Inorganic Spectroscopy
In the -2 box is 1 electron, L is -2*1= -2
Total value of L is therefore +4 +2 +0 -1 -2 or L=3.
Quantitative validity of the Russell-Saunders coupling scheme
The atomic energy levels arising from configurations np
3
, n = 2 – 6, of Group 15 elements.
Applying the L-S coupling scheme to the p
3
configuration, we get
three spectroscopic
terms, namely
4
S,
2
D, and
2
P, which give rise to five energy levels,
4
S11/2 (ground state),
2
D1½,
2
D2½,
2
P½, and
2
P1½.
The energy values of these five levels for all Group 15 elements. Also tabulated there are
the “weighted” term values for 2D and 2P. The energy of 2D(weighted) is simply (6 ×
2D2½ + 4 × 2D1½)/10, where the numerical factors “6” and “4” refer to the number of
components (2J + 1) of the states 2D2½ and 2D1½, respectively. The energy of
2P(weighted) can be calculated in a similar manner. These “weighted” term values
provide us with the approximate energy of the term, before spin-orbit interaction is
“turned on.”
The Crystal Field Splitting of Russell-Saunders terms
Term: The combination of an S value and an L value is called a term, and has a statistical
weight (i.e., number of possible microstates) equal to (2S+1)(2L+1).
Different orbitals (s, p, d, and f) split into the subsets of different energies by the effect of
crystal field depending upon whether they are in octahedral or tetrahedral environment.
Representation of Magnitude of d orbital splitting
The magnitude of the d orbital splitting is generally represented as a fraction of Δoct or
10Dq.
Effect on Ground Terms Energies by Crystal Field
The ground term energies for free ions are also affected by the influence of a crystal field
and an analogy is made between orbitals and ground terms that are related due to the
angular parts of their electron distribution.
Effect of Crystal Field in Octahedral Complexes
The effect of a crystal field on different orbitals in an octahedral field environment will
cause the following to occur:
d orbitals split to give t2g and eg subsets
D ground term states into T2g and Eg, (where upper case is used to denote states
and lower case orbitals).
f orbitals are split to give subsets known as t1g, t2g and a2g.
By analogy, the F ground term when split by a crystal field to T1g, T2g, and A2g.