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Monitoring of hydroxyapatite conversion by luminescence intensity of Eu~(3+) ions during mineralization of Eu~(3+)-doped β-Ca_2SiO_4

机译:Eu〜(3+)掺杂β-Ca_2SiO_4成矿过程中Eu〜(3+)离子的发光强度监测羟基磷灰石转化率

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摘要

β-Dicalcium silicate (β-Ca_2SiO_4) doped with Eu~(3+) was synthesized by sol-gel method. The luminescence intensity of the mineralization products formed during the hydroxyapatite (Ca_(10)(PO_4)_6(OH)_2, HA) conversion of Eu~(3+)-doped β-Ca_2SiO_4, in 0.25 M K_2HPO_4 solution, were detected using luminescence spectros-copy. The results indicated that the luminescence intensity of Eu~(3+) ion gradually depressed with prolonged mineralization time, and it could hardly be detected with the complete transformation from β-Ca_2SiO_4:Eu~(3+) to hydroxyapatite. The change of Eu~(3+) ionic concentrations in the mineralization products and the final solutions after conversion reaction, were further examined using energy-dispersive X-ray and inductively-coupled plasma mass spectrometry, respectively. This suggested that the process of mineralization can be monitored with the luminescence intensity of Eu~(3+) ions in the mineralization products. The current study will open up a new and simple in vivo avenue for in situ monitoring hydroxyapatite conversion with a fiber luminescence spectrometer.
机译:通过溶胶-凝胶法合成了掺有Eu〜(3+)的β-硅酸二钙(β-Ca_2SiO_4)。使用0.25 M K_2HPO_4溶液检测Eu〜(3+)掺杂的β-Ca_2SiO_4的羟基磷灰石(Ca_(10)(PO_4)_6(OH)_2,HA)转化过程中形成的矿化产物的发光强度。发光光谱。结果表明,随着矿化时间的延长,Eu〜(3+)离子的发光强度逐渐降低,从β-Ca_2SiO_4:Eu〜(3+)完全转变为羟基磷灰石几乎无法检测到。分别使用能量色散X射线和电感耦合等离子体质谱法进一步研究了矿化产物和转化反应后最终溶液中Eu〜(3+)离子浓度的变化。这表明可以用矿化产物中Eu〜(3+)离子的发光强度来监测矿化过程。当前的研究将为利用纤维发光光谱仪原位监测羟磷灰石转化率开辟一种新的简单的体内途径。

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