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Definition
Transition metals are d-block elements with partially filled 3d, 4d, and 5d orbitals.
Color Production
The transition metals are (somewhat imprecisely) described as being colored because their compounds frequently take on a characteristic hue (Table 1). For example, Ni2+ cations tend to exhibit green coloration, while Cu2+ tends to show green-blue tones. Cobalt, as Co2+, has been used since medieval times to color glass deep blue, and small amounts of impurity Cr3+ in colorless Al2O3 produce the color in ruby gemstones (Fig. 1). All these colors arise from electronic transitions between the ionic ground state and energy levels lying between 1.77 and 3.10 eV above it, giving absorption maxima in the visible wavelength range (400–700 nm). These low-lying energy levels arise from interactions of the d orbitals on the cation with neighboring atoms in a material and are a function of the symmetry of the surroundings [1,2,3]. The energy levels that occur...
References
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Tilley, R.J.D.: Chapter 7: Colour from atoms and ions. In: Colour and the Optical Properties of Materials, 2nd edn. Wiley, Chichester (2011)
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Schriver, D.F., Atkins, P.W., Langford, C.H.: Chapters 6, 14. In: Inorganic Chemistry, 2nd edn. Oxford University Press, Oxford (1994)
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Tilley, R.J.D. (2019). Transition Metal Ion Colors. In: Shamey, R. (eds) Encyclopedia of Color Science and Technology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27851-8_256-2
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DOI: https://doi.org/10.1007/978-3-642-27851-8_256-2
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Latest
Transition Metal Ion Colors- Published:
- 08 November 2019
DOI: https://doi.org/10.1007/978-3-642-27851-8_256-2
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Original
Transition-Metal Ion Colors- Published:
- 07 October 2014
DOI: https://doi.org/10.1007/978-3-642-27851-8_256-1