Skip to main content

Potassium-calcium decay system

  • Reference work entry
Geochemistry

Part of the book series: Encyclopedia of Earth Science ((EESS))

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).

Figure P33
figure 1_1-4020-4496-8_260

Decay scheme of potassium-40, showing relative energies of the parent and daughter nuclides (Firestone, 1996). Decay parameters from Steiger and Jäger (1977).

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 569.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD 499.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Bibliography

  • Baadsgaard, H. (1987) Rb–Sr and K–Ca isotope systematics in minerals from potassium horizons in the Prairie Evaporite Formation, Saskatchewan, Canada. Chem. Geol. (Isotope Geosci. Sect.), 66, 1–15.

    Google Scholar 

  • Firestone, R.B. (1996) Table of Isotopes, CD-ROM, 8th edn. New York: Wiley-Interscience.

    Google Scholar 

  • Kostoyanov, S.I. (1988) The K–Ca method and the excess-argon problem. Geochem. Int., 25, 38–43.

    Google Scholar 

  • Marshall, B.D. and DePaolo, D.J. (1982) Precise age determinations and petrogenetic studies using the K–Ca method. Geochim. Cosmochim. Acta, 46, 2537–45.

    Google Scholar 

  • Marshall, B.D. and DePaolo, D.J. (1989) Calcium isotopes in igneous rocks and the origin of granite. Geochim. Cosmochim. Acta, 53, 917–22.

    Google Scholar 

  • Marshall, B.D., Woodard, H.H. and DePaolo, D.J. (1986) K–Ca–Ar systematics of authigenic sanidine from Waukau, Wisconsin, and the diffusivity of argon. Geology, 14, 936–8.

    Google Scholar 

  • Nelson, D.R. and McCulloch, M.T. (1989) Petrogenetic applications of the 40K–40Ca radiogenic decay scheme—a reconnaissance study. Chem. Geol. (Isotope Geosci. Sect.), 79, 275–93.

    Google Scholar 

  • Shih, C.-Y., Nyquist, L.E., Bogard, D.D. and Wiesmann, H. (1994) K–Ca and Rb Sr dating of two lunar granites: relative chronometer resetting. Geochim. Cosmochim. Acta, 58, 3101–16.

    Google Scholar 

  • Steiger, R.H. and Jäger, E. (1977) Subcommission on geochronology: convention on the use of decay constants in geo-and cosmo-chronology. Earth Planet. Sci. Lett., 36, 359–62.

    Google Scholar 

Cross-references

Download references

Authors

Rights and permissions

Reprints and permissions

Copyright information

© 1998 Kluwer Academic Publishers

About this entry

Cite this entry

Marshall, B.D. (1998). Potassium-calcium decay system . In: Geochemistry. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4496-8_260

Download citation

  • DOI: https://doi.org/10.1007/1-4020-4496-8_260

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-412-75500-2

  • Online ISBN: 978-1-4020-4496-0

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics