Wave Mechanics Examples: The Sinusoidal Traveling Wave
This companion article provides self-study exercises for WM07, wave mechanics: The Sinusoidal
Traveling Wave. The central one-dimensional forms are
for propagation toward increasing x, and
for propagation toward decreasing x, when k > 0 and ω > 0. These forms are standard in
introductory wave mechanics [1, 2, 3, 4].
The exercises stay within the WM07 scope. They develop interpretation of the complete phase,
extraction of wavelength and period, evaluation of a wave at a specific event (x,t), fixed-time
spatial snapshots, fixed-position time histories, phase offsets, and propagation direction. The
explicit wave-speed relations c = ω∕k = fλ are reserved for WM08.
How to use this problem set
Attempt every exercise in Part I before consulting Part II. When a propagation direction is
requested, identify the sign of the temporal term or verify the answer by following a constant
phase. For numerical work, keep the distinction between spatial quantities (k,λ) and temporal
quantities (ω,T,f) visible at every step.
WM07 relations permitted in this set:
A fixed-time view is a spatial snapshot; a fixed-position view is a time history.
Part I: Exercises
Exercise 1: Read the parameters from the equation
Consider
where u and x are measured in meters and t in seconds.
Determine:
- the amplitude A;
- the Wavenumber k;
- the angular frequency ω;
- the phase constant ϕ;
- the propagation direction;
- the wavelength λ;
- the period T and ordinary frequency f.
Exercise 2: Right-moving or left-moving?
Assume every listed k and ω is positive. State the propagation direction of each disturbance.
- u1 = A cos(kx − ωt).
- u2 = A cos(kx + ωt).
- u3 = A sin(kx − ωt + π∕3).
- u4 = −A cos(kx + ωt).
- Explain why the minus sign in front of A in part (d) does not reverse the propagation
direction.
Exercise 3: Construct the wave equation
A sinusoidal wave has amplitude 3.0 cm, wavelength 0.80 m, period 0.50 s, and phase constant π∕6.
It propagates toward positive x.
- Calculate k.
- Calculate ω.
- Write the wave function in the form A cos(kx−ωt+ϕ), with u expressed in centimeters.
- Write the corresponding form if the same sinusoidal pattern instead propagates toward
negative x.
Exercise 4: Read a traveling wave from snapshots
The figure shows the same sinusoidal wave at two instants separated by 0.25 s.
Figure. Two snapshots of one sinusoidal profile. The crest positions are marked so the
translation can be read without relying on curve overlap.
Determine:
- the amplitude;
- the wavelength;
- the direction of propagation;
- the distance translated during the time interval;
- what fraction of one wavelength that translation represents;
- the period implied by the two snapshots.
Exercise 5: Evaluate the wave at one event
Let
where u is in millimeters, x in meters, and t in seconds.
Find:
- the phase 𝜃 at x = 0.50 m and t = 0.125 s;
- the displacement at that event;
- whether the result lies within the physically allowed range of the wave.
Exercise 6: Extract a spatial snapshot
A right-moving wave is
with u in centimeters, x in meters, and t in seconds.
- Write the spatial snapshot u(x, 0).
- Write the spatial snapshot at t = 1∕6 s.
- Determine the wavelength of either snapshot.
- Explain why changing the snapshot time changes the phase offset but not the
wavelength.
Exercise 7: Extract a time history
For the same wave used in Exercise 6,
find the time history observed at x = 0.50 m.
- Simplify u(0.50,t) as far as practical.
- Determine the period.
- Determine the frequency.
- Explain why the time history contains the same ω as the full traveling-wave expression.
Exercise 8: Spatial snapshot versus time history
The following two graphs are generated from the same traveling sinusoid.
Figure. Left: a fixed-time spatial snapshot. Right: a fixed-position time history. The
wavelength and period brackets are placed below the curves for visibility.
- Which horizontal axis represents position and which represents time?
- Read the wavelength from the spatial plot.
- Read the period from the temporal plot.
- Calculate k and ω.
- Explain why both graphs can describe the same two-variable function u(x,t).
Exercise 9: The role of the phase constant
Consider the two right-moving waves
and
- What is the phase difference Δϕ = ϕ2 − ϕ1?
- At t = 0, how far in x is a corresponding crest of u2 shifted relative to a crest of u1?
Express the answer in terms of λ.
- Does the phase constant change the wavelength?
- Does the phase constant reverse the propagation direction?
Exercise 10: Sine and cosine representations
Rewrite each wave in an equivalent form using the other trigonometric function.
- u = A cos(kx − ωt) as a sine.
- u = A sin(kx − ωt) as a cosine.
- Explain why the replacement does not change the physical class of wave represented.
Exercise 11: Dimensional consistency of complete phase
Assume x is measured in meters and t in seconds. For each expression, decide whether its
trigonometric argument is dimensionally valid.
- cos[(4 m−1)x − (7 s−1)t].
- cos[(4 m−1)x − 7t] when the number 7 is dimensionless.
- cos[kx − ωt + ϕ] with k in rad/m, ω in rad/s, and ϕ in radians.
- cos(k − ωt).
Exercise 12: Verify direction using constant phase
For the wave
a marked crest corresponds to a fixed phase 𝜃0.
- Write the constant-phase equation.
- Solve that equation for x as a function of t.
- Without introducing a numerical wave speed, explain from the sign of the
time-dependent term why the marked crest moves toward increasing x.
- Repeat the reasoning for A cos(kx + ωt + ϕ).
Exercise 13: Read a constant-phase track
The figure shows one constant-phase feature of a sinusoidal wave in an x–t diagram.
Figure. A marked phase feature appears at progressively larger positions as time increases.
Two widely separated points are labeled so the direction is clear.
- Is the wave propagating toward +x or −x?
- Which of the two phase forms, kx−ωt + ϕ or kx + ωt + ϕ, is consistent with the track
for positive k and ω?
- What does it mean physically that every point on the line has the same phase value?
- What additional relation will WM08 obtain from the slope of this line?
Exercise 14: Synthesis from measured wave data
A sinusoidal disturbance has the following measured properties:
- maximum displacement magnitude A = 12 mm;
- adjacent crests are separated by 0.60 m;
- at a fixed detector the time between consecutive maxima is 0.24 s;
- the wave moves toward positive x;
- at x = 0 and t = 0, the wave is at its positive maximum.
- Find k.
- Find ω.
- Choose a convenient phase constant ϕ.
- Construct a cosine traveling-wave function consistent with all of the observations.
- Verify from your equation that u(0, 0) = +A.
- State which measured fact determines the sign of the temporal term.
Part II: Complete Worked Solutions
Solution 1: Read the parameters from the equation
Compare
with
-
-
-
-
- The phase has the form kx−ωt+ϕ, so for positive k and ω the wave propagates toward
-
| λ | =  | (3)
|
| =  | (4)
|
| = 0.40 m . | (5) |
-
| T | = = = 0.25 s , | (6)
|
| f | = = 4.0 Hz . | (7) |
Common error. The coefficient 5π is k, not the wavelength. Wavelength is obtained from
2π∕k.
Solution 2: Right-moving or left-moving?
- kx − ωt corresponds to
- kx + ωt corresponds to
- Replacing cosine with sine changes only the phase convention. The kx − ωt structure
still gives
- The phase still contains kx + ωt, so the wave travels toward
- The factor −A flips the disturbance vertically. It is equivalent to adding a phase shift
of π because
It does not change the sign that controls translation through space.
Solution 3: Construct the wave equation
The data are
-
| k | =  | (8)
|
| =  | (9)
|
| = 2.5π rad/m . | (10) |
-
| ω | =  | (11)
|
| =  | (12)
|
| = 4π rad/s . | (13) |
- Positive-x propagation uses the minus temporal sign:
- For negative-x propagation,
Solution 4: Read a traveling wave from snapshots
From the plotted vertical scale, the extrema are +2 cm and −2 cm.
- Therefore
- Consecutive crests in either snapshot are separated by
- The marked crest shifts from x = 1 m to x = 2 m as time increases, so propagation is
toward
- The translation is
- Relative to the wavelength,
- A shift of λ∕4 corresponds to one quarter of a cycle in time. Since the snapshots are
separated by 0.25 s,
and hence
Solution 5: Evaluate the wave at one event
The phase is
At x = 0.50 m and t = 0.125 s,
| 𝜃 | = 2π(0.50) − 4π(0.125) +  | (14)
|
| = π − +  | (15)
|
| = . | (16) |
Thus
| u | = 6.0 cos mm | (17)
|
| = 6.0 mm | (18)
|
| = −3 mm | (19)
|
| ≈−5.20 mm . | (20) |
Since A = 6.0 mm, the allowed range is
The result lies inside this range, so it is physically consistent.
Solution 6: Extract a spatial snapshot
The full wave is
- At t = 0,
- At t = 1∕6 s,
so
u | = 2.5 cos(3πx − π + π∕4) cm | (21)
|
| = 2.5 cos(3πx − 3π∕4) cm . | (22) |
- Since k = 3π rad/m,
- Changing t changes only the additive phase offset −ωt + ϕ. The coefficient of x remains
k = 3π, so the wavelength remains unchanged.
Solution 7: Extract a time history
At x = 0.50 m,
| u(0.50,t) | = 2.5 cos ![[ π-]
3π (0.50 ) − 6πt + 4](https://images.physicslibrary.org/cache/objects/1161/make4ht/WaveMechanicsExamplesTheSinusoidalTravelingWave57x.png) | (23)
|
| = 2.5 cos  | (24)
|
| = 2.5 cos cm . | (25) |
The angular frequency is still
Therefore
| T | = = s , | (26)
|
| f | = = 3.0 Hz . | (27) |
Fixing x replaces kx by a constant phase contribution. It does not alter the coefficient of t, so the
time history retains the same ω as the full traveling wave.
Solution 8: Spatial snapshot versus time history
- The left graph has horizontal axis x and is the spatial snapshot. The right graph has
horizontal axis t and is the time history.
- The marked crest-to-crest separation is
- The marked maximum-to-maximum time separation is
-
| k | = = = π rad/m , | (28)
|
| ω | = = = 4π rad/s . | (29) |
- A two-variable wave function contains both dependences. Setting t = t0 produces a function
of x only; setting x = x0 produces a function of t only. These are different slices through the
same u(x,t).
Solution 9: The role of the phase constant
-
- At t = 0, a crest satisfies a constant phase. For u1 choose kx = 0. For u2, a
corresponding crest can satisfy
so
Using k = 2π∕λ,
Thus, at the same reference time, the u2 crest is shifted one quarter wavelength toward
smaller x relative to the corresponding u1 crest.
- No. The coefficient k is unchanged, so λ = 2π∕k is unchanged.
- No. Both phases contain kx − ωt, so both waves propagate toward +x.
Solution 10: Sine and cosine representations
Use
and
-
-
- The change merely alters the phase constant. Wavelength, period, amplitude, and
propagation direction remain the same. Thus sine and cosine are two phase conventions
for the same class of sinusoidal traveling wave [3, 1].
Solution 11: Dimensional consistency of complete phase
- Valid. The products
are dimensionless angular quantities.
- Invalid as written. If 7 is dimensionless, then 7t has units of time and cannot be
subtracted from a dimensionless spatial phase.
- Valid. kx, ωt, and ϕ are all angular phase terms.
- Invalid. k alone has dimensions of inverse length, whereas ωt is dimensionless. The
spatial term must be multiplied by a length such as x.
Solution 12: Verify direction using constant phase
A fixed feature satisfies
Solving for x gives
Since k > 0 and ω > 0, increasing t requires increasing x. Therefore the feature moves toward
+x.
For the opposite sign,
so
As t increases, x decreases. Therefore the feature moves toward −x.
The appearance of the ratio ω∕k anticipates WM08, where that ratio is identified and interpreted
explicitly as the propagation speed.
Solution 13: Read a constant-phase track
- The feature appears at larger x at later t, so the wave moves toward
- For positive k and ω, this is consistent with
- Every point on the line represents a different event (x,t) at which the wave has the
same phase. Thus the plotted line follows one recognizable wave feature such as a crest.
- WM08 will use the slope of the constant-phase line to obtain the propagation speed
and show that
Solution 14: Synthesis from measured wave data
The measured quantities are
-
| k | =  | (30)
|
| = rad/m . | (31) |
-
| ω | =  | (32)
|
| = rad/s . | (33) |
- At x = 0 and t = 0 the wave is at its positive maximum. For a cosine representation, the
simplest choice is
Any phase equivalent to 2πn would describe the same starting state.
- Since the wave moves toward positive x, use the minus temporal sign:
- At the origin of space and time,
- The observation that the wave moves toward positive x determines the minus sign in
kx − ωt.
What this set prepares you for
WM07E1 has treated the sinusoidal traveling wave as a kinematic object. The student can now
identify every parameter in
switch between spatial snapshots and time histories, evaluate the disturbance at an event, and
follow constant phase through space and time. WM08 will now make the natural quantitative
connection between the spatial and temporal rates of phase change by deriving the wave
speed.
Summary of skills practiced
After completing this set, you should be able to:
- read A, k, ω, and ϕ from a traveling-wave equation;
- determine propagation direction from the phase sign convention;
- recover λ, T, and f from k and ω;
- construct a sinusoidal traveling-wave equation from physical data;
- evaluate u(x,t) at a specified event;
- extract a fixed-time spatial snapshot and a fixed-position time history;
- interpret the phase constant as a shift rather than a change of direction;
- convert between sine and cosine phase conventions;
- check dimensional consistency of a complete wave phase;
- track a constant-phase feature in an x–t diagram.
References
The notation and traveling-wave conventions used in this problem set follow the same sources used
in WM07.
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] Samuel J. Ling, Jeff Sanny, and William Moebs, University Physics, Volume 1,
OpenStax, 2016, Chapter 16, especially Section 16.2, “Mathematics of Waves.”
[4] Richard P. Feynman, Robert B. Leighton, and Matthew Sands, The Feynman Lectures
on Physics, Volume I, Chapter 29, especially Section 29–3, “Sinusoidal waves.”
[5] Richard P. Feynman, Robert B. Leighton, and Matthew Sands, The Feynman Lectures
on Physics, Volume I, Chapter 48, especially Section 48–4, “Localized wave trains.”