Composition and temperature dependence of cation ordering in Ni-Mg olivine solid solutions: a time-of-flight neutron powder diffraction and EXAFS study

2001 ◽  
Vol 86 (10) ◽  
pp. 1170-1187 ◽  
Author(s):  
C. Michael B. Henderson ◽  
Simon A.T. Redfern ◽  
Ronald I. Smith ◽  
Kevin S. Knight ◽  
John M. Charnock
2000 ◽  
Vol 64 (1) ◽  
pp. 11-18 ◽  
Author(s):  
A. Pavese ◽  
G. Ferraris ◽  
V. Pischedda ◽  
P. Radaelli

AbstractPhengite 3T (Dora-Maira massif, Italian western Alps), with chemical composition K0.96Na0.01Al1.44Mg0.56(Si3.59 Al0.41)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.


1995 ◽  
Vol 28 (5) ◽  
pp. 494-502 ◽  
Author(s):  
J. K. Warner ◽  
A. K. Cheetham ◽  
D. E. Cox

The distribution of divalent iron and nickel over two metal sites of differing coordination geometry in NiFe2(PO4)2, sarcopside, has been investigated by resonant X-ray and time-of-flight neutron powder diffraction. To assess the reproducibility of the X-ray technique, data have been collected from instruments X7A at Brookhaven National Laboratory and 8.3 at the Synchrotron Radiation Source, Daresbury Laboratory, England, using wavelengths λ X1 = 1.7437 (3) Å and λ X2 = 1.7434 (1) Å, respectively, close to the Fe2+ K edge determined by X-ray absorption near-edge structure. The real part of the anomalous-scattering correction for iron at each energy, f′(Fe) X1 = −7.81 (9) and f′(Fe) X2 = −10.16 (6), was determined experimentally by diffraction from Fe3(PO4)2 under identical conditions. Occupancies obtained for iron at the M(1) site were found to be M(1) X1 = 0.366 (6) and M(1) X2 = 0.376 (3), compared with M(1) N = 0.26 (15) from time-of-flight neutron powder diffraction.


ChemInform ◽  
1989 ◽  
Vol 20 (40) ◽  
Author(s):  
C. W. JONES ◽  
P. D. BATTLE ◽  
P. LIGHTFOOT ◽  
W. T. A. HARRISON

1998 ◽  
Vol 278-281 ◽  
pp. 537-541 ◽  
Author(s):  
L. Giovanelli ◽  
O. Moze ◽  
Winfried A. Kockelmann ◽  
C.H. de Groot ◽  
F.R. de Boer ◽  
...  

2003 ◽  
Vol 15 (5) ◽  
pp. 1099-1104 ◽  
Author(s):  
Junichi Takahashi ◽  
Hisanori Yamane ◽  
Naoto Hirosaki ◽  
Yoshinobu Yamamoto ◽  
Takayuki Suehiro ◽  
...  

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