从时空热力学到韦尔横向引力

Ana Alonso-Serrano, Luis J. Garay, Marek Liška
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引用次数: 0

摘要

自相互作用引力子存在两种一致的理论:广义相对论和韦尔横向引力。后者的经典解与广义相对论相同,但局部对称性不同。我们认为,韦尔横向引力也自然产生于热力学论证。特别是,我们证明了局部因果钻石的热力学平衡与强等价原理编码了韦尔反引力的引力动力学,而不是广义相对论。我们以一种自洽的方式获得了这一结果,验证了我们最初假设的有效性,即熵与面积之间的比例关系以及韦尔横向引力中不同版本的等效原理。此外,我们将韦尔横向引力运动方程的热力学推导扩展到一类具有相同局部对称性的修正引力理论。为此,我们使用了这类理论中沃尔德熵的一般表达式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
From spacetime thermodynamics to Weyl transverse gravity
There exist two consistent theories of self-interacting gravitons: general relativity and Weyl transverse gravity. The latter has the same classical solutions as general relativity, but different local symmetries. We argue that Weyl transverse gravity also naturally arises from thermodynamic arguments. In particular, we show that thermodynamic equilibrium of local causal diamonds together with the strong equivalence principle encodes the gravitational dynamics of Weyl transverse gravity rather than general relativity. We obtain this result in a self-consistent way, verifying the validity of our initial assumptions, i.e. the proportionality between entropy and area and the different versions of the equivalence principle in Weyl transverse gravity. Furthermore, we extend the thermodynamic derivation of the equations of motion from Weyl transverse gravity to a class of modified theories of gravity with the same local symmetries. For this purpose, we employ the general expression for Wald entropy in such theories.
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