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镁取代羟基磷灰石在骨修复过程中的生物学行为。

Biological behavior of magnesium-substituted hydroxyapatite during bone repair.

机构信息

Laboratório de Ciências e Tecnologias da Saúde - LaCTS, Centro de Ciências da Saúde - CCS, Universidade Federal do Recôncavo da Bahia - UFRB, Av. Carlos Amaral, 1015, Cajueiro, CEP 44574-490, Santo Antônio de Jesus, BA, Brasil.

Laboratório de Bioengenharia Tecidual e Biomateriais - LBTB, Instituto de Ciências da Saúde - ICS, Universidade Federal da Bahia - UFBA, Av. Reitor Miguel Calmon, s/n, Vale do Canela, CEP 40110-100, Salvador, BA, Brasil.

出版信息

Braz J Biol. 2021 Jan-Feb;81(1):53-61. doi: 10.1590/1519-6984.217769.

Abstract

The aim of this study was to analyze the biological behavior and osteogenic potential of magnesium (Mg) substituted hydroxyapatite (HA) microspheres, implanted in a critical bone defect, considering that this ion is of great clinical interest, since it is closely associated with homeostasis and bone mineralization. For the purpose of this study, 30 rats were used to compose three experimental groups: GI - bone defect filled with HA microspheres; GII - bone defect filled with HA microspheres replaced with Mg; GIII - empty bone defect; evaluated at biological points of 15 and 45 days. The histological results, at 15 days, showed, in all the groups, a discrete chronic inflammatory infiltrate; biomaterials intact and surrounded by connective tissue; and bone neoformation restricted to the borders. At 45 days, in the GI and GII groups, an inflammatory response of discrete granulomatous chronic type was observed, and in the GIII there was a scarce presence of mononuclear inflammatory cells; in GI and GII, the microspheres were seen to be either intact or fragmented, surrounded by fibrous connective tissue rich in blood vessels; and discrete bone neoformation near the edges and surrounding some microspheres. In GIII, the mineralization was limited to the borders and the remaining area was filled by fibrous connective tissue. It was concluded that the biomaterials were biocompatible and osteoconductive, and the percentage of Mg used as replacement ion in the HA did not favor a greater bone neoformation in relation to the HA without the metal.

摘要

本研究旨在分析镁(Mg)替代羟基磷灰石(HA)微球在植入临界骨缺损后的生物学行为和成骨潜力,因为该离子与内稳定和骨矿化密切相关,具有重要的临床意义。为此,本研究使用 30 只大鼠组成三个实验组:GI-用 HA 微球填充骨缺损;GII-用 Mg 替代的 HA 微球填充骨缺损;GIII-空骨缺损;分别在 15 天和 45 天进行生物学评估。组织学结果显示,在所有组中,15 天时均存在离散的慢性炎症浸润;生物材料完整,周围有结缔组织;新骨形成仅限于边缘。45 天时,在 GI 和 GII 组中观察到离散的慢性肉芽肿性炎症反应,而在 GIII 组中单核炎症细胞的存在较少;在 GI 和 GII 组中,微球完整或碎裂,被富含血管的纤维结缔组织包围;边缘和周围一些微球处有离散的新骨形成。在 GIII 组中,矿化仅限于边缘,其余区域被纤维结缔组织填充。结论是,生物材料具有生物相容性和骨诱导性,HA 中用作替代离子的 Mg 百分比与不含金属的 HA 相比,并没有促进更大的新骨形成。

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