Abstract
We report on transport measurements of single crystals with different oxygen contents in the geometry , . Our data show that the vortices become confined between the Cu-O planes below a well-defined temperature at which the effective size of the vortex core is approximately equal to the period of the Cu-O layers. This confinement strongly increases the vortex liquid freezing temperature. A new melting line is found separating a vortex liquid and a smectic phase, which shows an oscillatory field dependence reflecting differences between commensurate and incommensurate smectic states.
- Received 26 June 2000
DOI:https://doi.org/10.1103/PhysRevLett.85.4594
©2000 American Physical Society