Calcium (Ca) has a total of 24 isotopes, from 34Ca to 57Ca. There are five observationally stable isotopes (40Ca, 42Ca through 44Ca and 46Ca), plus one isotope (48Ca) with such a long half-life that for all practical purposes it can be considered stable. The most abundant isotope 40Ca, as well as the rare 46Ca, are theoretically unstable on energetic grounds, but their decay has not been observed. Calcium also has a cosmogenic isotope, radioactive 41Ca, which has a half-life of 102,000 years. Unlike cosmogenic isotopes that are produced in the atmosphere, 41Ca is produced by neutron activation of 40Ca. Most of its production is in the upper metre or so of the soil column where the cosmogenic neutron flux is still sufficiently strong. 41Ca has received much attention in stellar studies because it decays to 41K, a critical indicator of solar-system anomalies.
All other isotopes have half-lives of 163 days or less, most under a minute. The least stable is 34Ca with a half-life shorter than 35 nanoseconds.
40Ca comprises about 97% of naturally occurring calcium. 40Ca is also one of the daughter products of 40K decay, along with 40Ar. While K-Ar dating has been used extensively in the geological sciences, the prevalence of 40Ca in nature has impeded its use in dating. Techniques using mass spectrometry and a double spike isotope dilution have been used for K-Ca age dating.
Standard atomic mass: 40.078(4) u
Contents |
nuclide symbol |
Z(p) | N(n) | isotopic mass (u) |
half-life[n 1] | decay mode(s)[1][n 2] |
daughter isotope(s)[n 3] |
nuclear spin |
representative isotopic composition (mole fraction) |
range of natural variation (mole fraction) |
---|---|---|---|---|---|---|---|---|---|
34Ca | 20 | 14 | 34.01412(32)# | <35 ns | p | 33K | 0+ | ||
35Ca | 20 | 15 | 35.00494(21)# | 25.7(2) ms | β+ (>99.9%) | 35K | 1/2+# | ||
β+, p (<.1%) | 34Ar | ||||||||
36Ca | 20 | 16 | 35.99309(4) | 102(2) ms | β+, p (56.8%) | 35Ar | 0+ | ||
β+ (43.2%) | 36K | ||||||||
37Ca | 20 | 17 | 36.985870(24) | 181.1(10) ms | β+, p (74.5%) | 36Ar | (3/2+) | ||
β+ (25.5%) | 36K | ||||||||
38Ca | 20 | 18 | 37.976318(5) | 440(8) ms | β+ | 38K | 0+ | ||
39Ca | 20 | 19 | 38.9707197(20) | 859.6(14) ms | β+ | 39K | 3/2+ | ||
40Ca[n 4] | 20 | 20 | 39.96259098(22) | Observationally Stable[n 5] | 0+ | 0.96941(156) | 0.96933-0.96947 | ||
41Ca | 20 | 21 | 40.96227806(26) | 1.02(7)×105 a | EC | 41K | 7/2- | Trace[n 6] | |
42Ca | 20 | 22 | 41.95861801(27) | Stable | 0+ | 0.00647(23) | 0.00646-0.00648 | ||
43Ca | 20 | 23 | 42.9587666(3) | Stable | 7/2- | 0.00135(10) | 0.00135-0.00135 | ||
44Ca | 20 | 24 | 43.9554818(4) | Stable | 0+ | 0.02086(110) | 0.02082-0.02092 | ||
45Ca | 20 | 25 | 44.9561866(4) | 162.67(25) d | β- | 45Sc | 7/2- | ||
46Ca | 20 | 26 | 45.9536926(24) | Observationally Stable[n 7] | 0+ | 4(3)×10−5 | 4×10−5-4×10−5 | ||
47Ca | 20 | 27 | 46.9545460(24) | 4.536(3) d | β- | 47Sc | 7/2- | ||
48Ca[n 8] | 20 | 28 | 47.952534(4) | 43(38)×1018 a | β-β-[n 9] | 48Ti | 0+ | 0.00187(21) | 0.00186-0.00188 |
49Ca | 20 | 29 | 48.955674(4) | 8.718(6) min | β- | 49Sc | 3/2- | ||
50Ca | 20 | 30 | 49.957519(10) | 13.9(6) s | β- | 50Sc | 0+ | ||
51Ca | 20 | 31 | 50.9615(1) | 10.0(8) s | β- (>99.9%) | 51Sc | (3/2-)# | ||
β-, n (<.1%) | 50Sc | ||||||||
52Ca | 20 | 32 | 51.96510(75) | 4.6(3) s | β- (98%) | 52Sc | 0+ | ||
β-, n (2%) | 51Sc | ||||||||
53Ca | 20 | 33 | 52.97005(54)# | 90(15) ms | β- (70%) | 53Sc | 3/2-# | ||
β-, n (30%) | 52Sc | ||||||||
54Ca | 20 | 34 | 53.97435(75)# | 50# ms [>300 ns] | β-, n | 53Sc | 0+ | ||
β- | 54Sc | ||||||||
55Ca | 20 | 35 | 54.98055(75)# | 30# ms [>300 ns] | β- | 55Sc | 5/2-# | ||
56Ca | 20 | 36 | 55.98557(97)# | 10# ms [>300 ns] | β- | 56Sc | 0+ | ||
57Ca | 20 | 37 | 56.99236(107)# | 5# ms | β- | 57Sc | 5/2-# | ||
β-, n | 56Sc |
Isotopes of potassium | Isotopes of calcium | Isotopes of scandium |
Index to isotope pages · Table of nuclides |