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  • Calvaria  (1)
  • Ion influxes  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 28 (1979), S. 57-63 
    ISSN: 1432-0827
    Keywords: Bone membrane ; Zeta potential ; Bone potassium ; Calvaria ; Bone extracellular fluid
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary Four-day-old chick calvaria were used to determine the passive concentrations of magnesium, sodium, and potassium in metabolically poisoned bone. When incubated in buffers containing the blood levels of sodium and magnesium, these calvaria contained sodium and magnesium at the identical concentrations found in freshly dissected calvaria. Calvarial sodium and magnesium levels could be varied by altering the buffer concentrations of these cations. The potassium content of metabolically poisoned calvaria incubated in buffers containing 4 mM potassium was less than 20% of the content of freshly dissected calvaria. When the buffer concentrations of sodium and potassium were systematically varied, ouabain-poisoned calvaria concentrated these cations in the bone extracellular fluid by a factor of approximately two above buffer cation levels. Presumably, the hydroxyapatite crystal zeta potential is responsible for this concentrative phenomenon. These results are discussed in terms of the control of the ionic content of the bone extracellular fluid by the postulated “bone membrane.”
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 32 (1980), S. 229-236 
    ISSN: 1432-0827
    Keywords: Bone ; Ion influxes ; Calcium ; Phosphate ; Exchange
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Notes: Summary Quantitative measurements were made of the ion fluxes of calcium and phosphate into and from calvaria (mouse or rat) when clamped in specially designed micro-Ussing chambers. The effects of varying concentrations of calcium were examined on the influx and efflux of calcium and of its counterion, phosphate. A comparable series of experiments was performed with varying phosphate concentrations. Both ions, as their concentrations increased, depressed their own influx, increased their own efflux, and significantly increased the equilibrium concentration, E/K, supported by the calvaria. Similarly, both ions, as their concentrations increased, affected the influx or efflux of their counterion only slightly but did depress the counterion's equilibrium level, E/K, significantly. In spite of these changes it was shown that calvaria effectively buffered the medium at physiological concentrations of calcium and phosphate. The buffering capacity, however, was small, and the balance, E/K, was modified by small uptake or loss of either ion. The small size of the interacting mineral pool was confirmed by direct measurement of the rapidly exchanging fractions of both calcium or phosphate. They were only ∼1% of the total ions present. The significance of these findings is discussed.
    Type of Medium: Electronic Resource
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