Abstract
Measurements of the isobutyric acid (IBA) concentration in a dilute silica gel, vs that in an IBA and water reservoir in equilibrium with the gel, show that first-order phase transitions occur at 15 and 19 °C, but not at 23 °C. The data show that the coexistence curve of this gel/mixture system is narrow, contained within that of the pure mixture, and lies below a broad region of apparent metastability. The existence of a metastable state above the critical temperature of the gel/mixture system is strikingly similar to the behavior observed for random-field magnets.
- Received 18 June 1996
DOI:https://doi.org/10.1103/PhysRevLett.77.2969
©1996 American Physical Society