Uranium-238: Difference between revisions
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'''Uranium-238''' ('''U-238''') is the most common isotope of [[uranium]] found in nature, with a | == Uranium-238 == | ||
[[File:Uranium03.jpg|thumb|right|Uranium ore containing uranium-238]] | |||
'''Uranium-238''' ('''U-238''') is the most common isotope of [[uranium]] found in nature, with a natural abundance of approximately 99.3%. It is a [[radioactive]] isotope with a half-life of about 4.468 billion years, making it useful for dating the age of the Earth. | |||
== Properties == | == Properties == | ||
Uranium-238 is a [[heavy metal]] with a [[density]] of about 19.1 g/cm_. It is weakly radioactive and undergoes [[alpha decay]] to form [[thorium-234]]. The decay chain of uranium-238, known as the [[uranium series]], eventually leads to the formation of [[lead-206]]. | |||
== Uses == | == Uses == | ||
== | Uranium-238 is not directly usable as [[nuclear fuel]] in its natural form, but it can be converted into [[plutonium-239]] through neutron capture and subsequent beta decay. Plutonium-239 is a fissile material that can be used in [[nuclear reactors]] and [[nuclear weapons]]. | ||
Uranium-238 is also used in [[depleted uranium]] applications, such as in armor-piercing projectiles and radiation shielding, due to its high density. | |||
== Occurrence == | |||
Uranium-238 is found in [[uranium ore]]s such as [[uraninite]] and [[carnotite]]. It is extracted through mining and then processed to separate it from other isotopes and impurities. | |||
== Health and Safety == | |||
While uranium-238 is less radioactive than other isotopes of uranium, it is still a health hazard if ingested or inhaled. Proper precautions must be taken when handling uranium and its compounds to prevent exposure to radiation and chemical toxicity. | |||
== | == Related pages == | ||
* [[Uranium-235]] | |||
* [[Nuclear fission]] | |||
* [[Radioactive decay]] | |||
* [[Nuclear reactor]] | |||
== | == References == | ||
{{reflist}} | |||
[[Category:Uranium]] | |||
[[Category:Isotopes]] | |||
[[Category:Nuclear materials]] | |||
Revision as of 11:56, 9 February 2025
Uranium-238

Uranium-238 (U-238) is the most common isotope of uranium found in nature, with a natural abundance of approximately 99.3%. It is a radioactive isotope with a half-life of about 4.468 billion years, making it useful for dating the age of the Earth.
Properties
Uranium-238 is a heavy metal with a density of about 19.1 g/cm_. It is weakly radioactive and undergoes alpha decay to form thorium-234. The decay chain of uranium-238, known as the uranium series, eventually leads to the formation of lead-206.
Uses
Uranium-238 is not directly usable as nuclear fuel in its natural form, but it can be converted into plutonium-239 through neutron capture and subsequent beta decay. Plutonium-239 is a fissile material that can be used in nuclear reactors and nuclear weapons.
Uranium-238 is also used in depleted uranium applications, such as in armor-piercing projectiles and radiation shielding, due to its high density.
Occurrence
Uranium-238 is found in uranium ores such as uraninite and carnotite. It is extracted through mining and then processed to separate it from other isotopes and impurities.
Health and Safety
While uranium-238 is less radioactive than other isotopes of uranium, it is still a health hazard if ingested or inhaled. Proper precautions must be taken when handling uranium and its compounds to prevent exposure to radiation and chemical toxicity.
Related pages
References
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