Isotopes of zirconium

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Naturally occurring zirconium (40Zr) is composed of four stable isotopes (one, 94Zr, may in the future be found radioactive), and one very long-lived radioisotope (96Zr), a primordial nuclide that decays via double beta decay with an observed half-life of 2.34 × 1019 years;[4] it can also undergo single beta decay, which is not yet observed, but the theoretically predicted value of t1/2 is 2.4 × 1020 years.[5] The second most stable radioisotope is 93Zr, which has a half-life of 1.61 million years. Thirty other radioisotopes have been observed from 77Zr to 114Zr; all have half-lives less than a day except for 95Zr (64.032 days), 88Zr (83.4 days), and 89Zr (78.36 hours). The most stable of the isomeric states is just 4.16 minutes for 89mZr.

Quick facts Main isotopes, Decay ...
Isotopes of zirconium (40Zr)
Main isotopes[1] Decay
Isotope abun­dance half-life (t1/2) mode pro­duct
88Zr synth 83.4 d ε 88Y
89Zr synth 78.36 h β+ 89Y
90Zr 51.5% stable
91Zr 11.2% stable
92Zr 17.1% stable
93Zr trace 1.61×106 y β 93Nb
94Zr 17.4% stable
95Zr synth 64.032 d β 95Nb
96Zr 2.80% 2.34×1019 y ββ 96Mo
Standard atomic weight Ar°(Zr)
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Radioactive isotopes above the theoretically stable mass numbers 90-92 decay by electron emission resulting in niobium isotopes, whereas those below by positron emission or electron capture, resulting in yttrium isotopes.

List of isotopes


More information Nuclide, Z ...
Nuclide
[n 1]
Z N Isotopic mass (Da)[6]
[n 2][n 3]
Discovery
year[7][8]
Half-life[1]
[n 4][n 5]
Decay
mode
[1]
Daughter
isotope

[n 6]
Spin and
parity[1]
[n 7][n 5]
Natural abundance (mole fraction)
Excitation energy Normal proportion[1] Range of variation
77Zr 40 37 76.96608(43)# 2017 100# μs 3/2−#
78Zr 40 38 77.95615(43)# 2001 50# ms
[>200 ns]
0+
79Zr 40 39 78.94979(32)# 1999 56(30) ms β+ 79Y 5/2+#
80Zr 40 40 79.940818(86)[9] 1987 4.6(6) s β+ 80Y 0+
81Zr 40 41 80.938211(11)[9] 1997 5.5(4) s β+ (99.88%) 81Y (3/2−)
β+, p (0.12%) 80Sr
82Zr 40 42 81.9317075(17) 1982 32(5) s β+ 82Y 0+
83Zr 40 43 82.92923591(70)[9] 1974 42(2) s β+ 83Y 1/2−#
β+, p (?%) 82Sr
83m1Zr 52.72(5) keV 1988 0.53(12) μs IT 83Zr (5/2−)
83m2Zr 77.04(7) keV 1988 1.8(1) μs IT 83Zr (7/2+)
84Zr 40 44 83.9233257(59) 1977 25.8(5) min β+ 84Y 0+
85Zr 40 45 84.9214432(69) 1963 7.86(4) min β+ 85Y (7/2+)
85mZr 292.2(3) keV 1976 10.9(3) s IT (?%) 85Zr 1/2−#
β+ (?%) 85Y
86Zr 40 46 85.9162968(38) 1951 16.5(1) h β+ 86Y 0+
87Zr 40 47 86.9148173(45) 1949 1.68(1) h β+ 87Y 9/2+
87mZr 335.84(19) keV 1972 14.0(2) s IT 87Zr 1/2−
88Zr[n 8] 40 48 87.9102207(58) 1951 83.4(3) d EC 88Y 0+
88mZr 2887.79(6) keV 1971 1.320(25) μs IT 88Zr 8+
89Zr 40 49 88.9088798(30) 1938 78.360(23) h β+ 89Y 9/2+
89mZr 587.82(10) keV 1940 4.161(10) min IT (93.77%) 89Zr 1/2−
β+ (6.23%) 89Y
90Zr[n 9] 40 50 89.90469876(13) 1924 Stable 0+ 0.5145(4)
90m1Zr 2319.000(9) keV 1963 809.2(20) ms IT 90Zr 5-
90m2Zr 3589.418(15) keV 1959 131(4) ns IT 90Zr 8+
91Zr[n 9] 40 51 90.90564021(10) 1934 Stable 5/2+ 0.1122(5)
91mZr 3167.3(4) keV 1975 4.35(14) μs IT 91Zr (21/2+)
92Zr[n 9] 40 52 91.90503534(10) 1924 Stable 0+ 0.1715(3)
93Zr[n 10] 40 53 92.90647066(49) 1950 1.61(5)×106 y β (73%)[10] 93m1Nb 5/2+
β (27%)[10] 93Nb
94Zr[n 9] 40 54 93.90631252(18) 1924 Observationally stable[n 11] 0+ 0.1738(4)
95Zr[n 9] 40 55 94.90804028(93) 1946 64.032(6) d β 95Nb 5/2+
96Zr[n 9][n 12] 40 56 95.90827762(12) 1934 2.34(17)×1019 y ββ[n 13] 96Mo 0+ 0.0280(2)
97Zr 40 57 96.91096380(13) 1951 16.749(8) h β 97mNb 1/2+
97mZr 1264.35(16) keV 1985 104.8(17) ns IT 97Zr 7/2+
98Zr 40 58 97.9127404(91) 1967 30.7(4) s β 98Nb 0+
98mZr 6601.9(11) keV 2006 1.9(2) μs IT 98Zr (17−)
99Zr 40 59 98.916675(11) 1970 2.1(1) s β 99mNb 1/2+
99mZr 251.96(9) keV 1970 336(5) ns IT 99Zr 7/2+
100Zr 40 60 99.9180105(87) 1970 7.1(4) s β 100Nb 0+
101Zr 40 61 100.9214585(89) 1970 2.29(8) s β 101Nb 3/2+
102Zr 40 62 101.9231542(94) 1970 2.01(8) s β 102Nb 0+
103Zr 40 63 102.9272041(99) 1987 1.38(7) s β (>99%) 103Nb (5/2−)
β, n (<1%) 102Nb
104Zr 40 64 103.929449(10) 1990 920(28) ms β (>99%) 104Nb 0+
β, n (<1%) 103Nb
105Zr 40 65 104.934022(13) 1992 670(28) ms β (>98%) 105Nb 1/2+#
β, n (<2%) 104Nb
106Zr 40 66 105.93693(22)# 1994 179(6) ms β (>98%) 106Nb 0+
β, n (<2%) 105Nb
107Zr 40 67 106.94201(32)# 1994 145.7(24) ms β (>77%) 107Nb 5/2+#
β, n (<23%) 106Nb
108Zr 40 68 107.94530(43)# 1997 78.5(20) ms β 108Nb 0+
108mZr 2074.5(8) keV 2011 540(30) ns IT 108Zr (6+)
109Zr 40 69 108.95091(54)# 1997 56(3) ms β 109Nb 5/2+#
110Zr 40 70 109.95468(54)# 1997 37.5(20) ms β 110Nb 0+
111Zr 40 71 110.96084(64)# 2010 24.0(5) ms β 111Nb 5/2+#
112Zr 40 72 111.96520(75)# 2010 43(21) ms β 112Nb 0+
113Zr 40 73 112.97172(32)# 2018 15# ms
[>550 ns]
3/2+
114Zr[12] 40 74 2021 0+
This table header & footer:
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  1. mZr  Excited nuclear isomer.
  2. ()  Uncertainty (1σ) is given in concise form in parentheses after the corresponding last digits.
  3. #  Atomic mass marked #: value and uncertainty derived not from purely experimental data, but at least partly from trends from the Mass Surface (TMS).
  4. Bold half-life  nearly stable, half-life longer than age of universe.
  5. #  Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
  6. Bold symbol as daughter  Daughter product is stable.
  7. () spin value  Indicates spin with weak assignment arguments.
  8. Second most powerful known neutron absorber
  9. Believed to decay by ββ to 94Mo with a half-life over 1.1×1017 years
  10. Theorized to also undergo β decay to 96Nb with a partial half-life greater than 2.4×1019 y[11]

Zirconium-88

88Zr is a radioisotope of zirconium with a half-life of 83.4 days. In January 2019, this isotope was discovered to have a thermal neutron capture cross section of approximately 861,000 barns; this is several orders of magnitude greater than predicted, and greater than that of any other nuclide except xenon-135.[13]

Zirconium-89

89Zr is a radioisotope of zirconium with a half-life of 78.36 hours, produced by proton irradiation of natural yttrium (89Y). Its most prominent gamma photon (99% of decays) has an energy of 909 keV and it emits a positron (as opposed to electron capture) about 23% of decays.[14] Zirconium-89 is employed in specialized diagnostic applications using positron emission tomography[15] imaging, for example, with zirconium-89 labeled antibodies (immuno-PET).[16]

Zirconium-93

More information Thermal, Fast ...
Yield, % per fission[17]
Thermal Fast 14 MeV
232Th not fissile 6.70 ± 0.40 5.58 ± 0.16
233U 6.979 ± 0.098 6.94 ± 0.07 5.38 ± 0.32
235U 6.346 ± 0.044 6.25 ± 0.04 5.19 ± 0.31
238U not fissile 4.913 ± 0.098 4.53 ± 0.13
239Pu 3.80 ± 0.03 3.82 ± 0.03 3.0 ± 0.3
241Pu 2.98 ± 0.04 2.98 ± 0.33 ?
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More information Nuclide, t1⁄2 ...
Nuclide t12 Yield Q[a 1] βγ
(Ma) (%)[a 2] (keV)
99Tc 0.2116.1385294 β
126Sn 0.230.10844050[a 3] βγ
79Se 0.330.0447151 β
135Cs 1.336.9110[a 4]269 β
93Zr 1.615.457591 βγ
107Pd 6.51.249933 β
129I 16.10.8410194 βγ
  1. Decay energy is split among β, neutrino, and γ if any.
  2. Per 65 thermal neutron fissions of 235U and 35 of 239Pu.
  3. Has decay energy 380 keV, but its decay product 126Sb has decay energy 3.67 MeV.
  4. Lower in thermal reactors because 135Xe, its predecessor, readily absorbs neutrons.
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93Zr is a radioisotope of zirconium with a half-life of 1.61 million years, decaying through emission of a low-energy beta particle. 73% of decays populate an excited state of niobium-93, which decays with a half-life of 13.9 years (almost entirely by internal conversion, emitting no gamma ray) to the stable ground state of 93Nb, while the remaining 27% of decays directly populate the ground state.[10] It is one of the 7 long-lived fission products. The low specific activity and low energy of its radiation limit the radioactive hazards of this isotope, and its insolubility makes it unlikely to escape a waste repository; all these are shared with palladium-107.

Nuclear fission produces it at a fission yield of 6.3% (thermal neutron fission of 235U), one of the most abundant fission products. Nuclear reactors usually contain large amounts of zirconium as fuel rod cladding (see zircalloy), and neutron irradiation of 92Zr also produces some 93Zr, though this is limited by 92Zr's low neutron capture cross section of 0.22 barns. Indeed, one of the primary reasons for using zirconium in fuel rod cladding is its low cross section.

93Zr also has a low neutron capture cross section of 0.7 barns.[18][19] Most fission zirconium consists of other isotopes; the other isotope with a significant neutron absorption cross section is 91Zr with a cross section of 1.24 barns. 93Zr is a less attractive candidate for disposal by nuclear transmutation than are 99Tc and 129I. The isotope could be recycled: if the effect on the neutron economy of 93
Zr
's higher cross section is deemed acceptable, irradiated cladding and fission product zirconium (which are mixed together in most current nuclear reprocessing methods) could be used to form new zircalloy cladding. Once the cladding is inside the reactor, the relatively low level radioactivity can be tolerated, but transport and manufacturing might require precautions not now taken.

See also

References

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