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Dissolution Kinetics of Iron-, Manganese-, and Copper-Containing Synthetic Hydroxyapatites

B. Suttera,c,*, L. R. Hossnera and D. W. Mingb

a Dep. of Soil and Crop Sciences, Texas A&M Univ., College Station, TX 77843
b NASA Johnson Space Center, Houston, TX 77058
c SETI Institute, NASA Ames Research Center, Moffett Field, CA 94035



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Fig. 1. Calcium release rates versus time for pure-SHA, Fe12-SHA, Mn11-SHA, and Cu12-SHA treated with deionized water, citric acid, and DTPA.

 


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Fig. 2. Phosphorus release rates versus time for pure-SHA, Fe12-SHA, Mn11-SHA, and Cu12-SHA treated with deionized water, citric acid, and DTPA.

 


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Fig. 3. Calcium/P molar ratio release versus time of Mn11-synthetic hydroxyapatite (SHA) treated with deionized (DI) water, DTPA, and citric acid. Line represents solid Ca/P SHA molar ratio as calculated from Table 2. Error bars are standard deviation of the mean.

 


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Fig. 4. Infrared spectra of pure-, Fe12-, Mn11-, and Cu12-synthetic hydroxyapatite (SHA) materials exposed to deionized water and 0.1 mM citric acid. Arrows indicate the vibrational modes of calcium citrate that occurred between 1573 and 1579 cm–1.

 


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Fig. 5. Manganese, Cu, and Fe release rates from Fe12-, Mn11-, and Cu12-synthetic hydroxyapatite (SHA) in deionized (DI) water and citric acid.

 


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Fig. 6. Manganese, Cu, and Fe release rates from Fe12-, Mn11-, and Cu12-synthetic hydroxyapatite (SHA) in DTPA.

 





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