Effect of equatorial line nodes on upper critical field and London penetration depth
arXiv:1405.2359 · doi:10.1103/PhysRevB.90.100507
Abstract
The upper critical field and its anisotropy are calculated for order parameters with line nodes at equators, , of the Fermi surface of uniaxial superconductors. It is shown that characteristic features found in Fe-based materials -- a nearly linear in a broad domain, a low and increasing on warming anisotropy -- can be caused by competing effects of the equatorial nodes and of the Fermi surface anisotropy. For certain material parameters, may change sign on warming in agreement with recorded behavior of FeTeS system. It is also shown that the anisotropy of the penetration depth decreases on warming to reach at in agreement with data available. For some materials may change on warming from at low s to at high s.
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