
General Properties of Flows     301 
 
The system obtained is far simpler for 
i
x
 than for x
i
. The preceding example is 
apparently rudimentary. However, it translates the fact that the model has attributed 
an important role to the parameter D, rather than to 
H
 which was chosen in order to 
establish the model. It is clear that we can have a better development with the 
parameter 
D
 than with 
H
. This problem of parameter choice is often encountered in 
order to best represent the range of solutions, for example, for solutions of boundary 
layer equations ([SCH 99], [YIH 77]). The term b(t) of [6.68] can depend on 
H
which must therefore express as a function of 
D
.  
The method can be applied to partial differential equations. We will later see 
some examples of this (section 6.4.2.6). Suitable variable changes also allows the 
modification or simplification of the differential problem (section 8.5.3.2). 
The practical limits of the preceding method are determined by the convergence 
of the entire series, but even more by the speed of convergence of the series 
obtained. Methods for accelerating the convergence can be used here ([ABR 65] 
p. 16, [BRE 91]). 
6.4.2.5.
 Regular perturbations and orders of magnitude 
In the domain of studies where the orders of magnitude of the terms are fixed, 
knowledge of a solution (exact or approximate) of an unperturbed problem allows 
the calculation of correctional terms for the solutions in the neighborhood of the 
base solution. 
The successive differential equations obtained are linear equations which all 
have the same linear operator, the right hand sides being known at each stage from 
the preceding solutions. Numerical solution is thus simplified. The computation of 
higher order terms of the solution by means of analytical developments, is generally 
difficult in practice, on account of its complexity. 
6.4.2.6.
 Applications in fluid mechanics  
With the exception of viscous stresses, taking account of other phenomena in 
fluid mechanics, when these are relatively weak, very often leads to regular 
perturbations: unsteady effects in established flow (in other words a flow which is 
independent of its initial conditions), effects of compressibility in steady flow, weak 
geometric changes, etc. 
Consider the established flow of an incompressible fluid with constant viscosity 
in a rectilinear pipe of arbitrary cross-section (Figure 6.13), and let us suppose that 
we have a Poiseuille flow, with a driving pressure gradient 
xp ww , parallel to the 
velocity in the direction Ox, which is a given function of time; the velocity satisfies 
the following equation (from [4.21]) and boundary conditions: