1. Shear energy dissipation and stellar structure
Binary stars whose rotation angular velocity differs from the instantaneous orbital angular velocity undergo oscillatory motions that induce differential rotation (Koenigsberger et al. Reference Koenigsberger, Moreno and Langer2021). In the presence of viscous turbulence, a fraction of the energy involved in the shearing motions can be converted into heat. This is an ingredient generally neglected in stellar structure calculations. In this paper we present results of an experiment to determine the effect on its structure of injecting heat into the outer layers of a massive star.
The Modules for Experiments in Stellar Astrophysics (MESA) spherically symmetric stellar evolution code (version 12778, Paxton et al. Reference Paxton2015) was used to evolve a binary system with ZAMS masses 186
$+$
186
$M_\odot$
, initial orbital period
$P_0=2.8$
d and SMC metallicity up to an age of 0.729 Myr, at which time an estimate of the internal tidal shear energy dissipation rate at several depths was injected. At this age, partway through the main sequence, the stellar mass is 162.5
$M_\odot$
, the radius is 17.66
$R_\odot$
, and the orbital period is 3.48 d.
The energy dissipation rate
$\dot{E}(r,\theta,\phi)$
was calculated in a 3D grid with the TIDESnvv codeFootnote † (Moreno et al. Reference Moreno, Koenigsberger and Harrington2011; Koenigsberger & Estrella-Trujillo Reference Koenigsberger and Estrella-Trujillo2024), assuming a polytrope with index 2.7, which approximates the internal structure of the MESA model at 0.729 Myr. The perturbed star was assumed to be initially rotating with a uniform, supersynchronous rotation rate
$\omega_\mathrm{rot}$
such that
$\omega_\mathrm{rot}/\Omega_\mathrm{orb}=1.4$
, where
$\Omega_\mathrm{orb}$
is the orbital angular velocity at periastron. The TIDESnvv calculation was performed for 10 layers, with radii as listed in column 1 of Table 1. The total
$\dot{E}$
value in each layer was averaged over the orbital cycle, interpolated to the MESA radial grid, and activated when the model reached an age of 0.729 Myr.
Results from the TIDESnvv calculation.

Table 1 Long description
A table with 10 rows and 6 columns comparing various parameters across different layers of a star. The columns are labeled as follows: R layer (solar radii), nu (viscosity in cm^2/s), t diss (dissipation time in years), tau sync (synchronization time in years), and E (energy dissipation rate in erg/s/layer). The table lists values for each parameter across different layers. For example, Row 1: R layer 7.59, nu 8.4 x 10^13, t diss 105.3, tau sync 1.2 x 10^9, E 1.9 x 10^35. Row 2: R layer 8.65, nu 1.5 x 10^14, t diss 79.3, tau sync 2.9 x 10^8, E 1.8 x 10^36.
Notes:
$r_\mathrm{layer}$
is the midpoint of each layer modeled.
$\left\lt\nu\right\gt$
is the turbulent viscosity average over the layer and over an orbital cycle, and is computed as
$\nu=\lambda \ell_t \Delta u_l$
, where
$\lambda$
is the fraction of local kinetic energy converted into heat,
$\ell_t$
is the characteristic length, here taken to be the width of the layers, and
$\Delta u_t$
is the relative velocity of volume elements with respect to their neighbors.
$\left\lt\dot{E}\right\gt$
is the tidal shear energy dissipation rate in each layer, averaged over orbital cycle, assuming
$\lambda=1$
(see Koenigsberger & Estrella-Trujillo Reference Koenigsberger and Estrella-Trujillo2024, for details). The synchronization timescale for each layer is
$\frac{1}{\tau_\mathrm{sync}} = \frac{1}{t_\mathrm{diss}} \frac{(\Omega-\omega)}{\Omega}q^2 \frac{Mr^2}{I}\left(\frac{r}{a}\right)^6$
, where
$t_\mathrm{diss}$
=
$r^2/\left\lt\nu\right\gt$
, I is the moment of inertial and a is the orbital separation (Zahn Reference Zahn2008).
Figure 1 shows the equatorial radius
$R_1$
, total luminosity
$L_1$
, mass-loss rate
$\dot{M}_1$
and total mass
$M_1$
as a function of time of the heated model, compared to the standard model. A sharp jump in
$R_1$
,
$L_1$
, and
$\dot{M}_1$
is observed in the heated model as the stellar structure adjusts to the extra energy in its outer layers, and these parameters remain high during the next
$\sim1$
Myr. The mass-loss rate increases because it depends directly on the luminosity (Vink et al. Reference Vink, de Koter and Lamers2001; Brott et al. Reference Brott2011). As a consequence of the larger mass-loss rate, the total mass of the star is reduced with respect to the standard model. Thus, we conclude that heat injection in a MESA massive-star binary model causes an increase in mass-loss rate, equatorial radius and luminosity with respect to a standard model.
Evolution of radius, luminosity, mass-loss rate, and mass as function of age for the tidally-heated model (red) and the standard model.

2. Implications and conclusions
TIDESnvv computes a turbulent viscosity
$\nu_t=\lambda \ell_t \Delta u_l$
at each timestep of the calculation using the instantaneous velocity of each volume element relative to its neighboring elements
$\Delta u_l$
and the element characteristic size
$\ell$
.
$\nu_t$
is a crucial ingredient in the calculation of synchronization timescales
$\tau_\mathrm{sync}$
.
The average
$\nu_t$
value in each layer of our model is listed in column 2 of Table 1 and the resulting values of
$\tau_\mathrm{sync}$
, calculated using the expression given by Zahn (Reference Zahn2008), in column 4 of this table. Whereas the surface layers synchronize with the orbital motion on short timescales, the timescales for the inner layers exceed the main sequence lifetime. Hence, the tidal perturbations due to asynchronous rotation persist throughout most of the lifetime of the star.
Our values of
$\tau_\mathrm{sync}$
are lower limits because in the calculation for this experiment we set
$\lambda=1$
. This proportionality factor
$\lambda\in[0,1]$
represents the fraction of kinetic energy that is dissipated and converted into heat, and in general,
$\lambda\lt1$
. A smaller
$\nu_t$
implies longer synchronization times. Thus, from an observational standpoint, the surface equatorial velocity may be in corotation but deeper layers may not be. As a consequence, the entire stellar structure may differ from that of a single-star model and several modes of stellar oscillations may be active.
There are several caveats to our results. Tidal perturbations are aspherical, with the largest amplitudes generally occurring around the equatorial latitudes. However, MESA calculates the 1D, spherically symmetric stellar structure, so we have adopted the average tidal shear energy dissipation over an entire shell for input into MESA. In reality, the actual values in the equator are significantly larger that in the poles, an effect that has unknown consequences on the stellar structure. Also, our turbulent viscosities are estimated using a simplistic formulation and a refinement is required. Finally, it is not clear how tidal perturbations interact with surface convective layers, a phenomenon that requires further investigation.
3. Acknowledgements
We gratefully acknowledge the work of Edmundo Moreno in writing the TIDES codes and the support from UNAM PAPIIT grant IN105723.



