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Promethium (Pm)

Atomic Number: 61 • Group: LREE

61
145.000
Pm
Promethium
LREE

Primary Uses

Betavoltaic nuclear batteries, Industrial thickness gauges, Radioluminescent light sources

Scarcity & Economic Profile

Crustal Abundance

~0

Primary Economic Driver

Lab research (radioactive)

Geological Scarcity

LowMediumHighExtremeTotal

Supply Risk

N/ALowMediumHighExtreme

Primary Mining Countries

N/A (Synthetic/Laboratory only)

Primary Processing Countries

N/A

Sources - Crustal Abundance

  1. Rudnick, R. L., & Gao, S. (2003). Composition of the Continental Crust. Treatise on Geochemistry, 3, 1-64.
  2. Taylor, S. R., & McLennan, S. M. (1985). The Continental Crust: Its Composition and Evolution. Blackwell Scientific Publications.
  3. Wedepohl, K. H. (1995). The composition of the continental crust. Geochimica et Cosmochimica Acta, 59(7), 1217-1232.
  4. U.S. Geological Survey. (2026). Mineral Commodity Summaries 2026. U.S. Department of the Interior.

Short Description

Promethium is the only rare earth element with no stable isotopes - every form is radioactive. The longest-lived isotope (Pm-145) has a half-life of just 17.7 years, meaning virtually none survives from Earth's formation. At any given moment, an estimated 500-600g exists across the entire planet as a trace product of spontaneous uranium fission. It is never mined. Commercial Pm-147 is produced either as a nuclear reactor fission byproduct (separated from spent fuel rods) or by neutron irradiation of Nd-146 in a reactor. Its primary application is betavoltaics - converting beta radiation directly into electricity for long-life atomic batteries once used in cardiac pacemakers (pre-1970s, before lithium cells) and still used in precision instruments, guided systems, and remote sensors. It is also used in industrial beta-ray thickness gauges for measuring thin films and materials, and historically in radioluminescent paint for military instrument dials before tritium alternatives became standard.