Xenon-132
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Naturally occurring xenon (54Xe) consists of seven
stable A stable is a building in which livestock, especially horses, are kept. It most commonly means a building that is divided into separate stalls for individual animals and livestock. There are many different types of stables in use today; the ...
isotopes and two very long-lived isotopes. Double electron capture has been observed in 124Xe (half-life ) and double beta decay in 136Xe (half-life ), which are among the longest measured half-lives of all nuclides. The isotopes 126Xe and 134Xe are also predicted to undergo double beta decay, but this has never been observed in these isotopes, so they are considered to be stable. Beyond these stable forms, 32 artificial
unstable isotope In numerous fields of study, the component of instability within a system is generally characterized by some of the outputs or internal states growing without bounds. Not all systems that are not stable are unstable; systems can also be mar ...
s and various isomers have been studied, the longest-lived of which is 127Xe with a half-life of 36.345 days. All other isotopes have half-lives less than 12 days, most less than 20 hours. The shortest-lived isotope, 108Xe, has a half-life of 58 μs, and is the heaviest known nuclide with equal numbers of protons and neutrons. Of known isomers, the longest-lived is 131mXe with a half-life of 11.934 days. 129Xe is produced by beta decay of 129I ( half-life: 16 million years); 131mXe, 133Xe, 133mXe, and 135Xe are some of the
fission product Nuclear fission products are the atomic fragments left after a large atomic nucleus undergoes nuclear fission. Typically, a large nucleus like that of uranium fissions by splitting into two smaller nuclei, along with a few neutrons, the release ...
s of both 235U and 239Pu, so are used as indicators of nuclear explosions. The artificial isotope 135Xe is of considerable significance in the operation of nuclear fission reactors. 135Xe has a huge cross section for thermal neutrons, 2.65×106 barns, so it acts as a neutron absorber or "
poison Poison is a chemical substance that has a detrimental effect to life. The term is used in a wide range of scientific fields and industries, where it is often specifically defined. It may also be applied colloquially or figuratively, with a broa ...
" that can slow or stop the chain reaction after a period of operation. This was discovered in the earliest nuclear reactors built by the American Manhattan Project for plutonium production. Because of this effect, designers must make provisions to increase the reactor's reactivity (the number of neutrons per fission that go on to fission other atoms of nuclear fuel) over the initial value needed to start the chain reaction. For the same reason, the fission products produced in a nuclear explosion and a power plant differ significantly as a large share of will absorb neutrons in a steady state reactor, while basically none of the will have had time to decay to Xenon before the explosion of the bomb removes it from the neutron radiation. Relatively high concentrations of radioactive xenon isotopes are also found emanating from nuclear reactors due to the release of this fission gas from cracked fuel rods or fissioning of uranium in cooling water. The concentrations of these isotopes are still usually low compared to the naturally occurring radioactive noble gas 222Rn. Because xenon is a
tracer Tracer may refer to: Science * Flow tracer, any fluid property used to track fluid motion * Fluorescent tracer, a substance such as 2-NBDG containing a fluorophore that is used for tracking purposes * Histochemical tracer, a substance used for tr ...
for two
parent isotope In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directly ...
s, Xe isotope ratios in
meteorite A meteorite is a solid piece of debris from an object, such as a comet, asteroid, or meteoroid, that originates in outer space and survives its passage through the atmosphere to reach the surface of a planet or Natural satellite, moon. When the ...
s are a powerful tool for studying the
formation of the solar system The formation of the Solar System began about 4.6 billion years ago with the gravitational collapse of a small part of a giant molecular cloud. Most of the collapsing mass collected in the center, forming the Sun, while the rest flattened into a ...
. The I-Xe method of dating gives the time elapsed between nucleosynthesis and the condensation of a solid object from the
solar nebula The formation of the Solar System began about 4.6 billion years ago with the gravitational collapse of a small part of a giant molecular cloud. Most of the collapsing mass collected in the center, forming the Sun, while the rest flattened into a ...
(xenon being a gas, only that part of it that formed after condensation will be present inside the object). Xenon isotopes are also a powerful tool for understanding terrestrial differentiation. Excess 129Xe found in carbon dioxide well gases from New Mexico was believed to be from the decay of
mantle A mantle is a piece of clothing, a type of cloak. Several other meanings are derived from that. Mantle may refer to: *Mantle (clothing), a cloak-like garment worn mainly by women as fashionable outerwear **Mantle (vesture), an Eastern Orthodox ve ...
-derived gases soon after Earth's formation. It has been suggested that the isotopic composition of atmospheric xenon fluctuated prior to the GOE before stabilizing, perhaps as a result of the rise in atmospheric O2.


List of isotopes

, - , 108Xe , style="text-align:right" , 54 , style="text-align:right" , 54 , , 58(+106−23) μs , α , 104Te , 0+ , , , - , 109Xe , style="text-align:right" , 54 , style="text-align:right" , 55 , , 13(2) ms , α , 105Te , , , , - , rowspan=2, 110Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 56 , rowspan=2, 109.94428(14) , rowspan=2, 310(190) ms
05(+35−25) ms, β+ , 110I , rowspan=2, 0+ , rowspan=2, , rowspan=2, , - , α , 106Te , - , rowspan=2, 111Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 57 , rowspan=2, 110.94160(33)# , rowspan=2, 740(200) ms , β+ (90%) , 111I , rowspan=2, 5/2+# , rowspan=2, , rowspan=2, , - , α (10%) , 107Te , - , rowspan=2, 112Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 58 , rowspan=2, 111.93562(11) , rowspan=2, 2.7(8) s , β+ (99.1%) , 112I , rowspan=2, 0+ , rowspan=2, , rowspan=2, , - , α (.9%) , 108Te , - , rowspan=4, 113Xe , rowspan=4 style="text-align:right" , 54 , rowspan=4 style="text-align:right" , 59 , rowspan=4, 112.93334(9) , rowspan=4, 2.74(8) s , β+ (92.98%) , 113I , rowspan=4, (5/2+)# , rowspan=4, , rowspan=4, , - , β+, p (7%) , 112Te , - , α (.011%) , 109Te , - , β+, α (.007%) , 109Sb , - , 114Xe , style="text-align:right" , 54 , style="text-align:right" , 60 , 113.927980(12) , 10.0(4) s , β+ , 114I , 0+ , , , - , rowspan=3, 115Xe , rowspan=3 style="text-align:right" , 54 , rowspan=3 style="text-align:right" , 61 , rowspan=3, 114.926294(13) , rowspan=3, 18(4) s , β+ (99.65%) , 115I , rowspan=3, (5/2+) , rowspan=3, , rowspan=3, , - , β+, p (.34%) , 114Te , - , β+, α (3×10−4%) , 111Sb , - , 116Xe , style="text-align:right" , 54 , style="text-align:right" , 62 , 115.921581(14) , 59(2) s , β+ , 116I , 0+ , , , - , rowspan=2, 117Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 63 , rowspan=2, 116.920359(11) , rowspan=2, 61(2) s , β+ (99.99%) , 117I , rowspan=2, 5/2(+) , rowspan=2, , rowspan=2, , - , β+, p (.0029%) , 116Te , - , 118Xe , style="text-align:right" , 54 , style="text-align:right" , 64 , 117.916179(11) , 3.8(9) min , β+ , 118I , 0+ , , , - , 119Xe , style="text-align:right" , 54 , style="text-align:right" , 65 , 118.915411(11) , 5.8(3) min , β+ , 119I , 5/2(+) , , , - , 120Xe , style="text-align:right" , 54 , style="text-align:right" , 66 , 119.911784(13) , 40(1) min , β+ , 120I , 0+ , , , - , 121Xe , style="text-align:right" , 54 , style="text-align:right" , 67 , 120.911462(12) , 40.1(20) min , β+ , 121I , (5/2+) , , , - , 122Xe , style="text-align:right" , 54 , style="text-align:right" , 68 , 121.908368(12) , 20.1(1) h , β+ , 122I , 0+ , , , - , 123Xe , style="text-align:right" , 54 , style="text-align:right" , 69 , 122.908482(10) , 2.08(2) h , EC , 123I , 1/2+ , , , - , style="text-indent:1em" , 123mXe , colspan="3" style="text-indent:2em" , 185.18(22) keV , 5.49(26) μs , , , 7/2(−) , , , - , 124Xe
Primordial Primordial may refer to: * Primordial era, an era after the Big Bang. See Chronology of the universe * Primordial sea (a.k.a. primordial ocean, ooze or soup). See Abiogenesis * Primordial nuclide, nuclides, a few radioactive, that formed before ...
radionuclide A radionuclide (radioactive nuclide, radioisotope or radioactive isotope) is a nuclide that has excess nuclear energy, making it unstable. This excess energy can be used in one of three ways: emitted from the nucleus as gamma radiation; transfer ...
, style="text-align:right" , 54 , style="text-align:right" , 70 , 123.905893(2) , 1.8(0.5 (stat), 0.1 (sys)) y , Double EC , 124Te , 0+ , 9.52(3)×10−4 , , - , 125Xe , style="text-align:right" , 54 , style="text-align:right" , 71 , 124.9063955(20) , 16.9(2) h , β+ , 125I , 1/2(+) , , , - , style="text-indent:1em" , 125m1Xe , colspan="3" style="text-indent:2em" , 252.60(14) keV , 56.9(9) s , IT , 125Xe , 9/2(−) , , , - , style="text-indent:1em" , 125m2Xe , colspan="3" style="text-indent:2em" , 295.86(15) keV , 0.14(3) μs , , , 7/2(+) , , , - , 126Xe , style="text-align:right" , 54 , style="text-align:right" , 72 , 125.904274(7) , colspan=3 align=center, Observationally StableSuspected of undergoing β+β+ decay to 126Te , 0+ , 8.90(2)×10−4 , , - , 127Xe , style="text-align:right" , 54 , style="text-align:right" , 73 , 126.905184(4) , 36.345(3) d , EC , 127I , 1/2+ , , , - , style="text-indent:1em" , 127mXe , colspan="3" style="text-indent:2em" , 297.10(8) keV , 69.2(9) s , IT , 127Xe , 9/2− , , , - , 128Xe , style="text-align:right" , 54 , style="text-align:right" , 74 , 127.9035313(15) , colspan=3 align=center, StableTheoretically capable of
spontaneous fission Spontaneous fission (SF) is a form of radioactive decay that is found only in very heavy chemical elements. The nuclear binding energy of the elements reaches its maximum at an atomic mass number of about 56 (e.g., iron-56); spontaneous breakdo ...
, 0+ , 0.019102(8) , , - , 129XeUsed in a method of radiodating groundwater and to infer certain events in the Solar System's history , style="text-align:right" , 54 , style="text-align:right" , 75 , 128.9047794(8) , colspan=3 align=center, Stable , 1/2+ , 0.264006(82) , , - , style="text-indent:1em" , 129mXe , colspan="3" style="text-indent:2em" , 236.14(3) keV , 8.88(2) d , IT , 129Xe , 11/2− , , , - , 130Xe , style="text-align:right" , 54 , style="text-align:right" , 76 , 129.9035080(8) , colspan=3 align=center, Stable , 0+ , 0.040710(13) , , - , 131Xe
Fission product Nuclear fission products are the atomic fragments left after a large atomic nucleus undergoes nuclear fission. Typically, a large nucleus like that of uranium fissions by splitting into two smaller nuclei, along with a few neutrons, the release ...
, style="text-align:right" , 54 , style="text-align:right" , 77 , 130.9050824(10) , colspan=3 align=center, Stable , 3/2+ , 0.212324(30) , , - , style="text-indent:1em" , 131mXe , colspan="3" style="text-indent:2em" , 163.930(8) keV , 11.934(21) d , IT , 131Xe , 11/2− , , , - , 132Xe , style="text-align:right" , 54 , style="text-align:right" , 78 , 131.9041535(10) , colspan=3 align=center, Stable , 0+ , 0.269086(33) , , - , style="text-indent:1em" , 132mXe , colspan="3" style="text-indent:2em" , 2752.27(17) keV , 8.39(11) ms , IT , 132Xe , (10+) , , , - , 133XeHas medical uses , style="text-align:right" , 54 , style="text-align:right" , 79 , 132.9059107(26) , 5.2475(5) d , β , 133Cs , 3/2+ , , , - , style="text-indent:1em" , 133mXe , colspan="3" style="text-indent:2em" , 233.221(18) keV , 2.19(1) d , IT , 133Xe , 11/2− , , , - , 134Xe , style="text-align:right" , 54 , style="text-align:right" , 80 , 133.9053945(9) , colspan=3 align=center, Observationally StableSuspected of undergoing ββ decay to 134Ba with a half-life over 11×1015 years , 0+ , 0.104357(21) , , - , style="text-indent:1em" , 134m1Xe , colspan="3" style="text-indent:2em" , 1965.5(5) keV , 290(17) ms , IT , 134Xe , 7− , , , - , style="text-indent:1em" , 134m2Xe , colspan="3" style="text-indent:2em" , 3025.2(15) keV , 5(1) μs , , , (10+) , , , - , 135XeMost powerful known neutron absorber, produced in nuclear power plants as a
decay product In nuclear physics, a decay product (also known as a daughter product, daughter isotope, radio-daughter, or daughter nuclide) is the remaining nuclide left over from radioactive decay. Radioactive decay often proceeds via a sequence of steps ( ...
of 135I, itself a decay product of 135Te, a
fission product Nuclear fission products are the atomic fragments left after a large atomic nucleus undergoes nuclear fission. Typically, a large nucleus like that of uranium fissions by splitting into two smaller nuclei, along with a few neutrons, the release ...
. Normally absorbs neutrons in the high neutron flux environments to become ''136Xe''; see iodine pit for more information
, style="text-align:right" , 54 , style="text-align:right" , 81 , 134.907227(5) , 9.14(2) h , β , 135Cs , 3/2+ , , , - , rowspan=2 style="text-indent:1em" , 135mXe , rowspan=2 colspan="3" style="text-indent:2em" , 526.551(13) keV , rowspan=2, 15.29(5) min , IT (99.99%) , 135Xe , rowspan=2, 11/2− , rowspan=2, , rowspan=2, , - , β (.004%) , 135Cs , - , 136Xe
Primordial Primordial may refer to: * Primordial era, an era after the Big Bang. See Chronology of the universe * Primordial sea (a.k.a. primordial ocean, ooze or soup). See Abiogenesis * Primordial nuclide, nuclides, a few radioactive, that formed before ...
radionuclide A radionuclide (radioactive nuclide, radioisotope or radioactive isotope) is a nuclide that has excess nuclear energy, making it unstable. This excess energy can be used in one of three ways: emitted from the nucleus as gamma radiation; transfer ...
, style="text-align:right" , 54 , style="text-align:right" , 82 , 135.907219(8) , 2.165(0.016 (stat), 0.059 (sys)) y , ββ , 136Ba , 0+ , 0.088573(44) , , - , style="text-indent:1em" , 136mXe , colspan="3" style="text-indent:2em" , 1891.703(14) keV , 2.95(9) μs , , , 6+ , , , - , 137Xe , style="text-align:right" , 54 , style="text-align:right" , 83 , 136.911562(8) , 3.818(13) min , β , 137Cs , 7/2− , , , - , 138Xe , style="text-align:right" , 54 , style="text-align:right" , 84 , 137.91395(5) , 14.08(8) min , β , 138Cs , 0+ , , , - , 139Xe , style="text-align:right" , 54 , style="text-align:right" , 85 , 138.918793(22) , 39.68(14) s , β , 139Cs , 3/2− , , , - , 140Xe , style="text-align:right" , 54 , style="text-align:right" , 86 , 139.92164(7) , 13.60(10) s , β , 140Cs , 0+ , , , - , rowspan=2, 141Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 87 , rowspan=2, 140.92665(10) , rowspan=2, 1.73(1) s , β (99.45%) , 141Cs , rowspan=2, 5/2(−#) , rowspan=2, , rowspan=2, , - , β, n (.043%) , 140Cs , - , rowspan=2, 142Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 88 , rowspan=2, 141.92971(11) , rowspan=2, 1.22(2) s , β (99.59%) , 142Cs , rowspan=2, 0+ , rowspan=2, , rowspan=2, , - , β, n (.41%) , 141Cs , - , 143Xe , style="text-align:right" , 54 , style="text-align:right" , 89 , 142.93511(21)# , 0.511(6) s , β , 143Cs , 5/2− , , , - , rowspan=2, 144Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 90 , rowspan=2, 143.93851(32)# , rowspan=2, 0.388(7) s , β , 144Cs , rowspan=2, 0+ , rowspan=2, , rowspan=2, , - , β, n , 143Cs , - , 145Xe , style="text-align:right" , 54 , style="text-align:right" , 91 , 144.94407(32)# , 188(4) ms , β , 145Cs , (3/2−)# , , , - , 146Xe , style="text-align:right" , 54 , style="text-align:right" , 92 , 145.94775(43)# , 146(6) ms , β , 146Cs , 0+ , , , - , rowspan=2, 147Xe , rowspan=2 style="text-align:right" , 54 , rowspan=2 style="text-align:right" , 93 , rowspan=2, 146.95356(43)# , rowspan=2, 130(80) ms
.10(+10−5) s, β , 147Cs , rowspan=2, 3/2−# , rowspan=2, , rowspan=2, , - , β, n , 146Cs * The isotopic composition refers to that in air.


Xenon-124

Xenon-124 is an isotope of xenon that undergoes double electron capture to tellurium-124 with a very long half life of years, more than 12 orders of magnitude longer than the age of the universe (). Such decays have been observed in the
XENON1T Xenon is a chemical element with the symbol Xe and atomic number 54. It is a dense, colorless, odorless noble gas found in Earth's atmosphere in trace amounts. Although generally unreactive, it can undergo a few chemical reactions such as the ...
detector in 2019, and are the rarest processes ever directly observed. (Even slower decays of other nuclei have been measured, but by detecting decay products that have accumulated over billions of years rather than observing them directly.)


Xenon-133

Xenon-133 (sold as a drug under the brand name ''Xeneisol'', ATC code ) is an isotope of xenon. It is a
radionuclide A radionuclide (radioactive nuclide, radioisotope or radioactive isotope) is a nuclide that has excess nuclear energy, making it unstable. This excess energy can be used in one of three ways: emitted from the nucleus as gamma radiation; transfer ...
that is
inhaled Inhalation (or Inspiration) happens when air or other gases enter the lungs. Inhalation of air Inhalation of air, as part of the cycle of breathing, is a vital process for all human life. The process is autonomic (though there are exceptions ...
to assess pulmonary function, and to image the
lung The lungs are the primary organs of the respiratory system in humans and most other animals, including some snails and a small number of fish. In mammals and most other vertebrates, two lungs are located near the backbone on either side of t ...
s. It is also used to image blood flow, particularly in the brain. 133Xe is also an important
fission product Nuclear fission products are the atomic fragments left after a large atomic nucleus undergoes nuclear fission. Typically, a large nucleus like that of uranium fissions by splitting into two smaller nuclei, along with a few neutrons, the release ...
. It is discharged to the atmosphere in small quantities by some nuclear power plants.


Xenon-135

Xenon-135 is a radioactive isotope of xenon, produced as a
fission product Nuclear fission products are the atomic fragments left after a large atomic nucleus undergoes nuclear fission. Typically, a large nucleus like that of uranium fissions by splitting into two smaller nuclei, along with a few neutrons, the release ...
of uranium. It has a half-life of about 9.2 hours and is the most powerful known neutron-absorbing nuclear poison (having a neutron absorption cross-section of 2 million barnsChart of the Nuclides 13th Edition). The overall yield of xenon-135 from fission is 6.3%, though most of this results from the radioactive decay of fission-produced tellurium-135 and iodine-135. Xe-135 exerts a significant effect on nuclear reactor operation (
xenon pit The iodine pit, also called the iodine hole or xenon pit, is a temporary disabling of a nuclear reactor due to buildup of short- lived nuclear poisons in the reactor core. The main isotope responsible is 135Xe, mainly produced by natural decay of ...
). It is discharged to the atmosphere in small quantities by some nuclear power plants.


Xenon-136

Xenon-136 is an isotope of xenon that undergoes double beta decay to
barium Barium is a chemical element with the symbol Ba and atomic number 56. It is the fifth element in group 2 and is a soft, silvery alkaline earth metal. Because of its high chemical reactivity, barium is never found in nature as a free element. Th ...
-136 with a very long half life of years, more than 10 orders of magnitude longer than the age of the universe (). It is being used in the Enriched Xenon Observatory experiment to search for neutrinoless double beta decay.


See also

*
Xenon isotope geochemistry Xenon isotope geochemistry uses the abundance of xenon (Xe) isotopes and total xenon to investigate how Xe has been generated, transported, fractionated, and distributed in planetary systems. Xe has nine stable or very long-lived isotopes. Radiogeni ...


References

* Isotope masses fro
Ame2003 Atomic Mass Evaluation
by Georges Audi, Aaldert Hendrik Wapstra, Catherine Thibault, Jean Blachot and Olivier Bersillon in ''Nuclear Physics'' A729 (2003). * Isotopic compositions and standard atomic masses from: ** ** * Half-life, spin, and isomer data selected from the following sources. ** ** ** {{Navbox element isotopes Xenon Xenon