whitlockite and calcium-magnesium-phosphate

Extensive DM contamination was found on Dacron bags that were incubated for prolonged periods of time in the rumen of steers fed alfalfa hay. The ash content of the contaminant was high, and most of it was acid-soluble X-ray analysis indicated the presence of hydroxylapatite and synthetic calcium magnesium phosphate or whitlockite. The contaminant appeared as a smooth coating on the Dacron fiber, suggesting that contamination was a gradual process rather than the result of entrapment of dislodged crystals from plant material. Contamination seemed to occur exponentially within the range of observations (0 to 42 d). Contamination also occurred in steers fed orchardgrass, although to a lesser extent than in steers fed alfalfa hay. The DM contamination was less than .04 g per bag (average bag weight was 1.2 g) during the first 10 d of incubation. However, correction for contamination might be required for studies involving longterm incubation or mineral digestion.

Topics: Animal Feed; Animals; Biocompatible Materials; Calcium; Calcium Phosphates; Cattle; Crystallization; Durapatite; Electron Probe Microanalysis; Hydroxyapatites; Male; Medicago sativa; Microscopy, Electron, Scanning; Minerals; Phosphates; Phosphorus; Polyethylene Terephthalates; Potassium; Rumen; Silicon; X-Ray Diffraction

All biological calcium phosphates form in various neutral aqueous solutions containing [CaCl2] = 1 or 3 mM, [MgCl2] = 0-9 mM, [Na2HPO4] = 0.1-90 mM and NaCl (total 300 mosM) kept quiescently at 37 degrees C for 21 days. In all solutions containing 1 mM Ca and in solutions with [Ca] = 3 mM and [PO4] less than 10 mM, heterogeneous nucleation of octa-calcium phosphate (for Mg/Ca less than or equal to 1) or brushite (for Mg/Ca greater than 1) was observed; the former transforming to apatite with time. In contrast, homogeneous nucleation of an unstable amorphous calcium magnesium phosphate occurred in solutions with [Ca] = 3 mM and [PO4] greater than or equal to 10 mM, transforming to apatite, to brushite, and to whitlockite (and newberyite) depending on Mg/Ca and [PO4] values.

Topics: Apatites; Calcium Phosphates; Chemical Precipitation; Crystallization; Durapatite; Hydrogen-Ion Concentration; Hydroxyapatites; Magnesium; Magnesium Compounds; Phosphates; Solutions; X-Ray Diffraction

This study correlated ultrastructural observations on the presence of beta-tricalcium phosphate (beta-TCP) in arrested dentin caries with physico-chemical observations on the in vitro formation of Mg-substituted beta-TCP. The ultrastructural studies were made using high-resolution transmission electron microscopy (TEM) with the capability of microdiffraction and microanalysis on sites less than 10 nm in diameter. Mg-substituted beta-TCP was obtained, by a precipitation method, from solutions with Mg/Ca molar ratios of 5/95 and higher. Such correlations led to the postulation of a possible chronological sequence of physico-chemical events occurring at the crystal level during the progress and arrest of caries in human dentin. It is suggested that the initial mechanism for the observed occurrence of large crystals of Mg-substituted beta-TCP and of apatite in the tubule lumen is due to the dissolution of the dentin mineral (a CO3- and Mg-rich calcium OH-apatite) and reprecipitation of Mg-substituted beta-TCP, followed by that of CO3- and Mg-poor apatite.

Topics: Calcium Phosphates; Chemical Phenomena; Chemistry, Physical; Crystallography; Dental Caries; Dentin; Electron Probe Microanalysis; Humans; Microscopy, Electron; Phosphates; X-Ray Diffraction