On the transition of a monocristalline tin sphere from the supraconductive into the non-supraconductive state
β Scribed by W.J. De Haas; O.A. Guinau
- Publisher
- Elsevier Science
- Year
- 1936
- Weight
- 518 KB
- Volume
- 3
- Category
- Article
- ISSN
- 0031-8914
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β¦ Synopsis
The transition from the s u p r a c o n d u c t i v e state to the non-supraconductive state of monocrystalline spheres of tin has been studied. First the t e m p e r a t u r e was held constant and a magnetic field applied, the intensity of which was gradually raised until s u p r a c o n d u c t i v i t y was entirely disturbed. The field was determined A ) on the pole of the sphere, B) on its equator, C) in a space between two hemispheres, D) in the space round the sphere, E) in a canal, parallel to the lines of force, F) in a canal perpendicular to them. The results can be described by ascribing to the sphere an a p p a r e n t permeability, equal to zero as long as the applied fieldstrength is lower t h a n ~ of the field which disturbs s u p r a c o n d u c t i v i t y entirely. This permeability zero must however be caused by a single current on the surface of the sphere and not by areal perfect diamagnetism of the material. The permeability increase s linearly with the difference of the applied fieldstrength and ~ of the critical fieldstrength, until it reaches the value one, when the applied fieldstrength reaches the critical one. F r o m thereon s u p r a c o n d u c t i v i t y is entirely disturbed and the " permeability remains equal to one. The field penetrates at ~ of the critical fieldstrength t h r o u g h o u t the sphere at once. A possible difference between the critical fieldstrengths, as deduced from these experiments and those, deduced from the measurements of the resistance of monocrystalline wires in a longitudinal field is discussed.
A second t y p e of transition has been studied. Here the external field remains constant and the t e m p e r a t u r e is raised. Until the critical fieldstrength is lowered so far t h a t the external field becomes ~ of it, neither on the pole nor in the space between the two hemispheres a field is found. The field on the e q u a t o r remains equal in t h a t i n t e r v a l to ~ the applied field. When the applied field is higher than ~ of the critical field, the field on the pole and in the space between the hemispheres increases, t h a t on the e q u a t o r decreases and this is always equal to the critical value at the given t e m p e r a t u r e . The sphere behaves first as a body with a permeability equal to zero, which increases linearly to one in the interval of transition.
π SIMILAR VOLUMES
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