Numerical calculation of the combinatorial entropy of partially ordered ice
arXiv:0707.1725 · doi:10.1063/1.2800002
Abstract
Using a one-parameter case as an example, we demonstrate that multicanonical simulations allow for accurate estimates of the residual combinatorial entropy of partially ordered ice. For the considered case corrections to an (approximate) analytical formula are found to be small, never exceeding 0.5%. The method allows one as well to calculate combinatorial entropies for many other systems.
Extended version: 7 pages, 10 figures (v1 is letter-type version)
References in corpus (6)
- An efficient, multiple range random walk algorithm to calculate the density of states
- Multicanonical Ensemble: A New Approach to Simulate First-order Phase Transitions
- Effect of pressure on the phase behavior and structure of water confined between nanoscale hydrophobic and hydrophilic plates
- A New Approach to Spin Glass Simulations
- Multicanonical Simulations Step by Step
- Residual Entropy of Ordinary Ice from Multicanonical Simulations
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