Spatio-temporal evolution of hydroxyapatite crystal thickness at the bone-implant interface

被引:10
作者
Le Cann, Sophie [1 ]
Tornquist, Elin [2 ]
Barreto, Isabella Silva [2 ]
Fraulob, Manon [1 ]
Lomami, Hugues Albini [1 ]
Verezhak, Mariana [3 ]
Guizar-Sicairos, Manuel [3 ]
Isaksson, Hanna [2 ]
Haiat, Guillaume [1 ]
机构
[1] Univ Paris Est Creteil, Univ Gustave Eiffel, MSME, CNRS UMR 8208, F-94010 Creteil, France
[2] Lund Univ, Dept Biomed Engn, S-22100 Lund, Sweden
[3] Paul Scherrer Inst, Forsch Str 111, CH-5232 Villigen, Switzerland
基金
欧洲研究理事会; 瑞士国家科学基金会; 欧盟地平线“2020”;
关键词
Bone-implant interface; Small-angle X-ray scattering; Osseointegration; Hydroxyapatite; TITANIUM IMPLANTS; BIOMECHANICAL PROPERTIES; SCAFFOLD ARCHITECTURE; ALVEOLAR BONE; NANOSTRUCTURE; DEFECTS; SIZE; OSSEOINTEGRATION; PARTICLES; STABILITY;
D O I
10.1016/j.actbio.2020.09.021
中图分类号
R318 [生物医学工程];
学科分类号
0831 ;
摘要
A better understanding of bone nanostructure around the bone-implant interface is essential to improve longevity of clinical implants and decrease failure risks. This study investigates the spatio-temporal evolution of mineral crystal thickness and plate orientation in newly formed bone around the surface of a metallic implant. Standardized coin-shaped titanium implants designed with a bone chamber were inserted into rabbit tibiae for 7 and 13 weeks. Scanning measurements with micro-focused small-angle X-ray scattering (SAXS) were carried out on newly formed bone close to the implant and in control mature cortical bone. Mineral crystals were thinner close to the implant (1.8 +/- 0.45 nm at 7 weeks and 2.4 +/- 0.57 nm at 13 weeks) than in the control mature bone tissue (2.5 +/- 0.21 nm at 7 weeks and 2.8 +/- 0.35 nm at 13 weeks), with increasing thickness over healing time (+30 % in 6 weeks). These results are explained by younger bone close to the implant, which matures during osseointegration. Thinner mineral crystals parallel to the implant surface within the first 100 um indicate that the implant affects the ultrastructure of neighbouring bone, potentially due to heterogeneous interfacial stresses, and suggest a longer maturation process of bone tissue and difficulty in binding to the metal. The bone growth kinetics within the bone chamber was derived from the spatio-temporal evolution of bone tissue's nanostructure, coupled with microtomographic imaging. The findings indicate that understanding mineral crystal thickness or plate orientation can improve our knowledge of osseointegration. (C) 2020 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:391 / 399
页数:9
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