Fraunhofer lines are a set of dark absorption lines in the optical spectrum of the Sun. They are the result of specific wavelengths of light from the Sun’s hot interior being absorbed by cooler atoms and ions in its photosphere. Each line corresponds to a particular electron transition in a specific element, allowing for the determination of the Sun’s chemical composition from Earth.
Fraunhofer Lines
- William Hyde Wollaston
- Joseph von Fraunhofer
In 1802, William Hyde Wollaston first noted the existence of dark lines in the solar spectrum. However, it was Joseph von Fraunhofer who, in 1814, independently rediscovered and systematically studied these lines using a high-quality prism and telescope, mapping over 570 of them. He labeled the most prominent lines with letters from A to K, a notation still used today. The profound significance of these lines was not understood until 1859, when Gustav Kirchhoff and Robert Bunsen established that the pattern of lines was unique to each chemical element. They realized that the dark lines in the solar spectrum matched the bright emission lines of known elements when heated. This 引领 to the groundbreaking conclusion that the Fraunhofer lines are absorption spectra. Light from the Sun’s continuous spectrum, produced by its hot, dense core (photosphere), passes through the cooler, less dense outer layers (chromosphere). Atoms in the chromosphere absorb photons at the precise frequencies corresponding to their allowed electronic transitions, re-emitting them in random directions. This process effectively removes those specific frequencies from the light reaching Earth, creating the dark lines. This discovery transformed astronomy from a science of position and motion to one of astrophysics, enabling the study of the physical nature and chemical makeup of distant stars.
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前体
- Isaac Newton’s work on light dispersion (1672)
- Development of the spectroscope
- Atomic theory proposing that matter is composed of discrete elements
应用
- discovery of helium in the sun’s spectrum before it was found on earth
- determination of the chemical composition of stars and other celestial objects
- measurement of stellar radial velocities via doppler shift
- studying stellar atmospheres and temperatures
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