Path integral derivation of the thermofield double state in causal diamonds

Abhijit Chakraborty, Carlos R. Ordóñez, Gustavo Valdivia-Mera
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Abstract

In this article, we follow the framework given in the article Physica A, 158, pg 58-63 (1989) by R. Laflamme to derive the thermofield double state for a causal diamond using the Euclidean path integral formalism, and subsequently derive the causal diamond temperature. The interpretation of the physical and fictitious system in the thermofield double state arises naturally from the boundary conditions of the fields defined on the Euclidean sections of the cylindrical background geometry $S^{1}_{\beta}\times \mathbb{R}$, where $\beta$ defines the periodicity of the Euclidean time coordinate and $S^{1}_{\beta}$ is the one-dimensional sphere (circle). The temperature detected by a static diamond observer at $x=0$ matches with the thermofield double temperature derived via this path integral procedure.
因果钻石中热场双态的路径积分推导
在这篇文章中,我们按照拉弗兰梅(R. Laflamme)在文章《物理学A》158,第58-63页(1989年)中给出的框架,利用欧几里得路径积分形式主义推导出因果钻石的热场双重态,并随后推导出因果钻石温度。对热场双重态中的物理和虚构系统的解释自然来自于在圆柱背景几何$S^{1}_\{beta}\times \mathbb{R}$的欧几里得截面上定义的场的边界条件,其中$\beta$定义了欧几里得时间坐标的周期性,$S^{1}_{\beta}$是一维球体(圆)。静态金刚石观测器在 $x=0$ 时检测到的温度与通过该路径积分过程得出的热场双温相匹配。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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