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caesium-137
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caesium-137

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Also known as Cs-137, 137Cs

Caesium-137 (), cesium-137 (US), or radiocaesium, is a radioactive isotope of caesium that is formed as one of the more common fission products by the nuclear fission of uranium-235 and other fissionable isotopes in nuclear reactors and nuclear weapons. Trace quantities also originate from spontaneous fission ofuranium-238. It is among the most problematic of the short-to-medium-lifetime fission products. Caesium has a relatively low boiling point of and easily becomes volatile when released suddenly at high temperature, as in the case of the nuclear accident and with nuclear explosions, and c

Key facts

Isotope.image
HD.17.095 (11966576463).jpg
Isotope.image_caption
A sealed caesium-137 radioactive source
Isotope.num_neutrons
82
Isotope.num_protons
55
Isotope.mass_number
137
Isotope.abundance
0 (trace)
Isotope.symbol
Cs
Isotope.parent
Xenon-137
Isotope.parent_mass
137
Isotope.parent_symbol
Xe
Isotope.parent_decay
b
Isotope.decay_product
barium-137m
Isotope.decay_mass
137m
Isotope.decay_symbol
Ba
Isotope.decay_product2
barium-137
Isotope.decay_mass2
137
Isotope.decay_symbol2
Ba
Isotope.mass
136.907

via Wikipedia infobox

Wikidata facts

Mass
136.907089464
Image
Cs-137 Pruefstrahler.JPG
Show 8 more facts
atomic number
55
neutron number
82
half-life
30.08
spin quantum number
3.5
parity quantum number
1
mass excess
-86545.606
binding energy
1149286.972
Commons category
Caesium-137
Sources (4)

via Wikidata · CC0

~16 min read

Article

25 sections
Contents
  • Decay
  • Uses
  • Health risks
  • Environmental contamination
  • Nuclear bomb fallout
  • <span lang="ru-Latn">Chernobyl</span> disaster
  • <span lang="ja-Latn">Fukushima Daiichi</span> disaster
  • Incidents and accidents
  • 1987 <span lang="pt-BR">Goiânia, Goiás</span>, Brazil
  • 1989 <span lang="uk-Latn">Kramatorsk</span>, Ukraine
  • 1994 <span lang="et">Tammiku</span>, Estonia
  • 1997 Georgia
  • 1998 <span lang="es-ES">Los Barrios, Cádiz</span>, Spain
  • 2009 <span lang="zh-Latn">Tongchuan, Shaanxi</span>, China
  • 2015 University of <span lang="no">Tromsø</span>, Norway
  • 2016 <span lang="fi">Helsinki</span>, Finland
  • 2019 Seattle, Washington, United States
  • 2023 Western Australia, Australia
  • 2023 <span lang="th-Latn">Prachinburi</span>, Thailand
  • 2024 <span lang="ru-Latn">Khabarovsk</span>, Russia
  • 2025 Indonesia and United States
  • See also
  • References
  • Bibliography
  • External links

Caesium-137 (), cesium-137 (US), or radiocaesium, is a radioactive isotope of caesium that is formed as one of the more common fission products by the nuclear fission of uranium-235 and other fissionable isotopes in nuclear reactors and nuclear weapons. Trace quantities also originate from spontaneous fission ofuranium-238. It is among the most problematic of the short-to-medium-lifetime fission products. Caesium has a relatively low boiling point of and easily becomes volatile when released suddenly at high temperature, as in the case of the nuclear accident and with nuclear explosions, and can travel very long distances in the air. After being deposited onto the soil as radioactive fallout, it moves and spreads easily in the environment because of the high water solubility of caesium's most common chemical compounds, which are salts. Caesium-137 was discovered by Glenn T. Seaborg and Margaret Melhase.

==Decay==

Gallery (3)

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