Further study of the cation ordering in phengite 3T by neutron powder diffraction
Mineralogical Magazine 64:1 (2000) 11-18
Abstract:
Phengite 3T (Dora-Maira massif, Italian western Alps), with chemical composition K0.96Na0.01Al1.44Mg0.56(Si3.59Al0.41)O10(OH)2 has been investigated using powder neutron diffraction, at the ILL (Institut Laue-Langevin) Facility, on the D2B diffractometer. Data sets were collected at 293 and 873 K, and the present results are compared with those obtained previously using the time-of-flight (TOF) technique, on the same compound. In the octahedral sheet, Al tends to order into the M2 site, in accordance with the measurements mentioned above, whereas the Al/Si tetrahedral ordering we observe (i.e. Si fully into T1 site) is at variance with that determined previously. These discrepancies are ascribed to the presence of talc impurities in the sample used previously (~6 wt.%), which affected the results obtained.Mechanical against chemical pressure in the Y(Ba1-xSrx)2Cu3O7-d system
Physica C Superconductivity and Its Applications 341-348:PART 1 (2000) 375-378
Abstract:
The structural refinement of YSrNeutron scattering studies of phase segregation in Pr0.7 Ca0.3 MnO3
Physica B: Condensed Matter 276-278 (2000) 551-553
Abstract:
The phase segregation in the narrow-bandwidth manganite Pr0.7Ca0.3MnO3 were investigated using high-resolution time-of-flight neutron powder diffraction. Results demonstrate that the phase segregation in Pr0.7Ca0.3MnO3 is unrelated to electronic phase segregation but is primarily driven by chemical disorder and intra-granular strains, similar to martensitic phase transitions.Charge, orbital and magnetic ordering in La0.333Ca0.667MnO3
EUROPEAN POWDER DIFFRACTION, PTS 1 AND 2 321-3 (2000) 818-822