Lead (
82Pb) has four stable
isotopes:
204Pb,
206Pb,
207Pb,
208Pb. Lead-204 is entirely a
primordial nuclide
In geochemistry, geophysics and nuclear physics, primordial nuclides, also known as primordial isotopes, are nuclides found on Earth that have existed in their current form since before Earth was formed. Primordial nuclides were present in the ...
and is not a
radiogenic nuclide
A radiogenic nuclide is a nuclide that is produced by a process of radioactive decay. It may itself be radioactive (a radionuclide) or stable (a stable nuclide).
Radiogenic nuclides (more commonly referred to as radiogenic isotopes) form some of ...
. The three isotopes lead-206, lead-207, and lead-208 represent the ends of three
decay chain
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
s: the
uranium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
(or radium series), the
actinium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
, and the
thorium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
, respectively; a fourth decay chain, the
neptunium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directly ...
, terminates with the
thallium
Thallium is a chemical element with the symbol Tl and atomic number 81. It is a gray post-transition metal that is not found free in nature. When isolated, thallium resembles tin, but discolors when exposed to air. Chemists William Crookes and ...
isotope
205Tl. The three series terminating in lead represent the decay chain products of long-lived primordial
238U,
235U, and
232Th, respectively. However, each of them also occurs, to some extent, as primordial isotopes that were made in supernovae, rather than radiogenically as daughter products. The fixed ratio of lead-204 to the primordial amounts of the other lead isotopes may be used as the baseline to estimate the extra amounts of radiogenic lead present in rocks as a result of decay from uranium and thorium. (See
lead–lead dating
Lead–lead dating is a method for dating geological samples, normally based on 'whole-rock' samples of material such as granite. For most dating requirements it has been superseded by uranium–lead dating (U–Pb dating), but in certain special ...
and
uranium–lead dating
Uranium–lead dating, abbreviated U–Pb dating, is one of the oldest and most refined of the radiometric dating schemes. It can be used to date rocks that formed and crystallised from about 1 million years to over 4.5 billion years ago with rout ...
).
The longest-lived
radioisotopes are
205Pb with a
half-life
Half-life (symbol ) is the time required for a quantity (of substance) to reduce to half of its initial value. The term is commonly used in nuclear physics to describe how quickly unstable atoms undergo radioactive decay or how long stable ato ...
of 17.3 million years and
202Pb with a half-life of 52,500 years. A shorter-lived naturally occurring radioisotope,
210Pb with a half-life of 22.2 years, is useful for studying the
sedimentation
Sedimentation is the deposition of sediments. It takes place when particles in suspension settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the ...
chronology of environmental samples on time scales shorter than 100 years.
The relative abundances of the four stable isotopes are approximately 1.5%, 24%, 22%, and 52.5%, combining to give a
standard atomic weight
The standard atomic weight of a chemical element (symbol ''A''r°(E) for element "E") is the weighted arithmetic mean of the relative isotopic masses of all isotopes of that element weighted by each isotope's abundance on Earth. For example, ...
(abundance-weighted average of the stable isotopes) of 207.2(1). Lead is the element with the heaviest stable isotope,
208Pb. (The more massive
209Bi, long considered to be stable, actually has a half-life of 2.01×10
19 years.)
208Pb is also a
doubly magic
In nuclear physics, a magic number is a number of nucleons (either protons or neutrons, separately) such that they are arranged into complete shells within the atomic nucleus. As a result, atomic nuclei with a 'magic' number of protons or neutron ...
isotope, as it has 82
protons and 126
neutrons.
It is the heaviest doubly magic nuclide known. A total of 43 lead isotopes are now known, including very unstable synthetic species.
The four primordial isotopes of lead are all
observationally stable
Stable nuclides are nuclides that are not radioactive and so (unlike radionuclides) do not spontaneously undergo radioactive decay. When such nuclides are referred to in relation to specific elements, they are usually termed stable isotopes.
Th ...
, meaning that they are predicted to undergo radioactive decay but no decay has been observed yet. These four isotopes are predicted to undergo
alpha decay
Alpha decay or α-decay is a type of radioactive decay in which an atomic nucleus emits an alpha particle (helium nucleus) and thereby transforms or 'decays' into a different atomic nucleus, with a mass number that is reduced by four and an ato ...
and become
isotopes of mercury
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 radioisoto ...
which are themselves radioactive or observationally stable.
In its fully ionized state, the isotope
205Pb also becomes stable.
List of isotopes
, -
,
178Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 96
, 178.003830(26)
, 0.23(15) ms
,
α
,
174Hg
, 0+
,
,
, -
,
179Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 97
, 179.00215(21)#
, 3.9(1.1) ms
, α
,
175Hg
, (9/2−)
,
,
, -
,
180Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 98
, 179.997918(22)
, 4.5(11) ms
, α
,
176Hg
, 0+
,
,
, -
, rowspan=2,
181Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 99
, rowspan=2, 180.99662(10)
, rowspan=2, 45(20) ms
, α (98%)
,
177Hg
, rowspan=2, (9/2−)
, rowspan=2,
, rowspan=2,
, -
,
β+ (2%)
,
181Tl
, -
, rowspan=2,
182Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 100
, rowspan=2, 181.992672(15)
, rowspan=2, 60(40) ms
5(+40−35) ms, α (98%)
,
178Hg
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, β
+ (2%)
,
182Tl
, -
, rowspan=2,
183Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 101
, rowspan=2, 182.99187(3)
, rowspan=2, 535(30) ms
, α (94%)
,
179Hg
, rowspan=2, (3/2−)
, rowspan=2,
, rowspan=2,
, -
, β
+ (6%)
,
183Tl
, -
, rowspan=2 style="text-indent:1em" ,
183mPb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 94(8) keV
, rowspan=2, 415(20) ms
, α
,
179Hg
, rowspan=2, (13/2+)
, rowspan=2,
, rowspan=2,
, -
, β
+ (rare)
,
183Tl
, -
, rowspan=2,
184Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 102
, rowspan=2, 183.988142(15)
, rowspan=2, 490(25) ms
, α
,
180Hg
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, β
+ (rare)
,
184Tl
, -
, rowspan=2,
185Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 103
, rowspan=2, 184.987610(17)
, rowspan=2, 6.3(4) s
, α
,
181Hg
, rowspan=2, 3/2−
, rowspan=2,
, rowspan=2,
, -
, β
+ (rare)
,
185Tl
, -
, rowspan=2 style="text-indent:1em" ,
185mPb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 60(40)# keV
, rowspan=2, 4.07(15) s
, α
,
181Hg
, rowspan=2, 13/2+
, rowspan=2,
, rowspan=2,
, -
, β
+ (rare)
,
185Tl
, -
, rowspan=2,
186Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 104
, rowspan=2, 185.984239(12)
, rowspan=2, 4.82(3) s
, α (56%)
,
182Hg
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, β
+ (44%)
,
186Tl
, -
, rowspan=2,
187Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 105
, rowspan=2, 186.983918(9)
, rowspan=2, 15.2(3) s
, β
+
,
187Tl
, rowspan=2, (3/2−)
, rowspan=2,
, rowspan=2,
, -
, α
,
183Hg
, -
, rowspan=2 style="text-indent:1em" ,
187mPb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 11(11) keV
, rowspan=2, 18.3(3) s
, β
+ (98%)
,
187Tl
, rowspan=2, (13/2+)
, rowspan=2,
, rowspan=2,
, -
, α (2%)
,
183Hg
, -
, rowspan=2,
188Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 106
, rowspan=2, 187.980874(11)
, rowspan=2, 25.5(1) s
, β
+ (91.5%)
,
188Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (8.5%)
,
184Hg
, -
, style="text-indent:1em" ,
188m1Pb
,
, colspan="3" style="text-indent:2em" , 2578.2(7) keV
, 830(210) ns
,
,
, (8−)
,
,
, -
, style="text-indent:1em" ,
188m2Pb
,
, colspan="3" style="text-indent:2em" , 2800(50) keV
, 797(21) ns
,
,
,
,
,
, -
,
189Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 107
, 188.98081(4)
, 51(3) s
, β
+
,
189Tl
, (3/2−)
,
,
, -
, rowspan=2 style="text-indent:1em" ,
189m1Pb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 40(30)# keV
, rowspan=2, 50.5(2.1) s
, β
+ (99.6%)
,
189Tl
, rowspan=2, 13/2+
, rowspan=2,
, rowspan=2,
, -
, α (.4%)
,
185Hg
, -
, style="text-indent:1em" ,
189m2Pb
,
, colspan="3" style="text-indent:2em" , 2475(30)# keV
, 26(5) μs
,
,
, (10)+
,
,
, -
, rowspan=2,
190Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 108
, rowspan=2, 189.978082(13)
, rowspan=2, 71(1) s
, β
+ (99.1%)
,
190Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (.9%)
,
186Hg
, -
, style="text-indent:1em" ,
190m1Pb
,
, colspan="3" style="text-indent:2em" , 2614.8(8) keV
, 150 ns
,
,
, (10)+
,
,
, -
, style="text-indent:1em" ,
190m2Pb
,
, colspan="3" style="text-indent:2em" , 2618(20) keV
, 25 μs
,
,
, (12+)
,
,
, -
, style="text-indent:1em" ,
190m3Pb
,
, colspan="3" style="text-indent:2em" , 2658.2(8) keV
, 7.2(6) μs
,
,
, (11)−
,
,
, -
, rowspan=2,
191Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 109
, rowspan=2, 190.97827(4)
, rowspan=2, 1.33(8) min
, β
+ (99.987%)
,
191Tl
, rowspan=2, (3/2−)
, rowspan=2,
, rowspan=2,
, -
, α (.013%)
,
187Hg
, -
, rowspan=2 style="text-indent:1em" ,
191mPb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 20(50) keV
, rowspan=2, 2.18(8) min
, β
+ (99.98%)
,
191Tl
, rowspan=2, 13/2(+)
, rowspan=2,
, rowspan=2,
, -
, α (.02%)
,
187Hg
, -
, rowspan=2,
192Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 110
, rowspan=2, 191.975785(14)
, rowspan=2, 3.5(1) min
, β
+ (99.99%)
,
192Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (.0061%)
,
188Hg
, -
, style="text-indent:1em" ,
192m1Pb
,
, colspan="3" style="text-indent:2em" , 2581.1(1) keV
, 164(7) ns
,
,
, (10)+
,
,
, -
, style="text-indent:1em" ,
192m2Pb
,
, colspan="3" style="text-indent:2em" , 2625.1(11) keV
, 1.1(5) μs
,
,
, (12+)
,
,
, -
, style="text-indent:1em" ,
192m3Pb
,
, colspan="3" style="text-indent:2em" , 2743.5(4) keV
, 756(21) ns
,
,
, (11)−
,
,
, -
,
193Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 111
, 192.97617(5)
, 5# min
, β
+
,
193Tl
, (3/2−)
,
,
, -
, style="text-indent:1em" ,
193m1Pb
,
, colspan="3" style="text-indent:2em" , 130(80)# keV
, 5.8(2) min
, β
+
,
193Tl
, 13/2(+)
,
,
, -
, style="text-indent:1em" ,
193m2Pb
,
, colspan="3" style="text-indent:2em" , 2612.5(5)+X keV
, 135(+25−15) ns
,
,
, (33/2+)
,
,
, -
, rowspan=2,
194Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 112
, rowspan=2, 193.974012(19)
, rowspan=2, 12.0(5) min
, β
+ (100%)
,
194Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (7.3×10
−6%)
,
190Hg
, -
,
195Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 113
, 194.974542(25)
, ~15 min
, β
+
,
195Tl
, 3/2#-
,
,
, -
, style="text-indent:1em" ,
195m1Pb
,
, colspan="3" style="text-indent:2em" , 202.9(7) keV
, 15.0(12) min
, β
+
,
195Tl
, 13/2+
,
,
, -
, style="text-indent:1em" ,
195m2Pb
,
, colspan="3" style="text-indent:2em" , 1759.0(7) keV
, 10.0(7) μs
,
,
, 21/2−
,
,
, -
, rowspan=2,
196Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 114
, rowspan=2, 195.972774(15)
, rowspan=2, 37(3) min
, β
+
,
196Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (3×10
−5%)
,
192Hg
, -
, style="text-indent:1em" ,
196m1Pb
,
, colspan="3" style="text-indent:2em" , 1049.20(9) keV
, <100 ns
,
,
, 2+
,
,
, -
, style="text-indent:1em" ,
196m2Pb
,
, colspan="3" style="text-indent:2em" , 1738.27(12) keV
, <1 μs
,
,
, 4+
,
,
, -
, style="text-indent:1em" ,
196m3Pb
,
, colspan="3" style="text-indent:2em" , 1797.51(14) keV
, 140(14) ns
,
,
, 5−
,
,
, -
, style="text-indent:1em" ,
196m4Pb
,
, colspan="3" style="text-indent:2em" , 2693.5(5) keV
, 270(4) ns
,
,
, (12+)
,
,
, -
,
197Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 115
, 196.973431(6)
, 8.1(17) min
, β
+
,
197Tl
, 3/2−
,
,
, -
, rowspan=3 style="text-indent:1em" ,
197m1Pb
, rowspan=3,
, rowspan=3 colspan="3" style="text-indent:2em" , 319.31(11) keV
, rowspan=3, 42.9(9) min
, β
+ (81%)
,
197Tl
, rowspan=3, 13/2+
, rowspan=3,
, rowspan=3,
, -
, IT (19%)
,
197Pb
, -
, α (3×10
−4%)
,
193Hg
, -
, style="text-indent:1em" ,
197m2Pb
,
, colspan="3" style="text-indent:2em" , 1914.10(25) keV
, 1.15(20) μs
,
,
, 21/2−
,
,
, -
,
198Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 116
, 197.972034(16)
, 2.4(1) h
, β
+
,
198Tl
, 0+
,
,
, -
, style="text-indent:1em" ,
198m1Pb
,
, colspan="3" style="text-indent:2em" , 2141.4(4) keV
, 4.19(10) μs
,
,
, (7)−
,
,
, -
, style="text-indent:1em" ,
198m2Pb
,
, colspan="3" style="text-indent:2em" , 2231.4(5) keV
, 137(10) ns
,
,
, (9)−
,
,
, -
, style="text-indent:1em" ,
198m3Pb
,
, colspan="3" style="text-indent:2em" , 2820.5(7) keV
, 212(4) ns
,
,
, (12)+
,
,
, -
,
199Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 117
, 198.972917(28)
, 90(10) min
, β
+
,
199Tl
, 3/2−
,
,
, -
, rowspan=2 style="text-indent:1em" ,
199m1Pb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 429.5(27) keV
, rowspan=2, 12.2(3) min
, IT (93%)
,
199Pb
, rowspan=2, (13/2+)
, rowspan=2,
, rowspan=2,
, -
, β
+ (7%)
,
199Tl
, -
, style="text-indent:1em" ,
199m2Pb
,
, colspan="3" style="text-indent:2em" , 2563.8(27) keV
, 10.1(2) μs
,
,
, (29/2−)
,
,
, -
,
200Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 118
, 199.971827(12)
, 21.5(4) h
, β
+
,
200Tl
, 0+
,
,
, -
, rowspan=2,
201Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 119
, rowspan=2, 200.972885(24)
, rowspan=2, 9.33(3) h
, EC (99%)
, rowspan=2,
201Tl
, rowspan=2, 5/2−
, rowspan=2,
, rowspan=2,
, -
, β
+ (1%)
, -
, style="text-indent:1em" ,
201m1Pb
,
, colspan="3" style="text-indent:2em" , 629.14(17) keV
, 61(2) s
,
,
, 13/2+
,
,
, -
, style="text-indent:1em" ,
201m2Pb
,
, colspan="3" style="text-indent:2em" , 2718.5+X keV
, 508(5) ns
,
,
, (29/2−)
,
,
, -
, rowspan=2,
202Pb
, rowspan=2,
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 120
, rowspan=2, 201.972159(9)
, rowspan=2, 5.25(28)×10
4 y
,
EC (99%)
,
202Tl
, rowspan=2, 0+
, rowspan=2,
, rowspan=2,
, -
, α (1%)
,
198Hg
, -
, rowspan=2 style="text-indent:1em" ,
202m1Pb
, rowspan=2,
, rowspan=2 colspan="3" style="text-indent:2em" , 2169.83(7) keV
, rowspan=2, 3.53(1) h
, IT (90.5%)
,
202Pb
, rowspan=2, 9−
, rowspan=2,
, rowspan=2,
, -
, EC (9.5%)
,
202Tl
, -
, style="text-indent:1em" ,
202m2Pb
,
, colspan="3" style="text-indent:2em" , 4142.9(11) keV
, 110(5) ns
,
,
, (16+)
,
,
, -
, style="text-indent:1em" ,
202m3Pb
,
, colspan="3" style="text-indent:2em" , 5345.9(13) keV
, 107(5) ns
,
,
, (19−)
,
,
, -
,
203Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 121
, 202.973391(7)
, 51.873(9) h
, EC
,
203Tl
, 5/2−
,
,
, -
, style="text-indent:1em" ,
203m1Pb
,
, colspan="3" style="text-indent:2em" , 825.20(9) keV
, 6.21(8) s
, IT
,
203Pb
, 13/2+
,
,
, -
, style="text-indent:1em" ,
203m2Pb
,
, colspan="3" style="text-indent:2em" , 2949.47(22) keV
, 480(7) ms
,
,
, 29/2−
,
,
, -
, style="text-indent:1em" ,
203m3Pb
,
, colspan="3" style="text-indent:2em" , 2923.4+X keV
, 122(4) ns
,
,
, (25/2−)
,
,
, -
,
204Pb
[Used in ]lead–lead dating
Lead–lead dating is a method for dating geological samples, normally based on 'whole-rock' samples of material such as granite. For most dating requirements it has been superseded by uranium–lead dating (U–Pb dating), but in certain special ...
,
, style="text-align:right" , 82
, style="text-align:right" , 122
, 203.9730436(13)
, colspan="3" style="text-align:center;",
Observationally Stable
Stable nuclides are nuclides that are not radioactive and so (unlike radionuclides) do not spontaneously undergo radioactive decay. When such nuclides are referred to in relation to specific elements, they are usually termed stable isotopes.
Th ...
[Believed to undergo α decay to 200Hg with a ]half-life
Half-life (symbol ) is the time required for a quantity (of substance) to reduce to half of its initial value. The term is commonly used in nuclear physics to describe how quickly unstable atoms undergo radioactive decay or how long stable ato ...
over 1.4×1020 years
, 0+
, 0.014(1)
, 0.0104–0.0165
, -
, style="text-indent:1em" ,
204m1Pb
,
, colspan="3" style="text-indent:2em" , 1274.00(4) keV
, 265(10) ns
,
,
, 4+
,
,
, -
, style="text-indent:1em" ,
204m2Pb
,
, colspan="3" style="text-indent:2em" , 2185.79(5) keV
, 67.2(3) min
,
,
, 9−
,
,
, -
, style="text-indent:1em" ,
204m3Pb
,
, colspan="3" style="text-indent:2em" , 2264.33(4) keV
, 0.45(+10−3) μs
,
,
, 7−
,
,
, -
,
205Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 123
, 204.9744818(13)
, 1.73(7)×10
7 y
, EC
,
205Tl
, 5/2−
,
,
, -
, style="text-indent:1em" ,
205m1Pb
,
, colspan="3" style="text-indent:2em" , 2.329(7) keV
, 24.2(4) μs
,
,
, 1/2−
,
,
, -
, style="text-indent:1em" ,
205m2Pb
,
, colspan="3" style="text-indent:2em" , 1013.839(13) keV
, 5.55(2) ms
,
,
, 13/2+
,
,
, -
, style="text-indent:1em" ,
205m3Pb
,
, colspan="3" style="text-indent:2em" , 3195.7(5) keV
, 217(5) ns
,
,
, 25/2−
,
,
, -
,
206Pb
[Final ]decay product
In nuclear physics, a decay product (also known as a daughter product, daughter isotope, radio-daughter, or daughter nuclide) is the remaining nuclide left over from radioactive decay. Radioactive decay often proceeds via a sequence of steps (de ...
of 4n+2 decay chain
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
(the Radium or Uranium series)
, Radium G
, style="text-align:right" , 82
, style="text-align:right" , 124
, 205.9744653(13)
, colspan="3" style="text-align:center;", Observationally Stable
[Experimental lower bound is years; the theoretical lifetime for α decay to 202Hg is years.]
, 0+
, 0.241(1)
, 0.2084–0.2748
, -
, style="text-indent:1em" ,
206m1Pb
,
, colspan="3" style="text-indent:2em" , 2200.14(4) keV
, 125(2) μs
,
,
, 7−
,
,
, -
, style="text-indent:1em" ,
206m2Pb
,
, colspan="3" style="text-indent:2em" , 4027.3(7) keV
, 202(3) ns
,
,
, 12+
,
,
, -
,
207Pb
[Final decay product of 4n+3 decay chain (the ]Actinium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
)
, Actinium D
, style="text-align:right" , 82
, style="text-align:right" , 125
, 206.9758969(13)
, colspan="3" style="text-align:center;", Observationally Stable
[Experimental lower bound is years; the theoretical lifetime for α decay to 203Hg is years. ]
, 1/2−
, 0.221(1)
, 0.1762–0.2365
, -
, style="text-indent:1em" ,
207mPb
,
, colspan="3" style="text-indent:2em" , 1633.368(5) keV
, 806(6) ms
, IT
,
207Pb
, 13/2+
,
,
, -
,
208Pb
[Final decay product of 4n decay chain (the ]Thorium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
)
, Thorium D
, style="text-align:right" , 82
, style="text-align:right" , 126
, 207.9766521(13)
, colspan="3" style="text-align:center;", Observationally Stable
[Experimental lower bound is years; the theoretical lifetime for α decay to 204Hg is years. ]
, 0+
, 0.524(1)
, 0.5128–0.5621
, -
, style="text-indent:1em" ,
208mPb
,
, colspan="3" style="text-indent:2em" , 4895(2) keV
, 500(10) ns
,
,
, 10+
,
,
, -
,
209Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 127
, 208.9810901(19)
, 3.253(14) h
, β
−
, ''
209Bi''
, 9/2+
, Trace
[Intermediate decay product of 237Np]
,
, -
, rowspan=2,
210Pb
, rowspan=2, Radium D
Radiolead
Radio-lead
, rowspan=2 style="text-align:right" , 82
, rowspan=2 style="text-align:right" , 128
, rowspan=2, 209.9841885(16)
, rowspan=2, 22.20(22) y
, β
− (100%)
,
210Bi
, rowspan=2, 0+
, rowspan=2, Trace
[Intermediate ]decay product
In nuclear physics, a decay product (also known as a daughter product, daughter isotope, radio-daughter, or daughter nuclide) is the remaining nuclide left over from radioactive decay. Radioactive decay often proceeds via a sequence of steps (de ...
of 238U
, rowspan=2,
, -
, α (1.9×10
−6%)
,
206Hg
, -
, style="text-indent:1em" ,
210mPb
,
, colspan="3" style="text-indent:2em" , 1278(5) keV
, 201(17) ns
,
,
, 8+
,
,
, -
,
211Pb
, Actinium B
, style="text-align:right" , 82
, style="text-align:right" , 129
, 210.9887370(29)
, 36.1(2) min
, β
−
,
211Bi
, 9/2+
, Trace
[Intermediate ]decay product
In nuclear physics, a decay product (also known as a daughter product, daughter isotope, radio-daughter, or daughter nuclide) is the remaining nuclide left over from radioactive decay. Radioactive decay often proceeds via a sequence of steps (de ...
of 235U
,
, -
,
212Pb
, Thorium B
, style="text-align:right" , 82
, style="text-align:right" , 130
, 211.9918975(24)
, 10.64(1) h
, β
−
,
212Bi
, 0+
, Trace
[Intermediate ]decay product
In nuclear physics, a decay product (also known as a daughter product, daughter isotope, radio-daughter, or daughter nuclide) is the remaining nuclide left over from radioactive decay. Radioactive decay often proceeds via a sequence of steps (de ...
of 232Th
,
, -
, style="text-indent:1em" ,
212mPb
,
, colspan="3" style="text-indent:2em" , 1335(10) keV
, 6.0(0.8) μs
, IT
,
212Pb
, (8+)
,
,
, -
,
213Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 131
, 212.996581(8)
, 10.2(3) min
, β
−
,
213Bi
, (9/2+)
,
,
, -
,
214Pb
, Radium B
, style="text-align:right" , 82
, style="text-align:right" , 132
, 213.9998054(26)
, 26.8(9) min
, β
−
,
214Bi
, 0+
, Trace
,
, -
, style="text-indent:1em" ,
214mPb
,
, colspan="3" style="text-indent:2em" , 1420(20) keV
, 6.2(0.3) μs
, IT
,
212Pb
, 8+#
,
,
, -
,
215Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 133
, 215.004660(60)
, 2.34(0.19) min
, β
−
,
215Bi
, 9/2+#
,
,
, -
,
216Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 134
, 216.008030(210)#
, 1.65(0.2) min
, β
−
,
216Bi
, 0+
,
,
, -
, style="text-indent:1em" ,
216mPb
,
, colspan="3" style="text-indent:2em" , 1514(20) keV
, 400(40) ns
, IT
,
216Pb
, 8+#
,
,
, -
,
217Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 135
, 217.013140(320)#
, 20(5) s
, β
−
,
217Bi
, 9/2+#
,
,
, -
,
218Pb
,
, style="text-align:right" , 82
, style="text-align:right" , 136
, 218.016590(320)#
, 15(7) s
, β
−
,
218Bi
, 0+
,
,
Lead-206
206Pb is the final step in the decay chain of
238U, the "radium series" or "uranium series". In a closed system, over time, a given mass of
238U will decay in a sequence of steps culminating in
206Pb. The production of intermediate products eventually reaches an equilibrium (though this takes a long time, as the half-life of
234U is 245,500 years). Once this stabilized system is reached, the ratio of
238U to
206Pb will steadily decrease, while the ratios of the other intermediate products to each other remain constant.
Like most radioisotopes found in the radium series,
206Pb was initially named as a variation of radium, specifically radium G. It is the decay product of both
210Po (historically called radium F) by
alpha decay
Alpha decay or α-decay is a type of radioactive decay in which an atomic nucleus emits an alpha particle (helium nucleus) and thereby transforms or 'decays' into a different atomic nucleus, with a mass number that is reduced by four and an ato ...
, and the much rarer
206Tl (radium E
II) by
beta decay
In nuclear physics, beta decay (β-decay) is a type of radioactive decay in which a beta particle (fast energetic electron or positron) is emitted from an atomic nucleus, transforming the original nuclide to an isobar of that nuclide. For e ...
.
Lead-206 has been proposed for use in
fast breeder nuclear fission reactor coolant over the use of natural lead mixture (which also includes other stable lead isotopes) as a mechanism to improve
neutron economy
Neutron economy is defined as the ratio of an adjoint weighted average of the excess neutron production divided by an adjoint weighted average of the fission production.
The distribution of neutron energies in a nuclear reactor differs from the f ...
and greatly suppress unwanted production of highly radioactive byproducts.
Lead-204, -207, and -208
204Pb is entirely
primordial
Primordial may refer to:
* Primordial era, an era after the Big Bang. See Chronology of the universe
* Primordial sea (a.k.a. primordial ocean, ooze or soup). See Abiogenesis
* Primordial nuclide, nuclides, a few radioactive, that formed before t ...
, and is thus useful for estimating the fraction of the other lead isotopes in a given sample that are also primordial, since the relative fractions of the various primordial lead isotopes is constant everywhere.
Any excess lead-206, -207, and -208 is thus assumed to be
radiogenic in origin,
allowing various uranium and thorium dating schemes to be used to estimate the age of rocks (time since their formation) based on the relative abundance of lead-204 to other isotopes.
207Pb is the end of the
actinium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
from
235U.
208Pb is the end of the
thorium series
In nuclear science, the decay chain refers to a series of radioactive decays of different radioactive decay products as a sequential series of transformations. It is also known as a "radioactive cascade". Most radioisotopes do not decay directl ...
from
232Th. While it only makes up approximately half of the composition of lead in most places on Earth, it can be found naturally enriched up to around 90% in thorium ores.
208Pb is the heaviest known stable nuclide and also the heaviest known
doubly magic
In nuclear physics, a magic number is a number of nucleons (either protons or neutrons, separately) such that they are arranged into complete shells within the atomic nucleus. As a result, atomic nuclei with a 'magic' number of protons or neutron ...
nucleus, as ''Z'' = 82 and
''N'' = 126 correspond to closed
nuclear shells.
As a consequence of this particularly stable configuration, its neutron capture
cross section
Cross section may refer to:
* Cross section (geometry)
** Cross-sectional views in architecture & engineering 3D
*Cross section (geology)
* Cross section (electronics)
* Radar cross section, measure of detectability
* Cross section (physics)
**Abs ...
is very low (even lower than that of
deuterium in the thermal spectrum), making it of interest for
lead-cooled fast reactor
The lead-cooled fast reactor is a nuclear reactor design that features a fast neutron spectrum and molten lead or lead-bismuth eutectic coolant.
Molten lead or lead-bismuth eutectic can be used as the primary coolant because especially lead, and ...
s.
Lead-212
212Pb-containing
radiopharmaceuticals have been trialed as therapeutic agents for the experimental cancer treatment
targeted alpha-particle therapy Targeted alpha-particle therapy (or TAT) is an in-development method of targeted radionuclide therapy of various cancers. It employs radioactive substances which undergo alpha decay to treat diseased tissue at close proximity. It has the potential t ...
.
References
Isotope masses from:
*
Isotopic compositions and standard atomic masses from:
*
*
Half-life, spin, and isomer data selected from the following sources.
*
*
*
{{Authority control
Lead
Lead