but also during the horizontal branch (HB) and the AGB phase.
As a result thermohaline mixing can also operate during these
evolutionary phases (Stancliffe 2010; Cantiello & Langer 2008).
Depending on the efficiency of thermohaline mixing during the RGB, the
can be exhausted at the end of this phase (e.g. in the models of
CZ07). However, stars that avoid extra mixing during the RGB are
observed (Charbonnel & Do Nascimento 1998). For these stars the 3He
reservoir is intact at He ignition, and thermohaline mixing has
the potential to play an important role during the HB and
AGB phases. This is confirmed by the evolutionary calculations
presented in Sects. 5.1 and 5.2.
5.1 Horizontal branch
After the core He-flash, helium is burned in the core, while
a H-burning shell is still active below the convective envelope.
In our 1
model we found that during this phase thermohaline mixing is present
and can spread through the whole radiative buffer layer. This is clear
in Fig. 5
where thermohaline mixing (red, cross hatched region) extends from the
H-shell to the convective envelope also after ignition of the core
He-burning (HB label in the plot). Accordingly surface abundances
change during this phase, as shown in Fig. 3. Here a change of surface abundances is also visible after the luminosity peak corresponding to the core He-flash.
Contrary to the 1
model, in our 1.5 and 2.0
models thermohaline mixing does not change the surface abundances during the HB phase. In the 1.5
model the instability succeeds in connecting the H-shell and the
convective envelope only at the end of the core He-burning (Fig. 6), while in the 2.0
model this is never achieved (Fig. 7).
In the latter case thermohaline diffusion is confined to a tiny layer
on top of the H-burning shell, never spreading through the radiative
layer (the red cross-hatched region in Fig. 7). This is due to a
-barrier, which stops the development of the instability. In Fig. 8 we show the profile of
for the 2.0
model at three successive times during core He-burning: the initial peak created by the reaction 3He(3He, 2p)4He gets smaller, while a dip begins to be visible at slightly higher mass coordinate, i.e. at a lower temperature. This
-barrier is responsible for stopping the instability; this process is discussed in greater detail in Appendix A.
In the 3.0
model the H-burning shell enters for the first time the chemically
homogeneous region after igniting He in the core. However, in this
case also thermohaline mixing does not change the surface abundances
because is not able to connect the H-burning shell with the convective
envelope.
We conclude that in our models thermohaline mixing during the HB changes the surface abundances only in stars with M <
.
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Figure 6:
Evolution of the internal structure of a
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Figure 7:
Evolution of the internal structure of a
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Figure 8:
Profiles of the reciprocal mean molecular weight ( |
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5.2 Asymptotic giant branch
The subsequent evolutionary phase is characterized by two burning shells and a degenerate core. The star burns H in a shell and the ashes of this process feed an underlying He-burning shell. This is referred to as the asymptotic giant branch (AGB) phase.
During the low-luminosity part of the AGB thermohaline mixing works
under the same conditions present in the last part of the HB phase (see
Fig. 5, label AGB). In 1.0
and 1.5
models, thermohaline mixing connects the shell source to the envelope.
As a consequence surface abundances change, as shown for
our 1.0
model in Fig. 3
(label AGB). Similarly to the RGB and HB phases,
no thermohaline mixing is present in models with an initial mass
higher than
.
During the most luminous part of the AGB the He shell periodically experiences thermal pulses (TPs); in stars more massive than
these
thermal pulses are associated with a deep penetration of the convective
envelope, the so-called third dredge-up (3DUP). In our
model we find thermohaline mixing to be present also in the TP-AGB. The
instability propagates through the thin radiative buffer region
(``thin'' in mass coordinates), and reaches the convective
envelope. This situation is illustrated in Fig. 11.
But there thermohaline mixing only leads to negligible changes in
the surface abundances. This because of to the very short timescale of
this evolutionary stage and because most of the
has already been burned in previous evolutionary phases. Overall in our
models we found no impact of thermohaline mixing on the surface
abundances of
and on the
ratio
during the TP-AGB phase. On the other hand thermohaline mixing can
affect the surface abundance of lithium, as we discuss
in Sect. 7.
We want to stress here that the presence and impact on surface
abundances of thermohaline mixing during the TP-AGB, critically depends
on the local
abundance and on the value of the efficiency factor
.
This is because the local
abundance is related to the previous history of mixing, which in turn also depends on the efficiency
of the diffusion process.
We do not know the correct value of
in stellar interiors. Indeed
could also depend on stellar parameters such as rotation, metallicity or magnetic fields (see Sect. 6),
and it could well be that it changes in the same star through different
evolutionary phases. Therefore our predictions for the changes of
surface abundances due to thermohaline mixing, especially during the
TP-AGB phase, are strongly affected by these uncertainties.
Further study is needed to clarify the picture.
6 Other mixing processes
6.1 Other mixing processes in our models
In our
and
models we found that in the relevant layers thermohaline mixing has
generally higher diffusion coefficients than rotational instabilities
and magnetic diffusion. Figure 9
clearly shows that rotational and magnetically induced chemical
diffusion is negligible compared to the thermohaline mixing in our
model. The only rotational instability acting on a shorter timescale is the dynamical shear instability, visible in Fig. 9
as a spike at the lower boundary of the convective envelope. This
instability works on the dynamical timescale in regions of a star where
a high degree of differential rotation is present; it sets in if
the energy that can be gained from the shear flow becomes comparable to
the work which has to be done against the potential for an adiabatic
turn-over of a mass element (``eddy'') (Heger 1998).
However, if present, this instability acts only in a very small
region (in mass coordinates) at the bottom of the convective
envelope. As a result thermohaline mixing is still setting the
timescale for the diffusion of chemical species from the convective
envelope to the H-burning shell.
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Figure 9:
Diffusion coefficients in the region between the H-burning shell and the convective envelope for the
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In models of
and
thermohaline mixing is less efficient due to the lower abundance of 3He.
At the same time rotational instabilities and magnetic diffusion
have bigger diffusion coefficients, mainly because these models have
initial equatorial velocities of 140 and 250
respectively. Figure 10
shows how during core He-burning rotational mixing and magnetic
diffusion become more important than thermohaline mixing in the
model. The radiative buffer layer is dominated by the Eddington-Sweet
circulation, dynamical shear, and magnetic diffusion. Yet the
rotational mixing diffusion coefficient is still too small to allow the
surface abundances to change appreciably in this phase,
in agreement with results from Palacios et al. (2006).
The same conclusion is valid for the magnetic diffusion, which has the
same order of magnitude as the rotational diffusion in the radiative
buffer layer. Our models are calculated with the Kippenhahn et al. (1980) prescription for thermohaline mixing, which implies a smaller diffusion coefficient with respect to that proposed by Ulrich (1972).
As a consequence the result that thermohaline mixing has in
general a higher impact than rotational mixing and magnetic diffusion
in the relevant layers is valid regardless of which of the two
prescriptions was chosen.
6.2 Critical model ingredients
The results described above are obtained with a particular model for rotational mixing and angular momentum transport, for which several assumptions need to be made. Here we discuss the two most important assumptions in the present context. The first assumption is that angular momentum transport in convection zones can be described with a diffusion approximation and a diffusion coefficient derived from the mixing length theory (Sect. 3). The result is near rigid rotation in convection zones. Recent 3D hydrodynamic models of rotating red giant convective zones (Steffen & Freytag 2007; Brun & Palacios 2009) indicate that the picture may be more complex. Brun & Palacios (2009) find radial profiles intermediate between constant angular momentum and constant angular velocity, with a large dependence on the rotation rate of the star. While no general conclusion can easily be drawn from these studies, we may wonder how a reduced angular momentum transport efficiency in the convective envelope might affect our results. While detailed models would be required to exhaustively answer this question, we can expect that a more rapidly rotating base of the convective envelope would lead to less shear, and would thus render shear mixing in the layers below the envelope less relevant.
A second crucial assumption is the adoption of magnetic angular momentum transport according to Spruit (2002). Even though the Spruit-Taylor dynamo has been criticized (Zahn et al. 2007; Denissenkov & Pinsonneault 2007), an effecient angular momentum transport mechanism like the Spruit-Taylor dynamo is clearly needed to understand the observed slow rotation of stellar remnants (Suijs et al. 2008; Heger et al. 2005). While angular momentum transport through gravity waves has been advocated as an interesting alternative (Talon & Charbonnel 2008,2003), it remains to be demonstrated that this mechanism can work to break the rotation of the helium core in the post-main sequence stages of stellar evolution. Therefore, while the reader should be aware of the related uncertainties, using the Spruit-Taylor dynamo at this time appears reasonable.
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Figure 10:
Diffusion coefficients in the region between the H burning shell and the convective envelope for the
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6.3 Interaction of instabilities
The discussion of the interactions of thermohaline motions with the
rotational instabilities and magnetic fields is complex. In this
respect Canuto (1999) argues that shear due to differential rotation decreases the efficiency of thermohaline mixing. Not only Denissenkov & Pinsonneault (2008)
claim that rotation-induced horizontal turbulent diffusion may suppress
thermohaline mixing. This is because horizontal diffusion (molecular
plus turbulent) may change the mean molecular weight of the fluid
element during its motion. They argue that this horizontal diffusion is
able to halt thermohaline mixing. We think this argument is correct in
an ideal situation, in which a single blob of material is crossing an
infinite, parallel slab.
Yet in a star the horizontal turbulence is acting on a shell, which can
be locally approximated to a parallel slab with periodic boundary
conditions in the horizontal direction. This horizontal layer (shell)
is rapidly homogenized by the horizontal turbulence. Fingers trying to
cross this horizontal layer are quickly disrupted and mixed. This
results in a rapid increase of the mean molecular weight
in the shell, so that the region will become unstable to
thermohaline mixing. A new generation of fingers is therefore
expected. But the presence of horizontal turbulence is probably making
fingers an unlikely geometrical configuration: blobs that travel a
small distance before the turbulence is mixing them on a horizontal
layer are more likely. This way thermohaline mixing is not stopped, but
only slowed down. This scenario would favor the Kippenhahn et al. (1980) prescription, which actually predicts blobs traveling a distance comparable to their size.
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Figure 11:
Evolution of the region between the H-burning shell source and the convective envelope during a thermal pulse in a
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Another interesting idea has been proposed by Charbonnel & Zahn (2007a).
They claim that internal magnetic fields can play a stabilizing role,
trying to counteract the destabilizing effect of the inverse
gradient. Their conclusion is that thermohaline mixing can be inhibited by a magnetic field stronger than
104-105 Gauss. But they warn that their analysis ignores both stellar rotation and the spatial variation of B, which results in neglecting any possible instability of the magnetic field itself (e.g., Spruit 1999).
The instability of magnetic fields below the convective envelope of RGB and AGB stars has been discussed by Busso et al. (2007) and Nordhaus et al. (2008). They argue that dynamo-produced buoyant magnetic fields could provide the source of extra mixing in these stars.
7 Lithium-rich giants
Lithium is a fragile element, which is destroyed at temperatures higher than about 3
106 K.
For this reason it is expected that lithium should decrease from
its initial value during the evolution of stars. On the other hand,
observations have shown that about
of giants show strong Li lines (e.g., Brown et al. 1989; Wallerstein & Sneden 1982). Some of these stars even show surface Li-abundances higher than the interstellar values.
For intermediate mass stars a possible solution was proposed by Cameron & Fowler (1971), who showed how a net production of 7Li can be achieved during hot-bottom burning (HBB). During HBB the convective envelope penetrates into the H-shell burning, where 7Be is produced by the pp-chain. In this situation the unstable isotope 7Be can be transported to cooler temperatures by the convective motions, decaying into 7Li in regions of the envelope where the temperature is low enough for lithium to survive. This results in Li-enrichment at the surface.
At solar metallicity stars below
do not experience hot-bottom burning (Forestini & Charbonnel 1997), whereas at Z=0 hot-bottom burning is found down to
(Siess et al. 2002).
For stars avoiding hot-bottom burning, some other mechanism is
needed in order to increase the Li surface-abundance.
A possibility is that some kind of extra mixing connects the
H-burning shell and the convective envelope, which in the literature is
often referred to as the cool bottom process (CBP). The work of Charbonnel & Balachandran (2000)
supports this hypothesis. Indeed they found Li-rich stars to be either
red giants at the luminosity bump or early-AGB stars before the second
dredge-up, in agreement with the idea that some internal mixing
occurs when the H-burning shell enters a homogeneous region.
A lithium production during the RGB evolution is also
supported by the recent observations of Gonzalez et al. (2009), who find lithium enriched red giants at the luminosity bump or at higher luminosities.
Uttenthaler et al. (2007) reported the detection of low-mass, Li-rich AGB stars in the galactic bulge. Interestingly two of the four stars which show surface-Li enhancement present no evidence for third dredge-up, and thermohaline mixing is advocated as a possible source for the extra mixing.
In our calculations we found that the Li surface-abundance is
affected by thermohaline mixing during the evolution of low-mass stars.
While Li is burned during the RGB and HB, thermohaline mixing has the
potential to enhance the Li surface-abundance during the
TP-AGB phase. To show this, we computed stellar evolution
calculations of the TP-AGB phase in 1 and 3
with different values of
.
An example of the evolution of the Li surface-abundance in the 3
model during one thermal pulse is shown in Fig. 12.
Our models qualitatively confirm that this instability can enhance the
surface Li abundances in low-mass AGB stars, even if we can
not quantitatively reproduce the high level of enrichment observed by Uttenthaler et al. (2007). To reach the values of Uttenthaler et al. (2007) a value of
much higher than those proposed by Kippenhahn et al. (1980) and Ulrich (1972) is needed. As discussed in Sect. 5.2, a quantitative study requires a better knowledge of the efficiency parameter for thermohaline mixing
.
The observations of Uttenthaler et al. (2007)
show that only 4 out of 27 galactic bulge stars are Li-enriched.
If thermohaline mixing is the physical process providing the high
Li-enrichment observed, we still have to understand why only 15%
of the sample show this strong enhancement. One possibility is that
these stars did not experience thermohaline mixing in previous
evolutionary phases. This would leave the
reservoir intact, leading to a much more efficient mixing during the TP-AGB phase.
![]() |
Figure 12:
Evolution of Li surface-abundance during one thermal pulse in a 3 |
Open with DEXTER |
This scenario requires a way to prevent the extra mixing during the RGB and HB phases. Charbonnel & Zahn (2007a) have proposed that strong magnetic fields stop thermohaline mixing in those red giants stars that are the descendants of Ap stars. They call these stars ``thermohaline deviant stars''.
Because the fraction of Ap stars relative to A stars (5-10%), the number of red giants that seem to avoid the extra mixing ()
and the observed fraction of Li-enriched AGB stars (15%) are
similar, it may be possible that we are looking at the same group
of stars at different evolutionary stages. If this is the case,
it remains to be understood why the process that inhibits the
mixing during the RGB and HB phases is not at work during
the AGB.
A further complication arises from the observations of Drake et al. (2002),
showing that the incidence of Li-rich giants is much higher among
fast-rotating objects. They consider single-K giants and find that
among rapid rotators (
)
a very large proportion (
)
is Li-rich, in contrast with a very low proportion (
)
of Li-rich stars among the much more common slowly rotating giants.
Thermohaline mixing is not driven by rotational energy, and if any
effect would be expected, it would be a lower efficiency of the
mixing with increasing shear and horizontal turbulence (Denissenkov & Pinsonneault 2008; Canuto 1999).
On the other hand, an increase in the mixing efficiency with the
rotation rate is expected if the physical mechanism behind the extra
mixing is magnetic buoyancy (Denissenkov et al. 2009; Nordhaus et al. 2008; Busso et al. 2007). In this case rotation is necessary to amplify the magnetic field below the convective envelope.
Another possibility is that lithium has an external origin, resulting from accretion and ingestion of planets or a brown dwarf by an expanding red giant (e.g., Siess & Livio 1999b,a). Mass transfer or wind accretion in a binary system is also a possible scenario.
The far-IR excess, which is observed in all fast rotating, Li enriched giants, is another interesting piece of the puzzle (Drake et al. 2002; Reddy & Lambert 2005). While models in which some kind of accretion process occurs could explain the IR excess, the internal production of lithium cannot reproduce these observations (but see Palacios et al. 2001). We refer to Drake et al. (2002) for an accurate review of the proposed mechanism for the formation of Li-rich giants.
8 Conclusion
We qualitatively confirm the results of CL07: thermohaline mixing in low-mass giants is capable
of destroying large quantities of 3He, as well as decreasing the ratio
.
Thermohaline mixing indeed starts when the H-burning shell source moves
into the chemically homogeneous layers established by the first
dredge-up. At solar metallicity we find that this process is
working only in stars with a mass below
.
This result is sensitive to the choice of the
parameter, which regulates the speed of thermohaline mixing.
Our models show further that thermohaline mixing remains important during core He-burning and can also operate on the AGB - including the thermally-pulsing AGB stage. Depending on the efficiency of the mixing process, this can result in considerable lithium enrichment.
Our calculations show that in the relevant layers thermohaline mixing generally has a higher diffusion coefficient than rotational instabilities and magnetic diffusion. However, we cannot address the interaction of thermohaline motions with differential rotation and magnetic fields, for which hydrodynamic calculations are required.
In stellar evolution codes thermohaline mixing is implemented
as a diffusive process. This process acts on a thermal timescale, but
the exact velocity of the motion depends on a parameter
.
This parameter is related to the geometry of the fingers
(or blobs) displacing the stellar material and is still a matter
of debate. The two widely used prescriptions have a parameter
that differs by two orders of magnitude. We used the Kippenhahn et al. (1980) prescription, even though we also investigated the effect of using different values of
in a few calculations. Charbonnel & Zahn (2007b) used a much more efficient thermohaline mixing (Ulrich 1972),
justifying their choice on the basis of laboratory experiments of
thermohaline mixing performed in water, and on the observations of
surface abundances of red giants.
But the physical conditions inside a star are very different from these laboratory experiments, which clearly cannot be used for a quantitative study of this hydrodynamic instability. Moreover it is not clear if thermohaline mixing is the only physical process responsible for the extra mixing, and therefore it is not possible to calibrate its efficiency against the observations.
We argue that is not possible at this stage to firmly identify
thermohaline mixing as the cause of the observed surface abundances in
low-mass giants (Gratton et al. 2000). In particular the long standing
problem cannot be considered as solved.
In agreement with CZ07 we claim that to clarify the picture it would be desirable to have realistic hydrodynamic simulations of thermohaline mixing.
M.C. thanks Steve N. Shore, Maria Lugaro, Onno Pols, Evert Glebbeek, Selma de Mink, Jonathan Braithwaite, Miro Mocák and John Lattanzio for helpful discussions. M.C. acknowledges support from the International Astronomical Union and from the Leids Kerkhoven-Bosscha Fonds.
Appendix A: how to stop thermohaline mixing
For models of
we found two situations in which thermohaline mixing fails to connect the H-burning shell with the convective envelope:
- 1.
- The envelope is receding in mass coordinates and the thermohaline mixing is not fast enough to catch-up. This situation is shown in Fig. 4.
- 2.
- A chain of reactions rising the mean molecular weight can create a barrier that stops the mixing process.


In the first one 3He and 4He produce 7Be that rapidly decays into 7Li. The lithium easily reacts with a proton producing two -particles;
this way the initial molecular weight of 8/9 rises to the
value 4/3. This occurs in the outer wing of the H-burning shell,
at a lower temperature with respect to the region where the mean
molecular weight inversion discussed by EDL06 and CZ07 is present.
As a consequence thermohaline mixing is halted
(see Figs. 7 and 8).
Therefore two sets of reactions play a role in the evolution of
thermohaline mixing in the region between the H-burning shell and the
convective envelope:
As a consequence, the efficiency in starting and stopping thermohaline mixing is regulated by the local abundance of 3He and 4He. The first reaction in the chain A.2 has a lower rate than reaction A.1 at the temperatures in the region of interest. However, 3He (4He,


Note that both scenarios 1. and 2. depend on
,
i.e. on the speed of the mixing process. Increasing the value of
makes thermohaline mixing more difficult to be stopped; therefore the value of the mass threshold depends on the choice of
.
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Footnotes
- ... mass
- During the main sequence of these stars, the pp chain operates partially burning hydrogen to 3He, but not beyond, into a wide zone outside the main energy-producing region. At the end of the core H-burning the first dredge-up mixes this 3He with the stellar envelope. Because the main sequence lifetime is longer for lower mass stars, these are able to produce bigger amounts of 3He.
All Figures
![]() |
Figure 1:
Evolution of the surface abundance of 3He for
|
Open with DEXTER | |
In the text |
![]() |
Figure 2:
Evolution of the region between the H-burning shell source and the
convective envelope in the RGB phase after the onset of thermohaline mixing for a
|
Open with DEXTER | |
In the text |
![]() |
Figure 3:
Evolution of the surface abundance profiles of the 12C/13C ratio (dotted red line) and 3He (dashed green line), and of the luminosity (solid blue line) from the onset of thermohaline mixing up to the AGB for a
|
Open with DEXTER | |
In the text |
![]() |
Figure 4:
Evolution of the region between the H-burning shell source and the
convective envelope in the RGB phase after the onset of thermohaline mixing for a
|
Open with DEXTER | |
In the text |
![]() |
Figure 5:
Evolution of the internal structure of a
|
Open with DEXTER | |
In the text |
![]() |
Figure 6:
Evolution of the internal structure of a
|
Open with DEXTER | |
In the text |
![]() |
Figure 7:
Evolution of the internal structure of a
|
Open with DEXTER | |
In the text |
![]() |
Figure 8:
Profiles of the reciprocal mean molecular weight ( |
Open with DEXTER | |
In the text |
![]() |
Figure 9:
Diffusion coefficients in the region between the H-burning shell and the convective envelope for the
|
Open with DEXTER | |
In the text |
![]() |
Figure 10:
Diffusion coefficients in the region between the H burning shell and the convective envelope for the
|
Open with DEXTER | |
In the text |
![]() |
Figure 11:
Evolution of the region between the H-burning shell source and the convective envelope during a thermal pulse in a
|
Open with DEXTER | |
In the text |
![]() |
Figure 12:
Evolution of Li surface-abundance during one thermal pulse in a 3 |
Open with DEXTER | |
In the text |
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