Mössbauer Analysis

Author(s):  
Ko Mibu ◽  
Masaaki Tanaka ◽  
Kohei Hamaya
Keyword(s):  
2012 ◽  
Vol 218 (1-3) ◽  
pp. 95-99 ◽  
Author(s):  
F. M. Gagliardi ◽  
J. D. Cashion

1989 ◽  
Vol 158 (1-3) ◽  
pp. 203-205 ◽  
Author(s):  
J.A. Sawicki ◽  
T. Tyliszczak ◽  
F.E. Wagner ◽  
J.H. Rolston ◽  
A.P. Hitchcock ◽  
...  
Keyword(s):  

1992 ◽  
Vol 69 (1-4) ◽  
pp. 513-516 ◽  
Author(s):  
I. Fall ◽  
J. -M. R. Génin
Keyword(s):  

1995 ◽  
Vol 140-144 ◽  
pp. 313-314 ◽  
Author(s):  
F. Malizia ◽  
F. Ronconi ◽  
P. Allia ◽  
M. Knobel ◽  
P. Tiberto ◽  
...  
Keyword(s):  

LACAME 2010 ◽  
2011 ◽  
pp. 167-173
Author(s):  
José Flávio Marcelino Borges ◽  
Marlon Luiz Hneda ◽  
André Maurício Brinatti ◽  
João Batista Marimon da Cunha ◽  
Jadir Aparecido Rosa ◽  
...  

1979 ◽  
Vol 43 (328) ◽  
pp. 552-553 ◽  
Author(s):  
C. Blaauw ◽  
C. G. White ◽  
W. Leiper ◽  
D. B. Clarke
Keyword(s):  

2017 ◽  
Vol 81 (2) ◽  
pp. 251-272 ◽  
Author(s):  
M. Lacalamita ◽  
E. Mesto ◽  
E. Kaneva ◽  
F. Scordari ◽  
G. Pedrazzi ◽  
...  

AbstractThe structures of tokkoite, K2Ca4[Si7O18OH](OH,F) and tinaksite, K2Ca2NaTi[Si7O18OH]O from the Murun massif (Russia) were refined from single-crystal X-ray diffraction data in the triclinic space group P1̄. Average crystallographic data are a ≈ 10.423, b ≈ 12.477, c ≈ 7.112 Å, α ≈ 89.92°, β ≈ 99.68°, γ ≈ 92.97°, V ≈ 910.5 Å3 for tokkoite; a ≈ 10.373, b ≈ 12.176, c ≈ 7.057 Å, α ≈ 90.82°, β ≈ 99.22°, γ ≈ 92.80°, V ≈ 878.5 Å3 for tinaksite. The substantial similarities between the geometrical parameters of the tokkoite and tinaksite structures led us to conclude that the two minerals are isostructural. However, major differences of tokkoite with respect to tinaksite are larger lattice constants, especially concerning the b parameter, longer <M–O> distances, especially <M1–O>; larger values of the M1–M3 and O20–O2 bond lengths, and a stronger distortion of the M1 polyhedron. Mössbauer analysis showed that significant trivalent iron is present, VIFe3+ 40.0(7)% in tokkoite and 12.8(3)% in tinaksite. It is confirmed that 2Ca(M1+M2)2+ + (F,OH)(O20)–↔ Ti(M1)4+ + Na(M2)+ + O(O20)– is the exchange reaction that describes the relation between tokkoite and tinaksite. In addition, this exchange reaction causes local stress involving mainly the M1 site and its interaction with the M2 and M3 sites.


Metals ◽  
2020 ◽  
Vol 10 (6) ◽  
pp. 725
Author(s):  
Valery Shabashov ◽  
Kirill Kozlov ◽  
Yurii Ustyugov ◽  
Andrey Zamatovskii ◽  
Timofey Tolmachev ◽  
...  

The effect of doping the ferrite alloy Fe-16Cr by the oversized impurities Sb and Au on the mechanism of the short-range ordering induced by “warm” severe plastic deformation was studied using the method of Mössbauer spectroscopy. A comparison between the results obtained and the positron annihilation data on the evolution of the defects of vacancy type stabilized by the impurities Sb and Au was performed. It has been established that the impurities Sb and Au entail a shift of the temperature region of short-range ordering realization in conditions of applying pressure torsion towards greater temperatures by 250 and 100 K, respectively.


Sign in / Sign up

Export Citation Format

Share Document