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In structure mechanics analysis, finite element methods are now
well estab lished and well documented techniques; their advantage
lies in a higher flexibility, in particular for: (i) The
representation of arbitrary complicated boundaries; (ii) Systematic
rules for the developments of stable numerical schemes ap
proximating mathematically wellposed problems, with various types
of boundary conditions. On the other hand, compared to finite
difference methods, this flexibility is paid by: an increased
programming complexity; additional storage require ment. The
application of finite element methods to fluid mechanics has been
lagging behind and is relatively recent for several types of
reasons: (i) Historical reasons: the early methods were invented by
engineers for the analysis of torsion, flexion deformation of
bearns, plates, shells, etc ... (see the historics in Strang and
Fix (1972) or Zienckiewicz (1977. (ii) Technical reasons: fluid
flow problems present specific difficulties: strong gradients, l of
the velocity or temperature for instance, may occur which a finite
mesh is unable to properly represent; a remedy lies in the various
upwind finite element schemes which recently turned up, and which
are reviewed in chapter 2 (yet their effect is just as
controversial as in finite differences). Next, waves can propagate
(e.g. in ocean dynamics with shallowwaters equations) which will be
falsely distorted by a finite non regular mesh, as Kreiss (1979)
pointed out. We are concerned in this course with the approximation
of incompressible, viscous, Newtonian fluids, i.e. governed by N
avier Stokes equations."
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