The weakly nonlinear response and nonaffine interpretation of the Johnson–Segalman/Gordon–Schowalter model
- Univ. of Illinois at Urbana-Champaign, IL (United States)
- Univ. of Illinois at Urbana-Champaign, IL (United States); Nike, Inc., Beaverton, OR (United States)
We derive new analytical solutions for the non-affine Johnson-Segalman/Gordon-Schowalter (JS/GS) constitutive equation with a general relaxation kernel in medium-amplitude oscillatory shear (MAOS) deformation. The results show time-strain separable (TSS) nonlinearity, therefore providing new physically-meaningful interpretation to the heuristic TSS nonlinear parameter in MAOS. The upper-convected, lower-convected, and corotational Maxwell models are all subsets of the results presented here. The model assumes that the microscale elements causing stress in the material slip compared to the continuum deformation. We introduce a visualization of the non-affine deformation field that acts on stress-generating elements to reinforce the hysical interpretation of the JS/GS class of models. Lastly, a case study is presented where previously published results, from fitting TSS models to MAOS data, can be re-interpreted based on the concept of non-affine motion of the JS/GS framework.
- Research Organization:
- Univ. of Illinois at Urbana-Champaign, IL (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC), Basic Energy Sciences (BES). Materials Sciences & Engineering Division; USDOE
- Grant/Contract Number:
- SC0020858; FG02-07ER46471
- OSTI ID:
- 1778691
- Alternate ID(s):
- OSTI ID: 1678798; OSTI ID: 1876430
- Journal Information:
- Journal of Rheology, Vol. 64, Issue 6; ISSN 0148-6055
- Publisher:
- Society of RheologyCopyright Statement
- Country of Publication:
- United States
- Language:
- English
The medium amplitude response of nonlinear Maxwell–Oldroyd type models in simple shear
|
journal | September 2021 |
Similar Records
ROCK DEFORMATION 2010 GORDON RESEARCH CONFERENCE, AUGUST 8-13, 2010
Single-point parallel disk correction for asymptotically nonlinear oscillatory shear