arXiv · 1401.1492
Indication for unsmooth horizon induced by quantum gravity interaction
Abstract
The angular ADM reduction of the BTZ spacetime yields a Liouville-type theory. The analysis of the resulting Liouville theory naturally leads to identification of the stretched horizon. The dynamics associated with the stretched horizon has a feature that seems consistent with the unsmooth horizon; the quantum gravity effects are essential for the unsmoothness. We show that the "anomaly" term in the stress-energy tensor is responsible for the Planck scale energy experienced by an infalling observer.
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I. Y. Park. 2014-10-29. Indication for unsmooth horizon induced by quantum gravity interaction. https://doi.org/10.1140/epjc%2Fs10052-014-3143-5
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