Magnetic compensation and ordering in the bimetallic oxalates: why are the 2D and 3D series so different?

Inorganic Chemistry

Volumn 48, Issue 7, 2009, Pages 3039-3046

  Fishman, Randy S ^a,b   Miguel, Clemente León ^a,b   Coronado, Eugenio ^a,b  

^a OAK RIDGE NATIONAL LABORATORY   (United States)

^b UNIVERSITY OF VALENCIA   (Spain)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 64349109673     PISSN: 00201669     EISSN: None     Source Type: Journal    
DOI: 10.1021/ic802341k     Document Type: Article

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36. 12 The low value of M(5T) may be caused by the substitution of S′ ) 5/2 Fe(III) ions into the Fe(II) sublattice.
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