Atomic Properties of Pm
- Atomic Number of Pm
- 61
- Atomic Mass of Pm
- 145.0000 u
- Electron Configuration
- [Xe] 4f5 6s2
- Electronegativity
- 1.13
- Block
- f-block
- Group
- —
- Period
- 6
Promethium (Pm) is element 61 on the periodic table. Atomic mass of Pm: 145.0000 u. Pm is in period 6. Melting point of Pm: 1315.00 K.Density of Pm: 7.26 g/cm³.
Promethium in everyday life and industry
No naturally occurring promethium exists to affect biology. Half-life is too short for significant environmental accumulation.
Discovered by J.A. Marinsky, L.E. Glendenin, C.D. Coryell in United States, 1945
Name origin: Named for the Greek god, Prometheus.
The only lanthanide with no stable isotopes. Pm-145 is longest-lived (t1/2 17.7 years). Trace amounts occur naturally from spontaneous fission of uranium. Pm-147 (t1/2 2.62 years) is the main commercial isotope—a pure beta emitter ideal for thickness gauges and betavoltaic batteries. Discovered 1945 by Marinsky, Glendenin, and Coryell in fission products at Oak Ridge.
Promethium has 0 naturally occurring isotopes, plus 2 notable radioactive isotopes.
| Isotope | Atomic Mass (u) | Abundance | Half-Life | Decay Mode |
|---|---|---|---|---|
| 14561Pm (Pm-145)Promethium-145 isotope | 144.9127559 | — | 17.7 years | EC, α |
| 14761Pm (Pm-147)Promethium-147 isotope | 146.915145 | — | 2.62 years | β⁻ |
Data source: NIH PubChem (aggregated from IUPAC, NIST)
Isotopes of Promethium have important real-world applications in science and industry.
The beta-particle-emitting isotope 147Pm (with a half-life of 2.68 years) is used in the nuclear fuel industry to measure the thickness of the inner surface layer of graphite in the cladding tube where the nuclear fuel rod is placed in a nuclear fuel reactor (Fig. IUPAC.61.1). The graphite serves as a protective layer against mechanical contact between the nuclear fuel rod and the Zircaloy cladding (fuel-rod holding tube) and as a diffusion barrier against fission products. By placing a layer of 147Pm along the inner surface of the cladding before the graphite, the long half-life of 147Pm and constant beta-particle emission provide a reliable and simple technique to measure the thickness of the graphite along the inner surface of the tube (called the beta-ray backscatter technique) [432], [433], [434]. The beta decay property of 147Pm makes this radioisotope an ideal candidate for nuclear batteries (beta voltaics). Long-lived power supplies for remote and sometimes hostile environmental conditions are needed for space and sea missions, and nuclear batteries can uniquely serve this role. A nuclear battery using beta voltaics can have an energy density (quantity of energy per unit mass) near a thousand watt-h per kilogram with 21 percent efficiency, which is much greater than the best chemical batteries [435].
It has been used as a source of radioactivity for thickness-measuring gages.
Does not occur naturally. Found among fission products of uranium, thorium, and plutonium.
Loading quiz...