Ca; at. wt 40.078; at. no. 20; valence 2. Group IIA (2). Alkaline earth metal. Occurrence in the earth's crust 3.64% (fifth element in order of abundance). Sea water contains about 400 g/ton. Naturally occurring isotopes: 40 (96.941%), 44 (2.086%), 42 (0.647%), 48 (0.187%), 43 (0.135%), 46 (0.004%). Known radioactive isotopes: 35-39, 41, 45, 47-51. Found naturally only in the form of its compds, never uncombined, in minerals such as limestone, dolomite, marble, chalk, iceland spar, gypsum, anhydrite, fluorite, apatite. Principal commercial source is limestone, q.v. Major commercial production by high temperature vacuum reduction of calcium oxide in aluminothermal process; less commonly by electrolysis followed by redistillation. Essential constituent of bones, shells, teeth, coral, pearls. Essential nutrient for animal life. First isolated by Davy in 1808. Produced by electrolysis of calcium chloride: Rathenau, Suter, DE 155433 (1903); Z. Elektrochem. 10, 502 (1904); Goodwin, J. Am. Chem. Soc. 27, 1403 (1905); also by thermal reduction of lime with silicon, or with aluminum. Prepn of the pure metal for laboratory use: Whaley, Inorg. Synth. 6, 18 (1960). Purifn of commercial material: Marshall, Whaley, ibid. 24. Reviews: Schaufler in Ullmanns Encyklop"adie der technischen Chemie vol. 4 (Munich, 3rd ed., 1953) pp 830-836; Mantell in C. A. Hampel, Rare Metals Handbook (Reinhold, New York, 1954) p 17-29. Review of calcium and its compounds: Goodenough, Stenger, “Magnesium, Calcium, Strontium, Barium and Radium” in Comprehensive Inorganic Chemistry Vol. 1, J. C. Bailar Jr. et al., Eds. (Pergamon Press, Oxford, 1973) pp 591-664; Chemistry of the Elements, N. N. Greenwood, A. Earnshaw, Eds. (Pergamon Press, New York, 1984) pp 117-154; R. L. Petersen, M. B. Freilich in Kirk-Othmer Encyclopedia of Chemical Technology vol. 4 (Wiley-Interscience, New York, 4th ed., 1992) pp 777-796. Book: R. P. Rubin, Calcium and Cellular Secretion (Plenum, New York, 1982) 276 pp.