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Absorption spectroscopy

physical science Maturity 11-13 Next article →

Absorption spectroscopy is a powerful analytical technique used to study matter.

Spectroscopy overview
Spectroscopy overview

It involves measuring how a sample absorbs electromagnetic radiation across different frequencies or wavelengths. When radiation interacts with a sample, the sample absorbs energy in the form of photons. This absorption causes the intensity of the radiation to change. The resulting pattern of varying absorption intensities is known as an absorption spectrum. This tool is vital because it allows scientists to identify specific substances and measure their concentration. It is used in fields ranging from analytical chemistry to deep-space astronomy.

The mechanism of absorption relies on the quantum mechanical properties of atoms and molecules.

Fraunhofer lines
Fraunhofer lines

For absorption to occur, the energy of the incoming photons must match the energy difference between two quantum mechanical states. When this match happens, the molecule or atom transitions from a lower state to a higher state. This specific event is called an absorption line. A spectrum is essentially a collection of many such lines. The frequency and intensity of these lines depend on the electronic and molecular structure of the sample. Environmental factors like temperature, pressure, and magnetic fields can also shift these frequencies.

Different types of electromagnetic radiation trigger different types of physical changes.

Identification of Ices in the Solar System
Identification of Ices in the Solar System

Rotational lines occur when the rotational state of a molecule changes, and these are found in the microwave region. Vibrational lines correspond to changes in the vibrational state of a molecule, typically appearing in the infrared region. Electronic lines involve changes in the electronic state of an atom or molecule, which are found in the ultraviolet and visible regions. Finally, X-ray absorption is associated with the excitation of inner shell electrons within atoms. Some transitions can even combine, such as rotation-vibration transitions, creating new lines at combined energy levels.

Scientists use various experimental arrangements to capture these spectra. The most common method involves directing a beam of radiation at a sample and detecting the intensity of the light that passes through it. This is known as the transmitted energy. By comparing the incident light to the transmitted light, researchers can calculate the exact amount of absorption. This is closely related to the transmission spectrum, which shows maximum intensity where absorption is weakest. Absorption spectra can also be related to emission spectra, which show how substances release energy, though the two patterns are not identical.

In laboratory settings, absorption spectroscopy is highly valued for its specificity and quantitative nature.

Identification of Ices in the Solar System
Identification of Ices in the Solar System

Specificity means that different compounds produce unique spectral patterns, allowing them to be distinguished in a mixture. For example, infrared gas analyzers can detect specific pollutants in the air by separating them from nitrogen or oxygen. To find the exact amount of a substance, scientists use the Beer-Lambert law. This law relates the absorption to the concentration of the material. To do this accurately, researchers must know the absorption coefficient of the compound or use a known calibration standard.

Remote sensing is another major application that allows for measurement without physical contact. This is useful in toxic or hazardous environments where humans cannot safely go. It also prevents cross-contamination of delicate samples. However, remote sensing faces unique challenges, such as background interference from the space between the sample and the instrument. Scientists often use differential optical absorption spectroscopy to overcome this. This method focuses on specific absorption features while ignoring broad-band interference like aerosol extinction. This technique is used by ground-based, airborne, and satellite-based sensors.

Astronomy represents perhaps the most profound use of this science.

Sodium in atmosphere of exoplanet HD 209458
Sodium in atmosphere of exoplanet HD 209458

Because light travels across the universe, astronomers can perform remote spectral sensing on objects billions of miles away. In 2001, researchers achieved the first direct chemical analysis of an exoplanet's atmosphere. They detected sodium in the atmosphere of the planet HD 209458 as it passed in front of its star.

Cumulative-absorption-spectrum-hubble-telescope
Cumulative-absorption-spectrum-hubble-telescope

Using tools like the Hubble Space Telescope, scientists can observe these absorption patterns to understand the composition of distant worlds. This connects the tiny movements of molecules to the largest structures in the cosmos.

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🖼️ Images & Media (6)
File:Spectroscopy overview.svg
Spectroscopy overview.svg
File:Sodium in atmosphere of exoplanet HD 209458.jpg
Sodium in atmosphere of exoplanet HD 209458.jpg
File:Fraunhofer lines.svg
Fraunhofer lines.svg
File:Emission spectrum-Fe.svg
Emission spectrum-Fe.svg
File:Identification of Ices in the Solar System.jpg
Identification of Ices in the Solar System.jpg
File:Cumulative-absorption-spectrum-hubble-telescope.jpg
Cumulative-absorption-spectrum-hubble-tele...
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