Definition
Chromium has four naturally occurring stable isotopes (50Cr, 52Cr, 53Cr, and 54Cr) with natural abundances of 4.35%, 83.79%, 9.50%, and 2.36%, respectively. Among these, 50Cr, 52Cr, and 54Cr are nonradiogenic, while 53Cr is the radiogenic product of 53Mn, an extinct nuclide with a half-life of 3.7 Myr. Chromium isotope variations in terrestrial samples are reported using the ratio 53Cr/52Cr, expressed in conventional delta notation (δ53Cr) relative to NIST SRM 979, a metallic Cr standard from the National Institute of Standards and Technology. In meteorite samples, the ratio 54Cr/52Cr is sometimes used to report nuclear synthetic anomalies (conventionally reported in epsilon notation). Chromium isotopes have a wide range of applications in cosmochemistry, geochemistry, and environmental remediation efforts.
Introduction
The earliest work on Cr isotopes was largely focused on cosmochemical processes, namely the application of the short-lived 53Mn-53Cr radiochronometer to...
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Cole, D.B., Wang, X., Qin, L., Planavsky, N.J., Reinhard, C.T. (2018). Chromium Isotopes. In: White, W. (eds) Encyclopedia of Geochemistry. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-39193-9_334-1
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DOI: https://doi.org/10.1007/978-3-319-39193-9_334-1
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