Isotopes of chlorine
Chlorine (Cl) has 24 isotopes with mass numbers ranging from 22Cl to 51Cl and 2 isomers (34mCl and 38mCl). There are two principal stable isotopes, 35Cl (75.78%) and 37Cl (24.22%), found in the relative proportions of 37.89:12.11, respectively, giving chlorine a relative atomic mass of 35.453. The longest-lived radioactive isotope is 36Cl, which has a half-life of 301,000 years. All other isotopes have half-lives under 1 hour, many less than one second. The shortest-lived are 29Cl and 30Cl, with half-lives less than 20 and 30 nanoseconds, respectively—the half-life of 28Cl is unknown.
Relative atomic mass: 35.453(2)
Chlorine-36 (36Cl)
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Trace amounts of radioactive 36Cl exist in the environment, in a ratio of about 7×10−13 to 1 with stable isotopes. 36Cl is produced in the atmosphere by spallation of 36Ar by interactions with cosmic ray protons. In the subsurface environment, 36Cl is generated primarily as a result of neutron capture by 35Cl or muon capture by 40Ca. 36Cl decays to either 36S (1.9%) or to 36Ar (98.1%), with a combined half-life of 308,000 years. The half-life of this hydrophilic nonreactive isotope makes it suitable for geologic dating in the range of 60,000 to 1 million years. Additionally, large amounts of 36Cl were produced by irradiation of seawater during atmospheric detonations of nuclear weapons between 1952 and 1958. The residence time of 36Cl in the atmosphere is about 1 week. Thus, as an event marker of 1950s water in soil and ground water, 36Cl is also useful for dating waters less than 50 years before the present. 36Cl has seen use in other areas of the geological sciences, forecasts, and elements.
Table
nuclide symbol |
Atomic Number | 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 | |||||||||
28Cl | 17 | 11 | 28.02851(54)# | p | 27S | (1+)# | |||
29Cl | 17 | 12 | 29.01411(21)# | <20 ns | p | 28S | (3/2+)# | ||
30Cl | 17 | 13 | 30.00477(21)# | <30 ns | p | 29S | (3+)# | ||
31Cl | 17 | 14 | 30.99241(5) | 150(25) ms | β+ (99.3%) | 31S | 3/2+ | ||
β+, p (.7%) | 30P | ||||||||
32Cl | 17 | 15 | 31.985690(7) | 298(1) ms | β+ (99.92%) | 32S | 1+ | ||
β+, α (.054%) | 28Si | ||||||||
β+, p (.026%) | 31P | ||||||||
33Cl | 17 | 16 | 32.9774519(5) | 2.511(3) s | β+ | 33S | 3/2+ | ||
34Cl | 17 | 17 | 33.97376282(19) | 1.5264(14) s | β+ | 34S | 0+ | ||
34mCl | 146.36(3) keV | 32.00(4) min | β+ (55.4%) | 34S | 3+ | ||||
IT (44.6%) | 34Cl | ||||||||
35Cl | 17 | 18 | 34.96885268(4) | Stable | 3/2+ | 0.7576(10) | 0.75644–0.75923 | ||
36Cl[n 3] | 17 | 19 | 35.96830698(8) | 3.01(2)×105 y | β− (98.1%) | 36Ar | 2+ | Trace[n 4] | approx. 7*10−13 |
ε (1.9%) | 36S | ||||||||
37Cl | 17 | 20 | 36.96590259(5) | Stable | 3/2+ | 0.2424(10) | 0.24077–0.24356 | ||
38Cl | 17 | 21 | 37.96801043(10) | 37.24(5) min | β− | 38Ar | 2− | ||
38mCl | 671.361(8) keV | 715(3) ms | IT | 38Cl | 5− | ||||
39Cl | 17 | 22 | 38.9680082(19) | 55.6(2) min | β− | 39Ar | 3/2+ | ||
40Cl | 17 | 23 | 39.97042(3) | 1.35(2) min | β− | 40Ar | 2− | ||
41Cl | 17 | 24 | 40.97068(7) | 38.4(8) s | β− | 41Ar | (1/2+,3/2+) | ||
42Cl | 17 | 25 | 41.97325(15) | 6.8(3) s | β− | 42Ar | |||
43Cl | 17 | 26 | 42.97405(17) | 3.07(7) s | β− (>99.9%) | 43Ar | 3/2+# | ||
β−, n (<.1%) | 42Ar | ||||||||
44Cl | 17 | 27 | 43.97828(12) | 0.56(11) s | β− (92%) | 44Ar | |||
β−, n (8%) | 43Ar | ||||||||
45Cl | 17 | 28 | 44.98029(13) | 400(40) ms | β− (76%) | 45Ar | 3/2+# | ||
β−, n (24%) | 44Ar | ||||||||
46Cl | 17 | 29 | 45.98421(77) | 232(2) ms | β−, n (60%) | 45Ar | |||
β− (40%) | 46Ar | ||||||||
47Cl | 17 | 30 | 46.98871(64)# | 101(6) ms | β− (97%) | 47Ar | 3/2+# | ||
β−, n (3%) | 46Ar | ||||||||
48Cl | 17 | 31 | 47.99495(75)# | 100# ms [>200 ns] | β− | 48Ar | |||
49Cl | 17 | 32 | 49.00032(86)# | 50# ms [>200 ns] | β− | 49Ar | 3/2+# | ||
50Cl | 17 | 33 | 50.00784(97)# | 20# ms | β− | 50Ar | |||
51Cl | 17 | 34 | 51.01449(107)# | 2# ms [>200 ns] | β− | 51Ar | 3/2+# |
- ↑ Abbreviations:
IT: Isomeric transition - ↑ Bold for stable isotopes
- ↑ Used in radiodating water
- ↑ Cosmogenic nuclide
Notes
- 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.
- Commercially available materials may have been subjected to an undisclosed or inadvertent isotopic fractionation. Substantial deviations from the given mass and composition can occur.
- 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.
References
- Isotope masses from:
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- Isotopic compositions and standard atomic masses from:
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- Half-life, spin, and isomer data selected from the following sources. See editing notes on this article's talk page.
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External links
Isotopes of sulfur | Isotopes of chlorine | Isotopes of argon |
Table of nuclides |
Isotopes of the chemical elements | |||||||||||||||||
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1 H |
2 He |
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3 Li |
4 Be |
5 B |
6 C |
7 N |
8 O |
9 F |
10 Ne |
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11 Na |
12 Mg |
13 Al |
14 Si |
15 P |
16 S |
17 Cl |
18 Ar |
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19 K |
20 Ca |
21 Sc |
22 Ti |
23 V |
24 Cr |
25 Mn |
26 Fe |
27 Co |
28 Ni |
29 Cu |
30 Zn |
31 Ga |
32 Ge |
33 As |
34 Se |
35 Br |
36 Kr |
37 Rb |
38 Sr |
39 Y |
40 Zr |
41 Nb |
42 Mo |
43 Tc |
44 Ru |
45 Rh |
46 Pd |
47 Ag |
48 Cd |
49 In |
50 Sn |
51 Sb |
52 Te |
53 I |
54 Xe |
55 Cs |
56 Ba |
72 Hf |
73 Ta |
74 W |
75 Re |
76 Os |
77 Ir |
78 Pt |
79 Au |
80 Hg |
81 Tl |
82 Pb |
83 Bi |
84 Po |
85 At |
86 Rn |
|
87 Fr |
88 Ra |
104 Rf |
105 Db |
106 Sg |
107 Bh |
108 Hs |
109 Mt |
110 Ds |
111 Rg |
112 Cn |
113 Uut |
114 Fl |
115 Uup |
116 Lv |
117 Uus |
118 Uuo |
|
57 La |
58 Ce |
59 Pr |
60 Nd |
61 Pm |
62 Sm |
63 Eu |
64 Gd |
65 Tb |
66 Dy |
67 Ho |
68 Er |
69 Tm |
70 Yb |
71 Lu |
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89 Ac |
90 Th |
91 Pa |
92 U |
93 Np |
94 Pu |
95 Am |
96 Cm |
97 Bk |
98 Cf |
99 Es |
100 Fm |
101 Md |
102 No |
103 Lr |
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