Geochronology/Lead–lead dating
Isotopes
editnuclide symbol |
historic name |
Z(p) | N(n) | isotopic mass (u) |
half-life | decay mode(s)[1][n 1] |
daughter isotope(s)[n 2] |
nuclear spin |
representative isotopic composition (mole fraction) |
range of natural variation (mole fraction) |
---|---|---|---|---|---|---|---|---|---|---|
excitation energy | ||||||||||
178Pb | 82 | 96 | 178.003830(26) | 0.23(15) ms | 0+ | |||||
179Pb | 82 | 97 | 179.00215(21)# | 3# ms | 5/2−# | |||||
180Pb | 82 | 98 | 179.997918(22) | 4.5(11) ms | 0+ | |||||
181Pb | 82 | 99 | 180.99662(10) | 45(20) ms | α (98%) | 177Hg | 5/2−# | |||
β+ (2%) | 181Tl | |||||||||
182Pb | 82 | 100 | 181.992672(15) | 60(40) ms [55(+40−35) ms] |
α (98%) | 178Hg | 0+ | |||
β+ (2%) | 182Tl | |||||||||
183Pb | 82 | 101 | 182.99187(3) | 535(30) ms | α (94%) | 179Hg | (3/2−) | |||
β+ (6%) | 183Tl | |||||||||
183mPb | 94(8) keV | 415(20) ms | α | 179Hg | (13/2+) | |||||
β+ (rare) | 183Tl | |||||||||
184Pb | 82 | 102 | 183.988142(15) | 490(25) ms | α | 180Hg | 0+ | |||
β+ (rare) | 184Tl | |||||||||
185Pb | 82 | 103 | 184.987610(17) | 6.3(4) s | α | 181Hg | 3/2− | |||
β+ (rare) | 185Tl | |||||||||
185mPb | 60(40)# keV | 4.07(15) s | α | 181Hg | 13/2+ | |||||
β+ (rare) | 185Tl | |||||||||
186Pb | 82 | 104 | 185.984239(12) | 4.82(3) s | α (56%) | 182Hg | 0+ | |||
β+ (44%) | 186Tl | |||||||||
187Pb | 82 | 105 | 186.983918(9) | 15.2(3) s | β+ | 187Tl | (3/2−) | |||
α | 183Hg | |||||||||
187mPb | 11(11) keV | 18.3(3) s | β+ (98%) | 187Tl | (13/2+) | |||||
α (2%) | 183Hg | |||||||||
188Pb | 82 | 106 | 187.980874(11) | 25.5(1) s | β+ (91.5%) | 188Tl | 0+ | |||
α (8.5%) | 184Hg | |||||||||
188m1Pb | 2578.2(7) keV | 830(210) ns | (8−) | |||||||
188m2Pb | 2800(50) keV | 797(21) ns | ||||||||
189Pb | 82 | 107 | 188.98081(4) | 51(3) s | β+ | 189Tl | (3/2−) | |||
189mPb | 40(30)# keV | 1# min | β+ (99.6%) | 189Tl | (13/2+) | |||||
α (.4%) | 185Hg | |||||||||
190Pb | 82 | 108 | 189.978082(13) | 71(1) s | β+ (99.1%) | 190Tl | 0+ | |||
α (.9%) | 186Hg | |||||||||
190m1Pb | 2614.8(8) keV | 150 ns | (10)+ | |||||||
190m2Pb | 2618(20) keV | 25 µs | (12+) | |||||||
190m3Pb | 2658.2(8) keV | 7.2(6) µs | (11)− | |||||||
191Pb | 82 | 109 | 190.97827(4) | 1.33(8) min | β+ (99.987%) | 191Tl | (3/2−) | |||
α (.013%) | 187Hg | |||||||||
191mPb | 20(50) keV | 2.18(8) min | β+ (99.98%) | 191Tl | 13/2(+) | |||||
α (.02%) | 187Hg | |||||||||
192Pb | 82 | 110 | 191.975785(14) | 3.5(1) min | β+ (99.99%) | 192Tl | 0+ | |||
α (.0061%) | 188Hg | |||||||||
192m1Pb | 2581.1(1) keV | 164(7) ns | (10)+ | |||||||
192m2Pb | 2625.1(11) keV | 1.1(5) µs | (12+) | |||||||
192m3Pb | 2743.5(4) keV | 756(21) ns | (11)− | |||||||
193Pb | 82 | 111 | 192.97617(5) | 5# min | β+ | 193Tl | (3/2−) | |||
193m1Pb | 130(80)# keV | 5.8(2) min | β+ | 193Tl | 13/2(+) | |||||
193m2Pb | 2612.5(5)+X keV | 135(+25−15) ns | (33/2+) | |||||||
194Pb | 82 | 112 | 193.974012(19) | 12.0(5) min | β+ (100%) | 194Tl | 0+ | |||
α (7.3×10−6%) | 190Hg | |||||||||
195Pb | 82 | 113 | 194.974542(25) | ~15 min | β+ | 195Tl | 3/2#- | |||
195m1Pb | 202.9(7) keV | 15.0(12) min | β+ | 195Tl | 13/2+ | |||||
195m2Pb | 1759.0(7) keV | 10.0(7) µs | 21/2− | |||||||
196Pb | 82 | 114 | 195.972774(15) | 37(3) min | β+ | 196Tl | 0+ | |||
α (3×10−5%) | 192Hg | |||||||||
196m1Pb | 1049.20(9) keV | <100 ns | 2+ | |||||||
196m2Pb | 1738.27(12) keV | <1 µs | 4+ | |||||||
196m3Pb | 1797.51(14) keV | 140(14) ns | 5− | |||||||
196m4Pb | 2693.5(5) keV | 270(4) ns | (12+) | |||||||
197Pb | 82 | 115 | 196.973431(6) | 8.1(17) min | β+ | 197Tl | 3/2− | |||
197m1Pb | 319.31(11) keV | 42.9(9) min | β+ (81%) | 197Tl | 13/2+ | |||||
IT (19%) | 197Pb | |||||||||
α (3×10−4%) | 193Hg | |||||||||
197m2Pb | 1914.10(25) keV | 1.15(20) µs | 21/2− | |||||||
198Pb | 82 | 116 | 197.972034(16) | 2.4(1) h | β+ | 198Tl | 0+ | |||
198m1Pb | 2141.4(4) keV | 4.19(10) µs | (7)− | |||||||
198m2Pb | 2231.4(5) keV | 137(10) ns | (9)− | |||||||
198m3Pb | 2820.5(7) keV | 212(4) ns | (12)+ | |||||||
199Pb | 82 | 117 | 198.972917(28) | 90(10) min | β+ | 199Tl | 3/2− | |||
199m1Pb | 429.5(27) keV | 12.2(3) min | IT (93%) | 199Pb | (13/2+) | |||||
β+ (7%) | 199Tl | |||||||||
199m2Pb | 2563.8(27) keV | 10.1(2) µs | (29/2−) | |||||||
200Pb | 82 | 118 | 199.971827(12) | 21.5(4) h | β+ | 200Tl | 0+ | |||
201Pb | 82 | 119 | 200.972885(24) | 9.33(3) h | EC (99%) | 201Tl | 5/2− | |||
β+ (1%) | 201Tl | |||||||||
201m1Pb | 629.14(17) keV | 61(2) s | 13/2+ | |||||||
201m2Pb | 2718.5+X keV | 508(5) ns | (29/2−) | |||||||
202Pb | 82 | 120 | 201.972159(9) | 52.5(28)×103 y | Electron capture (EC) (99%) | 202Tl | 0+ | |||
α (1%) | 198Hg | |||||||||
202m1Pb | 2169.83(7) keV | 3.53(1) h | IT (90.5%) | 202Pb | 9− | |||||
EC (9.5%) | 202Tl | |||||||||
202m2Pb | 4142.9(11) keV | 110(5) ns | (16+) | |||||||
202m3Pb | 5345.9(13) keV | 107(5) ns | (19−) | |||||||
203Pb | 82 | 121 | 202.973391(7) | 51.873(9) h | EC | 203Tl | 5/2− | |||
203m1Pb | 825.20(9) keV | 6.21(8) s | IT | 203Pb | 13/2+ | |||||
203m2Pb | 2949.47(22) keV | 480(7) ms | 29/2− | |||||||
203m3Pb | 2923.4+X keV | 122(4) ns | (25/2−) | |||||||
204Pb[n 3] | 82 | 122 | 203.9730436(13) | Observationally Stable[n 4] | 0+ | 0.014(1) | 0.0104–0.0165 | |||
204m1Pb | 1274.00(4) keV | 265(10) ns | 4+ | |||||||
204m2Pb | 2185.79(5) keV | 67.2(3) min | 9− | |||||||
204m3Pb | 2264.33(4) keV | 0.45(+10−3) µs | 7− | |||||||
205Pb | 82 | 123 | 204.9744818(13) | 15.3(7)×106 y | EC | 205Tl | 5/2− | |||
205m1Pb | 2.329(7) keV | 24.2(4) µs | 1/2− | |||||||
205m2Pb | 1013.839(13) keV | 5.55(2) ms | 13/2+ | |||||||
205m3Pb | 3195.7(5) keV | 217(5) ns | 25/2− | |||||||
206Pb[n 3][n 5] | Radium G | 82 | 124 | 205.9744653(13) | Observationally Stable[n 6] | 0+ | 0.241(1) | 0.2084–0.2748 | ||
206m1Pb | 2200.14(4) keV | 125(2) µs | 7− | |||||||
206m2Pb | 4027.3(7) keV | 202(3) ns | 12+ | |||||||
207Pb[n 3][n 7] | Actinium D | 82 | 125 | 206.9758969(13) | Observationally Stable[n 8] | 1/2− | 0.221(1) | 0.1762–0.2365 | ||
207mPb | 1633.368(5) keV | 806(6) ms | IT | 207Pb | 13/2+ | |||||
208Pb[n 9] | Thorium D | 82 | 126 | 207.9766521(13) | Observationally Stable[n 10] | 0+ | 0.524(1) | 0.5128–0.5621 | ||
208mPb | 4895(2) keV | 500(10) ns | 10+ | |||||||
209Pb | 82 | 127 | 208.9810901(19) | 3.253(14) h | β− | 209Bi | 9/2+ | Trace[n 11] | ||
210Pb | Radium D Radiolead Radio-lead |
82 | 128 | 209.9841885(16) | 22.3(22) y | β− (100%) | 210Bi | 0+ | Trace[n 12] | |
α (1.9×10−6%) | 206Hg | |||||||||
210mPb | 1278(5) keV | 201(17) ns | 8+ | |||||||
211Pb | Actinium B | 82 | 129 | 210.9887370(29) | 36.1(2) min | β− | 211Bi | 9/2+ | Trace[n 13] | |
212Pb | Thorium B | 82 | 130 | 211.9918975(24) | 10.64(1) h | β− | 212Bi | 0+ | Trace[n 14] | |
212mPb | 1335(10) keV | 5(1) µs | (8+) | |||||||
213Pb | 82 | 131 | 212.996581(8) | 10.2(3) min | β− | 213Bi | (9/2+) | |||
214Pb | Radium B | 82 | 132 | 213.9998054(26) | 26.8(9) min | β− | 214Bi | 0+ | Trace[n 12] | |
215Pb | 82 | 133 | 215.00481(44)# | 36(1) s | 5/2+# |
- ↑ Abbreviations:
EC: Electron capture
IT: Isomeric transition - ↑ Bold for stable isotopes, bold italics for nearly-stable isotopes (half-life longer than the age of the universe)
- ↑ 3.0 3.1 3.2 Used in lead-lead dating
- ↑ Believed to undergo α decay to 200Hg with a half-life over 1.4×1020 years
- ↑ Final decay product of 4n+2 decay chain (the Radium or Uranium series)
- ↑ Believed to undergo α decay to 202Hg with a half-life over 2.5×1021 years
- ↑ Final decay product of 4n+3 decay chain (the Actinium series)
- ↑ Believed to undergo α decay to 203Hg with a half-life over 1.9×1021 years
- ↑ Final decay product of 4n decay chain (the Thorium series)
- ↑ Heaviest observationally stable nuclide, believed to undergo α decay to 204Hg with a half-life over 2.6×1021 years
- ↑ Cluster decay product of 223Ra, which occurs in the decay chain of 235U
- ↑ 12.0 12.1 Intermediate decay product of 238U
- ↑ Intermediate decay product of 235U
- ↑ Intermediate decay product of 232Th
Notes
edit- Evaluated isotopic composition is for most but not all commercial samples.
- The precision of the isotope abundances and atomic mass is limited through variations. The given ranges should be applicable to any normal terrestrial material.
- Geologically exceptional samples are known in which the isotopic composition lies outside the reported range. The uncertainty in the atomic mass may exceed the stated value for such specimens.
- Values marked # are not purely derived from experimental data, but at least partly from systematic trends. Spins with weak assignment arguments are enclosed in parentheses.
- Uncertainties are given in concise form in parentheses after the corresponding last digits. Uncertainty values denote one standard deviation, except isotopic composition and standard atomic mass from IUPAC, which use expanded uncertainties.
- ↑ "Universal Nuclide Chart". nucleonica. Retrieved 2013-08-28.