Ban S, Maruno S
Department of Dental Material Science, School of Dentistry, Aichi-Gakuin University, Nagoya, Japan.
J Biomed Mater Res. 1998 Dec 5;42(3):387-95. doi: 10.1002/(sici)1097-4636(19981205)42:3<387::aid-jbm6>3.0.co;2-f.
Hydroxyapatite crystals were formed on a titanium electrode using the hydrothermal-electrochemical method in an autoclave with two electrodes. The electrolyte dissolving NaCl, K2HPO4, CaCl2.2H2O, trishydroxyaminomethane, and hydrochloric acid was maintained at 80 degrees - 200 degrees C. After loading of a constant current at 12.5 mA/cm2 for 1 h, the deposited amounts were measured through the weight gain of the electrode. The deposits were characterized by X-ray diffractometry, Fourier transform infrared spectroscopy, field emission-type scanning electron microscopy, field emission-type transmission electron microscopy, and energy dispersive X-ray spectroscopy. The deposited amount increased with electrolyte temperatures up to 150 degrees C and slightly decreased above that temperature. The deposits were identified as hydroxyapatite crystal rods grown along the c axis and perpendicular to the substrate. The crystallinity of the deposited hydroxyapatite increased continuously with the electrolyte temperature and closed to stoichiometric hydroxyapatite. At 150 degrees - 160 degrees C, the hydroxyapatite rod grew very homogeneously perpendicular to the substrate, and the edge of the needle had a flat hexagonal plane.
在带有两个电极的高压釜中,采用水热 - 电化学方法在钛电极上形成羟基磷灰石晶体。溶解有氯化钠、磷酸氢二钾、二水氯化钙、三羟甲基氨基甲烷和盐酸的电解液温度保持在80摄氏度至200摄氏度。在12.5毫安/平方厘米的恒定电流下加载1小时后,通过电极的重量增加来测量沉积量。通过X射线衍射、傅里叶变换红外光谱、场发射型扫描电子显微镜、场发射型透射电子显微镜和能量色散X射线光谱对沉积物进行表征。沉积量随着电解液温度升高至150摄氏度而增加,在该温度以上略有下降。沉积物被鉴定为沿c轴生长且垂直于基底的羟基磷灰石晶体棒。沉积的羟基磷灰石的结晶度随着电解液温度持续增加,并接近化学计量的羟基磷灰石。在150摄氏度至160摄氏度时,羟基磷灰石棒非常均匀地垂直于基底生长,并且针状晶体的边缘具有平坦的六边形平面。