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About: Uranium-234     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatFertileMaterials, within Data Space : dbpedia.org associated with source document(s)

Type: yago:Abstraction100002137yago:Actinoid114584110yago:Atom114619225yago:Group100031264yago:Isotope114619658yago:Material114580897yago:Matter100020827yago:Part113809207yago:PhysicalEntity100001930yago:Relation100031921yago:WikicatIsotopesOfUraniumdrugyago:Substance100019613yago:WikicatActinidesyago:WikicatFertileMaterials New Facet based on Instances of this Class

Uranium-234 (234U or U-234) is an isotope of uranium. In natural uranium and in uranium ore, 234U occurs as an indirect decay product of uranium-238, but it makes up only 0.0055% (55 parts per million) of the raw uranium because its half-life of just 245,500 years is only about 1/18,000 as long as that of 238U. Thus the rate of 234U to 238U in a natural sample is equivalent to the rate of their half lives to one another. The primary path of production of 234U via nuclear decay is as follows: uranium-238 nuclei emit an alpha particle to become thorium-234. Next, with a short half-life, 234Th nuclei emit a beta particle to become protactinium-234 (234Pa), or more likely a nuclear isomer denoted 234mPa. Finally, 234Pa or 234mPa nuclei emit another beta particle to become 234U nuclei.