Convected derivatives for differential constitutive equations
To date, no differential constitutive equation has been proposed that agrees with each of four important experimental observations in relaxation after step shear strains: that the stress is often factorable into time and strain-dependent functions, that the strain-dependent function is shear thinnin...
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Published in | Journal of non-Newtonian fluid mechanics Vol. 24; no. 3; pp. 331 - 342 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
1987
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | To date, no differential constitutive equation has been proposed that agrees with each of four important experimental observations in relaxation after step shear strains: that the stress is often factorable into time and strain-dependent functions, that the strain-dependent function is shear thinning, that the ratio of first normal stress difference to shear stress equals the shear strain—that is, the Lodge-Meissner relationship holds, and that there is a negative second normal stress difference. The Johnson-Segalman model satisfies three of these, but fails to satisfy the Lodge-Meissner relationship, because in step strains the principal stress and strain axes do not rotate together. Using a mathematical technique for forcing co-rotation of stress and strain axes in an arbitrary deformation, we here present an explicit differential constitutive equation that satisfies all four of the above experimental observations. |
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ISSN: | 0377-0257 1873-2631 |
DOI: | 10.1016/0377-0257(87)80045-9 |