Abstract
Fluoride (F) in urine has long been known to reflect intestinal F absorption as well as F liberation from a fluoride-rich skeleton, but blood plasma F has been believed only to show a limited absorption tide. Nobody seems to have observed plasma F values elevated due to the process of gradual F depletion of an F-rich skeleton. Some of the variations of plasma inorganic F may have been obscured by analytical methods, which have comprised the fraction of organically bound plasma F also. While the ionizable F (F−) of a young person’s fasting plasma generally is as low as 0.01–0.02 ppm, or 0.5–1 µM/1, the organically bound F may be 5 to 10 times higher. The nature of organic F bonding in plasma is not yet understood, but it is evident that the ionized or easily ionizable plasma F is the physiologically active fraction.
These investigations were supported in part by Patentmedelsfonden för odontologisk profylaxforskning (Swedish Patent Revenue Research Fund).
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© 1975 Springer-Verlag Berlin · Heidelberg
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Ericsson, Y. (1975). Bone-Body Fluid Fluoride Balance. In: Kuhlencordt, F., Kruse, HP. (eds) Calcium Metabolism, Bone and Metabolic Bone Diseases. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-80875-3_19
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DOI: https://doi.org/10.1007/978-3-642-80875-3_19
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