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Amelogenin control over apatite crystal growth is affected by the pH and degree of ionic saturation
Author(s) -
Habelitz S,
DenBesten PK,
Marshall SJ,
Marshall GW,
Li W
Publication year - 2005
Publication title -
orthodontics and craniofacial research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.664
H-Index - 55
eISSN - 1601-6343
pISSN - 1601-6335
DOI - 10.1111/j.1601-6343.2005.00343.x
Subject(s) - amelogenin , apatite , fluorapatite , nucleation , calcium , saturation (graph theory) , chemistry , mineralization (soil science) , phosphate , crystal growth , enamel paint , mineralogy , crystallization , biomineralization , materials science , crystallography , chemical engineering , biochemistry , composite material , mathematics , organic chemistry , combinatorics , nitrogen , engineering
Structured Abstract Authors – Habelitz S, DenBesten PK, Marshall SJ, Marshall GW, Li W Objective – To study the mechanisms which promote the interactions of amelogenin proteins with the forming mineral to establish suitable conditions for the biomimetic synthesis of enamel in vitro . Design – Saturated calcium phosphate solutions were used in conjunction with recombinant amelogenin proteins to induce mineral formation on glass‐ceramics substrates containing oriented fluoroapatite crystals (FAP). The height of mineral layers formed on these substrates within 24 h was measured by atomic force microscopy (AFM). Experimental Variables – The effect of protein concentration, pH and degree of saturation (DS) on the growth of apatite mineral was evaluated. Mineralization experiments were performed at 0, 0.4 and 1.6 mg/ml amelogenin concentrations. Mineralization solutions were used at pH values of 6.5, 7.4, 8.0 and 8.8 and DS of calcium and phosphate between 9 and 13. Outcome Measure – Height and morphology of mineralized layer formed on glass‐ceramic substrates as determined from AFM measurements. Results – Homogeneous nucleation and crystal growth of thin layers on the FAP were observed, when calcium and phosphate ions were added. The height of these layers grown on (001) planes of FAP was strongly dependent on the protein concentration and pH. At concentrations of 0 and 0.4 mg/ml crystal grew 5–15 nm on the FAP, while they grew approximately to 200 nm at 1.6 mg/ml. The enhanced crystal growth was observed only at pH 6.5, 7.4 and 8.0, while layers only 20 nm thick were obtained at pH 8.8. An increase in DS resulted in uncontrolled growth of calcium phosphate mineral covering large areas of the substrate. Conclusions – Protein concentration, pH and the saturation of the mineralizing solution need to be considered carefully to provide suitable conditions for amelogenin‐guided growth of apatite crystals.