Abhijit Chakraborty, Carlos R. Ordóñez, Gustavo Valdivia-Mera
{"title":"Path integral derivation of the thermofield double state in causal diamonds","authors":"Abhijit Chakraborty, Carlos R. Ordóñez, Gustavo Valdivia-Mera","doi":"arxiv-2312.03541","DOIUrl":null,"url":null,"abstract":"In this article, we follow the framework given in the article Physica A, 158,\npg 58-63 (1989) by R. Laflamme to derive the thermofield double state for a\ncausal diamond using the Euclidean path integral formalism, and subsequently\nderive the causal diamond temperature. The interpretation of the physical and\nfictitious system in the thermofield double state arises naturally from the\nboundary conditions of the fields defined on the Euclidean sections of the\ncylindrical background geometry $S^{1}_{\\beta}\\times \\mathbb{R}$, where $\\beta$\ndefines the periodicity of the Euclidean time coordinate and $S^{1}_{\\beta}$ is\nthe one-dimensional sphere (circle). The temperature detected by a static\ndiamond observer at $x=0$ matches with the thermofield double temperature\nderived via this path integral procedure.","PeriodicalId":501275,"journal":{"name":"arXiv - PHYS - Mathematical Physics","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2023-12-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Mathematical Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2312.03541","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
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.