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Synthesis and characterization of monetite and hydroxyapatite whiskers obtained by a hydrothermal method

机译:水热法制得的芒硝和羟基磷灰石晶须的合成与表征

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High temperature hydrothermal syntheses, using calcium nitrate tetrahydrate, sodium dihydrogen phosphate and urea as precursors, and characterization of hydroxyapatite (HAp) whiskers are reported herein. The morphology and chemical composition of the crystals from a monetite to a hydroxyapatite phase were controlled by varying the starting concentrations of the precursors and the solution pH through the amount of urea that is decomposed during heating. X-ray diffraction (XRD) analysis, infrared spectroscopy (IR), scanning electron microscopy (SEM), energy-dispersive X-ray spectroscopy (EDX), transmission electron microscopy (TEM) and high-resolution TEM (HRTEM) were used to investigate the products of the syntheses in order to find the optimum reaction conditions for obtaining the desired morphology and phase composition. Different morphologies ranging from single crystals of monetite through rods and plates of hydroxyapatite with different size distribution to whisker-like single hydroxyapatite crystal were achieved by simply varying the starting concentration of urea. Structural refinement of the hydroxyapatite whiskers confirmed a strong preferential orientation along the c-axis direction of the hexagonal crystal structure, which was significantly different from the usually observed random crystal orientation. TEM and SEM analysis of the apatite whiskers confirmed single crystal structure with the a c-axis orientation parallel to the long axis of the whiskers, with sizes up to 150 μm in length, 10 μm in width and with a thickness of about 300 om, that grew from the same centre of nucleation, forming flaky-like particles.
机译:本文报道了使用四水合硝酸钙,磷酸二氢钠和尿素作为前体的高温水热合成,以及羟基磷灰石(HAp)晶须的表征。通过改变前体的起始浓度和溶液的pH值(通过加热过程中分解的尿素量),可以控制从绿沸石到羟基磷灰石相的晶体的形态和化学组成。 X射线衍射(XRD)分析,红外光谱(IR),扫描电子显微镜(SEM),能量色散X射线光谱(EDX),透射电子显微镜(TEM)和高分辨率TEM(HRTEM)用于研究合成产物以找到获得所需形态和相组成的最佳反应条件。通过简单地改变尿素的起始浓度,获得了从形态不同的形态到从晶石的单晶到羟基磷灰石的棒和板的不同尺寸分布到晶须状的单一羟基磷灰石的晶体。羟基磷灰石晶须的结构细化证实了沿六方晶体结构的c轴方向的强烈优先取向,这与通常观察到的无规晶体取向显着不同。磷灰石晶须的TEM和SEM分析证实了c轴取向与晶须长轴平行的单晶结构,其长至150μm,宽至10μm,厚度约300 om,从相同的形核中心生长,形成片状颗粒。

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