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SCIENCE · INVESTIGATE AND EXPLAIN

Read a complete oscillation in three motion graphs

Connect displacement, velocity and acceleration at the same instant.

Learning outcome: Predict turning-point and equilibrium behavior, distinguish acceleration from velocity direction and explain phase relationships across a full cycle.

Starting recap

A Hookean spring exerts F = −kx; acceleration is F/m. Velocity is the slope of position versus time.

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Try

A block passes through equilibrium at its greatest speed. Why is its acceleration zero there?

Open the experiment

Predict

For the 1 kg release, predict the signs of displacement, velocity and acceleration at 0, 0.5, 1 and 1.5 seconds.

Experiment

Keep mass at 1 kg and inspect those four times and the 2 s return. Compare selected markers across the three graphs. Capture the two equilibrium crossings and explain why their velocities differ despite equal position and acceleration.

Trace an ideal spring through complete oscillations

Worked teaching model · synthetic values · Horizontal frictionless motion with an ideal massless Hookean spring of stiffness π² N/m (about 9.870 N/m), amplitude 0.200 m, released from rest at positive amplitude at t = 0. Changing mass prepares a separate release, not a mid-motion mass change. Exact harmonic formulas; plotted curves sample 161 states over the same 0–4 s window. No damping, driving, spring mass or real-apparatus errors. The time slider selects a state; no animation runs automatically.

Reset keeps your prediction, captures and practice history.

Displacement (m) · same time window for every mass-0.2500.2501234Time after release (s) · marker selects the same instant in all plots
Velocity (m/s) · same time window for every mass-1.501.501234Time after release (s) · marker selects the same instant in all plots
Acceleration (m/s²) · same time window for every mass-80801234Time after release (s) · marker selects the same instant in all plots

The block crosses equilibrium: restoring force and acceleration are zero, while speed is maximal. Compare slopes and zero crossings, not vertical heights across graphs with different units.

Selected harmonic state and timing
QuantityValueMeaning
Time0.500 sSince release from +0.200 m at rest
Displacement0.000000 mSigned position relative to equilibrium
Velocity-0.628319 m/sSigned slope of displacement-time curve
Acceleration0.000000 m/s²Slope of velocity-time curve; −kx/m
Restoring force0.000000 N−kx
Period2.000000 sOne complete return to the same position and direction
Frequency0.500000 Hz1 / period, cycles per second
Angular frequency3.141593 rad/s2π / period, not cycles per second
Potential / kinetic energy0.000000 / 0.197392 JSum 0.197392 J

All curves are calculated from the release conditions, not integrated numerically or measured. Very small roundoff values below 10⁻¹² in position or velocity are displayed and used as zero. Mass changes leave spring stiffness and release amplitude fixed.

At 0.50 s: x = 0.000 m; v = -0.628 m/s; a = 0.000 m/s².

Period 2.000 s; frequency 0.500 Hz. Potential 0.000000 J + kinetic 0.197392 J = 0.197392 J. Distinct graph units and fixed vertical scales are labeled.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Follow time, not just position

The earlier spring-energy investigation selected a position on one half-cycle. This lab selects elapsed time after release, so you can inspect both directions of travel. A 1 kg block starts at x = +0.200 m with zero velocity. The fixed spring stiffness is k = π² N/m, approximately 9.870 N/m, chosen to give a convenient 2 s period for this mass.

Before moving the time control, predict the first equilibrium crossing. The spring pulls toward equilibrium, so the block begins moving left. As it approaches x = 0, the restoring force weakens, but the accumulated velocity does not vanish. At 0.5 s, displacement and acceleration are zero while velocity is approximately −0.628319 m/s.

Compare the three graphs at one instant

The plots share the same 0–4 s time axis and mark the same selected instant. Their vertical axes have different units and fixed ranges: displacement in metres, velocity in metres per second, acceleration in metres per second squared. Equal visual heights across different plots do not mean equal physical quantities.

At 0 s, x = +0.200 m, v = 0 and a ≈ −1.973921 m/s². At 0.5 s, x = 0, v ≈ −0.628319 m/s and a = 0. At 1 s, x = −0.200 m, v = 0 and a ≈ +1.973921 m/s². At 1.5 s, x = 0 again, but v ≈ +0.628319 m/s. At 2 s, the complete starting state returns.

Capture 0.5 s and 1.5 s. The block has the same position, restoring force and energy at both crossings, but opposite velocity. Position alone does not specify where it will move next. The two turning points likewise have zero velocity but nonzero acceleration, which reverses the motion.

Relate slopes, force and phase

Velocity is the slope of the displacement-time graph. At a displacement maximum or minimum, that slope is zero. Near an equilibrium crossing, displacement changes most rapidly, so the velocity magnitude is largest. Acceleration is the slope of the velocity-time graph; velocity’s extrema occur where acceleration is zero.

The force law is F = −kx, where F is signed restoring force, k is positive stiffness and x is displacement from equilibrium. Newton’s law then gives a = −(k/m)x, with mass m in kilograms. Acceleration always points opposite displacement. It does not always point opposite velocity: when the block travels toward equilibrium it speeds up, and when it travels away it slows down.

Phase describes where the motion is in its repeating cycle. The velocity curve is shifted by a quarter-cycle relative to displacement; acceleration has the opposite sign to displacement at every instant. Use the explicit states and slopes to interpret those relationships rather than memorizing a shift direction without a sign convention.

A compact formula for this release

Let omega = √(k/m), measured in radians per second. At elapsed time t, measured in seconds, the phase angle is omega t. With amplitude A = 0.200 m and release from rest at +A:

x = A cos(omega t), v = −A omega sin(omega t), and a = −omega² x.

Cosine and sine describe the repeating phase. At phase 0, π/2, π, 3π/2 and 2π, the listed quarter-cycle states follow. A different starting position or velocity would require a different phase or amplitude. The OpenStax simple-harmonic-motion reference gives further background on these relations.

Optional: verify the formulas through rates of change

Differentiating x = A cos(omega t) gives v = −A omega sin(omega t); differentiating again gives a = −A omega² cos(omega t) = −omega² x. With omega² = k/m, this satisfies ma = −kx and the specified release conditions. The lab evaluates these formulas directly rather than advancing a numerical time integrator.

Transfer without calculating a sine

On the return half-cycle, the block is at x = +0.100 m and moving right. Give the signs of force and acceleration, and decide whether its speed is increasing or decreasing. Could the same position occur while speeding up?

Check the harmonic-motion transfer

Force and acceleration are negative because x is positive. With positive velocity and negative acceleration, speed is decreasing. On the first half-cycle at the same positive position, velocity is negative, so negative acceleration increases speed. The position is the same; direction of travel changes the speed trend.

Apply

At the positive turning point of an ideal horizontal spring oscillation, velocity and acceleration are:

Public practice checks a specific claim. It does not establish independent mastery.

Explain why zero velocity need not mean zero acceleration, why zero force need not mean rest, and why identical positions can occur with opposite velocities.

Continue

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