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Two-dimensional O(3) model coupled to two-dimensional quantum gravity

C. F. Baillie

D. A. Johnston*

  • Computer Science Department, University of Colorado, Boulder, Colorado 80309

  • Laboratoire de Physique Théorique et Particules Elémentaires, Universite Paris Sud, Batiment 211, F-91405 Orsay, France
  • Department of Mathematics, Heriot-Watt University, Edinburgh, EH14 4AS, Scotland

  • *Address from September 1993 to September 1994.

Phys. Rev. D 49, R603(R) – Published 15 January, 1994

DOI: https://doi.org/10.1103/PhysRevD.49.R603

Abstract

It has been suggested that the peak in the specific heat observed numerically for random surface actions with extrinsic curvature on dynamical lattices might be the result of a low mass bound state in an asymptotically free theory, rather than the signal for a real phase transition. The O(3) model on a fixed lattice displays just such behavior, but in general peaks appear to be weakened when the models concerned are put on dynamical lattices (i.e., coupled to two-dimensional quantum gravity). We therefore perform simulations of the O(3) model on dynamical φ3 graphs to see if there is still a peak in the specific heat and compare the results with those on fixed lattices.

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