Analysis of sound and vibration in linear viscoelastic materials is based on a relaxation function that is the time-dependent stress resulting from a unit step in strain. It is well established that relaxation functions decrease monotonically in time. The most common constitutive relaxation functions, such as the Kelvin–Voigt or General Maxwell Model, produce curves that must be monotonic. However, recently, the authors have produced a methodology that allows the use of discrete data for the time-dependent relaxation function. One result of this approach is the possibility of non-monotonic relaxation function input. This non-monotonic data may be the result of test and measurement errors. Alternatively, this non-monotonicity may be an actual anomalous physical result, such as in rock salt (He et al. 2019). The authors use validated viscoelastic finite element models in the time domain to determine the instability caused by such non-monotonic datasets. The study uses randomized non-monotonic datasets that maintain the fundamental material trend to find unstable or inaccurate results. A mathematical review highlights the conditions causing numerical instability in modern stepwise time integration solvers. The results provide clarity for viscoelastic analysts considering low-precision viscoelastic measurements or unusual physical properties. [Work supported by ONR under Grant N00014-22-1-2785.]
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