Abstract
The existence of a monocrystal of vortices in a monocrystalline niobium sample was reported for the first time by Thorel and Simon.1 We use this property to map the field around each vortex core by Fourier transformation of the Bragg peak integrated intensity, described elsewhere by Schelten and co-workers.2 The sample is a niobium monocrystal (7 × 25 × 9 mm) with a resistivity ratio of 80. The orientation of the vortex lattice with respect to the niobium crystalline axis is shown in Fig. 1.
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References
P. Thorel and Y. Simon, in Proc. 12th Intern. Conf. Low Temp. Phys., 1970, Academic Press of Japan, Tokyo (1971), p. 477.
D. Cribier, Y. Simon, and P. Thorel, Phys. Rev. Lett. 28, 1370 (1972).
P. Thorel, R. Kahn, Y. Simon, and D. Cribier, J. de Physique (to be published).
J. Schelten, H. Ullmaier, and G. Lippmann, Discussion Meeting on the Structure of the Mixed State, Jiilich, April 24, 1972 (unpublished); this volume.
A.A. Abrikosov, Zh. Eksperim. i. Teor. Fiz. 5, 1174 (1957).
J.M. Delrieu, J. Low Temp. Phys. 6, 197 (1972).
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Kahn, R., Thorel, P. (1974). Neutron Diffraction Test of Type II Theories in Relation to Temperature. In: Timmerhaus, K.D., O’Sullivan, W.J., Hammel, E.F. (eds) Low Temperature Physics-LT 13. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-2688-5_9
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DOI: https://doi.org/10.1007/978-1-4684-2688-5_9
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