Potassium-calcium decay system
January 14, 1999
Potassium has three isotopes (see Potassium); potassium-40 ( 40K) is radioactive and decays to both calcium-40 ( 40Ca) and argon-40 ( 40Ar). The combined half-life of 40K is 1.25 billion years. The branched decay scheme of 40K is shown in Figure P33. It decays by β- decay to 40Ca and to 40Ar by both electron capture and positron decay (see Potassium-argon decay system). Although 89.52% of the decays produce 40Ca, the system is of somewhat limited use due to the large natural abundance of 40Ca (96.9% of calcium, see Calcium).
Citation Information
Publication Year | 1999 |
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Title | Potassium-calcium decay system |
DOI | 10.1007/1-4020-4496-8_260 |
Authors | Brian D. Marshall |
Publication Type | Book Chapter |
Publication Subtype | Book Chapter |
Index ID | 70207829 |
Record Source | USGS Publications Warehouse |
USGS Organization | Geology, Geophysics, and Geochemistry Science Center |