Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Octahedral site preference energy OSPE

Measurements of absorption spectra of oxides, glasses and hydrates of transition metal ions have enabled crystal field stabilization energies (CFSE s) in tetrahedral and octahedral coordinations to be estimated in oxide structures (see table 2.5). The difference between the octahedral and tetrahedral CFSE is called the octahedral site preference energy (OSPE), and values are summarized in table 6.3. The OSPE s may be regarded as a measure of the affinity of a transition metal ion for an octahedral coordination site in an oxide structure such as spinel. Trivalent cations with high OSPE s are predicted to occupy octahedral sites in spinels and to form normal spinels. Thus, Cr3, Mn3, V3+... [Pg.248]

Crystal chemistry of spinels. A classic example showing that transition metal ions display distinct site preferences in oxides stems from studies of spinel crystal chemistry. The spinel structure contains tetrahedral and octahedral sites normal and inverse forms exist in which divalent and trivalent ions, respectively, fill the tetrahedral sites. The type of spinel formed by a cation is related to its octahedral site preference energy (OSPE), or difference between crystal field stabilization energies in octahedral and tetrahedral coordinations in an oxide structure. Trivalent and divalent cations with large site preference energies (e.g., Cr3 and Ni2+) tend to form normal and inverse spinels, respectively. The type of spinel adopted by cations with zero CFSE (e.g., Fe3+ and Mn2+) is controlled by the preferences of the second cation in the structure. [Pg.270]

A relationship between octahedral site preference energies (table 6.3) and distribution coefficients has been demonstrated for transition metal ions partitioned between olivine or pyroxene crystals and the groundmass of oceanic basalts, which is assumed to represent the composition of the magma from which the ferromagnesian silicates crystallized (Henderson and Dale, 1969 Dale and Henderson, 1972). Plots of In D against OSPE, such as those illustrated in fig. 7.8, show linear trends between the two parameters. [Pg.296]

Number of 3d electrons Cation Octahedral CFSE (E0) (kJ/mole) Tetrahedral Octahedral CFSE Site Preference (Ex) Energy (OSPE) (kJ/mole) (kJ/mole) n0/nt ... [Pg.249]


See other pages where Octahedral site preference energy OSPE is mentioned: [Pg.237]    [Pg.237]    [Pg.70]    [Pg.237]    [Pg.237]    [Pg.70]    [Pg.317]    [Pg.320]   


SEARCH



OSPED (

Octahedral site

Site preferences

Site-preference energy

© 2024 chempedia.info