Selenium has six natural isotopes that occur in significant quantities, along with the trace isotope 79Se, which occurs in minute quantities in uranium ores. Five of these isotopes are stable: 74Se, 76Se, 77Se, 78Se, and 80Se. The last three also occur as fission products, along with 79Se, which has a half-life about 330,000 years, and 82Se, which has the very long half-life of 8.76×1019 years as it decays via double beta decay to krypton-82 and for practical purposes can be considered to be stable. There are 23 other unstable isotopes that have been characterized, the longest-lived after 79Se being 75Se with its half-life 119.78 days, 72Se at 8.40 days, and 73Se at 7.15 hours. The others are all under an hour and most do not exceed 38 seconds.

List of isotopes

NuclideZNIsotopic mass (Da)Discovery yearHalf-lifeDecay modeDaughter isotopeSpin and parityNatural abundance (mole fraction)
Excitation energyNormal proportionRange of variation
63Se342962.98191(54)#13.2(39) msβ+, p (89%)62Ge3/2−#
β+ (11%)63As
2p? (<0.5%)61Ge
64Se343063.97117(54)#22.6(2) msβ+?64As0+
β+, p?63Ge
65Se343164.96455(32)#34.2(7) msβ+, p (87%)64Ge3/2−#
β+ (13%)65As
66Se343265.95528(22)#54(4) msβ+66As0+
β+, p?65Ge
67Se343366.949994(72)133(4) msβ+ (99.5%)67As5/2−#
β+, p (0.5%)66Ge
68Se343467.94182524(53)35.5(7) sβ+68As0+
69Se343568.9394148(16)27.4(2) sβ+ (99.95%)69As1/2−
β+, p (.052%)68Ge
69m1Se38.85(22) keV2.0(2) μsIT69Se5/2−
69m2Se574.0(4) keV955(16) nsIT69Se9/2+
70Se343669.9335155(17)41.1(3) minβ+70As0+
71Se343770.9322094(30)4.74(5) minβ+71As(5/2−)
71m1Se48.79(5) keV5.6(7) μsIT71Se(1/2−)
71m2Se260.48(10) keV19.0(5) μsIT71Se(9/2+)
72Se343871.9271405(21)8.40(8) dEC72As0+
73Se343972.9267549(80)7.15(9) hβ+73As9/2+
73mSe25.71(4) keV39.8(17) minIT (72.6%)73Se3/2−
β+ (27.4%)73As
74Se344073.922475933(15)Observationally Stable0+0.0086(3)
75Se344174.922522870(78)119.78(3) dEC75As5/2+
76Se344275.919213702(17)Stable0+0.0923(7)
77Se344376.919914150(67)Stable1/2−0.0760(7)
77mSe161.9223(10) keV17.36(5) sIT77Se7/2+
78Se344477.91730924(19)Stable0+0.2369 (22)
79Se344578.91849925(24)3.27(28)×105 yβ−79Br7/2+
79mSe95.77(3) keV3.900(18) minIT (99.94%)79Se1/2−
β− (0.056%)79Br
80Se344679.9165218(10)Observationally Stable0+0.4980(36)
81Se344780.9179930(10)18.45(12) minβ−81Br1/2−
81mSe103.00(6) keV57.28(2) minIT (99.95%)81Se7/2+
β− (0.051%)81Br
82Se344881.91669953(50)8.76(15)×1019 yβ−β−82Kr0+0.0882(15)
83Se344982.9191186(33)22.25(4) minβ−83Br9/2+
83mSe228.92(7) keV70.1(4) sβ−83Br1/2−
84Se345083.9184668(21)3.26(10) minβ−84Br0+
85Se345184.9222608(28)32.9(3) sβ−85Br(5/2)+
86Se345285.9243117(27)14.3(3) sβ−86Br0+
β−, n?85Br
87Se345386.9286886(24)5.50(6) sβ− (99.50%)87Br(3/2+)
β−, n (0.60%)86Br
88Se345487.9314175(36)1.53(6) sβ− (99.01%)88Br0+
β−, n (0.99%)87Br
89Se345588.9366691(40)430(50) msβ− (92.2%)89Br5/2+#
β−, n (7.8%)88Br
90Se345689.94010(35)210(80) msβ−90Br0+
β−, n?89Br
91Se345790.94570(47)270(50) msβ− (79%)91Br1/2+#
β−, n (21%)90Br
β−, 2n?89Br
92Se345891.94984(43)#90# ms [>300 ns]β−?92Br0+
β−, n?91Br
β−, 2n?90Br
92mSe3072(2) keV15.7(7) μsIT92Se(9−)
93Se345992.95614(43)#130# ms [>300 ns]β−?93Br1/2+#
β−, n?92Br
β−, 2n?91Br
93mSe678.2(7) keV420(100) nsIT93Se
94Se346093.96049(54)#50# ms [>300 ns]β−?94Br0+
β−, n?93Br
β−, 2n?92Br
94mSe2430.0(6) keV680(50) nsIT94Se(7−)
95Se346194.96730(54)#70# ms [>400 ns]β−?95Br3/2+#
β−, n?94Br
β−, 2n?93Br
96Se3462
97Se3463
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Use of radioisotopes

The isotope selenium-75 has radiopharmaceutical uses. For example, it is used in high-dose-rate endorectal brachytherapy, as an alternative to iridium-192.

In paleobiogeochemistry, the ratio in amount of selenium-82 to selenium-76 (i.e, the value of δ82/76Se) can be used to track down the redox conditions on Earth during the Neoproterozoic era in order to gain a deeper understanding of the rapid oxygenation that trigger the emergence of complex organisms.

See also

Daughter products other than selenium