Wave Mechanics: Right- and Left-Traveling Solutions
WM15 verified that every sufficiently smooth profile of the form
satisfies the one-dimensional wave equation
and that the same is true for every sufficiently smooth profile of the form
WM16 now asks the deeper structural question:
The answer is that the second-order wave operator can be separated into two first-order
propagation operators. Those two operators correspond to information moving at speeds +c and
−c. In characteristic coordinates, the wave equation then reduces to a particularly simple
mixed-derivative equation whose sufficiently smooth solutions have the form
This is the structural form underlying the classical d’Alembert solution of the one-dimensional
wave equation [1, 2, 4, 6].
WM16 derives this two-family structure. WM17 will take the next step: given an initial
displacement and initial velocity, determine the specific functions F and G.
1 One equation supports two directions
The homogeneous one-dimensional wave equation is
WM15 showed directly that
moves toward increasing x, while
moves toward decreasing x.
The two families are illustrated below.
Figure. The same shape-preserving idea produces two propagation families. A profile
depending on x − ct moves toward increasing x; a profile depending on x + ct moves toward
decreasing x.
The speed magnitude is the same in both cases. Only the direction changes.
2 The first-order equations retain direction information
For a right-moving wave
WM15 found
Therefore
For a left-moving wave
we have
so
These are first-order transport equations. Unlike the second-order wave equation, they remember
the propagation direction.
The distinction can be summarized as
This interpretation is standard in treatments of traveling-wave solutions and characteristics
[4, 6].
3 Factor the wave operator
Because c is constant and the partial derivatives commute for a sufficiently smooth function, we
may write
 u | = utt + cutx − cuxt − c2u
xx | (16)
|
| = utt − c2u
xx. | (17) |
Thus the wave equation can be factored as
This factorization is the PDE analogue of factoring an algebraic expression such as
It hints that two first-order propagation mechanisms are embedded inside the second-order wave
equation.
4 Characteristic coordinates
Introduce the coordinates
and
The coordinate ξ stays constant along a right-moving feature. The coordinate η stays constant
along a left-moving feature.
If
then
so
If
then
so
Figure. The two families of characteristic lines in the x-t plane. Solid lines carry constant
ξ = x − ct and move toward increasing x; dashed lines carry constant η = x + ct and move
toward decreasing x.
These lines are called characteristics. They organize how information propagates through the
solution.
5 Rewrite the wave equation in characteristic coordinates
Let
Since
we obtain
Differentiating again,
Similarly,
so
Differentiating again,
Therefore
| utt − c2u
xx | = c2U
ξξ − 2c2U
ξη + c2U
ηη | (35)
|
| − c2 | (36)
|
| = −4c2U
ξη. | (37) |
The wave equation therefore becomes
For c≠0,
This is much simpler than the original PDE.
6 Integrate the transformed equation
The equation
means
Therefore Uη cannot depend on ξ. It can depend only on η:
Integrating with respect to η gives
where the “constant of integration” with respect to η may still be an arbitrary function of
ξ.
Returning to x and t,
Thus, on a suitable domain and for sufficiently smooth functions, the general solution of the
homogeneous one-dimensional constant-speed wave equation is the sum of one right-moving profile
and one left-moving profile [4, 6].
7 What “general solution” means here
The statement
is stronger than the verification result in WM15.
WM15 showed:
WM16 shows, under the usual smoothness assumptions for a classical solution,
The arbitrary functions F and G have not yet been determined. That requires initial or boundary
data.
This distinction is essential:
8 The physical displacement is the sum of the two components
Suppose
and
Then the physical field is
The addition is point by point.
Figure. At any fixed time, the observed displacement is the point-by-point sum of a
right-moving component and a left-moving component. Linearity allows both components
to coexist without changing the governing equation.
Because the wave equation is linear, the two components propagate independently in the ideal
model even while their sum may display interference.
9 Standing waves fit naturally into the two-family picture
Take equal-amplitude sinusoidal components
| uR(x,t) | = A cos(kx − ωt), | (52)
|
| uL(x,t) | = A cos(kx + ωt). | (53) |
For the ideal wave equation,
Adding the two components gives
| u(x,t) | = A cos(kx − ωt) + A cos(kx + ωt) | (55)
|
| = 2A cos(kx) cos(ωt). | (56) |
Therefore the Standing Waves studied earlier are not a separate species of solution. They are a
particular superposition of equal right- and left-moving components.
This connects the standing-wave material of WM10 directly to the two-family structure of the
wave equation.
10 A compact structural map
Figure. The logical chain from the second-order wave equation to its right- and left-moving
solution families. WM17 will determine the two arbitrary functions from initial data.
11 Worked example 1: identify both traveling components
Consider
Identify the direction and speed of each component and state the wave equation it satisfies.
The first term is
so it moves toward increasing x at speed
The second term can be written as
where
Therefore it moves toward decreasing x at the same speed magnitude,
Because each term separately satisfies the wave equation and the equation is linear, their sum
satisfies
12 Worked example 2: a non-obvious solution written as two traveling pieces
Consider
Since
and
this function satisfies
for any constant c.
Can it really be written in right- and left-moving form?
Use the identity
Therefore
Define
and
Then
This example shows that the two-family representation applies to more than localized pulses and
sinusoids.
13 Worked example 3: decompose a standing wave
Suppose
with x in meters and t in seconds.
Use
Then
| u(x,t) | = 3.0 mm cos(3x − 12t) | (75)
|
| + 3.0 mm cos(3x + 12t). | (76) |
Hence the standing wave is the sum of
and
The common wave speed is
14 Worked example 4: verify a general two-family expression
Consider
The first term is a function of x− 2t only, and the second is a function of x + 2t only. Therefore, by
the WM15 result, each separately satisfies
Linearity then implies that the sum also satisfies
A direct check gives the same result.
For the first term,
and
For the second term,
and
Thus
while
Therefore the PDE is satisfied everywhere.
15 Worked example 5: infer speed from the first-order relation
At one point in a known pure one-way wave, measurements give
and
Suppose the wave is known to be purely right-moving. Then
Hence
| c | = − | (92)
|
| = − | (93)
|
| = 80 m/s . | (94) |
The sign relation is consistent with rightward propagation because ut and ux have opposite
signs.
This diagnostic is valid only when the field is known to contain a single traveling family. If both
F and G are present simultaneously, the local ratio −ut∕ux generally does not equal
c.
16 Worked example 6: connect the two-family solution to string mechanics
A stretched string has Tension
and linear mass density
The string wave speed is
| c | =  | (97)
|
| =  | (98)
|
| =  | (99)
|
| ≈ 94.9 m/s . | (100) |
Suppose a sinusoidal component has
Then
gives
| ω | = (94.9)(6.0) | (103)
|
| ≈ 569 rad/s . | (104) |
A possible pair of equal-amplitude traveling components is therefore
and
Both components satisfy the same mechanically derived string equation
17 Common mistakes
- Mistake: thinking x − ct means left-moving because of the minus sign. Holding the
argument constant gives x = ct + constant, so the feature moves toward +x.
- Mistake: applying ut = −cux to a field containing both right- and left-moving
components. That first-order equation applies to a pure right-moving component.
- Mistake: treating the factorization of the wave operator as ordinary scalar
multiplication without remembering that the factors are differential operators.
- Mistake: concluding that a solution must look like a pulse or sinusoid. The arbitrary
functions F and G can have many sufficiently smooth shapes.
- Mistake: assuming the two functions F and G are known once the PDE is written.
Initial or boundary data are needed to determine them.
- Mistake: forgetting the smoothness assumptions behind the classical derivative
manipulations.
18 What WM16 establishes
The one-dimensional constant-speed wave equation
contains two characteristic propagation families:
and
For a sufficiently smooth classical solution on a suitable domain,
The two components propagate in opposite directions at the same speed magnitude
c.
The next problem is not to discover the form of the solution, but to determine the two arbitrary
functions from physical data. That is the purpose of WM17: initial conditions and the d’Alembert
solution.
References
References
[1] A. P. French, Vibrations and Waves, M.I.T. Introductory Physics Series, W. W.
Norton & Company, 1971.
[2] Frank S. Crawford, Jr., Waves, Berkeley Physics Course, Volume 3, McGraw-Hill,
1968.
[3] William Moebs, Samuel J. Ling, and Jeff Sanny, University Physics, Volume 1,
OpenStax, 2016, Section 16.2, “Mathematics of Waves.”
[4] Richard P. Feynman, Robert B. Leighton, and Matthew Sands, The Feynman Lectures
on Physics, Volume I, Chapter 47, “Sound. The Wave Equation.”
[5] Richard P. Feynman, Robert B. Leighton, and Matthew Sands, The Feynman Lectures
on Physics, Volume I, Chapter 48, “Beats.”
[6] Massachusetts Institute of Technology, 8.03SC Physics III: Vibrations and Waves,
Lecture 10, “Traveling Waves,” MIT OpenCourseWare.