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Published December 2000 | Accepted Version + Published
Journal Article Open

Deformations of accreting neutron star crusts and gravitational wave emission

Abstract

Motivated by the remarkably narrow range of measured spin frequencies of ∼20 accreting (and weakly magnetic) neutron stars in the Galaxy, Bildsten conjectured that their spin-up had been halted by the emission of gravitational waves. If so, then the brightest persistent X-ray source on the sky, Scorpius X-1, should be detected by gravitational wave interferometers within 10 years. Bildsten pointed out that small non-axisymmetric temperature variations in the accreted crust will lead to 'wavy' electron capture layers, and the resulting horizontal density variations near e− capture layers create a mass quadrupole moment. Neglecting the elastic response of the crust, Bildsten estimated that even e− capture layers in the thin outer crust can develop the quadrupole necessary to balance accretion torque with gravitational waves, Q₂₂ ∼ 10³⁷ -10³⁸ g cm⁻² for accretion rates Ṁ ∼ 10⁻¹⁰-2x10⁻⁸ M_⊙ yr⁻¹. We present a full calculation of the crust's elastic adjustment to the density perturbations induced by the temperature-sensitive e− capture reactions. We find that, due to the tendency of the denser material to sink rather than spread sideways, neglecting the elastic response of the crust overestimates, by a factor of 20–50, the Q₂₂ that results from a wavy capture layer in the thin outer crust. However, we find that this basic picture, when applied to capture layers in the deep inner crust, can still generate Q₂₂ in the necessary range, as long as there are ≲5 per cent lateral temperature variations at densities in excess of 10¹² g cm−³, and as long as the crustal breaking strain is high enough. By calculating the thermal flow throughout the core and the crust, we find that temperature gradients this large are easily maintained by asymmetric heat sources or lateral composition gradients in the crust. If the composition or heating asymmetries are independent of the accretion rate, then for Ṁ ≲ 5x10⁻¹⁰-2x10⁻⁹ M_⊙ yr⁻¹ the induced quadrupole moments have approximately the same scaling, ∝M¹/², as that necessary to balance the accretion torque at the same spin frequency for all Ṁ. Temperature gradients in the deep crust lead to a modulation in the thermal emission from the surface of the star that is correlated with Q₂₂. In addition, a ∼0.5 per cent lateral variation in the nuclear charge-to-mass ratio in the crust will also result in a Q₂₂ sufficient to halt spin-up from accretion even in the absence of a lateral temperature gradient. We also derive a general relation between the stresses and strains in the crust and the maximum quadrupole moment they can generate. We show, under quite general conditions, that maintaining a Q₂₂ of the magnitude necessary to balance the accretion torque requires a dimensionless strain σ ∼ 10⁻² at near-Eddington accretion rates, of order the breaking strain of conventional materials. This leads us to speculate that accreting neutron stars reach the same equilibrium spin because they all are driven to the maximum Q₂₂ that the crust can sustain.

Additional Information

© 2000 RAS, MNRAS. Accepted 2000 July 25. Received 2000 June 7; in original form 2000 January 4. We thank Andrew Cumming, Chris McKee and Kip Thorne for many initial discussions. Ed Brown provided much assistance with the construction and cross-checking of our thermal models. Patrick Brady shared his notes on normalizations and detectability of pulsar GW signals. D. I. Jones pointed out an error in our treatment of NS wobble, and suggested the outlines of the correct answer. GU acknowledges the Fannie and John Hertz foundation for fellowship support. This research was supported by NASA via grants NAG5-4093, NAG5-8658 and NAGW-4517, and by the National Science Foundation under Grant No. PHY94-07 194. LB is a Cottrell Scholar of the Research Corporation.

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August 19, 2023
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