Physical Properties
Rhenium is a transition metal. Like the other members of the group it is less reactive than the typical metals but more reactive than the less typical metals. The transition metals are characterized by having the outermost electron shell containing two electrons and the next inner shell an increasing number of electrons. Because of the small energy differences between the valence shells, a number of oxidation states occur. The metal occurs in nature in association with molybdenite, MoS2, which in turn is associated with chalocopyrite in porphyry copper ores. Molybdenite occurring in quartz veins does not contain rhenium.
Atomic number |
75 |
Atomic weight |
186.207 |
Relative abundance in the Earth’s crust, % |
7 × 10–8 |
Density at 20°C, g/cm3 |
21.0 |
Metallic radius, pm |
137 |
Ionic radius (VII), pm |
53 |
Melting point, °C |
3,180 |
Boiling point, °C |
5,870 |
Heat of fusion, kJ/mol |
33 |
Heat of sublimation  ΔH B (monatomic gas) |
+ 779 (± 8) kJ/mol |
Enthalpy of formation of Re2O7, kJ/mol |
–1,241 |
El... |
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References
Habashi F (2003) Metals from ores. An introduction to extractive metallurgy. Métallurgie Extractive Québec, Quebec City, Canada. Distributed by Laval University Bookstore, www.zone.ul.ca
Nadler HG (1997) Rhenium and rhenium compounds. In: Habashi F (ed) Handbook of extractive metallurgy. Wiley-VCH, Weinheim, pp 1491–1502
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Habashi, F. (2013). Rhenium, 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_387
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