Chemistry Reference
In-Depth Information
A root of the quartic equation (2.241) is given in this case by the simple
trigonometric relation:
p cot
g ¼
cos v
ð
2
:
246
Þ
74 g
90 ð
45 u
60 Þ
provided 54
0
the interbond angle resulting fromenergy optimization opens beyond 90 .
The four p AOs directed according to C 3v symmetry:
p 1
:
. This shows that for v =
<
:
¼
z cos
g þ
x sin
g
p
2
1
2 x sin
p 2 ¼
z cos
g
g þ
y sin
g
ð
2
:
247
Þ
p
3
1
2 x sin
p 3
¼
z cos
g
g
y sin
g
2
p 4
¼
z
are still normalized, but no longer orthogonal to each other:
<
:
1
2 sin 2
cos 2
h
p 1 j
p 2 i¼h
p 1 j
p 3 i¼h
p 2 j
p 3
g
g
ð
2
:
248
Þ
h
p 1
j
p 4
i¼h
p 2
j
p 4
i¼h
p 3
j
p 4
cos
g
Orthogonality can be restored by mixing in a certain amount of s
(Magnasco, 2007; Torkington, 1951):
8
<
:
p
p
1
1
3
b 1
¼
as
þ
bp 1
¼
p ð
s sin v
z cos vÞþ
p
x
¼
p
b
þ
p
x
1
1
1
1
3
1
6
1
¼
þ
¼
p ð
s sin v
z cos
p
þ
p
¼
p
p
þ
p
b 2
as
bp 2
x
y
b
x
y
1
1
1
2
1
3
1
6
1
p ð
p
p
p
p
p
b 3 ¼
as
þ
bp 3 ¼
s sin v
z cos
x
y
¼
b
x
y
ð
:
Þ
2
249
l
¼
cs
þ
dp 4 ¼
scos
z sin v
ð
2
:
250
Þ
since:
p
2
1
=
2
p cot
1
=
2
3cos 2
3cos 2
1
3
1
g
1
sin
1
g
a
¼
p
;
b
¼
p
3
g ;
c
¼
g;
d
¼
sin 2
sin 2
g
g
ð
2
:
251
Þ
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