![]() Xe buildup in the reactor after a reduction in power or a shutdown and is often managed by letting the 135 The xenon pit is a phenomenon of excess neutron absorption through 135 Xe will be destroyed by neutron capture after a reactor shutdown, or in a molten salt reactor that continuously removes xenon from its fuel, a fast neutron reactor, or a nuclear weapon. Because of this, much of the 135Xe produced in current thermal reactors (as much as >90% at steady-state full power) will be converted to extremely long-lived (half-life on the order of 10 21 years) 136Ĭs despite the relatively short half life of 135 6.3333% for 235U and thermal neutrons) but also has the highest known thermal neutron capture cross section of any nuclide. Its precursor 135Xe has a high fission product yield (e.g. The low decay energy, lack of gamma radiation, and long half-life of 135Cs make this isotope much less hazardous than 137Cs or 134Cs. Except in the Molten salt reactor, where Cs-135 is created as a completely separate stream outside the fuel (after the decay of bubble-separated Xe-135). In most types of nuclear reprocessing, it stays with the medium-lived fission products (including 137Ĭs which can only be separated from Cs-135 via isotope separation) rather than with other long-lived fission products. Caesium-135 is one of the seven long-lived fission products and the only alkaline one. It decays via emission of a low-energy beta particle into the stable isotope barium-135. ^ Lower in thermal reactors because 135Xe, its predecessor, readily absorbs neutrons.Ĭaesium-135 is a mildly radioactive isotope of caesium with a half-life of 2.3 million years.^ Has decay energy 380 keV, but its decay product 126Sb has decay energy 3.67 MeV.^ Per 65 thermal neutron fissions of 235U and 35 of 239Pu.^ Decay energy is split among β, neutrino, and γ if any.134Cs also captures neutrons with a cross section of 140 barns, becoming long-lived radioactive 135Cs.Ĭaesium-134 undergoes beta decay (β −), producing 134Ba directly and emitting on average 2.23 gamma ray photons (mean energy 0.698 MeV). The proportion between the two will change with continued neutron irradiation. The combined yield of 133Cs and 134Cs is given as 6.7896%. It is also not produced by nuclear weapons because 133Cs is created by beta decay of original fission products only long after the nuclear explosion is over. Caesium-134 is not produced via beta decay of other fission product nuclides of mass 134 since beta decay stops at stable 134Xe. It is produced both directly (at a very small yield because 134Xe is stable) as a fission product and via neutron capture from nonradioactive 133Cs (neutron capture cross section 29 barns), which is a common fission product. The second, symbol s, is defined by taking the fixed numerical value of the caesium frequency, Δ ν Cs, the unperturbed ground-state hyperfine transition frequency of the caesium-133 atom, to be 9 192 631 770 when expressed in the unit Hz, which is equal to s −1.Ĭaesium-134 has a half-life of 2.0652 years. Since 1967, the official definition of a second is: The SI base unit of time, the second, is defined by a specific caesium-133 transition. ^ Theoretically capable of spontaneous fissionĬaesium-131, introduced in 2004 for brachytherapy by Isoray, has a half-life of 9.7 days and 30.4 keV energy.Ĭaesium-133 is the only stable isotope of caesium.^ a b # – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).^ ( ) spin value – Indicates spin with weak assignment arguments.^ Bold symbol as daughter – Daughter product is stable.^ Bold italics symbol as daughter – Daughter product is nearly stable.^ # – Atomic mass marked #: value and uncertainty derived not from purely experimental data, but at least partly from trends from the Mass Surface (TMS). ![]() ^ ( ) – Uncertainty (1 σ) is given in concise form in parentheses after the corresponding last digits.As a result, the input function of these isotopes can be estimated as a function of time. Once caesium enters the ground water, it is deposited on soil surfaces and removed from the landscape primarily by particle transport. All other isotopes have half-lives less than 2 weeks, most under an hour.īeginning in 1945 with the commencement of nuclear testing, caesium radioisotopes were released into the atmosphere where caesium is absorbed readily into solution and is returned to the surface of the Earth as a component of radioactive fallout. With a half-life of 30.1671 years and 134Cs with a half-life of 2.0652 years. The longest-lived radioisotopes are 135Cs with a half-life of 2.3 million years, 137 ![]() The atomic masses of these isotopes range from 112 to 151. ![]() Caesium ( 55Cs) has 40 known isotopes, making it, along with barium and mercury, one of the elements with the most isotopes.
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