Promethium
Promethium is a radioactive rare-earth metal with no stable isotopes at all, which means it's essentially absent from the natural world except in vanishingly small traces produced by uranium decay. First made artificially in 1945, it's named after Prometheus, the Titan of Greek myth who stole fire for humanity — a fitting nod to a discovery born from nuclear science.
- Group · Period
- — · 6
- At room temp
- solid
- Melts at
- 1315 K
- Density
- 7.26 g/cm³
- Discovered
- 1945
Uses
Because promethium doesn’t occur naturally in any usable quantity, all of it used today is produced artificially, typically as a byproduct of nuclear reactor operation. Its most practical application takes advantage of the steady, low-energy radiation given off by the isotope promethium-147: it has been used in luminous paints and dials as a safer substitute for older radium-based formulas, and in betavoltaic devices, effectively long-life nuclear batteries, that convert its radioactive decay directly into a small but extremely durable electric current for equipment that needs power for years without maintenance.
Beyond these specialized uses, promethium hasn’t found the broad industrial role that many of its lanthanide neighbors have, largely because its radioactivity and scarcity make it far more difficult and costly to work with.
History
Promethium was first produced and positively identified in 1945 by American chemists Jacob A. Marinsky, Lawrence E. Glendenin and Charles D. Coryell at Oak Ridge National Laboratory, who isolated it from the fission products created inside a nuclear reactor. Its existence had actually been predicted years earlier, since it was the one missing element in the lanthanide row of the periodic table, but because none of its isotopes are stable, no one had been able to find it occurring naturally. The team named it promethium after Prometheus, the Titan of Greek mythology who gave fire to humanity, a name meant to capture both the achievement of nuclear science and the caution its power demands.
Fun facts
- Promethium has no stable isotopes, and only trace amounts exist naturally on Earth, formed briefly by the spontaneous fission of uranium.
- It's named after Prometheus, the Titan from Greek mythology who stole fire from the gods to give to humanity.
- Promethium-147 gives off a steady, low-energy stream of radiation, which has been used to power long-lasting betavoltaic 'nuclear batteries.'
Frequently asked questions
Does promethium exist naturally on Earth at all?
Only in extraordinarily tiny amounts. Because every isotope of promethium is radioactive and decays relatively quickly, none of it has survived from Earth's formation the way stable elements have. The minute traces that do exist today are constantly being created and destroyed as a byproduct of uranium's spontaneous fission in certain ores.
Why is promethium named after a Titan from Greek mythology?
The scientists who first produced and identified it at Oak Ridge National Laboratory in 1945 chose the name to reflect both the promise and the danger of nuclear science, much like Prometheus's gift of fire brought humanity great benefit at real personal cost. It was a deliberate, symbolic choice rather than one based on a person, place or mineral, as many earlier element names had been.
What is promethium actually used for if it's radioactive and rare?
Its steady, relatively low-energy radioactive decay makes it useful in a few specialized applications rather than everyday products. Promethium-147 has been used in luminous paint as a safer alternative to older radium-based paints, and in betavoltaic devices, sometimes called nuclear batteries, that convert its decay directly into a small, extremely long-lasting electric current.
Compounds
1 notable compound containing Pm
- Pm2O3oxide
Promethium(III) oxide
A rare, faintly pink-tinged oxide of one of the only entirely synthetic, intensely radioactive lanthanides, made in milligram quantities for research rather than everyday use.
Used for: Research-scale compound; the element itself has seen use in tritium-free luminous devices
Isotopes
38 known isotopes
Swipe to see all columns →
| Isotope | Natural abundance | Half-life | Decay mode | Mass excess | Binding energy / nucleon | Decay width |
|---|---|---|---|---|---|---|
| Pm-145 | — | 17.7 Y | Electron capture (100%), Alpha decay (2.8e-7%) | -81,267.51 keV | 8,302.66 keV | 8.17 × 10-25 eV |
| Pm-146 | — | 5.53 Y | Electron capture (65.7%), Beta-minus decay (34.3%) | -79,454.36 keV | 8,288.66 keV | 2.61 × 10-24 eV |
| Pm-147 | — | 2.6234 Y | Beta-minus decay (100%) | -79,041.98 keV | 8,284.37 keV | 5.51 × 10-24 eV |
Show all 38 isotopes
| Pm-128 | — | 1.0 s | Electron capture (100%), ECP, Alpha decay | -48,220 keV | 8,075 keV | 4.56 × 10-16 eV |
| Pm-129 | — | 2.4 s | Electron capture / beta-plus decay (100%), Proton emission, ECP | -53,180 keV | 8,114 keV | 1.90 × 10-16 eV |
| Pm-130 | — | 2.6 s | Electron capture / beta-plus decay (100%), ECP | -55,470 keV | 8,131 keV | 1.75 × 10-16 eV |
| Pm-131 | — | 6.3 s | Electron capture / beta-plus decay (100%) | -59,770 keV | 8,163 keV | 7.24 × 10-17 eV |
| Pm-132 | — | 6.2 s | Electron capture / beta-plus decay (100%), ECP (0.00005%) | -61,628 keV | 8,177 keV | 7.36 × 10-17 eV |
| Pm-133 | — | 13.5 s | Electron capture / beta-plus decay (100%) | -65,407.65 keV | 8,204.28 keV | 3.38 × 10-17 eV |
| Pm-134 | — | 5 s | Electron capture / beta-plus decay (100%) | -66,763.91 keV | 8,213.41 keV | 9.12 × 10-17 eV |
| Pm-135 | — | 49 s | Electron capture / beta-plus decay (100%) | -70,062.33 keV | 8,236.79 keV | 9.31 × 10-18 eV |
| Pm-136 | — | 300 s | Electron capture / beta-plus decay (100%) | -71,169.92 keV | 8,243.72 keV | 1.52 × 10-18 eV |
| Pm-137 | — | 2.4 m | Electron capture / beta-plus decay (100%) | -74,072.86 keV | 8,263.65 keV | 3.17 × 10-18 eV |
| Pm-138 | — | 10 s | Electron capture / beta-plus decay (100%) | -74,914.37 keV | 8,268.36 keV | 4.56 × 10-17 eV |
| Pm-139 | — | 4.15 m | Electron capture / beta-plus decay (100%) | -77,501.03 keV | 8,285.55 keV | 1.83 × 10-18 eV |
| Pm-140 | — | 9.2 s | Electron capture / beta-plus decay (100%) | -78,212.05 keV | 8,289.1 keV | 4.96 × 10-17 eV |
| Pm-141 | — | 20.90 m | Electron capture / beta-plus decay (100%) | -80,522.93 keV | 8,303.94 keV | 3.64 × 10-19 eV |
| Pm-142 | — | 40.5 s | Electron capture / beta-plus decay (100%) | -81,141.54 keV | 8,306.66 keV | 1.13 × 10-17 eV |
| Pm-143 | — | 265 d | Electron capture / beta-plus decay (100%), Beta-plus decay (0.0000057%) | -82,960.66 keV | 8,317.73 keV | 1.99 × 10-23 eV |
| Pm-144 | — | 363 d | Electron capture / beta-plus decay (100%) | -81,416.12 keV | 8,305.3 keV | 1.45 × 10-23 eV |
| Pm-148 | — | 5.368 d | Beta-minus decay (100%) | -76,865.88 keV | 8,268.23 keV | 9.84 × 10-22 eV |
| Pm-149 | — | 53.08 h | Beta-minus decay (100%) | -76,064.4 keV | 8,261.53 keV | 2.39 × 10-21 eV |
| Pm-150 | — | 2.698 h | Beta-minus decay (100%) | -73,597.34 keV | 8,243.81 keV | 4.70 × 10-20 eV |
| Pm-151 | — | 28.40 h | Beta-minus decay (100%) | -73,386.26 keV | 8,241.27 keV | 4.46 × 10-21 eV |
| Pm-152 | — | 4.12 m | Beta-minus decay (100%) | -71,254.47 keV | 8,226.13 keV | 1.85 × 10-18 eV |
| Pm-153 | — | 5.25 m | Beta-minus decay (100%) | -70,648 keV | 8,221.15 keV | 1.45 × 10-18 eV |
| Pm-154 | — | 2.68 m | Beta-minus decay (100%) | -68,266.6 keV | 8,204.72 keV | 2.84 × 10-18 eV |
| Pm-155 | — | 41.5 s | Beta-minus decay (100%) | -66,940.01 keV | 8,195.3 keV | 1.10 × 10-17 eV |
| Pm-156 | — | 26.70 s | Beta-minus decay (100%) | -64,166.85 keV | 8,176.73 keV | 1.71 × 10-17 eV |
| Pm-157 | — | 10.56 s | Beta-minus decay (100%) | -62,297.12 keV | 8,164.15 keV | 4.32 × 10-17 eV |
| Pm-158 | — | 4.8 s | Beta-minus decay (100%) | -59,106.14 keV | 8,143.36 keV | 9.50 × 10-17 eV |
| Pm-159 | — | 1.5 s | Beta-minus decay (100%) | -56,554.35 keV | 8,126.86 keV | 3.04 × 10-16 eV |
| Pm-160 | — | 725 ms | Beta-minus decay (100%), Beta-minus, neutron emission | -52,894.64 keV | 8,103.64 keV | 6.29 × 10-16 eV |
| Pm-161 | — | 1.05 s | Beta-minus decay (100%), Beta-minus, neutron emission | -50,086.59 keV | 8,086 keV | 4.35 × 10-16 eV |
| Pm-162 | — | 0.63 s | Beta-minus decay (100%), Beta-minus, neutron emission | -46,040 keV | 8,061 keV | 7.24 × 10-16 eV |
| Pm-163 | — | 0.43 s | Beta-minus decay (100%), Beta-minus, neutron emission | -42,960 keV | 8,042 keV | 1.06 × 10-15 eV |
| Pm-164 | — | — | Beta-minus decay (100%), Beta-minus, neutron emission | -38,360 keV | 8,014 keV | — |
| Pm-165 | — | — | Beta-minus decay (100%), Beta-minus, neutron emission | -34,670 keV | 7,992 keV | — |