3.8 The Schr¨odinger and the Korteweg–de Vries Equations 81
As a simple model of turbulence, c is replaced by the fluid velocity field
u (x , t) to obtain the well-known Burgers equation
u
t
+ uu
x
= νu
xx
, (3.7.9)
where ν is the kinematic viscosity.
Thus the Burgers equation is a balance b etween time evolution, non-
linearity, and diffusion. This is the simplest nonlinear model equation f or
diffusive waves in fluid dynamics. Burgers (1948) first developed this equa-
tion primarily to shed light on the study of turbulence described by the
interaction of the two opposite effects of convection and d iffusion. However,
turbulence is more complex in the sense that it is both three dimensional
and statistically random in nature. Equat ion (3.7.9) arises in many phys-
ical problems including one-dimensional turbulence (where this equ ation
had its origin), sound waves in a viscous medium, shock waves in a viscous
medium, waves in fluid-filled viscous elastic tubes, and magnetohydrody-
namic waves in a medium with finite electrical conductivity. We note that
(3.7.9) is parabolic provided the coefficient of u
x
is constant, whereas the
resulting (3.7.9) with ν = 0 is hyperbolic. More importantly, the proper-
ties of the solution of the parabolic equation are significantly different from
those of the hyperbolic equation.
3.8 The Schr¨odinger and t he Korteweg–de Vries
Equations
We consider the following Fourier integral representation of a quasi-mono-
chromatic plane wave solution
u (x , t)=
∞
−∞
F (k)exp[i {kx − ω (k) t}] dk, (3.8.1)
where the spectrum function F (k) is determined from the given ini-
tial or boundary conditions and has the property F (−k)=F
∗
(k), and
ω = ω (k) is the dispersion relation. We assume that the initial wave is
slowly modulated as it propagates in a dispersive medium. For such a quasi-
monochromatic wave, most of the energy is confined in a neighborhood of
a specified wave number k = k
0
, so that spectrum function F (k) has a
sharp peak around the point k = k
0
with a narrow wave number width
k − k
0
= δk = O (ε), and the dispersion relation ω (k) can be expanded
about k
0
in the form
ω = ω
0
+ ω
′
0
(δk)+
1
2!
ω
′′
0
(δk)
2
+
1
3!
ω
′′′
0
(δk)
3
+ ··· , (3.8.2)
where ω
0
= ω (k
0
), ω
′
0
= ω
′
(k
0
), ω
′′
0
= ω
′′
(k
0
), and ω
′′′
0
= ω
′′′
(k
0
).