2012
DOI: 10.1103/physrevlett.108.191601
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Strong Coupling Isotropization of Non-Abelian Plasmas Simplified

Abstract: We study the isotropization of a homogeneous, strongly coupled, non-abelian plasma by means of its gravity dual. We compare the time evolution of a large number of initially anisotropic states as determined, on the one hand, by the full nonlinear Einstein's equations and, on the other, by the Einstein's equations linearized around the final equilibrium state. The linear approximation works remarkably well even for states that exhibit large anisotropies. For example, it predicts with a 20% accuracy the isotropi… Show more

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Cited by 140 publications
(252 citation statements)
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References 27 publications
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“…We find that only disturbances in the geometry originating deep in the bulk, very close to the horizon, generate significant nonlinearities. This is broadly consistent with earlier work [8,9]. However, for a very wide variety of initial disturbances, including ones which generate extremely large pressure anisotropies, we find remarkably little nonlinearity in the equilibration dynamics, often below the part-per-mille level.…”
Section: Jhep07(2015)116supporting
confidence: 79%
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“…We find that only disturbances in the geometry originating deep in the bulk, very close to the horizon, generate significant nonlinearities. This is broadly consistent with earlier work [8,9]. However, for a very wide variety of initial disturbances, including ones which generate extremely large pressure anisotropies, we find remarkably little nonlinearity in the equilibration dynamics, often below the part-per-mille level.…”
Section: Jhep07(2015)116supporting
confidence: 79%
“…In this paper, we extend previous work on the dynamics of homogeneous but anisotropic N = 4 SYM plasma [7][8][9]. We examine the influence on the equilibration dynamics of a non-zero global U(1) charge density, or a background magnetic field.…”
Section: Jhep07(2015)116mentioning
confidence: 86%
See 1 more Smart Citation
“…table 2 in appendix E for detail. 9 Therefore, h tr is regular at r ∼ 1 if the other functions are also regular. Finally, we get three dynamical equations for h xx , h rr and h tt .…”
Section: Jhep01(2014)138mentioning
confidence: 99%
“…where 9) defines the other conserved parameters and we set E y = 0. Note that dx i /dt = E x i /E t and therefore the projection of null geodesics onto flat (constant-r) slices follows straight lines.…”
Section: Jhep01(2014)138mentioning
confidence: 99%