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CONCEPTS, DEFINITIONS AND METHODS                    23

               2.2  THE FLUID MECHANICS OF FLUID-STRUCTURE
                     INTERACTIONS

               2.2.1  General character and equations of fluid flow
               Trying to give a selective encapsulation of  the  ‘fluids’ side of fluid-structure  interactions
               is more challenging than  the equivalent effort on  the  ‘structures’ side, as attempted in
               Section 2.1.  Solution of  the  equations of  motion  of  the  fluid  is  much  more  difficult.
               The equations are  in  most  cases  inherently nonlinear, for one  thing; moreover, unlike
               the situation in solid mechanics, linearization is not physically justifiable in many cases,
               and solution of even the linearized equations is not trivial. Thus, complete analytical and,
               despite the vast advances in computational fluid dynamic (CFD) techniques and computing
               power,  complefe numerical  solutions are  confined  to  only  some  classes  of  problems.
               Consequently, there exists a  large set of  approximations and  specialized techniques for
               dealing with different types of  problems, which is at the root of the difficulty remarked
               at the outset. The interested reader is referred to the classical texts in fluid dynamics [e.g.
               Lamb (1957), Milne-Thomson (1949, 1958), Prandtl (1952), Landau  & Lifshitz (1959),
               Schlichting (1960)] and more modem texts [e.g. Batchelor (1967), White (1 974), Hinze
               (1975), Townsend (1976), Telionis (1981)l; a wonderful refresher is Tritton’s (1988) book.
                 Excluding  non-Newtonian, stratified, rarefied,  multi-phase and  other  ‘unusual’ fluid
               flows,+  the basic fluid mechanics is governed by  the continuity (i.e. conservation of mass)
               and the Navier-Stokes  (Le. conservation of momentum) equations. For a homogeneous,
               isothermal,  incompressible fluid  flow  of  constant density and  viscosity, with  no  body
               forces, these are given by
                                             v.v=o,                                 (2.62)
                                     av                1
                                     - + (V. V)V = -- vp+ vv*v,                     (2.63)
                                      at              P
               where V is the flow velocity vector, p  is the static pressure, p the fluid density and w the
               kinematic viscosity. The fluid stress tensor (Batchelor 1967),

                                           a;; = -pa;, + 2pe;j,                     (2.64)
               used in the derivation of  (2.63), is also directly  useful for the purposes of  this book: its
               components on the surface of a body in contact with the fluid determine the forces on the
               body; p is the dynamic viscosity coefficient, and e;; are the components of  strain in the
               fluid. In cylindrical coordinates, for example, where i, j  = (r, 8, x) and V = {V, Vo, V,}T,
               the components of  e;j(= e;;) are
                                     av,          ar!          1 avo  v
                               e,  = -      err = -      em = --  + 2,
                                     ax ’         ar ’         r  a&’   r           (2.65)
                                                                     e,,  = 2 [a, -4.
                 erH=T[rs(T)+;z], av,                                     1  av  av,
                          a
                                                                                +
                      1
                                     1
                              v8
                 ‘Non-Newtonian fluids are nevertheless in the majority, in the process industries and biological systems, for
               instance. Polymer melts, lubricants, paints, and fluids involved in synthetic-fibre-, plastics- and food-processing
               are generally non-Newtonian, rheological fluids (Barnes et al. 1989).
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