| ||||||||||||||||||||||||||||||||||||||
Standard atomic weight Ar°(Lu) | ||||||||||||||||||||||||||||||||||||||
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Naturally occurring lutetium (71Lu) is composed of one stable isotope 175Lu (97.41% natural abundance) and one long-lived radioisotope, 176Lu with a half-life of 37 billion years (2.59% natural abundance). Forty radioisotopes have been characterized, with the most stable, besides 176Lu, being 174Lu with a half-life of 3.31 years, and 173Lu with a half-life of 1.37 years. All of the remaining radioactive isotopes have half-lives that are less than 9 days, and the majority of these have half-lives that are less than half an hour. This element also has 18 meta states, with the most stable being 177mLu (t1/2 160.4 days), 174mLu (t1/2 142 days) and 178mLu (t1/2 23.1 minutes).
The known isotopes of lutetium range in mass number from 149 to 190. The primary decay mode before the most abundant stable isotope, 175Lu, is electron capture (with some alpha and positron emission), and the primary mode after is beta emission. The primary decay products before 175Lu are isotopes of ytterbium and the primary products after are isotopes of hafnium. All isotopes of lutetium are either radioactive or, in the case of 175Lu, observationally stable, meaning that 175Lu is predicted to be radioactive but no actual decay has been observed. [4]
Nuclide [n 1] | Z | N | Isotopic mass (Da) [n 2] [n 3] | Half-life [n 4] [n 5] | Decay mode [n 6] | Daughter isotope [n 7] | Spin and parity [n 8] [n 5] | Natural abundance (mole fraction) | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Excitation energy [n 5] | Normal proportion | Range of variation | |||||||||||||||||
149Lu [5] | 71 | 78 | 450+170 −100 ns | p | 148Yb | 11/2− | |||||||||||||
150Lu | 71 | 79 | 149.97323(54)# | 43(5) ms | p (80%) | 149Yb | (2+) | ||||||||||||
β+ (20%) | 150Yb | ||||||||||||||||||
150mLu | 34(15) keV | 80(60) μs [30(+95−15) μs] | p | 149Yb | (1, 2) | ||||||||||||||
151Lu | 71 | 80 | 150.96757682 | 80.6(5) ms | p (63.4%) | 150Yb | (11/2−) | ||||||||||||
β+ (36.6%) | 151Yb | ||||||||||||||||||
151mLu | 77(5) keV | 16(1) μs | p | 150Yb | (3/2+) | ||||||||||||||
152Lu | 71 | 81 | 151.96412(21)# | 650(70) ms | β+ (85%) | 152Yb | (5−, 6−) | ||||||||||||
β+, p (15%) | 151Tm | ||||||||||||||||||
153Lu | 71 | 82 | 152.95877(22) | 0.9(2) s | α (70%) | 149Tm | 11/2− | ||||||||||||
β+ (30%) | 153Yb | ||||||||||||||||||
153m1Lu | 80(5) keV | 1# s | IT | 153Lu | 1/2+ | ||||||||||||||
153m2Lu | 2502.5(4) keV | >0.1 μs | IT | 153Lu | 23/2− | ||||||||||||||
153m3Lu | 2632.9(5) keV | 15(3) μs | IT | 153m2Lu | 27/2− | ||||||||||||||
154Lu | 71 | 83 | 153.95752(22)# | 1# s | β+? | 154Yb | (2−) | ||||||||||||
α? | 150Tm | ||||||||||||||||||
154m1Lu | 58(13) keV | 1.12(8) s | β+ | 154Yb | (9+) | ||||||||||||||
β+p? | 153Tm | ||||||||||||||||||
β+α? | 150Er | ||||||||||||||||||
α? | 150Tm | ||||||||||||||||||
154m2Lu | >2562 keV | 35(3) μs | IT | 154Lu | (17+) | ||||||||||||||
155Lu | 71 | 84 | 154.954316(22) | 68.6(16) ms | α (76%) | 151Tm | (11/2−) | ||||||||||||
β+ (24%) | 155Yb | ||||||||||||||||||
155m1Lu | 20(6) keV | 138(8) ms | α (88%) | 151Tm | (1/2+) | ||||||||||||||
β+ (12%) | 155Yb | ||||||||||||||||||
155m2Lu | 1781.0(20) keV | 2.70(3) ms | (25/2−) | ||||||||||||||||
156Lu | 71 | 85 | 155.95303(8) | 494(12) ms | α (95%) | 152Tm | (2)− | ||||||||||||
β+ (5%) | 156Yb | ||||||||||||||||||
156mLu | 220(80)# keV | 198(2) ms | α (94%) | 152Tm | (9)+ | ||||||||||||||
β+ (6%) | 156Yb | ||||||||||||||||||
157Lu | 71 | 86 | 156.950098(20) | 6.8(18) s | β+ | 157Yb | (1/2+, 3/2+) | ||||||||||||
α | 153Tm | ||||||||||||||||||
157mLu | 21.0(20) keV | 4.79(12) s | β+ (94%) | 157Yb | (11/2−) | ||||||||||||||
α (6%) | 153Tm | ||||||||||||||||||
158Lu | 71 | 87 | 157.949313(16) | 10.6(3) s | β+ (99.09%) | 158Yb | 2− | ||||||||||||
α (.91%) | 154Tm | ||||||||||||||||||
159Lu | 71 | 88 | 158.94663(4) | 12.1(10) s | β+ (99.96%) | 159Yb | 1/2+# | ||||||||||||
α (.04%) | 155Tm | ||||||||||||||||||
159mLu | 100(80)# keV | 10# s | 11/2−# | ||||||||||||||||
160Lu | 71 | 89 | 159.94603(6) | 36.1(3) s | β+ | 160Yb | 2−# | ||||||||||||
α (10−4%) | 156Tm | ||||||||||||||||||
160mLu | 0(100)# keV | 40(1) s | |||||||||||||||||
161Lu | 71 | 90 | 160.94357(3) | 77(2) s | β+ | 161Yb | 1/2+ | ||||||||||||
161mLu | 166(18) keV | 7.3(4) ms | IT | 161Lu | (9/2−) | ||||||||||||||
162Lu | 71 | 91 | 161.94328(8) | 1.37(2) min | β+ | 162Yb | (1−) | ||||||||||||
162m1Lu | 120(200)# keV | 1.5 min | β+ | 162Yb | 4−# | ||||||||||||||
IT (rare) | 162Lu | ||||||||||||||||||
162m2Lu | 300(200)# keV | 1.9 min | |||||||||||||||||
163Lu | 71 | 92 | 162.94118(3) | 3.97(13) min | β+ | 163Yb | 1/2(+) | ||||||||||||
164Lu | 71 | 93 | 163.94134(3) | 3.14(3) min | β+ | 164Yb | 1(−) | ||||||||||||
165Lu | 71 | 94 | 164.939407(28) | 10.74(10) min | β+ | 165Yb | 1/2+ | ||||||||||||
166Lu | 71 | 95 | 165.93986(3) | 2.65(10) min | β+ | 166Yb | (6−) | ||||||||||||
166m1Lu | 34.37(5) keV | 1.41(10) min | β+ (58%) | 166Yb | 3(−) | ||||||||||||||
IT (42%) | 166Lu | ||||||||||||||||||
166m2Lu | 42.9(5) keV | 2.12(10) min | 0(−) | ||||||||||||||||
167Lu | 71 | 96 | 166.93827(3) | 51.5(10) min | β+ | 167Yb | 7/2+ | ||||||||||||
167mLu | 0(30)# keV | >1 min | 1/2(−#) | ||||||||||||||||
168Lu | 71 | 97 | 167.93874(5) | 5.5(1) min | β+ | 168Yb | (6−) | ||||||||||||
168mLu | 180(110) keV | 6.7(4) min | β+ (95%) | 168Yb | 3+ | ||||||||||||||
IT (5%) | 168Lu | ||||||||||||||||||
169Lu | 71 | 98 | 168.937651(6) | 34.06(5) h | β+ | 169Yb | 7/2+ | ||||||||||||
169mLu | 29.0(5) keV | 160(10) s | IT | 169Lu | 1/2− | ||||||||||||||
170Lu | 71 | 99 | 169.938475(18) | 2.012(20) d | β+ | 170Yb | 0+ | ||||||||||||
170mLu | 92.91(9) keV | 670(100) ms | IT | 170Lu | (4)− | ||||||||||||||
171Lu | 71 | 100 | 170.9379131(30) | 8.24(3) d | β+ | 171Yb | 7/2+ | ||||||||||||
171mLu | 71.13(8) keV | 79(2) s | IT | 171Lu | 1/2− | ||||||||||||||
172Lu | 71 | 101 | 171.939086(3) | 6.70(3) d | β+ | 172Yb | 4− | ||||||||||||
172m1Lu | 41.86(4) keV | 3.7(5) min | IT | 172Lu | 1− | ||||||||||||||
172m2Lu | 65.79(4) keV | 0.332(20) μs | (1)+ | ||||||||||||||||
172m3Lu | 109.41(10) keV | 440(12) μs | (1)+ | ||||||||||||||||
172m4Lu | 213.57(17) keV | 150 ns | (6−) | ||||||||||||||||
173Lu | 71 | 102 | 172.9389306(26) | 1.37(1) y | EC | 173Yb | 7/2+ | ||||||||||||
173mLu | 123.672(13) keV | 74.2(10) μs | 5/2− | ||||||||||||||||
174Lu | 71 | 103 | 173.9403375(26) | 3.31(5) y | β+ | 174Yb | (1)− | ||||||||||||
174m1Lu | 170.83(5) keV | 142(2) d | IT (99.38%) | 174Lu | 6− | ||||||||||||||
EC (.62%) | 174Yb | ||||||||||||||||||
174m2Lu | 240.818(4) keV | 395(15) ns | (3+) | ||||||||||||||||
174m3Lu | 365.183(6) keV | 145(3) ns | (4−) | ||||||||||||||||
175Lu | 71 | 104 | 174.9407718(23) | Observationally stable [n 9] | 7/2+ | 0.9741(2) | |||||||||||||
175m1Lu | 1392.2(6) keV | 984(30) μs | (19/2+) | ||||||||||||||||
175m2Lu | 353.48(13) keV | 1.49(7) μs | 5/2− | ||||||||||||||||
176Lu [n 10] [n 11] | 71 | 105 | 175.9426863(23) | 3.701(17)×1010 y | β− | 176Hf | 7− | 0.0259(2) | |||||||||||
EC (0.45(26)%) [1] | 176Yb | ||||||||||||||||||
176mLu | 122.855(6) keV | 3.664(19) h | β− (99.9%) | 176Hf | 1− | ||||||||||||||
EC (.095%) | 176Yb | ||||||||||||||||||
177Lu | 71 | 106 | 176.9437581(23) | 6.6475(20) d | β− | 177Hf | 7/2+ | ||||||||||||
177m1Lu | 150.3967(10) keV | 130(3) ns | 9/2− | ||||||||||||||||
177m2Lu | 569.7068(16) keV | 155(7) μs | 1/2+ | ||||||||||||||||
177m3Lu | 970.1750(24) keV | 160.44(6) d | β− (78.3%) | 177Hf | 23/2− | ||||||||||||||
IT (21.7%) | 177Lu | ||||||||||||||||||
177m4Lu | 3900(10) keV | 7(2) min [6(+3−2) min] | 39/2− | ||||||||||||||||
178Lu | 71 | 107 | 177.945955(3) | 28.4(2) min | β− | 178Hf | 1(+) | ||||||||||||
178mLu | 123.8(26) keV | 23.1(3) min | β− | 178Hf | 9(−) | ||||||||||||||
179Lu | 71 | 108 | 178.947327(6) | 4.59(6) h | β− | 179Hf | 7/2(+) | ||||||||||||
179mLu | 592.4(4) keV | 3.1(9) ms | IT | 179Lu | 1/2(+) | ||||||||||||||
180Lu | 71 | 109 | 179.94988(8) | 5.7(1) min | β− | 180Hf | 5+ | ||||||||||||
180m1Lu | 13.9(3) keV | ~1 s | IT | 180Lu | 3− | ||||||||||||||
180m2Lu | 624.0(5) keV | ≥1 ms | (9−) | ||||||||||||||||
181Lu | 71 | 110 | 180.95197(32)# | 3.5(3) min | β− | 181Hf | (7/2+) | ||||||||||||
182Lu | 71 | 111 | 181.95504(21)# | 2.0(2) min | β− | 182Hf | (0,1,2) | ||||||||||||
183Lu | 71 | 112 | 182.95736(9) | 58(4) s | β− | 183Hf | (7/2+) | ||||||||||||
184Lu | 71 | 113 | 183.96103(22)# | 20(3) s | β− | 184Hf | (3+) | ||||||||||||
185Lu | 71 | 114 | 184.96354(32)# | 20# s | 7/2+# | ||||||||||||||
186Lu | 71 | 115 | 185.96745(43)# | 6# s | |||||||||||||||
187Lu | 71 | 116 | 186.97019(43)# | 7# s | 7/2+# | ||||||||||||||
188Lu | 71 | 117 | 187.97443(43)# | 1# s | |||||||||||||||
189Lu [6] | 71 | 118 | |||||||||||||||||
190Lu [7] | 71 | 119 | |||||||||||||||||
This table header & footer: |
EC: | Electron capture |
IT: | Isomeric transition |
p: | Proton emission |
Lutetium (177Lu) chloride, sold under the brand name Lumark among others, is used for radiolabeling other medicines, either as an anti-cancer therapy or for scintigraphy (medical radio-imaging). Its most common side effects are anaemia (low red blood cell counts), thrombocytopenia (low blood platelet counts), leucopenia (low white blood cell counts), lymphopenia (low levels of lymphocytes, a particular type of white blood cell), nausea (feeling sick), vomiting and mild and temporary hair loss. [8] [9]
Protactinium (91Pa) has no stable isotopes. The four naturally occurring isotopes allow a standard atomic weight to be given.
Thallium (81Tl) has 41 isotopes with atomic masses that range from 176 to 216. 203Tl and 205Tl are the only stable isotopes and 204Tl is the most stable radioisotope with a half-life of 3.78 years. 207Tl, with a half-life of 4.77 minutes, has the longest half-life of naturally occurring Tl radioisotopes. All isotopes of thallium are either radioactive or observationally stable, meaning that they are predicted to be radioactive but no actual decay has been observed.
Naturally occurring platinum (78Pt) consists of five stable isotopes (192Pt, 194Pt, 195Pt, 196Pt, 198Pt) and one very long-lived (half-life 4.83×1011 years) radioisotope (190Pt). There are also 34 known synthetic radioisotopes, the longest-lived of which is 193Pt with a half-life of 50 years. All other isotopes have half-lives under a year, most under a day. All isotopes of platinum are either radioactive or observationally stable, meaning that they are predicted to be radioactive but no actual decay has been observed. Platinum-195 is the most abundant isotope.
Naturally occurring tungsten (74W) consists of five isotopes. Four are considered stable (182W, 183W, 184W, and 186W) and one is slightly radioactive, 180W, with an extremely long half-life of 1.8 ± 0.2 exayears (1018 years). On average, two alpha decays of 180W occur per gram of natural tungsten per year, so for most practical purposes, 180W can be considered stable. Theoretically, all five can decay into isotopes of element 72 (hafnium) by alpha emission, but only 180W has been observed to do so. The other naturally occurring isotopes have not been observed to decay (they are observationally stable), and lower bounds for their half-lives have been established:
Natural hafnium (72Hf) consists of five observationally stable isotopes (176Hf, 177Hf, 178Hf, 179Hf, and 180Hf) and one very long-lived radioisotope, 174Hf, with a half-life of 7.0×1016 years. In addition, there are 34 known synthetic radioisotopes, the most stable of which is 182Hf with a half-life of 8.9×106 years. This extinct radionuclide is used in hafnium–tungsten dating to study the chronology of planetary differentiation.
Naturally occurring ytterbium (70Yb) is composed of seven stable isotopes: 168Yb, 170Yb–174Yb, and 176Yb, with 174Yb being the most abundant. 30 radioisotopes have been characterized, with the most stable being 169Yb with a half-life of 32.014 days, 175Yb with a half-life of 4.185 days, and 166Yb with a half-life of 56.7 hours. All of the remaining radioactive isotopes have half-lives that are less than 2 hours, and the majority of these have half-lives that are less than 20 minutes. This element also has 18 meta states, with the most stable being 169mYb.
Natural holmium (67Ho) contains one observationally stable isotope, 165Ho. The below table lists 36 isotopes spanning 140Ho through 175Ho as well as 33 nuclear isomers. Among the known synthetic radioactive isotopes; the most stable one is 163Ho, with a half-life of 4,570 years. All other radioisotopes have half-lives not greater than 1.117 days in their ground states, and most have half-lives under 3 hours.
Naturally occurring gadolinium (64Gd) is composed of 6 stable isotopes, 154Gd, 155Gd, 156Gd, 157Gd, 158Gd and 160Gd, and 1 radioisotope, 152Gd, with 158Gd being the most abundant (24.84% natural abundance). The predicted double beta decay of 160Gd has never been observed; only a lower limit on its half-life of more than 1.3×1021 years has been set experimentally.
Naturally occurring praseodymium (59Pr) is composed of one stable isotope, 141Pr. Thirty-eight radioisotopes have been characterized with the most stable being 143Pr, with a half-life of 13.57 days and 142Pr, with a half-life of 19.12 hours. All of the remaining radioactive isotopes have half-lives that are less than 5.985 hours and the majority of these have half-lives that are less than 33 seconds. This element also has 15 meta states with the most stable being 138mPr, 142mPr and 134mPr.
Naturally occurring lanthanum (57La) is composed of one stable (139La) and one radioactive (138La) isotope, with the stable isotope, 139La, being the most abundant (99.91% natural abundance). There are 39 radioisotopes that have been characterized, with the most stable being 138La, with a half-life of 1.02×1011 years; 137La, with a half-life of 60,000 years and 140La, with a half-life of 1.6781 days. The remaining radioactive isotopes have half-lives that are less than a day and the majority of these have half-lives that are less than 1 minute. This element also has 12 nuclear isomers, the longest-lived of which is 132mLa, with a half-life of 24.3 minutes. Lighter isotopes mostly decay to isotopes of barium and heavy ones mostly decay to isotopes of cerium. 138La can decay to both.
Naturally occurring barium (56Ba) is a mix of six stable isotopes and one very long-lived radioactive primordial isotope, barium-130, identified as being unstable by geochemical means (from analysis of the presence of its daughter xenon-130 in rocks) in 2001. This nuclide decays by double electron capture (absorbing two electrons and emitting two neutrinos), with a half-life of (0.5–2.7)×1021 years (about 1011 times the age of the universe).
Antimony (51Sb) occurs in two stable isotopes, 121Sb and 123Sb. There are 37 artificial radioactive isotopes, the longest-lived of which are 125Sb, with a half-life of 2.75856 years; 124Sb, with a half-life of 60.2 days; and 126Sb, with a half-life of 12.35 days. All other isotopes have half-lives less than 4 days, most less than an hour. There are also many isomers, the longest-lived of which is 120m1Sb with a half-life of 5.76 days.
Naturally occurring cadmium (48Cd) is composed of 8 isotopes. For two of them, natural radioactivity was observed, and three others are predicted to be radioactive but their decays have not been observed, due to extremely long half-lives. The two natural radioactive isotopes are 113Cd (beta decay, half-life is 8.04 × 1015 years) and 116Cd (two-neutrino double beta decay, half-life is 2.8 × 1019 years). The other three are 106Cd, 108Cd (double electron capture), and 114Cd (double beta decay); only lower limits on their half-life times have been set. Three isotopes—110Cd, 111Cd, and 112Cd—are theoretically stable. Among the isotopes absent in natural cadmium, the most long-lived are 109Cd with a half-life of 462.6 days, and 115Cd with a half-life of 53.46 hours. All of the remaining radioactive isotopes have half-lives that are less than 2.5 hours and the majority of these have half-lives that are less than 5 minutes. This element also has 12 known meta states, with the most stable being 113mCd (t1/2 14.1 years), 115mCd (t1/2 44.6 days) and 117mCd (t1/2 3.36 hours).
The alkaline earth metal strontium (38Sr) has four stable, naturally occurring isotopes: 84Sr (0.56%), 86Sr (9.86%), 87Sr (7.0%) and 88Sr (82.58%). Its standard atomic weight is 87.62(1).
Arsenic (33As) has 32 known isotopes and at least 10 isomers. Only one of these isotopes, 75As, is stable; as such, it is considered a monoisotopic element. The longest-lived radioisotope is 73As with a half-life of 80 days.
Naturally occurring zinc (30Zn) is composed of the 5 stable isotopes 64Zn, 66Zn, 67Zn, 68Zn, and 70Zn with 64Zn being the most abundant. Twenty-eight radioisotopes have been characterised with the most stable being 65Zn with a half-life of 244.26 days, and then 72Zn with a half-life of 46.5 hours. All of the remaining radioactive isotopes have half-lives that are less than 14 hours and the majority of these have half-lives that are less than 1 second. This element also has 10 meta states.
Naturally occurring vanadium (23V) is composed of one stable isotope 51V and one radioactive isotope 50V with a half-life of 2.71×1017 years. 24 artificial radioisotopes have been characterized (in the range of mass number between 40 and 65) with the most stable being 49V with a half-life of 330 days, and 48V with a half-life of 15.9735 days. All of the remaining radioactive isotopes have half-lives shorter than an hour, the majority of them below 10 seconds, the least stable being 42V with a half-life shorter than 55 nanoseconds, with all of the isotopes lighter than it, and none of the heavier, have unknown half-lives. In 4 isotopes, metastable excited states were found (including 2 metastable states for 60V), which adds up to 5 meta states.
Naturally occurring scandium (21Sc) is composed of one stable isotope, 45Sc. Twenty-seven radioisotopes have been characterized, with the most stable being 46Sc with a half-life of 83.8 days, 47Sc with a half-life of 3.35 days, and 48Sc with a half-life of 43.7 hours and 44Sc with a half-life of 3.97 hours. All the remaining isotopes have half-lives that are less than four hours, and the majority of these have half-lives that are less than two minutes, the least stable being proton unbound 39Sc with a half-life shorter than 300 nanoseconds. This element also has 13 meta states with the most stable being 44m2Sc.
Naturally occurring titanium (22Ti) is composed of five stable isotopes; 46Ti, 47Ti, 48Ti, 49Ti and 50Ti with 48Ti being the most abundant. Twenty-one radioisotopes have been characterized, with the most stable being 44Ti with a half-life of 60 years, 45Ti with a half-life of 184.8 minutes, 51Ti with a half-life of 5.76 minutes, and 52Ti with a half-life of 1.7 minutes. All of the remaining radioactive isotopes have half-lives that are less than 33 seconds, and the majority of these have half-lives that are less than half a second.
Mendelevium (101Md) is a synthetic element, and thus a standard atomic weight cannot be given. Like all artificial elements, it has no stable isotopes. The first isotope to be synthesized was 256Md in 1955. There are 17 known radioisotopes, ranging in atomic mass from 244Md to 260Md, and 5 isomers. The longest-lived isotope is 258Md with a half-life of 51.3 days, and the longest-lived isomer is 258mMd with a half-life of 57 minutes.