We probe, using a model system, elastic and kinetic energies for sheared
granular materials. For large enough P/Ey (pressure/Young's modulus) and
P/ρv2 (P/kinetic energy density) elastic dominates kinetic energy, and
energy fluctuations become primarily elastic in nature. This regime has likely
been reached in recent experiments. We consider a generalization of the
granular temperature, Tg, with both kinetic and elastic terms and that
changes smoothly from one regime to the other. This Tg is roughly consistent
with a temperature adapted from equilibrium statistical mechanics.Comment: 4 pages, 4 figure