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CRYSTALLISATION OF APATITE STOICHIOMETRIC IONOMER GLASSES FOR MEDICAL APPLICATIONS AND OPTOELECTRONICS

机译:磷灰石化学计量离子聚合物玻璃的结晶

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摘要

Substitution of fluorine for oxygen strongly influences the crystallization of 4.5SiO_2-3Al_2O_3-1.5P_2O_5-(5-z)CaO-zCaF_2 glasses. A glass with z = 0 crystallized to whitlockite and anorthite. Introduction of F caused the formation of FAP instead of whitlockite, and inhibited anorthite formation. For z = 1, only FAP was formed. For z > 2, mullite also crystallized. The inhibition of anorthite favors mullite formation, probably due to the high Al:Si ratio of the glasses and, following FAP crystallization, the lack of charge balancing cations for maintaining the Al(Ⅳ) state. Al is mainly Al(Ⅳ) for z = 0, while F causes the formation of Al(Ⅴ) and Al(Ⅵ). These seem to disappear on heat treatment at Tpl and (Tp1+Tp2)/2, but new Al(Ⅴ) and Al(Ⅵ) species often appear on heating to Tp2. The F is present initially as F-Ca(n) and Al-F-Ca(n) species. The former appear to be used preferentially in forming FAP. The P in the glass is present initially as Al-O-PO_4~(3-) type species, but forms FAP and a small amount of AlPO_4. A small amount of P remains in the residual glass as PO_4 tetrahedra, coordinated primarily by Al.
机译:用氟代替氧强烈影响4.5SiO_2-3Al_2O_3-3-1.5P_2O_5-(5-z)CaO-zCaF_2玻璃的结晶。 z = 0的玻璃结晶为辉锰矿和钙长石。 F的引入引起FAP的形成而不是辉锰矿,并且抑制了钙长石的形成。对于z = 1,仅形成FAP。当z> 2时,莫来石也结晶。抑制钙长石有利于莫来石的形成,这可能是由于玻璃中Al:Si的比例高,以及在FAP结晶后,缺乏保持Al(Ⅳ)状态的电荷平衡阳离子所致。当z = 0时,Al主要是Al(Ⅳ),而F引起Al(Ⅴ)和Al(Ⅵ)的形成。这些似乎在Tpl和(Tp1 + Tp2)/ 2热处理时消失,但是在加热到Tp2时经常出现新的Al(Ⅴ)和Al(Ⅵ)物种。 F最初以F-Ca(n)和Al-F-Ca(n)形式存在。前者似乎优先用于形成FAP。玻璃中的P最初以Al-O-PO_4〜(3-)型物质存在,但会形成FAP和少量的AlPO_4。少量的P以PO_4四面体的形式保留在残留的玻璃中,主要由Al配位。

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