Electronic Resource
Copenhagen
:
International Union of Crystallography (IUCr)
Applied crystallography online
3 (1970), S. 357-360
ISSN:
1600-5767
Source:
Crystallography Journals Online : IUCR Backfile Archive 1948-2001
Topics:
Geosciences
,
Physics
Notes:
The dilation of the α-Fe lattice by manganese (0 to 2.4 at.%) has been determined by lattice parameter and density measurements at 25°C. The results may be described within experimental error by the linear expressions Q = QFe−0.0071 × (at.% Mn) g.cm−3 (density measurement) and a0 = aFe + 0.00067 × (at.% Mn) Å (X-ray measurement). The virtual absence of dilation at Mn contents below 0.6at.%, reported in two previous investigations, is suggested as having resulted from internal oxidation of Mn.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1107/S0021889870006428
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