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La ions in precipitated hydroxyapatites

机译:沉淀的羟基磷灰石中的La离子

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摘要

Hydroxyapatites were synthesized by precipitation from an aqueous solution with La~(3+) (0-0.75%) and with carbonate (0-6.1%) at controlled pH 7.0. Uptake of La~(3+) was 90-95% complete. Relatively low Ca/P (1.54-1.63) ratios were attributed to nonstoichiometry. Carbonate in samples was identified by IR spectroscopy as B-type carbonate. Lattice parameters of the hexagonal apatite structure were not affected by the La~(3+) content. Noncarbonated samples heated to 800 deg C transform partially to #beta#-Ca_3(PO_4)_2. Thermogravimetric analysis showed release of 0.4 mol adsorbed and 1 mol crystalline water up to 400 deg C and decomposition of carbonate up to 900 deg C in the samples. Luminescence data obtained for Gd-containing hydroxyapatites prove that Gd~(3+) ions are not incorporated in the precipitated hydroxyapatite. These findings suggest that, in the La-containing samples, La~(3+) is surface adsorbed and not incorporated in hydroxyapatite.
机译:通过在受控pH 7.0下从具有La〜(3+)(0-0.75%)和碳酸盐(0-6.1%)的水溶液中沉淀来合成羟基磷灰石。 La〜(3+)的吸收完成90-95%。 Ca / P(1.54-1.63)比率相对较低归因于非化学计量。样品中的碳酸盐通过红外光谱法鉴定为B型碳酸盐。六方磷灰石结构的晶格参数不受La〜(3+)含量的影响。加热到800摄氏度的非碳酸化样品部分转化为#beta#-Ca_3(PO_4)_2。热重分析表明样品中释放出0.4 mol吸附的水和1 mol结晶水,直至400摄氏度,碳酸盐分解到900摄氏度。获得的含Gd羟基磷灰石的发光数据证明,Gd〜(3+)离子未掺入沉淀的羟基磷灰石中。这些发现表明,在含La的样品中,La〜(3+)是表面吸附的,没有掺入羟基磷灰石中。

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