The red colour of the gem, ruby is predominantly due to
The beautiful red color of the gem, ruby, is a fascinating example of how impurities in a crystal structure can create vibrant hues. Ruby is essentially a variety of the mineral corundum, which is aluminum oxide ($\text{Al}_2\text{O}_3$). Pure corundum is colorless.
The red color in ruby is caused by the presence of chromium ions ($\text{Cr}^{3+}$) as an impurity within the corundum lattice. Some of the aluminum ions ($\text{Al}^{3+}$) in the $\text{Al}_2\text{O}_3$ structure are replaced by chromium ions ($\text{Cr}^{3+}$). The $\text{Cr}^{3+}$ ions are responsible for absorbing certain wavelengths of light and emitting red light, which gives the ruby its characteristic red color.
When white light falls on the ruby crystal, the $\text{Cr}^{3+}$ ions absorb light in the green and blue regions of the spectrum. This absorption excites the electrons in the $\text{Cr}^{3+}$ ions to higher energy levels. As these electrons return to their ground state, they emit photons of light predominantly in the red region of the spectrum. This process of light emission following absorption is known as luminescence.
Specifically, the emission of red light by the $\text{Cr}^{3+}$ ions in ruby is a type of luminescence called fluorescence. Fluorescence is characterized by the rapid emission of light after the excitation source is removed. The absorbed energy is quickly re-emitted as light of a different wavelength (longer wavelength, thus red) within a very short time frame (typically nanoseconds).
Therefore, the red color of ruby is predominantly due to the red emission through fluorescence of $\text{Cr}^{3+}$ ions present as impurities in the corundum structure.
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