6 research outputs found

    R-modes of neutron stars with the superfluid core

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    We investigate the modal properties of the rr-modes of rotating neutron stars with the core filled with neutron and proton superfluids, taking account of entrainment effects between the superfluids. The stability of the rr-modes against gravitational radiation reaction is also examined considering viscous dissipation due to shear and a damping mechanism called mutual friction between the superfluids in the core. We find the rr-modes in the superfluid core are split into ordinary rr-modes and superfluid rr-modes, which we call, respectively, ror^o- and rsr^s-modes. The two superfluids in the core flow together for the ror^o-modes, while they counter-move for the rsr^s-modes. For the ror^o-modes, the coefficient κ0limΩ0ω/Ω\kappa_0\equiv\lim_{\Omega\to 0}\omega/\Omega is equal to 2m/[l(l+1)]2m/[l^\prime(l^\prime+1)], almost independent of the parameter η\eta that parameterizes the entrainment effects between the superfluids, where Ω\Omega is the angular frequency of rotation, ω\omega the oscillation frequency observed in the corotating frame of the star, and ll^\prime and mm are the indices of the spherical harmonic function representing the angular dependence of the rr-modes. For the rsr^s-modes, on the other hand, κ0\kappa_0 is equal to 2m/[l(l+1)]2m/[l^\prime(l^\prime+1)] at η=0\eta=0 (no entrainment), and it almost linearly increases as η\eta is increased from η=0\eta=0. The mutual friction in the superfluid core is found ineffective to stabilize the rr-mode instability caused by the ror^o-mode except in a few narrow regions of η\eta. The rr-mode instability caused by the rsr^s-modes, on the other hand, is extremely weak and easily damped by dissipative processes in the star.Comment: 22 pages, 22 figures, accepted for publication in the Astrophysical Journa

    A recent trend in sciences on mantle-derived materials, with special emphases on refertilization, rheology, and ophiolite problems: a report of the Fifth International Conference on Orogenic Lherzolite

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