A perspective on the Wilshire creep equations

IF 0.4 Q4 MATERIALS SCIENCE, CHARACTERIZATION & TESTING
J. Brear
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引用次数: 0

Abstract

The Wilshire creep equations were introduced around fifteen years ago. Their aim was to address the non-physical extrapolation of power-law models, especially to high stresses, and the unrealistic values for activation energy and stress exponent that often arise from simple fits to data. In application they have met with some success, also with some difficulties which have largely been addressed empirically. No detailed mathematical analysis of the model seems to have been performed. This paper considers the fundamental characteristics of the Wilshire equations, as originally given, commencing with their internal consistency. It is found that the strain-time equation is incompatible with those for minimum creep-rate and rupture life. A consistent rate equation is derived, enabling the model to address the creep process rather than merely its results. Predictions made using the original and developed models are compared with actual materials behaviour; this reveals aspects of the approach which require reconsideration. The upper limit imposed by the ultimate tensile strength, and departures from a simple power law emerge as the key characteristics to be preserved and considered further.
威尔希尔蠕变方程透视
威尔希尔蠕变方程大约在15年前被引入。他们的目的是解决幂律模型的非物理外推问题,特别是对高应力的外推,以及激活能和应力指数的不切实际的值,这些值通常是由简单的数据拟合引起的。在应用中,他们取得了一些成功,也遇到了一些困难,这些困难在很大程度上已经通过经验得到了解决。似乎没有对该模型进行详细的数学分析。本文从Wilshire方程的内部一致性出发,考虑了其最初给出的基本特征。研究发现,应变-时间方程与最小蠕变率和断裂寿命方程不相容。导出了一致的速率方程,使模型能够处理蠕变过程,而不仅仅是其结果。将使用原始模型和开发模型进行的预测与实际材料行为进行比较;这揭示了需要重新考虑的方法的各个方面。极限抗拉强度施加的上限,以及对简单幂律的偏离,成为需要进一步保留和考虑的关键特征。
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来源期刊
Strength Fracture and Complexity
Strength Fracture and Complexity MATERIALS SCIENCE, CHARACTERIZATION & TESTING-
CiteScore
1.30
自引率
0.00%
发文量
15
期刊介绍: Strength, Fracture and Complexity: An International Journal is devoted to solve the strength and fracture unifiedly in non linear and systematised manner as complexity system. An attempt is welcome to challenge to get the clue to a new paradigm or to studies by fusing nano, meso microstructural, continuum and large scaling approach. The concept, theoretical and/or experimental, respectively are/is welcome. On the other hand the presentation of the knowledge-based data for the aims is welcome, being useful for the knowledge-based accumulation. Also, deformation and fracture in geophysics and geotechnology may be another one of interesting subjects, for instance, in relation to earthquake science and engineering.
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