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大鼠牙本质磷蛋白在体外诱导和抑制羟基磷灰石形成的作用

Induction and inhibition of hydroxyapatite formation by rat dentine phosphoprotein in vitro.

作者信息

Lussi A, Crenshaw M A, Linde A

机构信息

Dental Research Center, University of North Carolina, Chapel Hill 27599.

出版信息

Arch Oral Biol. 1988;33(9):685-91. doi: 10.1016/0003-9969(88)90124-0.

Abstract

Highly phosphorylated rat incisor phosphoprotein (PP-H) was purified and covalently attached to agarose beads. The beads were incubated for 24 h in solutions having an ionic strength of 0.165, a molar Ca/P ratio of 1.67, and a pH of 7.4. The calcium-phosphate concentration products [( Ca][P]) in the stable incubation solutions ranged from 1.0 to 1.8 mM2, from which no spontaneous precipitation occurred. In a timed series mineral formation was monitored by SEM and X-ray diffraction. The inhibitory capacity of PP-H, free solution, was also studied. The first mineral appeared after 10 min at a [Ca][P] product as low as 1.2 mM2; X-ray diffraction showed that the mineral was (hydroxy)apatite. Thus small amounts of PP-H attached to a surface are capable of inducing mineral formation in vitro at comparatively low supersaturation, whereas PP-H is a mineral inhibitor when free in solution.

摘要

高度磷酸化的大鼠门齿磷蛋白(PP-H)被纯化并共价连接到琼脂糖珠上。将这些珠子在离子强度为0.165、摩尔钙/磷比为1.67且pH为7.4的溶液中孵育24小时。稳定孵育溶液中的磷酸钙浓度乘积[(Ca][P])范围为1.0至1.8 mM²,在此范围内未发生自发沉淀。通过扫描电子显微镜(SEM)和X射线衍射监测了在一定时间序列内的矿物质形成情况。还研究了游离溶液中PP-H的抑制能力。在[Ca][P]乘积低至1.2 mM²时,10分钟后出现了第一种矿物质;X射线衍射表明该矿物质是(羟基)磷灰石。因此,附着在表面的少量PP-H能够在相对较低的过饱和度下体外诱导矿物质形成,而游离于溶液中的PP-H是一种矿物质抑制剂。

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