Why Observed IR Bands Are Fewer Than Expected (Based on 3N-5 or 3N-6 Rule)?
When predicting the number of fundamental vibrational modes of a molecule, we use the 3N-6
rule (for non-linear molecules) or 3N-5 rule (for linear molecules), where N is the number of
atoms. However, the number of IR absorption bands observed experimentally is often less than
the number predicted.
1- No Change in Dipole Moment During Vibration (IR Inactivity)
For a vibration to be IR active, it must cause a change in the dipole moment of the molecule. If a
vibration does not cause any change in dipole moment, it will not absorb infrared radiation, and
hence it will be IR inactive.
Example: Symmetric stretching of CO₂: Although the two C=O bonds stretch and contract
simultaneously, the center of positive and negative charges remains the same → No change in
dipole moment → IR inactive.
2- Degenerate Vibrations (Same Frequency)
Sometimes, different vibrational motions happen at the same energy and same frequency —
they are called degenerate vibrations. As a result, they appear as a single band, even though
multiple vibrations exist.
Example: In CO₂, the scissoring motions (bending vibrations) in two different planes are
degenerate → They absorb at the same frequency, producing only one IR band.
3- Bands Are Very Close Together (Coalescence)
Some vibrational frequencies are so close to each other that they merge into a single broad band.
The instrument may not be able to resolve them separately.
Example: In larger organic molecules, C-H bending vibrations often occur very close to each
other and appear as a single broad peak.
4- Weak Absorption Bands (Low Intensity)
Some vibrational modes produce very weak absorption because the change in dipole moment
during vibration is very small. Such bands may be too weak to detect with ordinary IR
spectrometers.
Example: Overtones (vibrations at multiples of fundamental frequencies) are typically very
weak and sometimes not observed.
5- Fundamental Frequency Outside the IR Range
Some vibrations may have frequencies too high or too low to fall within the normal IR range
(typically 4000 cm⁻¹ to 400 cm⁻¹). Therefore, they are missed during standard IR analysis.
Example:
Very strong triple bonds (like C≡N) have stretching frequencies that can sometimes be
near the higher edge of IR range.
Very low-frequency metal-ligand vibrations (in complexes) may fall in the far IR region
(below 400 cm⁻¹), which standard IR spectrometers cannot detect.
6- Instrumental Limitations
Sometimes, even if the band is present, limitations of the spectrometer such as resolution,
sensitivity, or detector range can prevent proper observation.
Example: In early IR spectrometers, weak overtones and combination bands were often
undetected.
7- Overlapping of Fundamental and Overtone/Combination Bands
Overtones (vibrations at twice or three times the fundamental frequency) and combination bands
(sum or difference of two vibrational modes) can overlap with fundamental vibrations. This can
cause confusion, missing out or misinterpreting expected bands.
Example: In aromatic compounds, C-H overtone bands sometimes overlap with fundamental
C=C stretching bands.