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Concept of temperature in multi-horizon spacetimes: Analysis of Schwarzschild-De Sitter metric

机译:多地平线时空中的温度概念:Schwarzschild-De Sitter度量分析

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摘要

In case of spacetimes with single horizon, there exist several well-established procedures for relating the surface gravity of the horizon to a thermodynamic temperature. Such procedures, however, cannot be extended in a straightforward manner when a spacetime has multiple horizons. In particular, it is not clear whether there exists a notion of global temperature characterizing the multi-horizon spacetimes. We examine the conditions under which a global temperature can exist for a spacetime with two horizons using the example of Schwarzschild-De Sitter (SDS) spacetime. We systematically extend different procedures (like the expectation value of stress tensor, response of particle detectors, periodicity in the Euclidean time etc.) for identifying a temperature in the case of spacetimes with single horizon to the SDS spacetime. This analysis is facilitated by using a global coordinate chart which covers the entire SDS manifold. We find that all the procedures lead to a consistent picture characterized by the following features: (a) In general, SDS spacetime behaves like a non-equilibrium system characterized by two temperatures. (b) It is not possible to associate a global temperature with SDS spacetime except when the ratio of the two surface gravities is rational (c) Even when the ratio of the two surface gravities is rational, the thermal nature depends on the coordinate chart used. There exists a global coordinate chart in which there is global equilibrium temperature while there exist other charts in which SDS behaves as though it has two different temperatures. The coordinate dependence of the thermal nature is reminiscent of the flat spacetime in Minkowski and Rindler coordinate charts. The implications are discussed.
机译:在具有单个地平线的时空的情况下,存在几种完善的程序来将地平线的表面重力与热力学温度相关联。但是,当时空具有多个视野时,无法以简单的方式扩展此类过程。特别是,尚不清楚是否存在表征多水平时空的全球温度的概念。我们以Schwarzschild-De Sitter(SDS)时空为例,研究存在两个水平的时空存在全球温度的条件。我们系统地扩展了不同的过程(例如应力张量的期望值,粒子检测器的响应,欧几里得时间的周期性等),以在单层时空到SDS时空的情况下识别温度。通过使用覆盖整个SDS流形的全局坐标图可以简化此分析。我们发现,所有过程都会导致具有以下特征的图像一致:(a)通常,SDS时空的行为类似于以两个温度为特征的非平衡系统。 (b)不可能将全球温度与SDS时空相关联,除非两个表面重力的比率是合理的(c)即使两个表面重力的比率是合理的,热性质也取决于所使用的坐标图。存在一个全局坐标图,其中存在全局平衡温度,而存在其他图,其中SDS表现为好像它具有两个不同的温度。热性质的坐标依赖性使人联想到Minkowski和Rindler坐标图中的平面时空。讨论了含义。

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