Protactinium is a radioactive metal formed in the decay chain of uranium but not thorium (Fig. 1). It exists in two crystalline forms: α-Protactinium is tetragonal body-centered (a = 393.1 pm, c = 323.6 pm) and β protactinium is cubic face-centered (a = 501.9 pm). Protactinium isotope 231Pa (t 1/2 = 32,480 years) is the most important of all 24 known isotopes. The isotope 233Pa is of special importance because it is formed as an intermediate in the production of fissile 233U from non-fissile 232Th by neutron capture:
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Habashi F (2003) Metals from ores. An introduction to extractive metallurgy. Métallurgie Extractive Québec, Québec City. Distributed by Laval University Bookstore, www.zone.ul.ca
Luig H et al (1997) Radioactive metals. General. In: Habashi F (ed) Handbook of extractive metallurgy. Wiley, Weinheim, pp 1585–1598
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Habashi, F. (2013). Protactinium, Physical and Chemical Properties. In: Kretsinger, R.H., Uversky, V.N., Permyakov, E.A. (eds) Encyclopedia of Metalloproteins. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-1533-6_400
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