Calcium
:See also Calcium, New York, United States.
Isotopes
Calcium has six stable isotopes, two of which occur in nature: stable Ca-40 and radioactive Ca-41 with a half-life = 103,000 years. 97% of the element is in the form of Ca-40. Ca-40 is one of the daughter products of K-40 decay, along with Ar-40. While K-Ar dating has been used extensively in the geological sciences, the prevalence of Ca-40 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. Unlike cosmogenic isotopes that are produced in the atmosphere, Ca-41 is produced by neutron activation of Ca-40. Most of its production is in the upper metre or so of the soil column where the cosmogenic neutron flux is still sufficiently strong. Ca-41 has received much attention in stellar studies because Ca-41 decays to K-41, a critical indicator of solar-system anomalies.
Related Topics:
Isotope - Radioactive - Half-life - K-Ar dating - Geological - Mass spectrometry - K - Cosmogenic isotope - Atmosphere - Neutron
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See also: disorders of calcium metabolism
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~ Table of Content ~
| ► | Introduction |
| ► | Notable characteristics |
| ► | Applications |
| ► | History |
| ► | Compounds |
| ► | Isotopes |
| ► | External links |
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