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§8.5  The Corotational Derivatives  and the Nonlinear Viscoelastic  Models  249

                               Note that there is  an important difference  between  the problems  in the last  two  ex-
                            amples.  In Example  8.4-1  the velocity  profile  is  prescribed,  and we  have  derived  an  ex-
                            pression  for  the shear stress  required to maintain the motion; the equation  of motion was
                            not used.  In Example  8.4-2 no assumption was  made about the velocity  distribution, and
                            we derived  the velocity  distribution by using  the equation  of motion.

        .5  THE COROTATIONAL DERIVATIVES AND THE
            NONLINEAR VISCOELASTIC MODELS
                            In the previous  section it was  shown  that the inclusion  of  time derivatives  (or time inte-
                            grals) in the stress  tensor expression  allows for  the description  of  elastic  effects.  The lin-
                            ear  viscoelastic  models  can  describe  the  complex  viscosity  and  the  transmission  of
                            small-amplitude  shearing  waves.  It  can  also  be  shown  that  the  linear  models  can de-
                            scribe  elastic  recoil, although the results  are restricted  to flows with  negligible displace-
                            ment gradients  (and hence of little practical interest).
                               In this section we introduce the hypothesis ' 1 2  that the relation between the stress ten-
                            sor  and  the kinematic tensors  at a fluid particle  should  be independent  of  the instanta-
                            neous  orientation  of  that  particle  in  space.  This  seems  like  a  reasonable  hypothesis;  if
                            you  measure  the stress-strain  relation  in a  rubber  band, it  should  not matter whether
                            you  are stretching  the rubber  band  in the north-south direction or the east-west  direc-
                            tion, or  even  rotating  as  you  take  data  (provided,  of  course, that you  do not rotate  so
                            rapidly that centrifugal  forces  interfere with the measurements).
                               One way  to implement the above  hypothesis  is  to introduce at each fluid particle a
                            corotating coordinate frame.  This orthogonal frame  rotates with  the local instantaneous
                            angular  velocity  as  it moves  along  with  the fluid particle through  space  (see  Fig.  8.5-1).
                            In  the  corotating  coordinate  system  we  can  now  write  down  some  kind  of  relation





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                               1
                                 G. Jaumann, Grundlagen der Bewegungslehre, Leipzig (1905); Sitzungsberichte Akad. Wiss. Wien, Ha,  120,
                            385-530 (1911); S. Zaremba, Bull. Int. Acad. Set,  Cracooie, 594-614,614-621 (1903). Gustaf Andreas Johannes
                            Jaumann (1863-1924) (pronounced "Yow-mahn") who taught at the German university in Briinn  (now
                            Brno), for whom the "Jaumann derivative" is named, was  an important contributor to the field  of
                            continuum mechanics at the beginning of the twentieth century; he was  the first to give the equation of
                            change for entropy, including the "entropy flux" and  the "rate of entropy production" (see §24.1).
                               2
                                 J. G. Oldroyd, Proc. Roy. Soc,  A245, 278-297 (1958). For  an extension of the corotational idea, see
                            L. E. Wedgewood, Rheol. Ada,  38, 91-99  (1999).
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