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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).

Publication Year 1999
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
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