where the asterisk is used to indicate an isotopic substitution. When we take
a ratio of the above two equations, such treatments will cancel each other and
we can get
8.652
*
1013 s^1
which reduces to
8.652
*
1013 s^1
*
Because the frequency ratio is related to a reduced mass ratio,it doesn’t mat-
ter what units we use to express the reduced mass ratio. Rather than express
the reduced masses in atomic values (on the order of 10^27 kg or so), we can
simply use grams per mole as the unit of mass. The reduced mass of^1 H^35 Cl
is therefore 0.9722 (grams per mole), whereas the reduced mass of^1 H^37 Cl is
0.9737 (grams per mole). The above equation becomes
8.652
*
1013 s^1
0
0
.
.
9
9
7
7
2
3
2
(^7)
g
g
/
/
m
m
o
o
l
l
The units cancel, yielding a ratio that has the same value no matter what units
of mass are used. Evaluating:
8.652
*
1013 s^1
0.9992
This rearranges to * 8.659
1013 s^1 , or 2884 cm^1 (to four significant
figures). This is a relatively insignificant change, although it is easily de-
tectable. However, for^2 H^35 Cl:
8.652
*
1013 s^1
0
1
.9
.8
7
9
2
1
2
(^) g
g
/
/
m
m
o
o
(^) l
l
8.652
*
1013 s^1
0.7170 (unitless)
* 6.203
1013 s^1 or 2069 cm^1 (to four significant figures)
This predicts a shift of over 800 wavenumbers. The measured vibrational fre-
quency of^2 H^35 Cl is 2091 cm^1 , which agrees with the assumption of an ideal
system.
It is not necessary to convert a wavenumber value into a frequency value
when doing an example like the one above, because the two quantities are di-
rectly proportional to each other. Also, even if a molecule isn’t a diatomic mole-
cule, and even though a normal mode consists of the vibrations of all atoms in
the molecule, in many cases for stretching-type motions a “diatomic approxi-
mation” can be made for isotopic substitution. The next example illustrates.
Example 14.13
If the symmetric O–H stretch for water occurs at 3657 cm^1 , predict the fre-
quency of the O–D stretch of D 2 O (D is^2 H) assuming that the O–H stretch
acts as a diatomic species.
2
1
k
*
2
1
k
486 CHAPTER 14 Rotational and Vibrational Spectroscopy