W0053
Magnetic Ordering of the Rare Earth Ions R3+ in R2Ba4Cu7O15-d (R=Er, Dy). G. Böttger (a), P. Fischer (a), P. Allenspach (a), A. Dönni (b), Y. Aoki (c), H. Sato (c), (a) Laboratory for Neutron Scattering, ETH Zurich & PSI, Paul Scherrer Institute, CH - 5232 Villigen PSI, Switzerland, (b) Dept. of Physics, Niigata University, Ikarashi-Ninomachi 8050, Niigata 950-21, Japan, (c) Dept. of Physics, Faculty of Science, Tokyo Metropolitan University, Japan
The polycrystalline samples of R2Ba4Cu7O15-d (R=Er, Dy; 0.05<=d<=0.7) prepared by a sol-gel-method have been investigated by X-ray and neutron diffraction, specific heat and magnetic susceptibility measurements. The high superconducting transition temperatures Tc=89 K for Er2Ba4Cu7O14.92 and Tc=91 K for Dy2Ba4Cu7O14.95 indicate a good sample quality. Specific heat measurements for Er2Ba4Cu7O15-d show a magnetic phase transition at TN=0.54 K for d~0.1 and at TN=0.50 K for d~0.7. For the first time we observed a quasi 3D antiferromagnetic order of the Er3+ ions in Er2Ba4Cu7O14.92 using neutron diffraction. The magnetic Er moments are oriented parallel to the b-axis. While the specific heat data of Er2Ba4Cu7O14.92 can be interpreted with an anisotropic 2D-Ising model, the specific heat data of Er2Ba4Cu7O14.3 can only be understood by assuming two different types of magnetic clusters to be present in this sample. Furthermore, the importance of dipolar interaction and superexchange for the observed magnetic ordering will be discussed.