Fang, Hua and Lovelace, Geoffrey (2005) Tidal coupling of a Schwarzschild black hole and circularly orbiting moon. Physical Review D, 72 (12). Art. No. 124016. ISSN 05562821. http://resolver.caltech.edu/CaltechAUTHORS:FANprd05

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Abstract
We describe the possibility of using the laser interferometer space antenna (LISA) 's gravitationalwave observations to study, with high precision, the response of a massive central body (e.g. a black hole or a soliton star) to the tidal gravitational pull of an orbiting, compact, smallmass object (a white dwarf, neutron star, or smallmass black hole). Motivated by this LISA application, we use firstorder perturbation theory to study tidal coupling for a special, idealized case: a Schwarzschild black hole of mass M, tidally perturbed by a "moon" with mass µ<<M in a circular orbit at a radius b>>M with orbital angular velocity Omega. We investigate the details of how the tidal deformation of the hole gives rise to an induced quadrupole moment [script I]ij in the hole's external gravitational field at large radii, including the vicinity of the moon. In the limit that the moon is static, we find, in Schwarzschild coordinates and ReggeWheeler gauge, the surprising result that there is no induced quadrupole moment. We show that this conclusion is gauge dependent and that the static, induced quadrupole moment for a black hole is inherently ambiguous, and we contrast this with an earlier result of Suen, which gave, in a very different gauge, a nonzero static induced quadrupole moment with a sign opposite to what one would get for a fluid central body. For the orbiting moon and the central Schwarzschild hole, we find (in agreement with a recent result of Poisson) a timevarying induced quadrupole moment that is proportional to the time derivative of the moon's tidal field, [script I]ij=(32/45)M6[script E]dotij and that therefore is out of phase with the tidal field by a spatial angle pi/4 and by a temporal phase shift pi/2. This induced quadrupole moment produces a gravitational force on the moon that reduces its orbital energy and angular momentum at the same rate as the moon's tidal field sends energy and angular momentum into the hole's horizon. As a partial analog of a result derived long ago by Hartle for a spinning hole and a static distant companion, we show that the orbiting moon's tidal field induces a tidal bulge on the hole's horizon, and that the rate of change of the horizon shape (i.e. the horizon shear) leads the perturbing tidal field at the horizon by an angle 4MOmega. We prefer to avoid introducing an ingoing null geodesic, as Hartle did in his definition of the phase shift, because the moon is in the central body's near zone (b<<1/Omega) and thus should interact with the horizon instantaneously, not causally. We discuss the implications of these results for LISA's future observations of tidal coupling, including the inappropriateness of using the concepts of tidal polarizability and tidal lag or lead angle, for the massive central body, when discussing LISA's observations.
Item Type:  Article 

Additional Information:  ©2005 The American Physical Society (Received 31 May 2005; published 16 December 2005) We are grateful to Kip Thorne for suggesting this problem and for his encouragement and advice, and to Yasushi Mino for helpful discussions. This research was supported in part by NASA Grants No. NAG512834 and No. NAG510707 and NSF Grant No. PNY0099568. We used MATHEMATICA and MAPLE to verify some of the equations in this paper. 
Record Number:  CaltechAUTHORS:FANprd05 
Persistent URL:  http://resolver.caltech.edu/CaltechAUTHORS:FANprd05 
Alternative URL:  http://dx.doi.org/10.1103/PhysRevD.72.124016 
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ID Code:  2025 
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Deposited On:  02 Mar 2006 
Last Modified:  26 Dec 2012 08:47 
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