|
|
|
|
Isotopes of uranium
|
| |
|
| |
Uranium (U) is a naturally occurring element with no stable isotopes. In other words, all uranium is radioactive and hence vanishing by radioactive decay, yet it is also found in great quantity in the earth's crust. The natural isotopes are uranium-234, uranium-235, and uranium-238, with the average atomic mass in nature being 238.02891(3) u. In addition, other useful isotopes such as uranium-232 have been produced in mass quantity in breeder reactors.
Historically, isotopes of uranium were known as
Naturally occurring uranium is composed of three major isotopes, uranium-238 (99.28% natural abundance), uranium-235 (0.71%), and uranium-234 (0.0054%).

Discussion
Ask a question about 'Isotopes of uranium'
Start a new discussion about 'Isotopes of uranium'
Answer questions from other users
|
Encyclopedia
Uranium (U) is a naturally occurring element with no stable isotopes. In other words, all uranium is radioactive and hence vanishing by radioactive decay, yet it is also found in great quantity in the earth's crust. The natural isotopes are uranium-234, uranium-235, and uranium-238, with the average atomic mass in nature being 238.02891(3) u. In addition, other useful isotopes such as uranium-232 have been produced in mass quantity in breeder reactors.
Historically, isotopes of uranium were known as
- uranium II, 234U
- actino-uranium, 235U
- uranium I, 238U
Naturally occurring uranium is composed of three major isotopes, uranium-238 (99.28% natural abundance), uranium-235 (0.71%), and uranium-234 (0.0054%). All three isotopes are radioactive, creating radioisotopes, with the most abundant and stable being uranium-238 with a half-life of 4.51 years (close to the age of the Earth), uranium-235 with a half-life of 7.13 years, and uranium-234 with a half-life of 2.48 years.
Uranium-238 is an a emitter, decaying through the 18-member uranium natural decay series into lead-206. The constant rates of decay in these series makes comparison of the ratios of parent to daughter elements useful in radiometric dating. Uranium-233 is made from thorium-232 by neutron bombardment.
The isotope uranium-235 is important for both nuclear reactors and nuclear weapons because it is the only isotope existing in nature to any appreciable extent that is fissile, that is, can be broken apart by thermal neutrons. The isotope uranium-238 is also important because it absorbs neutrons to produce a radioactive isotope that subsequently decays to the isotope plutonium-239, which also is fissile.
Table
nuclide symbol | Z(p) | N(n) | isotopic mass (u) | half-life | nuclear spin | representative isotopic composition (mole fraction) | range of natural variation (mole fraction) |
|---|
| excitation energy |
|---|
| 217U | 92 | 125 | 217.02437(9) | 26(14) ms [16(+21-6) ms] | 1/2-# | | | | 218U | 92 | 126 | 218.02354(3) | 6(5) ms | 0+ | | | | 219U | 92 | 127 | 219.02492(6) | 55(25) µs [42(+34-13) µs] | 9/2+# | | | | 220U | 92 | 128 | 220.02472(22)# | 60# ns | 0+ | | | | 221U | 92 | 129 | 221.02640(11)# | 700# ns | 9/2+# | | | | 222U | 92 | 130 | 222.02609(11)# | 1.4(7) µs [1.0(+10-4) µs] | 0+ | | | | 223U | 92 | 131 | 223.02774(8) | 21(8) µs [18(+10-5) µs] | 7/2+# | | | | 224U | 92 | 132 | 224.027605(27) | 940(270) µs | 0+ | | | | 225U | 92 | 133 | 225.02939# | 61(4) ms | (5/2+)# | | | | 226U | 92 | 134 | 226.029339(14) | 269(6) ms | 0+ | | | | 227U | 92 | 135 | 227.031156(18) | 1.1(1) min | (3/2+) | | | | 228U | 92 | 136 | 228.031374(16) | 9.1(2) min | 0+ | | | | 229U | 92 | 137 | 229.033506(6) | 58(3) min | (3/2+) | | | | 230U | 92 | 138 | 230.033940(5) | 20.8 d | 0+ | | | | 231U | 92 | 139 | 231.036294(3) | 4.2(1) d | (5/2)(+#) | | | | 232U | 92 | 140 | 232.0371562(24) | 68.9(4) y | 0+ | | | | 233U | 92 | 141 | 233.0396352(29) | 1.592(2)×105 y | 5/2+ | | | | 234U | 92 | 142 | 234.0409521(20) | 2.455(6)×105 y | 0+ | [0.000054(5)] | 0.000050-0.000059 | | 234mU | 1421.32(10) keV | 33.5(20) µs | 6- | | | | 235U | 92 | 143 | 235.0439299(20) | 7.04(1)×108 y | 7/2- | [0.007204(6)] | 0.007198-0.007207 | | 235mU | 0.0765(4) keV | ~26 min | 1/2+ | | | | 236U | 92 | 144 | 236.045568(2) | 2.342(3)×107 y | 0+ | | | | 236m1U | 1052.89(19) keV | 100(4) ns | (4)- | | | | 236m2U | 2750(10) keV | 120(2) ns | (0+) | | | | 237U | 92 | 145 | 237.0487302(20) | 6.75(1) d | 1/2+ | | | | 238U | 92 | 146 | 238.0507882(20) | 4.468(3)×109 y | 0+ | [0.992742(10)] | 0.992739-0.992752 | | 238mU | 2557.9(5) keV | 280(6) ns | 0+ | | | | 239U | 92 | 147 | 239.0542933(21) | 23.45(2) min | 5/2+ | | | | 239m1U | 20(20)# keV | >250 ns | (5/2+) | | | | 239m2U | 133.7990(10) keV | 780(40) ns | 1/2+ | | | | 240U | 92 | 148 | 240.056592(6) | 14.1(1) h | 0+ | | | | 241U | 92 | 149 | 241.06033(32)# | 5# min | 7/2+# | | | | 242U | 92 | 150 | 242.06293(22)# | 16.8(5) min | 0+ | | |
|
| |
|
|