Tidal heating of quantum black holes and their imprints on gravitational waves
The characteristic difference between a black hole and other exotic compact objects (ECOs) is the presence of the horizon. The horizon of a classical black hole acts as a one-way membrane. Due to this nature, any perturbation on the black hole must satisfy ingoing boundary conditions at the horizon....
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description | The characteristic difference between a black hole and other exotic compact objects (ECOs) is the presence of the horizon. The horizon of a classical black hole acts as a one-way membrane. Due to this nature, any perturbation on the black hole must satisfy ingoing boundary conditions at the horizon. For an ECO either the horizon is replaced or modified with a surface with nonzero reflectivity. This results in a modification of the boundary condition of the perturbation around such systems. In this work, we study how tidal heating of an ECO gets modified due to the presence of a reflective surface and what implication it brings for the gravitational wave observations. We argue that the position of the reflective surface, ϵ ≳ 10−5, can have an observational impact in extreme mass ratio inspirals. We also discuss a possible degeneracy between ϵ and reflectivity, | R |2, in the context of parameter estimation. |
doi_str_mv | 10.1103/PhysRevD.102.064040 |
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The horizon of a classical black hole acts as a one-way membrane. Due to this nature, any perturbation on the black hole must satisfy ingoing boundary conditions at the horizon. For an ECO either the horizon is replaced or modified with a surface with nonzero reflectivity. This results in a modification of the boundary condition of the perturbation around such systems. In this work, we study how tidal heating of an ECO gets modified due to the presence of a reflective surface and what implication it brings for the gravitational wave observations. We argue that the position of the reflective surface, ϵ ≳ 10−5, can have an observational impact in extreme mass ratio inspirals. We also discuss a possible degeneracy between ϵ and reflectivity, | R |2, in the context of parameter estimation.</description><identifier>ISSN: 2470-0010</identifier><identifier>EISSN: 2470-0029</identifier><identifier>DOI: 10.1103/PhysRevD.102.064040</identifier><language>eng</language><publisher>College Park: American Physical Society</publisher><subject>Black holes ; Boundary conditions ; Gravitation ; Gravitational waves ; Heating ; Horizon ; Parameter estimation ; Perturbation ; Reflectance ; Tidal effects</subject><ispartof>Physical review. 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The horizon of a classical black hole acts as a one-way membrane. Due to this nature, any perturbation on the black hole must satisfy ingoing boundary conditions at the horizon. For an ECO either the horizon is replaced or modified with a surface with nonzero reflectivity. This results in a modification of the boundary condition of the perturbation around such systems. In this work, we study how tidal heating of an ECO gets modified due to the presence of a reflective surface and what implication it brings for the gravitational wave observations. We argue that the position of the reflective surface, ϵ ≳ 10−5, can have an observational impact in extreme mass ratio inspirals. We also discuss a possible degeneracy between ϵ and reflectivity, | R |2, in the context of parameter estimation.</description><subject>Black holes</subject><subject>Boundary conditions</subject><subject>Gravitation</subject><subject>Gravitational waves</subject><subject>Heating</subject><subject>Horizon</subject><subject>Parameter estimation</subject><subject>Perturbation</subject><subject>Reflectance</subject><subject>Tidal effects</subject><issn>2470-0010</issn><issn>2470-0029</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNo9kM1OwzAQhC0EElXpE3CxxDllbSd1fUTlp0gVIFTO0dbZNClp3NpJUd8eowKnnV3NjkYfY9cCxkKAun2rjuGdDvdjAXIMkxRSOGMDmWpIAKQ5_9cCLtkohA1EOQGjhRiwl2VdYMMrwq5u19yVfN9j2_VbvmrQfvLKNRQ4tgXvKqo9r7c7X7dd4K7la4-HuouPro0RX3igcMUuSmwCjX7nkH08Pixn82Tx-vQ8u1skVmrdJTQ1RppSUJlZUlYjSdSKVhIR7aSgKRQmS9FaCyItsrgSFuWq1NqgphTUkN2ccnfe7XsKXb5xvY81Qi7TTBippkpElzq5rHcheCrzWH6L_pgLyH_Y5X_s4kHmJ3bqG8JrZT8</recordid><startdate>20200915</startdate><enddate>20200915</enddate><creator>Datta, Sayak</creator><general>American Physical Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7U5</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0002-4774-0298</orcidid></search><sort><creationdate>20200915</creationdate><title>Tidal heating of quantum black holes and their imprints on gravitational waves</title><author>Datta, Sayak</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c277t-e89929f1ef5ce3c7ae2a73eb2aaac6de80d954accc014d580deadfbf779a7e403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Black holes</topic><topic>Boundary conditions</topic><topic>Gravitation</topic><topic>Gravitational waves</topic><topic>Heating</topic><topic>Horizon</topic><topic>Parameter estimation</topic><topic>Perturbation</topic><topic>Reflectance</topic><topic>Tidal effects</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Datta, Sayak</creatorcontrib><collection>CrossRef</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Physical review. D</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Datta, Sayak</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tidal heating of quantum black holes and their imprints on gravitational waves</atitle><jtitle>Physical review. D</jtitle><date>2020-09-15</date><risdate>2020</risdate><volume>102</volume><issue>6</issue><spage>1</spage><pages>1-</pages><artnum>064040</artnum><issn>2470-0010</issn><eissn>2470-0029</eissn><abstract>The characteristic difference between a black hole and other exotic compact objects (ECOs) is the presence of the horizon. The horizon of a classical black hole acts as a one-way membrane. Due to this nature, any perturbation on the black hole must satisfy ingoing boundary conditions at the horizon. For an ECO either the horizon is replaced or modified with a surface with nonzero reflectivity. This results in a modification of the boundary condition of the perturbation around such systems. In this work, we study how tidal heating of an ECO gets modified due to the presence of a reflective surface and what implication it brings for the gravitational wave observations. We argue that the position of the reflective surface, ϵ ≳ 10−5, can have an observational impact in extreme mass ratio inspirals. We also discuss a possible degeneracy between ϵ and reflectivity, | R |2, in the context of parameter estimation.</abstract><cop>College Park</cop><pub>American Physical Society</pub><doi>10.1103/PhysRevD.102.064040</doi><orcidid>https://orcid.org/0000-0002-4774-0298</orcidid></addata></record> |
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subjects | Black holes Boundary conditions Gravitation Gravitational waves Heating Horizon Parameter estimation Perturbation Reflectance Tidal effects |
title | Tidal heating of quantum black holes and their imprints on gravitational waves |
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