| |||||||||||||||||||||||||||||||||
Standard atomic weight Ar°(Tl) | |||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
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.
Thallium-202 (half-life 12.23 days) can be made in a cyclotron [4] while thallium-204 (half-life 3.78 years) is made by the neutron activation of stable thallium in a nuclear reactor. [5]
In the fully ionized state, the isotope 205Tl becomes beta-radioactive, decaying to 205Pb, [6] but 203Tl remains stable.
205Tl is the decay product of bismuth-209, an isotope that was once thought to be stable but is now known to undergo alpha decay with an extremely long half-life of 2.01×1019 y. [7] 205Tl is at the end of the neptunium series decay chain.
Nuclide [8] [n 1] | Historic name | Z | N | Isotopic mass (Da) [9] [n 2] [n 3] | Half-life [n 4] | Decay mode [n 5] | Daughter isotope [n 6] | Spin and parity [n 7] [n 4] | Natural abundance (mole fraction) | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Excitation energy [n 4] | Normal proportion | Range of variation | |||||||||||||||||
176Tl [10] | 81 | 95 | 176.00059(21)# | 2.4+1.6 −0.7 ms | p (~63%) | 175Hg | (3−, 4−, 5−) | ||||||||||||
α (~37%) | 172Au | ||||||||||||||||||
176mTl | ~671 keV | 290+200 −80 μs | p (~50%) | 175Hg | |||||||||||||||
α (~50%) | 172mAu | ||||||||||||||||||
177Tl [11] | 81 | 96 | 176.996427(27) | 18(5) ms | α (73%) | 173Au | (1/2+) | ||||||||||||
p (27%) | 176Hg | ||||||||||||||||||
177mTl | 807(18) keV | 230(40) μs | p (51%) | 176Hg | (11/2−) | ||||||||||||||
α (49%) | 173Au | ||||||||||||||||||
178Tl [12] | 81 | 97 | 177.99490(12)# | 255(9) ms | α (62%) | 174Au | (4-,5-) | ||||||||||||
β+ (38%) | 178Hg | ||||||||||||||||||
β+, SF (0.15%) | (various) | ||||||||||||||||||
179Tl [13] | 81 | 98 | 178.99109(5) | 437(9) ms | α (60%) | 175Au | (1/2+) | ||||||||||||
β+ (40%) | 179Hg | ||||||||||||||||||
179m1Tl | 825(10)# keV | 1.41(2) ms | α | 175Au | (11/2−) | ||||||||||||||
IT (rare) | 179Tl | ||||||||||||||||||
β+ (rare) | 179Hg | ||||||||||||||||||
179m2Tl | 904.5(9) keV | 119(14) ns | IT | 179Tl | (9/2−) | ||||||||||||||
180Tl [14] | 81 | 99 | 179.98991(13)# | 1.09(1) s | β+ (93%) | 180Hg | 4-# | ||||||||||||
α (7%) | 176Au | ||||||||||||||||||
β+, SF (0.0032%) | 100Ru, 80Kr [15] | ||||||||||||||||||
181Tl [16] | 81 | 100 | 180.986257(10) | 2.9(1) s | β+ (91.4%) | 181Hg | 1/2+# | ||||||||||||
α (8.6%) | 177Au | ||||||||||||||||||
181mTl | 834.9(4) keV | 1.40(3) ms | IT (99.60%) | 181Tl | (9/2−) | ||||||||||||||
α (0.40%) | 177Au | ||||||||||||||||||
182Tl | 81 | 101 | 181.98567(8) | 2.0(3) s | β+ (96%) | 182Hg | 2−# | ||||||||||||
α (4%) | 178Au | ||||||||||||||||||
182m1Tl | 100(100)# keV | 2.9(5) s | α | 178Au | (7+) | ||||||||||||||
β+ (rare) | 182Hg | ||||||||||||||||||
182m2Tl | 600(140)# keV | 10− | |||||||||||||||||
183Tl | 81 | 102 | 182.982193(10) | 6.9(7) s | β+ (98%) | 183Hg | 1/2+# | ||||||||||||
α (2%) | 179Au | ||||||||||||||||||
183m1Tl | 630(17) keV | 53.3(3) ms | IT (99.99%) | 183Tl | 9/2−# | ||||||||||||||
α (.01%) | 179Au | ||||||||||||||||||
183m2Tl | 976.8(3) keV | 1.48(10) μs | (13/2+) | ||||||||||||||||
184Tl | 81 | 103 | 183.98187(5) | 9.7(6) s | β+ | 184Hg | 2−# | ||||||||||||
184m1Tl | 100(100)# keV | 10# s | β+ (97.9%) | 184Hg | 7+# | ||||||||||||||
α (2.1%) | 180Au | ||||||||||||||||||
184m2Tl | 500(140)# keV | 47.1 ms | IT (99.911%) | (10−) | |||||||||||||||
α (.089%) | 180Au | ||||||||||||||||||
185Tl | 81 | 104 | 184.97879(6) | 19.5(5) s | α | 181Au | 1/2+# | ||||||||||||
β+ | 185Hg | ||||||||||||||||||
185mTl | 452.8(20) keV | 1.93(8) s | IT (99.99%) | 185Tl | 9/2−# | ||||||||||||||
α (.01%) | 181Au | ||||||||||||||||||
β+ | 185Hg | ||||||||||||||||||
186Tl | 81 | 105 | 185.97833(20) | 40# s | β+ | 186Hg | (2−) | ||||||||||||
α (.006%) | 182Au | ||||||||||||||||||
186m1Tl | 320(180) keV | 27.5(10) s | β+ | 186Hg | (7+) | ||||||||||||||
186m2Tl | 690(180) keV | 2.9(2) s | (10−) | ||||||||||||||||
187Tl | 81 | 106 | 186.975906(9) | ~51 s | β+ | 187Hg | (1/2+) | ||||||||||||
α (rare) | 183Au | ||||||||||||||||||
187mTl | 335(3) keV | 15.60(12) s | α | 183Au | (9/2−) | ||||||||||||||
IT | 187Tl | ||||||||||||||||||
β+ | 187Hg | ||||||||||||||||||
188Tl | 81 | 107 | 187.97601(4) | 71(2) s | β+ | 188Hg | (2−) | ||||||||||||
188m1Tl | 40(30) keV | 71(1) s | β+ | 188Hg | (7+) | ||||||||||||||
188m2Tl | 310(30) keV | 41(4) ms | (9−) | ||||||||||||||||
189Tl | 81 | 108 | 188.973588(12) | 2.3(2) min | β+ | 189Hg | (1/2+) | ||||||||||||
189mTl | 257.6(13) keV | 1.4(1) min | β+ (96%) | 189Hg | (9/2−) | ||||||||||||||
IT (4%) | 189Tl | ||||||||||||||||||
190Tl | 81 | 109 | 189.97388(5) | 2.6(3) min | β+ | 190Hg | 2(−) | ||||||||||||
190m1Tl | 130(90)# keV | 3.7(3) min | β+ | 190Hg | 7(+#) | ||||||||||||||
190m2Tl | 290(70)# keV | 750(40) μs | (8−) | ||||||||||||||||
190m3Tl | 410(70)# keV | >1 μs | 9− | ||||||||||||||||
191Tl | 81 | 110 | 190.971786(8) | 20# min | β+ | 191Hg | (1/2+) | ||||||||||||
191mTl | 297(7) keV | 5.22(16) min | β+ | 191Hg | 9/2(−) | ||||||||||||||
192Tl | 81 | 111 | 191.97223(3) | 9.6(4) min | β+ | 192Hg | (2−) | ||||||||||||
192m1Tl | 160(50) keV | 10.8(2) min | β+ | 192Hg | (7+) | ||||||||||||||
192m2Tl | 407(54) keV | 296(5) ns | (8−) | ||||||||||||||||
193Tl | 81 | 112 | 192.97067(12) | 21.6(8) min | β+ | 193Hg | 1/2(+#) | ||||||||||||
193mTl | 369(4) keV | 2.11(15) min | IT (75%) | 193Tl | 9/2− | ||||||||||||||
β+ (25%) | 193Hg | ||||||||||||||||||
194Tl | 81 | 113 | 193.97120(15) | 33.0(5) min | β+ | 194Hg | 2− | ||||||||||||
α (10−7%) | 190Au | ||||||||||||||||||
194mTl | 300(200)# keV | 32.8(2) min | β+ | 194Hg | (7+) | ||||||||||||||
195Tl | 81 | 114 | 194.969774(15) | 1.16(5) h | β+ | 195Hg | 1/2+ | ||||||||||||
195mTl | 482.63(17) keV | 3.6(4) s | IT | 195Tl | 9/2− | ||||||||||||||
196Tl | 81 | 115 | 195.970481(13) | 1.84(3) h | β+ | 196Hg | 2− | ||||||||||||
196mTl | 394.2(5) keV | 1.41(2) h | β+ (95.5%) | 196Hg | (7+) | ||||||||||||||
IT (4.5%) | 196Tl | ||||||||||||||||||
197Tl | 81 | 116 | 196.969575(18) | 2.84(4) h | β+ | 197Hg | 1/2+ | ||||||||||||
197mTl | 608.22(8) keV | 540(10) ms | IT | 197Tl | 9/2− | ||||||||||||||
198Tl | 81 | 117 | 197.97048(9) | 5.3(5) h | β+ | 198Hg | 2− | ||||||||||||
198m1Tl | 543.5(4) keV | 1.87(3) h | β+ (54%) | 198Hg | 7+ | ||||||||||||||
IT (46%) | 198Tl | ||||||||||||||||||
198m2Tl | 687.2(5) keV | 150(40) ns | (5+) | ||||||||||||||||
198m3Tl | 742.3(4) keV | 32.1(10) ms | (10−)# | ||||||||||||||||
199Tl | 81 | 118 | 198.96988(3) | 7.42(8) h | β+ | 199Hg | 1/2+ | ||||||||||||
199mTl | 749.7(3) keV | 28.4(2) ms | IT | 199Tl | 9/2− | ||||||||||||||
200Tl | 81 | 119 | 199.970963(6) | 26.1(1) h | β+ | 200Hg | 2− | ||||||||||||
200m1Tl | 753.6(2) keV | 34.3(10) ms | IT | 200Tl | 7+ | ||||||||||||||
200m2Tl | 762.0(2) keV | 0.33(5) μs | 5+ | ||||||||||||||||
201Tl [n 8] | 81 | 120 | 200.970819(16) | 72.912(17) h | EC | 201Hg | 1/2+ | ||||||||||||
201mTl | 919.50(9) keV | 2.035(7) ms | IT | 201Tl | (9/2−) | ||||||||||||||
202Tl | 81 | 121 | 201.972106(16) | 12.23(2) d | β+ | 202Hg | 2− | ||||||||||||
202mTl | 950.19(10) keV | 572(7) μs | 7+ | ||||||||||||||||
203Tl | 81 | 122 | 202.9723442(14) | Observationally Stable [n 9] | 1/2+ | 0.2952(1) | 0.29494–0.29528 | ||||||||||||
203mTl | 3400(300) keV | 7.7(5) μs | (25/2+) | ||||||||||||||||
204Tl | 81 | 123 | 203.9738635(13) | 3.78(2) y | β− (97.1%) | 204Pb | 2− | ||||||||||||
EC (2.9%) | 204Hg | ||||||||||||||||||
204m1Tl | 1104.0(4) keV | 63(2) μs | (7)+ | ||||||||||||||||
204m2Tl | 2500(500) keV | 2.6(2) μs | (12−) | ||||||||||||||||
204m3Tl | 3500(500) keV | 1.6(2) μs | (20+) | ||||||||||||||||
205Tl [n 10] | 81 | 124 | 204.9744275(14) | Observationally Stable [n 11] | 1/2+ | 0.7048(1) | 0.70472–0.70506 | ||||||||||||
205m1Tl | 3290.63(17) keV | 2.6(2) μs | 25/2+ | ||||||||||||||||
205m2Tl | 4835.6(15) keV | 235(10) ns | (35/2–) | ||||||||||||||||
206Tl | Radium E | 81 | 125 | 205.9761103(15) | 4.200(17) min | β− | 206Pb | 0− | Trace [n 12] | ||||||||||
206mTl | 2643.11(19) keV | 3.74(3) min | IT | 206Tl | (12–) | ||||||||||||||
207Tl | Actinium C | 81 | 126 | 206.977419(6) | 4.77(2) min | β− | 207Pb | 1/2+ | Trace [n 13] | ||||||||||
207mTl | 1348.1(3) keV | 1.33(11) s | IT (99.9%) | 207Tl | 11/2– | ||||||||||||||
β− (.1%) | 207Pb | ||||||||||||||||||
208Tl | Thorium C" | 81 | 127 | 207.9820187(21) | 3.053(4) min | β− | 208Pb | 5+ | Trace [n 14] | ||||||||||
209Tl | 81 | 128 | 208.985359(8) | 2.161(7) min | β− | 209Pb | 1/2+ | Trace [n 15] | |||||||||||
210Tl | Radium C″ | 81 | 129 | 209.990074(12) | 1.30(3) min | β− (99.991%) | 210Pb | (5+)# | Trace [n 12] | ||||||||||
β−, n (.009%) | 209Pb | ||||||||||||||||||
211Tl | 81 | 130 | 210.993480(50) | 80(16) s | β− (97.8%) | 211Pb | 1/2+ | ||||||||||||
β−, n (2.2%) | 210Pb | ||||||||||||||||||
212Tl | 81 | 131 | 211.998340(220)# | 31(8) s | β− (98.2%) | 212Pb | (5+) | ||||||||||||
β−, n (1.8%) | 211Pb | ||||||||||||||||||
213Tl | 81 | 132 | 213.001915(29) | 24(4) s | β− (92.4%) | 213Pb | 1/2+ | ||||||||||||
β−, n (7.6%) | 212Pb | ||||||||||||||||||
214Tl | 81 | 133 | 214.006940(210)# | 11(2) s | β− (66%) | 214Pb | 5+# | ||||||||||||
β−, n (34%) | 213Pb | ||||||||||||||||||
215Tl | 81 | 134 | 215.010640(320)# | 10(4) s | β− (95.4%) | 215Pb | 1/2+# | ||||||||||||
β−, n (4.6%) | 214Pb | ||||||||||||||||||
216Tl | 81 | 135 | 216.015800(320)# | 6(3) s | β− | 216Pb | 5+# | ||||||||||||
β−, n (<11.5%) | 215Pb | ||||||||||||||||||
This table header & footer: |
EC: | Electron capture |
IT: | Isomeric transition |
n: | Neutron emission |
p: | Proton emission |
Thallium-201 (201Tl) is a synthetic radioisotope of thallium. It has a half-life of 73 hours and decays by electron capture, emitting X-rays (~70–80 keV), and photons of 135 and 167 keV in 10% total abundance. [17] Thallium-201 is synthesized by the neutron activation of stable thallium in a nuclear reactor, [17] [18] or by the 203Tl(p, 3n)201Pb nuclear reaction in cyclotrons, as 201Pb naturally decays to 201Tl afterwards. [19] It is a radiopharmaceutical, as it has good imaging characteristics without excessive patient radiation dose. It is the most popular isotope used for thallium nuclear cardiac stress tests. [20]
Fluorine (9F) has 19 known isotopes ranging from 13
F
to 31
F
and two isomers. Only fluorine-19 is stable and naturally occurring in more than trace quantities; therefore, fluorine is a monoisotopic and mononuclidic element.
There are 39 known isotopes of radon (86Rn), from 193Rn to 231Rn; all are radioactive. The most stable isotope is 222Rn with a half-life of 3.823 days, which decays into 218
Po
. Six isotopes of radon, 217, 218, 219, 220, 221, 222Rn, occur in trace quantities in nature as decay products of, respectively, 217At, 218At, 223Ra, 224Ra, 225Ra, and 226Ra. 217Rn and 221Rn are produced in rare branches in the decay chain of trace quantities of 237Np; 222Rn is an intermediate step in the decay chain of 238U; 219Rn is an intermediate step in the decay chain of 235U; and 220Rn occurs in the decay chain of 232Th.
Astatine (85At) has 41 known isotopes, all of which are radioactive; their mass numbers range from 188 to 229. There are also 24 known metastable excited states. The longest-lived isotope is 210At, which has a half-life of 8.1 hours; the longest-lived isotope existing in naturally occurring decay chains is 219At with a half-life of 56 seconds.
There are 42 isotopes of polonium (84Po). They range in size from 186 to 227 nucleons. They are all radioactive. 210Po with a half-life of 138.376 days has the longest half-life of any naturally-occurring isotope of polonium and is the most common isotope of polonium. It is also the most easily synthesized polonium isotope. 209Po, which does not occur naturally, has the longest half-life of all isotopes of polonium at 124 years. 209Po can be made by using a cyclotron to bombard bismuth with protons, as can 208Po.
Bismuth (83Bi) has 41 known isotopes, ranging from 184Bi to 224Bi. Bismuth has no stable isotopes, but does have one very long-lived isotope; thus, the standard atomic weight can be given as 208.98040(1). Although bismuth-209 is now known to be radioactive, it has classically been considered to be a stable isotope because it has a half-life of approximately 2.01×1019 years, which is more than a billion times the age of the universe. Besides 209Bi, the most stable bismuth radioisotopes are 210mBi with a half-life of 3.04 million years, 208Bi with a half-life of 368,000 years and 207Bi, with a half-life of 32.9 years, none of which occurs in nature. All other isotopes have half-lives under 1 year, most under a day. Of naturally occurring radioisotopes, the most stable is radiogenic 210Bi with a half-life of 5.012 days. 210mBi is unusual for being a nuclear isomer with a half-life multiple orders of magnitude longer than that of the ground state.
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 erbium (68Er) is composed of six stable isotopes, with 166Er being the most abundant. Thirty-nine radioisotopes have been characterized with between 74 and 112 neutrons, or 142 to 180 nucleons, with the most stable being 169Er with a half-life of 9.4 days, 172Er with a half-life of 49.3 hours, 160Er with a half-life of 28.58 hours, 165Er with a half-life of 10.36 hours, and 171Er with a half-life of 7.516 hours. All of the remaining radioactive isotopes have half-lives that are less than 3.5 hours, and the majority of these have half-lives that are less than 4 minutes. This element also has numerous meta states, with the most stable being 167mEr.
Naturally occurring terbium (65Tb) is composed of one stable isotope, 159Tb. Thirty-seven radioisotopes have been characterized, with the most stable being 158Tb with a half-life of 180 years, 157Tb with a half-life of 71 years, and 160Tb with a half-life of 72.3 days. All of the remaining radioactive isotopes have half-lives that are less than 6.907 days, and the majority of these have half-lives that are less than 24 seconds. This element also has 27 meta states, with the most stable being 156m1Tb, 154m2Tb and 154m1Tb.
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 silver (47Ag) is composed of the two stable isotopes 107Ag and 109Ag in almost equal proportions, with 107Ag being slightly more abundant. Notably, silver is the only element with all stable istopes having nuclear spins of 1/2. Thus both 107Ag and 109Ag nuclei produce narrow lines in nuclear magnetic resonance spectra.
Natural yttrium (39Y) is composed of a single isotope yttrium-89. The most stable radioisotopes are 88Y, which has a half-life of 106.6 days, and 91Y, with a half-life of 58.51 days. All the other isotopes have half-lives of less than a day, except 87Y, which has a half-life of 79.8 hours, and 90Y, with 64 hours. The dominant decay mode below the stable 89Y is electron capture and the dominant mode after it is beta emission. Thirty-five unstable isotopes have been characterized.
Bromine (35Br) has two stable isotopes, 79Br and 81Br, and 35 known radioisotopes, the most stable of which is 77Br, with a half-life of 57.036 hours.
Germanium (32Ge) has five naturally occurring isotopes, 70Ge, 72Ge, 73Ge, 74Ge, and 76Ge. Of these, 76Ge is very slightly radioactive, decaying by double beta decay with a half-life of 1.78 × 1021 years (130 billion times the age of the universe).
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.
Magnesium (12Mg) naturally occurs in three stable isotopes: 24
Mg, 25
Mg, and 26
Mg. There are 19 radioisotopes that have been discovered, ranging from 18
Mg to 40
Mg. The longest-lived radioisotope is 28
Mg with a half-life of 20.915(9) h. The lighter isotopes mostly decay to isotopes of sodium while the heavier isotopes decay to isotopes of aluminium. The shortest-lived is proton-unbound 18
Mg with a half-life of 4.0(3.4) zeptoseconds.
Berkelium (97Bk) is an artificial 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 243Bk in 1949. There are twenty known radioisotopes, from 233Bk and 233Bk to 253Bk, and six nuclear isomers. The longest-lived isotope is 247Bk with a half-life of 1,380 years.
Einsteinium (99Es) is a synthetic element, and thus a standard atomic weight cannot be given. Like all synthetic elements, it has no stable isotopes. The first isotope to be discovered was 253Es in 1952. There are 18 known radioisotopes from 240Es to 257Es, and 4 nuclear isomers. The longest-lived isotope is 252Es with a half-life of 471.7 days, or around 1.293 years.
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.