
4. Renormalization techniques, in systems exhibiting
some kind of universality in the relations between
their behaviors at different scales, for example,
scale invariance (see the section ‘‘Renormalization:
an iterated multiscale approach’’).
We will first present the principles of multiple-
scale method, detail its technical implementation on
simple abstract examples and cite some typical
applications. Then we will articulate this technique
with more general multiscale methods in a brief
overview (see the section ‘‘A brief overview of
multiscale approaches’’). The range of multiscale
approaches and technical tools will then be illus-
trated and compared in the context of diffusion,
Brownian motion, and transport phenomena (see the
section ‘‘Summary: the exemplary case of
diffusion’’).
Multiple-Scale Method: Principles
Context: Singular Perturbations and Secular
Divergences
Multiple-scale methods have been developed to
handle situations in which the dynamics involves a
small parameter (e.g., the ratio of the masses of
different subsystems, the strength of an additional
interaction, the amplitude of an applied field)
directly controlling the separation between the
different characteristic timescales of the evolution
and, specifically, such that the behavior for = 0 is
qualitatively different from the behavior for small
( 1 but finite); in other words, when a weak
influence, of strength controlled by 1, does not
have only weak consequences. Typically, this occurs
when represents the strength of a weak coupling
between otherwise independent subsystems or when
a vanishing value = 0 changes a characteristic time,
the sign of a friction coefficient, the order of the
highest time derivative in case of ordinary differ-
ential equations (turning points), or the type of
partial differential equations in case of spatially
extended systems. Accordingly, a naive perturbative
approach with respect to , that is, an expansion
taking as a basic approximation the behavior for
= 0, cannot bridge the qualitative gap with
behaviors observed for >0. It thus fails to give a
full account of the system evolution at all times: one
speaks of singular perturbation.
A historical example arose in celestial mechanics,
in the celebrated nonintegrable three-body problem,
involving the Sun, a big planet and a smaller one, of
respective masses m
1
, m
2
< m
1
and m
3
m
2
. The
straightforward approach would be to consider the
presence of the small planet as a small perturbation
of the integrable two-body problem for the masses
m
1
and m
2
. But when one tries to determine the
solution as a series in powers of the mass ratio
= m
3
=m
2
, unbounded terms appear, the so-called
secular terms, increasing without bounds as fast as t,
hence of ill-defined order and impairing the very
consistency of the perturbation approach at long
times t > 1=. Accordingly, the perturbation expan-
sion is not uniformly convergent in time, preventing
from using it to investigate asymptotics and deter-
mine the fate of the three-body system: the influence
of the small planet on the motion of the bigger one,
although seemingly a weak perturbation, might
ultimately modify its trajectory around the Sun, at
least in some resonant cases.
The origin of secular terms lies in a phenomenon
of resonance, which is best explained on an
example: the Duffing oscillator
€
x þ x = x
3
with
1. When looking for a solution in the form
x(t) =
P
n
x
n
(t), each component x
n
(t) has to be
bounded in order to get a consistent perturbation
expansion, in which the hierarchy of terms of
different orders remains valid forever: x
nþ1
(t)
x
n
(t). These components should satisfy the following
sequence of equations:
€
x
0
þ x
0
¼ 0;
€
x
1
þ x
1
¼x
3
0
; ...
ðlinearized operator Lx
€
x þ xÞ½1
It gives x
0
(t) = ae
it
þ c.c., from which follows a
secular contribution (3i=2)ajaj
2
t e
it
in x
1
(t). In
general, solving perturbatively
_
z = f (z, ) for an
expansion z(, t) =
P
n
n
z
n
(t) yields a hierarchical
sequence of equations of the form
_
z
n
= Lz
n
þ ’
n
(z
0
, z
1
, ..., z
n1
) for n 1, where L = Df (z
0
, = 0)
comes from the linearization in z
0
of the unperturbed
evolution law. A secular divergence arises in z
n
as
soon as ’
n
contains an additive contribution which is
an eigenvector of L (part of a mathematical result
known as the Fredholm alternative). The appearance
of secular terms reflects a singular feature of the
dynamics: the fact that the limits as ! 0andt !1
do not commute. As a rule, such noninversion is
associated with generalized secular divergences: the
fast, short-term dynamics finally contributes to the
slow, long-term behavior. This feature is a clue
towards using multiple-scale method.
Technical Principles
The first step is to perform rescalings leading to
dimensionless variables and functions, which evidence
a small control parameter , related to scale separation
and providing a natural parameter for a perturbation
approach. The basic principle of multiple-scale
method is to introduce additional independent time
466 Multiscale Approaches