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
i¼
g
g
ð
2
:
248
Þ
h
p
1
j
p
4
i¼h
p
2
j
p
4
i¼h
p
3
j
p
4
i¼
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
vÞ
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
vÞ
x
y
¼
b
x
y
ð
:
Þ
2
249
l
¼
cs
þ
dp
4
¼
scos
vþ
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