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负责水合和脱水牙本质断裂功差异的断裂增韧机制。

Fracture-toughening mechanisms responsible for differences in work to fracture of hydrated and dehydrated dentine.

作者信息

Kahler Bill, Swain Michael V, Moule Alex

机构信息

Biomaterials Science Research Unit, Faculty of Dentistry, and Aerospace, Mechanical and Mechatronic Engineering, University of Sydney, NSW 2006, Australia.

出版信息

J Biomech. 2003 Feb;36(2):229-37. doi: 10.1016/s0021-9290(02)00327-5.

Abstract

This study investigates the nature of deformation and differences in the mechanisms of fracture and properties of dentine where there has been a loss of moisture, as may occur with removal of the pulp in the endodontic treatment of teeth. Controlled fracture toughness testing was conducted on bovine teeth to determine the influence of hydration on the work of fracture of dentine. Significant differences (p<0.01) were observed between the fracture toughness of hydrated (554+/-27.7J/m2) and dehydrated (113+/-17.8J/m2) dentine. Observations of the crack tip region during crack extension revealed extensive ligament formation occurred behind the crack tip. These ligaments provide considerable stability to the crack by significantly increasing the work of fracture, thereby acting as a fracture-toughening mechanism. Micro-cracking, reported as a fracture-toughening mechanism in bone, is also clearly seen. A zone of in-elastic deformation may occur as hydrated specimens revealed upon crack extension, a region about the tip that appeared to suck water into the structure and to exude water behind the crack tip. In dehydrated dentine, no in-elastic zone was observed. Micro-cracking is present though the cracks are smaller, straighter and with less opening than hydrated dentine. Only limited ligament formation just behind the crack tip was observed. These differences resulted in a significantly lower work of fracture with unstable brittle fracture characteristics. Based on these results, several fracture-toughening mechanisms were identified in dentine, with micro-cracking not considered the most important. These findings may be relevant for bone, a similar mineralised hydrated tissue.

摘要

本研究调查了牙本质在水分流失时的变形性质、断裂机制及性能差异,这种水分流失可能发生在牙齿牙髓治疗中牙髓被去除的情况下。对牛牙进行了控制断裂韧性测试,以确定水合作用对牙本质断裂功的影响。观察到水合牙本质(554±27.7J/m²)和脱水牙本质(113±17.8J/m²)的断裂韧性存在显著差异(p<0.01)。在裂纹扩展过程中对裂纹尖端区域的观察表明,在裂纹尖端后方形成了大量的韧带。这些韧带通过显著增加断裂功为裂纹提供了相当大的稳定性,从而起到断裂增韧机制的作用。在骨中作为断裂增韧机制报道的微裂纹也清晰可见。当水合标本在裂纹扩展时显示,可能会出现一个非弹性变形区,裂纹尖端周围的一个区域似乎会将水吸入结构中,并在裂纹尖端后方渗出水分。在脱水牙本质中,未观察到非弹性区。虽然存在微裂纹,但与水合牙本质相比,裂纹更小、更直且开口更小。仅在裂纹尖端后方观察到有限的韧带形成。这些差异导致断裂功显著降低,具有不稳定的脆性断裂特征。基于这些结果,在牙本质中确定了几种断裂增韧机制,其中微裂纹并非最重要的机制。这些发现可能与骨有关,骨是一种类似的矿化水合组织。

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