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SCIENCE · INVESTIGATE AND EXPLAIN

Derive spring topology and shift the equilibrium coordinate

Separate an equilibrium offset from the stiffness that sets harmonic frequency.

Learning outcome: Derive all three stiffnesses for two different k2 values. Compute each equilibrium first, then compare periods at the same mass. Double mass in a written changed case and predict the period factor before calculating. Draw which quantity is shared in a series connection and which in a parallel connection.

Starting recap

Derive the restoring equation, retain initial conditions and distinguish exact harmonic results from approximation and calibration assumptions.

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Try

For k1=k2=8 N/m and m=2 kg, the single, parallel and series stiffnesses are 8,16,4 N/m. Their equilibrium extensions are 2.5,1.25,5 m in the stipulated ideal model. Angular frequencies are 2,sqrt(8),sqrt(2) rad/s; the large extensions are mathematical parameters, not apparatus instructions.

Open the experiment

Predict

In an ideal vertical oscillator, constant gravity primarily changes which quantity?

Experiment

Derive all three stiffnesses for two different k2 values. Compute each equilibrium first, then compare periods at the same mass. Double mass in a written changed case and predict the period factor before calculating. Draw which quantity is shared in a series connection and which in a parallel connection.

Derive stiffness and shift a vertical equilibrium

Worked teaching model · synthetic values · Massless ideal springs k1=8 N/m and selected k2, g=10 m/s². Compare single, parallel and series configurations under the same total vertical mass; springs remain linear with adequate extension range. No physical assembly.

Reset keeps your prediction, captures and practice history.

Parallel restoring force about equilibrium

net force (N)displacement from equilibrium (m)-0.30.34.8-4.8

Axes rescale independently. Curves join sampled coordinates; a joining segment is not additional measured evidence. Read physical units rather than screen angles or apparent slopes.

Parallel restoring force about equilibrium: numerical coordinates
displacement from equilibrium (m)net force (N)
-0.34.8
-0.294.64
-0.284.48
-0.274.32
-0.264.16
-0.254
-0.243.84
-0.233.68
-0.223.52
-0.213.36
-0.23.2
-0.193.04
-0.182.88
-0.172.72
-0.162.56
-0.152.4
-0.142.24
-0.132.08
-0.121.92
-0.111.76
-0.11.6
-0.091.44
-0.081.28
-0.071.12
-0.060.96
-0.050.8
-0.040.64
-0.030.48
-0.020.32
-0.010.16
00
0.01-0.16
0.02-0.32
0.03-0.48
0.04-0.64
0.05-0.8
0.06-0.96
0.07-1.12
0.08-1.28
0.09-1.44
0.1-1.6
0.11-1.76
0.12-1.92
0.13-2.08
0.14-2.24
0.15-2.4
0.16-2.56
0.17-2.72
0.18-2.88
0.19-3.04
0.2-3.2
0.21-3.36
0.22-3.52
0.23-3.68
0.24-3.84
0.25-4
0.26-4.16
0.27-4.32
0.28-4.48
0.29-4.64
0.3-4.8

Series restoring force about equilibrium

net force (N)displacement from equilibrium (m)-0.30.31.2-1.2

Axes rescale independently. Curves join sampled coordinates; a joining segment is not additional measured evidence. Read physical units rather than screen angles or apparent slopes.

Series restoring force about equilibrium: numerical coordinates
displacement from equilibrium (m)net force (N)
-0.31.2
-0.291.16
-0.281.12
-0.271.08
-0.261.04
-0.251
-0.240.96
-0.230.92
-0.220.88
-0.210.84
-0.20.8
-0.190.76
-0.180.72
-0.170.68
-0.160.64
-0.150.6
-0.140.56
-0.130.52
-0.120.48
-0.110.44
-0.10.4
-0.090.36
-0.080.32
-0.070.28
-0.060.24
-0.050.2
-0.040.16
-0.030.12
-0.020.08
-0.010.04
00
0.01-0.04
0.02-0.08
0.03-0.12
0.04-0.16
0.05-0.2
0.06-0.24
0.07-0.28
0.08-0.32
0.09-0.36
0.1-0.4
0.11-0.44
0.12-0.48
0.13-0.52
0.14-0.56
0.15-0.6
0.16-0.64
0.17-0.68
0.18-0.72
0.19-0.76
0.2-0.8
0.21-0.84
0.22-0.88
0.23-0.92
0.24-0.96
0.25-1
0.26-1.04
0.27-1.08
0.28-1.12
0.29-1.16
0.3-1.2
Calculated values under the declared model
QuantityValueUnit
Single effective stiffness8N/m
Single vertical equilibrium extension2.5m
Single angular frequency2rad/s
Single period3.14159s
Parallel effective stiffness16N/m
Parallel vertical equilibrium extension1.25m
Parallel angular frequency2.82843rad/s
Parallel period2.22144s
Series effective stiffness4N/m
Series vertical equilibrium extension5m
Series angular frequency1.41421rad/s
Series period4.44288s

Topology changes stiffness; a constant gravitational force shifts equilibrium without changing the linear stiffness.

Parallel springs share displacement and their forces add. Series springs share force and their extensions add, yielding 1/keff=1/k1+1/k2. With downward y from unstretched length, m yddot=mg−keff y. Set q=y−mg/keff to obtain qddot=−(keff/m)q. This assumes ideal massless springs and the stated linear regime.

Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.

Topology changes stiffness; a constant gravitational force shifts equilibrium without changing the linear stiffness.

Parallel springs share displacement and their forces add. Series springs share force and their extensions add, yielding 1/keff=1/k1+1/k2. With downward y from unstretched length, m yddot=mg−keff y. Set q=y−mg/keff to obtain qddot=−(keff/m)q. This assumes ideal massless springs and the stated linear regime.

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

Understand

Derive equivalent stiffness from constraints

Two parallel springs undergo the same extension x and provide forces k1x and k2x; their total force is (k1+k2)x. For massless springs in series, the same force F acts through each, while total extension is F/k1+F/k2. Thus k_parallel=k1+k2 and 1/k_series=1/k1+1/k2. These results depend on the stated geometry and ideal massless connectors, not merely on seeing two springs.

Translate a vertical force law

Choose downward y measured from the unstretched configuration. For attached mass m, m y double-dot=mg−keff y. Equilibrium is y_eq=mg/keff. With q=y−y_eq, the equation becomes m q double-dot=−keff q. Gravity supplies a constant offset but does not change the linear restoring slope. The frequency is sqrt(keff/m), not sqrt(g/y) using an arbitrary instantaneous extension.

Predict changes before computing

Increasing mass lengthens the period by its square-root factor. Increasing effective stiffness shortens it. Under the same mass, parallel springs are stiffer than either alone and series springs softer than either alone. Displacement must be measured from each configuration’s own equilibrium before comparing restoring forces; the unstretched reference and equilibrium reference are different.

State the limits of the equivalent model

The derivation assumes linear spring response, negligible spring/connector masses and geometry that remains fixed. A heavy spring has distributed motion and a constrained support can add other modes. The workbench stipulates enough linear extension range for every virtual configuration; it does not claim that a real spring can safely stretch to the computed equilibrium.

Worked original case

For k1=k2=8 N/m and m=2 kg, the single, parallel and series stiffnesses are 8,16,4 N/m. Their equilibrium extensions are 2.5,1.25,5 m in the stipulated ideal model. Angular frequencies are 2,sqrt(8),sqrt(2) rad/s; the large extensions are mathematical parameters, not apparatus instructions.

Investigation

Derive all three stiffnesses for two different k2 values. Compute each equilibrium first, then compare periods at the same mass. Double mass in a written changed case and predict the period factor before calculating. Draw which quantity is shared in a series connection and which in a parallel connection.

Public numerical transfer practice

Try a new practice case

Two ideal springs of stiffness 6 and 3 N/m are in series. What is their effective stiffness in N/m?

This public, unsaved check is not a secure assessment. Explain the derivative, integral or boundary in the retained course evidence workspace.

Sources and evidence boundary

Original derivations and assigned numerical cases checked 30 October 2026 against the official AP Physics C Mechanics framework and OpenStax harmonic motion and pendulums. These are supplied or generated records, not physical measurements or performed laboratory time. Do not construct rotating equipment, release loads or conduct launch experiments. Public feedback and retained self-reports do not certify independent mastery.

Apply

In an ideal vertical oscillator, constant gravity primarily changes which quantity?

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

What would fail if one series connector had a significant accelerating mass?

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