By A H Mueller

This ebook might be of serious curiosity to complicated scholars and researchers within the quarter of excessive power theoretical physics. Being the main entire and up to date overview quantity on Perturbative QCD, it serves as a really worthwhile textbook or reference e-book. many of the reports during this quantity are the simplest which were written at the topic anyplace.

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1992) Intrinsic Josephson effects in BizSrzCaCuZOg single crystals, Phys. Rev. Leu. 68, 2394-2397 28. H. (1991) Penetration of ac magnetic fields in type-II superconductors, Phys. Rev. Lett. 67, 2219-2222 43 29. Coffey M. and Clem, J. R (1992) Theory of rf magnetic permeability of type-II superconductors in slab geometry with an oblique applied static magnetic field, Phys. B 45,10527-10532 30. , Yeshurun, Y. and Holtzberg, F. (1991) Evidence for surface barriers and their effect on irreversibility and lower critical field measurements in YBaCuO crystals, Phys.

L) then down: this cycle is reversible. ) regime, then a large hysteresis is observed: the dissipation, which had dropped to zero, remains negligible as the field is decreased. 3-c), which is very 37 delicate to determine from other techniques and which is well defined in our measurement. From its value, we have obtained a conservative estimate of the anisotropy parameter yat 60K (-70): this has been published elsewhere [38]. 5. Analysis of the "lock-in transition" We may now analyse in detail how the vortex lattice unlocks from the parallel configuration and evolves towards a tilted lattice with straight effective cores [18-20].

All curves collapse now into a single master curve, but depart from the latter at various angles 9. The arrow locates HcW . 3-c X" data before the low field maximum is reached, now plotted as a function of the parallel component HI/. 3-b). The occurence of this extra dissipation entirely due to a parallel field -henceforward refered to as X"(HI/)- strongly suggests that vortices present in the sample are Josephson vortices which remain locked inbetween the layers as the field is increased from zero at a given angle.

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