Organic Analysis (AQA A-Level Chemistry): Revision Notes
3.6.3 Infrared Spectroscopy
Infrared (IR) spectroscopy is a key analytical technique. It involves the absorption of infrared radiation by chemical bonds, allowing the identification of specific functional groups within a molecule. This technique can also highlight the role of certain gases in global warming due to their IR absorption characteristics.
How Infrared Spectroscopy Works
Absorption of Infrared Radiation
- Bonds in a molecule absorb infrared (IR) radiation at specific frequencies.
- The frequency of absorption is related to the vibrational frequency of the bond, which depends on:
- The mass of the atoms involved.
- The bond strength and length.
- When IR radiation passes through a compound, bonds absorb energy at characteristic frequencies, causing them to vibrate. These absorbed frequencies are detected and represented as peaks on an IR spectrum.
Analysing the IR Spectrum
An infrared spectrum is a graph plotting absorption against wavenumber (cm). The position of each peak helps identify the functional groups present in the molecule.
Key Regions of the IR Spectrum
The Fingerprint Region (Below 1500 cm)
- This region contains a complex pattern of peaks due to bond bending, rotations, and other deformations.
- Unique for each molecule: It acts like a "fingerprint" that can confirm the identity of a compound when compared to a known sample.
- Impurities: Additional peaks in this region compared to a known spectrum indicate the presence of impurities.
The Functional Group Region (Above 1500 cm⁻¹)
- This region is more straightforward to interpret, as it contains signals associated with specific functional groups.
- Key peaks in this region correspond to common bonds in organic molecules, making it possible to identify the structure of a compound.
Identifying Functional Groups Using IR Spectra
Common IR Absorption Ranges
Stretch:
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A peak just under 3000 cm⁻¹ is common for bonds in almost all organic molecules. Stretch:
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Alcohols: Broad peak between 3230 and 3550 cm⁻¹.
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Carboxylic Acids: Very broad peak between 2500 and 3000 cm⁻¹. Stretch (Carbonyl Group):
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A sharp peak between 1680 and 1750 cm⁻¹, indicating the presence of an aldehyde, ketone, carboxylic acid, or ester.
Example of Interpretation If an IR spectrum shows a broad peak at 3300 cm⁻¹ and a sharp peak at 1700 cm⁻¹:
- The broad peak suggests an group (likely an alcohol).
- A sharp peak indicates a group, suggesting the compound could be a carboxylic acid.
Using the Fingerprint Region for Molecule Identification
How to Use the Fingerprint Region
- This region is often too complex to identify individual functional groups.
- However, comparing the fingerprint region of an unknown spectrum with a known pure sample can confirm the identity of a molecule.
- If the spectra match exactly, the compounds are the same. Any additional peaks indicate impurities.
Infrared Absorption and Global Warming
Role of Greenhouse Gases
- The Earth absorbs sunlight (UV and visible radiation) and re-emits it as infrared radiation.
- Greenhouse gases like carbon dioxide (), methane (), and water vapour absorb this IR radiation effectively.
- The absorption of IR radiation by these gases traps heat in the atmosphere, contributing to global warming.
How IR Absorption Relates to Climate Change
- Increased levels of greenhouse gases lead to higher absorption of IR radiation.
- This increased IR absorption raises global temperatures, amplifying the greenhouse effect.
- The efficiency of a greenhouse gas in trapping heat is directly related to the amount of IR it can absorb.
Summary of Key Points
- Bonds absorb IR radiation at characteristic wavenumbers, allowing for the identification of functional groups.
- IR Spectrum Regions:
- Fingerprint Region: Unique to each molecule, useful for confirming identity.
- Functional Group Region: Used to identify specific functional groups.
- Global Warming Connection: Greenhouse gases absorb IR radiation, which contributes to climate change.