Abstract
The low-temperature behavior of the a-b plane penetration depth, , is a probe of the pairing state in . A group-theoretic analysis shows that in orthorhombic or tetragonal crystals all singlet pairing states other than ‘‘s wave’’ would lead to Δ(T)==(T)-(0)∼T. In contrast, for an isotropic system, there are combinations of singlet pairing states and field directions that would give rise to Δλ(T)∼. We reanalyze the surface impedance data of Fiory et al. [Phys. Rev. Lett. 61, 1419 (1988)], and show that these data exhibit neither a BCS temperature dependence nor a linear temperature dependence at low temperature, but instead follow Δ(T)∼. This behavior is probably not intrinsic, and possible explanations are discussed.
- Received 10 July 1990
DOI:https://doi.org/10.1103/PhysRevB.43.2778
©1991 American Physical Society