Bibcode
                                    
                            Díaz, A. J.; Khomenko, E.; Collados, M.
    Bibliographical reference
                                    Astronomy and Astrophysics, Volume 564, id.A97, 16 pp.
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                        4
            
                        2014
            
  Journal
                                    
                            Citations
                                    36
                            Refereed citations
                                    36
                            Description
                                    Aims: We study the modification of the classical criterion for
the linear onset and growth rate of the Rayleigh-Taylor instability
(RTI) in a partially ionized (PI) plasma in the one-fluid description by
considering a generalized induction equation.  Methods: The
governing linear equations and appropriate boundary conditions,
including gravitational terms, are derived and applied to the case of
the RTI in a single interface between two partially ionized plasmas. The
boundary conditions lead to an equation for the frequencies in which
some have positive complex parts, marking the appearance of the RTI. We
study the ambipolar term alone first, extending the result to the full
induction equation later.  Results: The configuration is always
unstable because of the presence of a neutral species. In the classical
stability regime, the growth rate is small, since the collisions prevent
the neutral fluid to fully develop the RTI. For parameters in the
classical instability regime, the growth rate is lowered, but the
differences with the compressible MHD case are small for the considered
theoretical values of the collision frequencies and diffusion
coefficients for solar prominences.  Conclusions: The PI modifies
some aspects of the linear RTI instability, since it takes into account
that neutrals do not feel the stabilizing effect of the magnetic field.
For the set of parameters representative for solar prominences, our
model gives the resulting timescale comparable to observed lifetimes of
RTI plumes.
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                        Felipe García