|
91
Pa
231.0
|
| Classification: | Protactinium is an actinide metal |
| Color: | silvery |
| Atomic weight: | 231.0359, no stable isotopes |
| State: | solid |
| Melting point: | 1570 oC, 1843 K |
| Boiling point: | 4000 oC, 4273 K |
| Shells: | 2,8,18,32,20,9,2 |
| Electron configuration: | [Rn] 5f2 6d1 7s2 |
| Density @ 20oC: | 15.4 g/cm3 |
| Atomic volume: | 15.0 cm3/mol |
| Structure: | fcc: face-centered cubic |
| Hardness: |
Discovery of Protactinium
The discovery story of protactinium spans several years. Kasimir Fajans and Oswald Göhring discovered protactinium in 1913. They called the element 'brevium' because the isotope they had found (protactinium-234) has a very short half-life (1.17 minutes). (1)
Otto Hahn and Lise Meitner discovered a much longer lived isotope in 1917: protactinium-231 (half-life of 32 670 years). Hahn and Meitner were searching for a 'mother substance' that decayed to actinium.
Otto Hahn wrote that their goal was "to find that substance which... forms the starting point for the actinium series, and to determine whether and through which intermediates actinium is derived." (1)
Their work was interrupted by the First World War. In 1917 they examined silica residue they had extracted from pitchblende (uranium oxide) over two years earlier.
They identified protactinium-231 by establishing that no known substance could have emitted the alpha particles that were observed and by the actinium produced.
Frederic Soddy and John Cranston also discover protactinium independently in 1917. (1)
In 1927 by Astrid Von Grosse isolated protactinium oxide (Pa2O5). In 1934 he isolated the element from the oxide by converting it to the iodide (PaI5) and then decomposed it using a heated filament in a high vacuum. (2)
The element name comes from a combination of the Greek word 'protos' meaning first and 'actinium.'
Appearance & Characteristics
Protactinium is harmful due to its radioactivity and is also toxic.
Characteristics:
Protactinium is a very rare shiny, silvery, highly radioactive metal that tarnishes slowly in air to the oxide.
Almost all naturally occurring protactinium is the 231 isotope. It emits alpha radiation and is produced through the decay of uranium-235.
Protactinium is one of the rarest and most expensive naturally occurring elements.
The largest amount of protactinium obtained so far has been 125 grams in 1961 from the Great Britain Atomic Energy Authority. The extraction was made from 60 tons of nuclear waste material. (3)
Uses of Protactinium
Protactinium is used mainly for research purposes.
Protactinium-231 combined with the thorium-230 can be used to date marine sediments. (4)
Abundance & Isotopes
Abundance solar system: negligible
Cost, pure: $280 per g
Cost, bulk: per 100g
Source: Protactinium occurs naturally in minute amounts (up to 3 parts per million) in uranium ores. Protactinium can also obtained as a by-product of uranium processing.
Isotopes: Protactinium has 27 isotopes whose half-lives are known, with mass numbers 212 to 238. Protactinium has no stable isotopes. Its longest lived isotopes are 231Pa, with a half-life of 32,760 years, 233Pa with a half-life of 26.967 days and 230Pa with a half-life of 17.4 days.
Energies
Heat of fusion: 12.34 kJ mol-1
1st ionization energy: 568 kJ mol-1
3rd ionization energy: kJ mol-1
Heat of vaporization: 481 kJ mol-1
2nd ionization energy: kJ mol-1
Electron affinity: kJ mol-1
Oxidation & Electrons
Minimum oxidation number: 0
Min. common oxidation no.: 0
Electronegativity (Pauling Scale): 1.5
Maximum oxidation number: 5
Max. common oxidation no.: 5
Polarizability volume: 25.4 Å3
Reactions & Compounds
Reaction with 15 M HNO3:
Oxide(s): PaO PaO2 Pa2O5
Hydride(s): PaH3
Reaction with 6 M NaOH: none
Chloride(s): PaCl4 PaCl5
Radius
Ionic radius (2+ ion): pm
Ionic radius (2- ion): pm
Ionic radius (3+ ion): 118 pm
Ionic radius (1- ion): pm
Conductivity
References
2. John Emsley, Nature's building blocks: an A-Z guide to the elements., Oxford University Press, 2003 page 348.
3. Andrew Ede, The chemical element: a historical perspective., Greenwood Publishing Group, 2006page 146.
4. John P Rafferty, Geochronology, Dating, and Precambrian Time: The Beginning of the World as We Know It., The Rosen Publishing Group, 2010 page 152.
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