Protactinium in the context of Uranium-234


Protactinium in the context of Uranium-234

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👉 Protactinium in the context of Uranium-234

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

Uranium-234 nuclei decay by alpha emission to thorium-230, except for the tiny fraction (here less than 2 per trillion) of nuclei that undergo spontaneous fission.

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Protactinium in the context of Uranium-233

Uranium-233 (
U
or U-233) is a fissile isotope of uranium that is bred from thorium-232 as part of the thorium fuel cycle. Uranium-233 was investigated for use in nuclear weapons and as a reactor fuel. It has been used successfully in experimental nuclear reactors and has been proposed for much wider use as a nuclear fuel. It has a half-life of 159,200 years to alpha decay and is a part of the neptunium decay chain.

Uranium-233 is produced by the neutron irradiation of thorium-232. When thorium-232 absorbs a neutron, it becomes thorium-233, which has a half-life of about 22 minutes. Thorium-233 decays into protactinium-233 through beta decay. Protactinium-233 has a longer half-life of about 27 days to further decay into uranium-233; some proposed molten salt reactor designs attempt to physically isolate the protactinium from further neutron capture before beta decay can occur, to maintain the neutron economy (if it misses the U window, the next fissile target is U, meaning a total of 4 neutrons needed to trigger fission).

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Protactinium in the context of Mononuclidic element

A mononuclidic element or monotopic element is one of the 21 chemical elements that is found naturally on Earth essentially as a single nuclide (which may, or may not, be a stable nuclide). This single nuclide will have a characteristic atomic mass. Thus, the element's natural isotopic abundance is dominated by one isotope that is either stable or very long-lived. There are 19 elements in the first category (which are both monoisotopic and mononuclidic), and 2 (bismuth and protactinium) in the second category (mononuclidic but not monoisotopic, since they have zero, not one, stable nuclides). A list of the 21 mononuclidic elements is given at the end of this article.

Of the 26 monoisotopic elements that, by definition, have only one stable isotope, seven are not considered mononuclidic, due to the presence of a significant fraction of a very long-lived (primordial) radioisotope. These elements are vanadium, rubidium, indium, lanthanum, europium, lutetium, and rhenium.

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Protactinium in the context of Kazimierz Fajans

Kazimierz Fajans (Kasimir Fajans in many American publications; 27 May 1887 – 18 May 1975) was a Polish-Jewish physical chemist, a pioneer in the science of radioactivity and the co-discoverer of chemical element protactinium.

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Protactinium in the context of Isotopes of protactinium

Protactinium (91Pa) has no stable isotopes. As Pa occurs in usable quantity, and comprises virtually all of the element, it defines the standard atomic weight.

Thirty radioisotopes of protactinium have been characterized, ranging from Pa to Pa. The most stable isotopes are Pa with a half-life of 32,700 years, Pa with a half-life of 26.975 days, and Pa with a half-life of 17.4 days. All of the remaining radioactive isotopes have half-lives less than 1.6 days, and the majority of these have half-lives less than 1.8 seconds. This element also has five meta states, Pa (t1/2 1.15 milliseconds), Pa (t1/2 = 308 nanoseconds), Pa (t1/2 = 69 nanoseconds), Pa (t1/2 = 420 nanoseconds), and Pa (t1/2 = 1.16 minutes).

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