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体内牙本质龋。扫描电子显微镜与显微放射照相术联合研究

Dentine caries in vivo. Combined scanning electron microscopic and microradiographic investigation.

作者信息

Arends J, Ruben J, Jongebloed W L

机构信息

Dental School, Groningen, The Netherlands.

出版信息

Caries Res. 1989;23(1):36-41. doi: 10.1159/000261152.

Abstract

Dentine subjected to an in vivo demineralization challenge by plaque looses substantial amounts of mineral and is expected to change its ultrastructure. Results are presented of a combined microradiography and scanning electron microscopy (SEM) study on in vivo demineralized human dentine. The tissue was first demineralized in vivo under plaque for 3 weeks and subsequently analyzed by microradiography and SEM. In 6 participants dentine was positioned in a full prosthesis just under M2 in such a way that the outer surface of the tissue was 1.5 mm lower than the surface of the prosthesis; plaque accumulation takes place in the recessed area. A special technique allows SEM observations (at a given distance from the outer surface) on broken thin sections of demineralized dentine with a mineral content determined by microradiography. The results show that the ultrastructure of the dentine changes during severe demineralization. The main ultrastructural features are, however, still largely intact, even if half of the mineral originally present has been lost. In dentine with a mineral content of about 25 vol%, the dentinal tubules are enlarged by about 30%. In vivo demineralized dentine looses mineral in substantial amounts both from intertubular and from peritubular regions.

摘要

受到菌斑体内脱矿挑战的牙本质会损失大量矿物质,并预期其超微结构会发生改变。本文呈现了一项关于体内脱矿人牙本质的显微放射照相术和扫描电子显微镜(SEM)联合研究的结果。该组织首先在菌斑下进行3周的体内脱矿,随后通过显微放射照相术和SEM进行分析。在6名参与者中,将牙本质置于M2下方的全口义齿中,使组织的外表面比义齿表面低1.5毫米;菌斑在凹陷区域积聚。一种特殊技术允许在脱矿牙本质的薄切片断裂处进行SEM观察(在距外表面给定距离处),其矿物质含量由显微放射照相术确定。结果表明,在严重脱矿过程中牙本质的超微结构发生变化。然而,即使最初存在的一半矿物质已经流失,主要的超微结构特征在很大程度上仍然完好无损。在矿物质含量约为25%(体积)的牙本质中,牙本质小管大约扩大了30%。体内脱矿的牙本质在管间区域和管周区域都会大量流失矿物质。

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