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Standard atomic weight Ar°(Gd) | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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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. [5]
Thirty-three radioisotopes have been characterized, with the most stable being alpha-decaying 152Gd (naturally occurring) with a half-life of 1.08×1014 years, and 150Gd with a half-life of 1.79×106 years. All of the remaining radioactive isotopes have half-lives less than 100 years, the majority of these having half-lives less than 24.6 seconds. Gadolinium isotopes have 10 metastable isomers, with the most stable being 143mGd (t1/2 = 110 seconds), 145mGd (t1/2 = 85 seconds) and 141mGd (t1/2 = 24.5 seconds).
The primary decay mode at atomic weights lower than the most abundant stable isotope, 158Gd, is electron capture, and the primary mode at higher atomic weights is beta decay. The primary decay products for isotopes lighter than 158Gd are isotopes of europium and the primary products of heavier isotopes are isotopes of terbium.
Nuclide [n 1] | Z | N | Isotopic mass (Da) [6] [n 2] [n 3] | Half-life [1] [n 4] [n 5] | Decay mode [1] [n 6] | Daughter isotope [n 7] [n 8] | Spin and parity [1] [n 9] [n 5] | Natural abundance (mole fraction) | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Excitation energy [n 5] | Normal proportion [1] | Range of variation | |||||||||||||||||
135Gd | 64 | 71 | 134.95250(43)# | 1.1(2) s | β+ (98%) | 135Eu | (5/2+) | ||||||||||||
β+, p (98%) | 134Sm | ||||||||||||||||||
136Gd | 64 | 72 | 135.94730(32)# | 1# s [>200 ns] | β+? | 136Eu | 0+ | ||||||||||||
β+, p? | 135Sm | ||||||||||||||||||
137Gd | 64 | 73 | 136.94502(32)# | 2.2(2) s | β+ | 137Eu | (7/2)+# | ||||||||||||
β+, p? | 136Sm | ||||||||||||||||||
138Gd | 64 | 74 | 137.94025(22)# | 4.7(9) s | β+ | 138Eu | 0+ | ||||||||||||
138mGd | 2232.6(11) keV | 6.2(0.2) μs | IT | 138Gd | (8−) | ||||||||||||||
139Gd | 64 | 75 | 138.93813(21)# | 5.7(3) s | β+ | 139Eu | 9/2−# | ||||||||||||
β+, p? | 138Sm | ||||||||||||||||||
139mGd [n 10] | 250(150)# keV | 4.8(9) s | β+ | 139Eu | 1/2+# | ||||||||||||||
β+, p? | 138Sm | ||||||||||||||||||
140Gd | 64 | 76 | 139.933674(30) | 15.8(4) s | β+ (67(8)%) | 140Eu | 0+ | ||||||||||||
EC (33(8)%) | |||||||||||||||||||
141Gd | 64 | 77 | 140.932126(21) | 14(4) s | β+ (99.97%) | 141Eu | (1/2+) | ||||||||||||
β+, p (0.03%) | 140Sm | ||||||||||||||||||
141mGd | 377.76(9) keV | 24.5(5) s | β+ (89%) | 141Eu | (11/2−) | ||||||||||||||
IT (11%) | 141Gd | ||||||||||||||||||
142Gd | 64 | 78 | 141.928116(30) | 70.2(6) s | EC (52(5)%) | 142Eu | 0+ | ||||||||||||
β+ (48(5)%) | |||||||||||||||||||
143Gd | 64 | 79 | 142.92675(22) | 39(2) s | β+ | 143Eu | 1/2+ | ||||||||||||
β+, p? | 142Sm | ||||||||||||||||||
β+, α? | 139Pm | ||||||||||||||||||
143mGd | 152.6(5) keV | 110.0(14) s | β+ | 143Eu | 11/2− | ||||||||||||||
β+, p? | 142Sm | ||||||||||||||||||
β+, α? | 139Pm | ||||||||||||||||||
144Gd | 64 | 80 | 143.922963(30) | 4.47(6) min | β+ | 144Eu | 0+ | ||||||||||||
144mGd | 3433.1(5) keV | 145(30) ns | IT | 144Gd | (10+) | ||||||||||||||
145Gd | 64 | 81 | 144.921710(21) | 23.0(4) min | β+ | 145Eu | 1/2+ | ||||||||||||
145mGd | 749.1(2) keV | 85(3) s | IT (94.3%) | 145Gd | 11/2− | ||||||||||||||
β+ (5.7%) | 145Eu | ||||||||||||||||||
146Gd | 64 | 82 | 145.9183185(44) | 48.27(10) d | EC | 146Eu | 0+ | ||||||||||||
147Gd | 64 | 83 | 146.9191010(20) | 38.06(12) h | β+ | 147Eu | 7/2− | ||||||||||||
147mGd | 8587.8(5) keV | 510(20) ns | IT | 147Gd | 49/2+ | ||||||||||||||
148Gd | 64 | 84 | 147.9181214(16) | 86.9(39) y [2] | α [n 11] | 144Sm | 0+ | ||||||||||||
149Gd | 64 | 85 | 148.9193477(36) | 9.28(10) d | β+ | 149Eu | 7/2− | ||||||||||||
α (4.3×10−4%) | 145Sm | ||||||||||||||||||
150Gd | 64 | 86 | 149.9186639(65) | 1.79(8)×106 y | α [n 12] | 146Sm | 0+ | ||||||||||||
151Gd | 64 | 87 | 150.9203549(32) | 123.9(10) d | EC | 151Eu | 7/2− | ||||||||||||
α (1.1×10−6%) | 147Sm | ||||||||||||||||||
152Gd [n 13] | 64 | 88 | 151.9197984(11) | 1.08(8)×1014 y | α [n 14] | 148Sm | 0+ | 0.0020(1) | |||||||||||
153Gd | 64 | 89 | 152.9217569(11) | 240.6(7) d | EC | 153Eu | 3/2− | ||||||||||||
153m1Gd | 95.1737(8) keV | 3.5(4) μs | IT | 153Gd | 9/2+ | ||||||||||||||
153m2Gd | 171.188(4) keV | 76.0(14) μs | IT | 153Gd | (11/2−) | ||||||||||||||
154Gd | 64 | 90 | 153.9208730(11) | Observationally Stable [n 15] | 0+ | 0.0218(2) | |||||||||||||
155Gd [n 16] | 64 | 91 | 154.9226294(11) | Observationally Stable [n 17] | 3/2− | 0.1480(9) | |||||||||||||
155mGd | 121.10(19) keV | 31.97(27) ms | IT | 155Gd | 11/2− | ||||||||||||||
156Gd [n 16] | 64 | 92 | 155.9221301(11) | Stable | 0+ | 0.2047(3) | |||||||||||||
156mGd | 2137.60(5) keV | 1.3(1) μs | IT | 156Gd | 7- | ||||||||||||||
157Gd [n 16] | 64 | 93 | 156.9239674(10) | Stable | 3/2− | 0.1565(4) | |||||||||||||
157m1Gd | 63.916(5) keV | 460(40) ns | IT | 157Gd | 5/2+ | ||||||||||||||
157m2Gd | 426.539(23) keV | 18.5(23) μs | IT | 157Gd | 11/2− | ||||||||||||||
158Gd [n 16] | 64 | 94 | 157.9241112(10) | Stable | 0+ | 0.2484(8) | |||||||||||||
159Gd [n 16] | 64 | 95 | 158.9263958(11) | 18.479(4) h | β− | 159Tb | 3/2− | ||||||||||||
160Gd [n 16] | 64 | 96 | 159.9270612(12) | Observationally Stable [n 18] | 0+ | 0.2186(3) | |||||||||||||
161Gd | 64 | 97 | 160.9296763(16) | 3.646(3) min | β− | 161Tb | 5/2− | ||||||||||||
162Gd | 64 | 98 | 161.9309918(43) | 8.4(2) min | β− | 162Tb | 0+ | ||||||||||||
163Gd | 64 | 99 | 162.93409664(86) | 68(3) s | β− | 163Tb | 7/2+ | ||||||||||||
163mGd | 138.22(20) keV | 23.5(10) s | IT? | 163Gd | 1/2− | ||||||||||||||
β− | 163Tb | ||||||||||||||||||
164Gd | 64 | 100 | 163.9359162(11) | 45(3) s | β− | 164Tb | 0+ | ||||||||||||
164mGd | 1095.8(4) keV | 589(18) ns | IT | 164Gd | (4−) | ||||||||||||||
165Gd | 64 | 101 | 164.9393171(14) | 11.6(10) s | β− | 165Tb | 1/2−# | ||||||||||||
166Gd | 64 | 102 | 165.9416304(17) | 5.1(8) s | β− | 166Tb | 0+ | ||||||||||||
166mGd | 1601.5(11) keV | 950(60) ns | IT | 166Gd | (6−) | ||||||||||||||
167Gd | 64 | 103 | 166.9454900(56) | 4.2(3) s | β− | 167Tb | 5/2−# | ||||||||||||
168Gd | 64 | 104 | 167.94831(32)# | 3.03(16) s | β− | 168Tb | 0+ | ||||||||||||
169Gd | 64 | 105 | 168.95288(43)# | 750(210) ms | β− | 169Tb | 7/2−# | ||||||||||||
β−, n? (<0.7%) [7] | 168Tb | ||||||||||||||||||
170Gd | 64 | 106 | 169.95615(54)# | 675+94 −75 ms [7] | β− | 170Tb | 0+ | ||||||||||||
β−, n? (<3%) [7] | 169Tb | ||||||||||||||||||
171Gd | 64 | 107 | 170.96113(54)# | 392+145 −136 ms [7] | β− | 171Tb | 9/2+# | ||||||||||||
β−, n? (<10%) [7] | 170Tb | ||||||||||||||||||
172Gd | 64 | 108 | 171.96461(32)# | 163+113 −99 ms [7] | β− | 172Tb | 0+# | ||||||||||||
β−, n? (<50%) [7] | 171Tb | ||||||||||||||||||
This table header & footer: |
EC: | Electron capture |
IT: | Isomeric transition |
With a half-life of 86.9±3.9 year via alpha decay alone, [2] gadolinium-148 would be ideal for radioisotope thermoelectric generators. However, gadolinium-148 cannot be economically synthesized in sufficient quantities to power a RTG. [8]
Gadolinium-153 has a half-life of 240.4±10 d and emits gamma radiation with strong peaks at 41 keV and 102 keV. It is used as a gamma ray source for X-ray absorptiometry and fluorescence, for bone density gauges for osteoporosis screening, and for radiometric profiling in the Lixiscope portable x-ray imaging system, also known as the Lixi Profiler. In nuclear medicine, it serves to calibrate the equipment needed like single-photon emission computed tomography systems (SPECT) to make x-rays. It ensures that the machines work correctly to produce images of radioisotope distribution inside the patient. This isotope is produced in a nuclear reactor from europium or enriched gadolinium. [9] It can also detect the loss of calcium in the hip and back bones, allowing the ability to diagnose osteoporosis. [10]
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.
There are seven stable isotopes of mercury (80Hg) with 202Hg being the most abundant (29.86%). The longest-lived radioisotopes are 194Hg with a half-life of 444 years, and 203Hg with a half-life of 46.612 days. Most of the remaining 40 radioisotopes have half-lives that are less than a day. 199Hg and 201Hg are the most often studied NMR-active nuclei, having spin quantum numbers of 1/2 and 3/2 respectively. All isotopes of mercury are either radioactive or observationally stable, meaning that they are predicted to be radioactive but no actual decay has been observed. These isotopes are predicted to undergo either alpha decay or double beta decay.
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.
There are two natural isotopes of iridium (77Ir), and 37 radioisotopes, the most stable radioisotope being 192Ir with a half-life of 73.83 days, and many nuclear isomers, the most stable of which is 192m2Ir with a half-life of 241 years. All other isomers have half-lives under a year, most under a day. All isotopes of iridium are either radioactive or observationally stable, meaning that they are predicted to be radioactive but no actual decay has been observed.
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:
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.
Naturally occurring thulium (69Tm) is composed of one stable isotope, 169Tm. Thirty-nine radioisotopes have been characterized, with the most stable being 171Tm with a half-life of 1.92 years, 170Tm with a half-life of 128.6 days, 168Tm with a half-life of 93.1 days, and 167Tm with a half-life of 9.25 days. All of the remaining radioactive isotopes have half-lives that are less than 64 hours, and the majority of these have half-lives that are less than 2 minutes. This element also has 26 meta states, with the most stable being 164mTm, 160mTm and 155mTm.
Naturally occurring dysprosium (66Dy) is composed of 7 stable isotopes, 156Dy, 158Dy, 160Dy, 161Dy, 162Dy, 163Dy and 164Dy, with 164Dy being the most abundant. Twenty-nine radioisotopes have been characterized, with the most stable being 154Dy with a half-life of 1.4 million years, 159Dy with a half-life of 144.4 days, and 166Dy with a half-life of 81.6 hours. All of the remaining radioactive isotopes have half-lives that are less than 10 hours, and the majority of these have half-lives that are less than 30 seconds. This element also has 12 meta states, with the most stable being 165mDy, 147mDy and 145mDy.
Naturally occurring europium (63Eu) is composed of two isotopes, 151Eu and 153Eu, with 153Eu being the most abundant (52.2% natural abundance). While 153Eu is observationally stable (theoretically can undergo alpha decay with half-life over 5.5×1017 years), 151Eu was found in 2007 to be unstable and undergo alpha decay. The half-life is measured to be (4.62 ± 0.95(stat.) ± 0.68(syst.)) × 1018 years which corresponds to 1 alpha decay per two minutes in every kilogram of natural europium. Besides the natural radioisotope 151Eu, 36 artificial radioisotopes have been characterized, with the most stable being 150Eu with a half-life of 36.9 years, 152Eu with a half-life of 13.516 years, 154Eu with a half-life of 8.593 years, and 155Eu with a half-life of 4.7612 years. The majority of the remaining radioactive isotopes, which range from 130Eu to 170Eu, have half-lives that are less than 12.2 seconds. This element also has 18 metastable isomers, with the most stable being 150mEu (t1/2 12.8 hours), 152m1Eu (t1/2 9.3116 hours) and 152m5Eu (t1/2 96 minutes).
Naturally occurring samarium (62Sm) is composed of five stable isotopes, 144Sm, 149Sm, 150Sm, 152Sm and 154Sm, and two extremely long-lived radioisotopes, 147Sm and 148Sm, with 152Sm being the most abundant. 146Sm is also fairly long-lived, but is not long-lived enough to have survived in significant quantities from the formation of the Solar System on Earth, although it remains useful in radiometric dating in the Solar System as an extinct radionuclide. It is the longest-lived nuclide that has not yet been confirmed to be primordial.
Naturally occurring neodymium (60Nd) is composed of 5 stable isotopes, 142Nd, 143Nd, 145Nd, 146Nd and 148Nd, with 142Nd being the most abundant (27.2% natural abundance), and 2 long-lived radioisotopes, 144Nd and 150Nd. In all, 33 radioisotopes of neodymium have been characterized up to now, with the most stable being naturally occurring isotopes 144Nd (alpha decay, a half-life (t1/2) of 2.29×1015 years) and 150Nd (double beta decay, t1/2 of 7×1018 years), and for practical purposes they can be considered to be stable as well. All of the remaining radioactive isotopes have half-lives that are less than 12 days, and the majority of these have half-lives that are less than 70 seconds; the most stable artificial isotope is 147Nd with a half-life of 10.98 days. This element also has 13 known meta states with the most stable being 139mNd (t1/2 5.5 hours), 135mNd (t1/2 5.5 minutes) and 133m1Nd (t1/2 ~70 seconds).
Naturally occurring cerium (58Ce) is composed of 4 stable isotopes: 136Ce, 138Ce, 140Ce, and 142Ce, with 140Ce being the most abundant and the only one theoretically stable; 136Ce, 138Ce, and 142Ce are predicted to undergo double beta decay but this process has never been observed. There are 35 radioisotopes that have been characterized, with the most stable being 144Ce, with a half-life of 284.893 days; 139Ce, with a half-life of 137.640 days and 141Ce, with a half-life of 32.501 days. All of the remaining radioactive isotopes have half-lives that are less than 4 days and the majority of these have half-lives that are less than 10 minutes. This element also has 10 meta states.
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).
There are 39 known isotopes and 17 nuclear isomers of tellurium (52Te), with atomic masses that range from 104 to 142. These are listed in the table below.
Tin (50Sn) is the element with the greatest number of stable isotopes. This is probably related to the fact that 50 is a "magic number" of protons. In addition, twenty-nine unstable tin isotopes are known, including tin-100 (100Sn) and tin-132 (132Sn), which are both "doubly magic". The longest-lived tin radioisotope is tin-126 (126Sn), with a half-life of 230,000 years. The other 28 radioisotopes have half-lives of less than a year.
Natural palladium (46Pd) is composed of six stable isotopes, 102Pd, 104Pd, 105Pd, 106Pd, 108Pd, and 110Pd, although 102Pd and 110Pd are theoretically unstable. The most stable radioisotopes are 107Pd with a half-life of 6.5 million years, 103Pd with a half-life of 17 days, and 100Pd with a half-life of 3.63 days. Twenty-three other radioisotopes have been characterized with atomic weights ranging from 90.949 u (91Pd) to 128.96 u (129Pd). Most of these have half-lives that are less than 30 minutes except 101Pd, 109Pd, and 112Pd.
Naturally occurring ruthenium (44Ru) is composed of seven stable isotopes. Additionally, 27 radioactive isotopes have been discovered. Of these radioisotopes, the most stable are 106Ru, with a half-life of 373.59 days; 103Ru, with a half-life of 39.26 days and 97Ru, with a half-life of 2.9 days.
Naturally occurring zirconium (40Zr) is composed of four stable isotopes (of which one 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 2.0×1019 years; 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. The second most stable radioisotope is 93Zr, which has a half-life of 1.53 million years. Thirty other radioisotopes have been observed. All have half-lives less than a day except for 95Zr (64.02 days), 88Zr (83.4 days), and 89Zr (78.41 hours). The primary decay mode is electron capture for isotopes lighter than 92Zr, and the primary mode for heavier isotopes is beta decay.
Copper (29Cu) has two stable isotopes, 63Cu and 65Cu, along with 28 radioisotopes. The most stable radioisotope is 67Cu with a half-life of 61.83 hours. Most of the others have half-lives under a minute. Unstable copper isotopes with atomic masses below 63 tend to undergo β+ decay, while isotopes with atomic masses above 65 tend to undergo β− decay. 64Cu decays by both β+ and β−.
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.