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舌形贝贝壳磷灰石的热分解

Thermal decomposition of Lingula shell apatite.

作者信息

Iijima M, Kamemizu H, Wakamatsu N, Goto T, Moriwaki Y

机构信息

Asahi University School of Denistry, Dental Materials and Technology, Gifu, Japan.

出版信息

Calcif Tissue Int. 1991 Aug;49(2):128-33. doi: 10.1007/BF02565135.

Abstract

Lingula shell is composed of apatite with a preferred orientation. The shell apatites of Lingula unguis(Lu) and Lingula shantoungensis(Ls) were characterized and compared with apatite of human tooth enamel. Insight into the Lingula apatite was studied by following the change of lattice parameter, transformation to beta-tricalcium phosphate (beta-TCP), and the loss and change of CO3, OH, and H2O after heating up to 1,000 degrees C in air and N2 for 24 hours. The OH stretching band was not observed in unheated apatites and in apatites heated in dried N2. Lu and Ls apatite produced 26 and 17 wt% of beta-TCP at 700 degrees C, respectively. Fifty to 60% of H2O was lost at 200 degrees C, being accompanied by a drastic contraction of the a- and c-axis and a drastic decrease in the crystallinity. These results indicate that (1) Lu and Ls shell apatite is CO3 containing F + Cl-apatite, and (2) the structural H2O of the Lingula apatite is loosely bounded such that they are lost at lower temperature than tooth enamel.

摘要

海豆芽外壳由具有择优取向的磷灰石组成。对长身海豆芽(Lu)和山东海豆芽(Ls)的外壳磷灰石进行了表征,并与人类牙釉质的磷灰石进行了比较。通过跟踪晶格参数的变化、向β-磷酸三钙(β-TCP)的转变以及在空气中和氮气中加热至1000℃24小时后CO3、OH和H2O的损失及变化,对海豆芽磷灰石进行了深入研究。在未加热的磷灰石和在干燥氮气中加热的磷灰石中未观察到OH伸缩带。Lu和Ls磷灰石在700℃时分别产生了26%和17%的β-TCP。在200℃时损失了50%至60%的H2O,同时伴随着a轴和c轴的急剧收缩以及结晶度的急剧下降。这些结果表明:(1)Lu和Ls外壳磷灰石是含F + Cl-的CO3磷灰石,(2)海豆芽磷灰石的结构H2O结合松散,以至于它们在比牙釉质更低的温度下就会损失。

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