Crystal field stabilization energy CFSE

The cations in these compounds are Fe and/or Fe". In iron oxides, Fe " is always in the high spin (unpaired d electrons) state. As Fe with five d electrons has no crystal field stabilization energy (CFSE see Chap. 6), regardless of whether it is octa-hedrally or tetrahedrally coordinated, there is little preference for one or the other type of site. For Fe , on the other hand, CFSE is higher for octahedral than for tetrahedral coordination, so the octahedral coordination is favoured. 

The M-ferrihydrite coprecipitate contains M-O/OH-Fe and M-O/OH-M as well as Fe-O/OH-Fe linkages. The transition elements stabilize ferrihydrite in the order, Mn < Ni < Co < Cu < Zn (Cornell, 1988 Giovanoli Cornell, 1992). This order does not correspond with that of the electronegativities or the crystal field stabilization energies (CFSE) of these elements, nor does it match the order of binding constants for the M-surface complexes. If Zn is omitted from the series, however, there is a reasonable cor-... 

Crystal field stabilization energy, CFSE. Each electron in a t2g orbital stabilizes a transition metal ion in octahedral coordination by 0.4Ao, whereas every electron in an eg orbital destabilizes it by 0.6Ao. The crystal field stabilization energy, CFSE, represents the algebraic sum of these factors. Cations may have... 

There are several approaches for obtaining spectral data for low-abundance transition metal ions, rare minerals and crystals of small dimensions. Data for a transition element in its chemical compounds, such as hydrates, aqueous solutions, molten salts or simple oxides, may be extrapolated to minerals containing the cation. Such data for synthetic transition metal-doped corundum and periclase phases used to describe principles of crystal field theory in chapter 2, appear in table 2.5, for example. There is a growing body of visible to near-infrared spectral data for transition metal-bearing minerals, however, and much of this information is reviewed in this chapter and the following one. These results form the data-base from which crystal field stabilization energies (CFSE s) of most of the transition metal ions in common oxide and silicate minerals may be estimated. 

Perhaps a more fundamental application of crystal field spectral measurements, and the one that heralded the re-discovery of crystal field theory by Orgel in 1952, is the evaluation of thermodynamic data for transition metal ions in minerals. Energy separations between the 3d orbital energy levels may be deduced from the positions of crystal field bands in an optical spectrum, malting it potentially possible to estimate relative crystal field stabilization energies (CFSE s) of the cations in each coordination site of a mineral structure. These data, once obtained, form the basis for discussions of thermodynamic properties of minerals and interpretations of transition metal geochemistry described in later chapters. 

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+... 

Crystal field stabilization energy (CFSE). 399 01. 408-413 Crystal lattices, and efficiency of packing, 118-122 Crystallography. 74-85 Crystals, imperfections in. 263-265... 

The energy difference between the actual distribution of electrons and that for all electrons in the uniform field levels is called the crystal field stabilization energy (CFSE). It is equal in magnitude to the ligand field stabilization energy (LFSE) described later in this chapter. 

Table 8.5 summarizes the electron configurations possible for 10 electrons in an octahedral crystal field, provides specific examples of transition metals with these configurations, and tabulates the crystal field stabilization energies (CFSE)... 

We have assumed implicitly that Cr3+ ions will not occur in tetrahedral holes in an oxide lattice. Cr + is a species. In the crystal field theory, such ions lead to particularly good stabilization of octahedral coordination. For example, the coordinate bond energy of Cr(H20) + is 120 kcal, of which 9 represent crystal field stabilization energy (CFSE) (35). In fact, there are no known chromias with crystal struc-... 

For silicates composed of transition metal cations, crystal field stabilization energy (CFSE) affects dissolution rates. Thus, the rate of dissolution in acidic water of structurally similar orthosilicates follows the order... 

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