Abstract
Until the atomic era Sr2+ was of limited biological interest, being used primarily to remove traces of gas from vacuum tubes and to impart red color for tracer bullets, signal rockets, flares, and fireworks (1). To a limited degree Sr2+ compounds are also used in ceramics, drugs, greases, and special iron compositions. In 1968 a mere 12,500 tons of Sr2+ were produced in the free world (2). The advent of radioactive Sr2+, a fission product of nuclear reaction, presented a radiological hazard to the biosphere because of its long half-life (28 years), its affinity for deposition in bone, and its similarity to Ca2+. The voluminous literature concerning radiological effects of90 Sr, its distribution in the biosphere and transport through the food chain, and the dynamics of Sr2+ metabolism in man, lower animals, and plants significantly contributed to our knowledge of the naturally occurring stable element, although their effects have nothing in common except affinity to bone.
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Rosenthal, H.L. (1981). Content of Stable Strontium in Man and Animal Biota. In: Skoryna, S.C. (eds) Handbook of Stable Strontium. Springer, Boston, MA. https://doi.org/10.1007/978-1-4684-3698-3_30
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DOI: https://doi.org/10.1007/978-1-4684-3698-3_30
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