Abstract
The phase diagram of solid oxygen in the magnetic-field-temperature () plane is revealed by magnetization and magnetotransmission measurements. The high-field phase of solid oxygen, which we term the phase, is induced at the temperature below 42 K. The transition fields at the and transitions are almost temperature independent, with the phase boundary being very steep. This phase boundary indicates that the entropy change is very small at the and transitions, in contrast to the entropy-driven transition at zero field. We argue that the phase differs from the high-temperature phase in terms of entropy; the molecular rotation is inhibited in the phase, whereas permitted in the phase. This finding consolidates the novelty of the phase.
- Received 15 May 2015
DOI:https://doi.org/10.1103/PhysRevB.92.064109
©2015 American Physical Society