half-life (t1/2)
131Cs
9.7 d
133Cs
100%
134Cs
synth
2.0648 y
ε
135Cs
1.33×106 y
β−
synth
30.17 y[2]
β−
Standard atomic weight Ar°(Cs)
Caesium (55Cs) has 41 known isotopes, the atomic masses of these isotopes range from 112 to 152. Only one isotope, 133Cs, is stable. The longest-lived radioisotopes are 135Cs with a half-life of 1.33 million years, 137
Cs
with a half-life of 30.1671 years and 134Cs with a half-life of 2.0652 years. All other isotopes have half-lives less than 2 weeks, most under an hour.
Beginning in 1945 with the commencement of nuclear testing, caesium radioisotopes were released into the atmosphere where caesium is absorbed readily into solution and is returned to the surface of the Earth as a component of radioactive fallout. Once caesium enters the ground water, it is deposited on soil surfaces and removed from the landscape primarily by particle transport. As a result, the input function of these isotopes can be estimated as a function of time.
Excitation energy[n 8]
112Cs
55
57
111.95030(33)#
500(100) μs
111Xe
1+#
108I
113Cs
55
58
112.94449(11)
16.7(7) μs
p (99.97%)
112Xe
5/2+#
β+ (.03%)
113Xe
114Cs
55
59
113.94145(33)#
0.57(2) s
β+ (91.09%)
114Xe
(1+)
β+, p (8.69%)
113I
β+, α (.19%)
110Te
α (.018%)
110I
115Cs
55
60
114.93591(32)#
1.4(8) s
β+ (99.93%)
115Xe
9/2+#
β+, p (.07%)
114I
116Cs
55
61
115.93337(11)#
0.70(4) s
β+ (99.67%)
116Xe
(1+)
β+, p (.279%)
115I
β+, α (.049%)
112Te
116mCs
100(60)# keV
3.85(13) s
β+ (99.48%)
116Xe
4+, 5, 6
β+, p (.51%)
115I
β+, α (.008%)
112Te
117Cs
55
62
116.92867(7)
8.4(6) s
β+
117Xe
(9/2+)#
117mCs
150(80)# keV
6.5(4) s
β+
117Xe
3/2+#
118Cs
55
63
117.926559(14)
14(2) s
β+ (99.95%)
118Xe
2
β+, p (.042%)
117I
β+, α (.0024%)
114Te
118mCs
100(60)# keV
17(3) s
β+ (99.95%)
118Xe
(7−)
β+, p (.042%)
117I
β+, α (.0024%)
114Te
119Cs
55
64
118.922377(15)
43.0(2) s
β+
119Xe
9/2+
β+, α (2×10−6%)
115Te
119mCs
50(30)# keV
30.4(1) s
β+
119Xe
3/2(+)
120Cs
55
65
119.920677(11)
61.2(18) s
β+
120Xe
2(−#)
β+, α (2×10−5%)
116Te
β+, p (7×10−6%)
119I
120mCs
100(60)# keV
57(6) s
β+
120Xe
(7−)
β+, α (2×10−5%)
116Te
β+, p (7×10−6%)
119I
121Cs
55
66
120.917229(15)
155(4) s
β+
121Xe
3/2(+)
121mCs
68.5(3) keV
122(3) s
β+ (83%)
121Xe
9/2(+)
IT (17%)
121Cs
122Cs
55
67
121.91611(3)
21.18(19) s
β+
122Xe
1+
β+, α (2×10−7%)
118Te
122m1Cs
45.8 keV
>1 μs
(3)+
122m2Cs
140(30) keV
3.70(11) min
β+
122Xe
8−
122m3Cs
127.0(5) keV
360(20) ms
(5)−
123Cs
55
68
122.912996(13)
5.88(3) min
β+
123Xe
1/2+
123m1Cs
156.27(5) keV
1.64(12) s
IT
123Cs
(11/2)−
123m2Cs
231.63+X keV
114(5) ns
(9/2+)
124Cs
55
69
123.912258(9)
30.9(4) s
β+
124Xe
1+
124mCs
462.55(17) keV
6.3(2) s
IT
124Cs
(7)+
125Cs
55
70
124.909728(8)
46.7(1) min
β+
125Xe
1/2(+)
125mCs
266.6(11) keV
900(30) ms
(11/2−)
126Cs
55
71
125.909452(13)
1.64(2) min
β+
126Xe
1+
126m1Cs
273.0(7) keV
>1 μs
126m2Cs
596.1(11) keV
171(14) μs
127Cs
55
72
126.907418(6)
6.25(10) h
β+
127Xe
1/2+
127mCs
452.23(21) keV
55(3) μs
(11/2)−
128Cs
55
73
127.907749(6)
3.640(14) min
β+
128Xe
1+
129Cs
55
74
128.906064(5)
32.06(6) h
β+
129Xe
1/2+
130Cs
55
75
129.906709(9)
29.21(4) min
β+ (98.4%)
130Xe
1+
β− (1.6%)
130Ba
130mCs
163.25(11) keV
3.46(6) min
IT (99.83%)
130Cs
5−
β+ (.16%)
130Xe
131Cs
55
76
130.905464(5)
9.689(16) d
131Xe
5/2+
132Cs
55
77
131.9064343(20)
6.480(6) d
β+ (98.13%)
132Xe
2+
β− (1.87%)
132Ba
55
78
132.905451933(24)
Stable
7/2+
1.0000
134Cs[n 10]
55
79
133.906718475(28)
2.0652(4) y
β−
134Ba
4+
EC (3×10−4%)
134Xe
134mCs
138.7441(26) keV
2.912(2) h
IT
134Cs
8−
135Cs[n 10]
55
80
134.9059770(11)
2.3 x106 y
β−
135Ba
7/2+
135mCs
1632.9(15) keV
53(2) min
IT
135Cs
19/2−
136Cs
55
81
135.9073116(20)
13.16(3) d
β−
136Ba
5+
136mCs
518(5) keV
19(2) s
β−
136Ba
8−
IT
136Cs
55
82
136.9070895(5)
30.1671(13) y
β− (95%)
137mBa
7/2+
β− (5%)
137Ba
138Cs
55
83
137.911017(10)
33.41(18) min
β−
138Ba
3−
138mCs
79.9(3) keV
2.91(8) min
IT (81%)
138Cs
6−
β− (19%)
138Ba
139Cs
55
84
138.913364(3)
9.27(5) min
β−
139Ba
7/2+
140Cs
55
85
139.917282(9)
63.7(3) s
β−
140Ba
1−
141Cs
55
86
140.920046(11)
24.84(16) s
β− (99.96%)
141Ba
7/2+
β−, n (.0349%)
140Ba
142Cs
55
87
141.924299(11)
1.689(11) s
β− (99.9%)
142Ba
0−
β−, n (.091%)
141Ba
143Cs
55
88
142.927352(25)
1.791(7) s
β− (98.38%)
143Ba
3/2+
β−, n (1.62%)
142Ba
144Cs
55
89
143.932077(28)
994(4) ms
β− (96.8%)
144Ba
1(−#)
β−, n (3.2%)
143Ba
144mCs
300(200)# keV
<1 s
β−
144Ba
(>3)
IT
144Cs
145Cs
55
90
144.935526(12)
582(6) ms
β− (85.7%)
145Ba
3/2+
β−, n (14.3%)
144Ba
146Cs
55
91
145.94029(8)
0.321(2) s
β− (85.8%)
146Ba
1−
β−, n (14.2%)
145Ba
147Cs
55
92
146.94416(6)
0.235(3) s
β− (71.5%)
147Ba
(3/2+)
β−, n (28.49%)
146Ba
148Cs
55
93
147.94922(62)
146(6) ms
β− (74.9%)
148Ba
β−, n (25.1%)
147Ba
149Cs
55
94
148.95293(21)#
150# ms [>50 ms]
β−
149Ba
3/2+#
β−, n
148Ba
150Cs
55
95
149.95817(32)#
100# ms [>50 ms]
β−
150Ba
β−, n
149Ba
151Cs
55
96
150.96219(54)#
60# ms [>50 ms]
β−
151Ba
3/2+#
β−, n
150Ba
EC:
IT:
n:
p:
Caesium-131, introduced in 2004 for brachytherapybyIsoray,[5] has a half-life of 9.7 days and 30.4 keV energy.
Caesium-133 is the only stable isotope of caesium. The SI base unit of time, the second, is defined by a specific caesium-133 transition. Since 1967, the official definition of a second is:
The second, symbol s, is defined by taking the fixed numerical value of the caesium frequency, ΔνCs, the unperturbed ground-state hyperfine transition frequency of the caesium-133 atom,[6] to be 9192631770 when expressed in the unit Hz, which is equal to s−1.
Caesium-134 has a half-life of 2.0652 years. It is produced both directly (at a very small yield because 134Xe is stable) as a fission product and via neutron capture from nonradioactive 133Cs (neutron capture cross section29barns), which is a common fission product. Caesium-134 is not produced via beta decay of other fission product nuclides of mass 134 since beta decay stops at stable 134Xe. It is also not produced by nuclear weapons because 133Cs is created by beta decay of original fission products only long after the nuclear explosion is over.
The combined yield of 133Cs and 134Cs is given as 6.7896%. The proportion between the two will change with continued neutron irradiation. 134Cs also captures neutrons with a cross section of 140 barns, becoming long-lived radioactive 135Cs.
Caesium-134 undergoes beta decay (β−), producing 134Ba directly and emitting on average 2.23 gamma ray photons (mean energy 0.698 MeV).[7]
Nuclide
(Ma)
(%)[a 2]
(keV)
0.211
6.1385
294
β
0.230
0.1084
4050[a 3]
βγ
0.327
0.0447
151
β
1.33
6.9110[a 4]
269
β
1.53
5.4575
91
βγ
6.5
1.2499
33
β
15.7
0.8410
194
βγ
Caesium-135 is a mildly radioactive isotope of caesium with a half-life of 2.3 million years. It decays via emission of a low-energy beta particle into the stable isotope barium-135. Caesium-135 is one of the seven long-lived fission products and the only alkaline one. In most types of nuclear reprocessing, it stays with the medium-lived fission products (including 137
Cs which can only be separated from Cs-135 via isotope separation) rather than with other long-lived fission products. Except in the Molten salt reactor, where Cs-135 is created as a completely separate stream outside the fuel (after the decay of bubble-separated Xe-135). The low decay energy, lack of gamma radiation, and long half-life of 135Cs make this isotope much less hazardous than 137Csor134Cs.
Its precursor 135Xe has a high fission product yield (e.g. 6.3333% for 235U and thermal neutrons) but also has the highest known thermal neutron capture cross section of any nuclide. Because of this, much of the 135Xe produced in current thermal reactors (as much as >90% at steady-state full power)[8] will be converted to extremely long-lived (half-life on the order of 1021 years) 136
Xe before it can decay to 135
Cs despite the relatively short half life of 135
Xe. Little or no 135
Xe will be destroyed by neutron capture after a reactor shutdown, or in a molten salt reactor that continuously removes xenon from its fuel, a fast neutron reactor, or a nuclear weapon. The xenon pit is a phenomenon of excess neutron absorption through 135
Xe buildup in the reactor after a reduction in power or a shutdown and is often managed by letting the 135
Xe decay away to a level at which neutron flux can be safely controlled via control rods again.
A nuclear reactor will also produce much smaller amounts of 135Cs from the nonradioactive fission product 133Cs by successive neutron capture to 134Cs and then 135Cs.
The thermal neutron capture cross section and resonance integralof135Cs are 8.3 ± 0.3 and 38.1 ± 2.6 barns respectively.[9] Disposal of 135Cs by nuclear transmutation is difficult, because of the low cross section as well as because neutron irradiation of mixed-isotope fission caesium produces more 135Cs from stable 133Cs. In addition, the intense medium-term radioactivity of 137Cs makes handling of nuclear waste difficult.[10]
Caesium-136 has a half-life of 13.16 days. It is produced both directly (at a very small yield because 136Xe is beta-stable) as a fission product and via neutron capture from long-lived 135Cs (neutron capture cross section 8.702 barns), which is a common fission product. Caesium-136 is not produced via beta decay of other fission product nuclides of mass 136 since beta decay stops at almost-stable 136Xe. It is also not produced by nuclear weapons because 135Cs is created by beta decay of original fission products only long after the nuclear explosion is over. 136Cs also captures neutrons with a cross section of 13.00 barns, becoming medium-lived radioactive 137Cs. Caesium-136 undergoes beta decay (β−), producing 136Ba directly.
Caesium-137, with a half-life of 30.17 years, is one of the two principal medium-lived fission products, along with 90Sr, which are responsible for most of the radioactivityofspent nuclear fuel after several years of cooling, up to several hundred years after use. It constitutes most of the radioactivity still left from the Chernobyl accident and is a major health concern for decontaminating land near the Fukushima nuclear power plant.[11] 137Cs beta decays to barium-137m (a short-lived nuclear isomer) then to nonradioactive barium-137. Caesium-137 does not emit gamma radiation directly, all observed radiation is due to the daughter isotope barium-137m.
137Cs has a very low rate of neutron capture and cannot yet be feasibly disposed of in this way unless advances in neutron beam collimation (not otherwise achievable by magnetic fields), uniquely available only from within muon catalyzed fusion experiments (not in the other forms of Accelerator Transmutation of Nuclear Waste) enables production of neutrons at high enough intensity to offset and overcome these low capture rates; until then, therefore, 137Cs must simply be allowed to decay.
137Cs has been used as a tracer in hydrologic studies, analogous to the use of 3H.
The other isotopes have half-lives from a few days to fractions of a second. Almost all caesium produced from nuclear fission comes from beta decay of originally more neutron-rich fission products, passing through isotopes of iodine then isotopes of xenon. Because these elements are volatile and can diffuse through nuclear fuel or air, caesium is often created far from the original site of fission.
Hydrogen and
alkali metals
Alkaline
earth metals
Pnictogens
Chalcogens
Halogens
Noble gases
12 3 4
5 6 7 8 9 10 11 12
13 14 15 16 17 18 19 20
21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38
39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56