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 experimentPredict
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.
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Parallel restoring force about equilibrium
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) |
|---|---|
| -0.3 | 4.8 |
| -0.29 | 4.64 |
| -0.28 | 4.48 |
| -0.27 | 4.32 |
| -0.26 | 4.16 |
| -0.25 | 4 |
| -0.24 | 3.84 |
| -0.23 | 3.68 |
| -0.22 | 3.52 |
| -0.21 | 3.36 |
| -0.2 | 3.2 |
| -0.19 | 3.04 |
| -0.18 | 2.88 |
| -0.17 | 2.72 |
| -0.16 | 2.56 |
| -0.15 | 2.4 |
| -0.14 | 2.24 |
| -0.13 | 2.08 |
| -0.12 | 1.92 |
| -0.11 | 1.76 |
| -0.1 | 1.6 |
| -0.09 | 1.44 |
| -0.08 | 1.28 |
| -0.07 | 1.12 |
| -0.06 | 0.96 |
| -0.05 | 0.8 |
| -0.04 | 0.64 |
| -0.03 | 0.48 |
| -0.02 | 0.32 |
| -0.01 | 0.16 |
| 0 | 0 |
| 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
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) |
|---|---|
| -0.3 | 1.2 |
| -0.29 | 1.16 |
| -0.28 | 1.12 |
| -0.27 | 1.08 |
| -0.26 | 1.04 |
| -0.25 | 1 |
| -0.24 | 0.96 |
| -0.23 | 0.92 |
| -0.22 | 0.88 |
| -0.21 | 0.84 |
| -0.2 | 0.8 |
| -0.19 | 0.76 |
| -0.18 | 0.72 |
| -0.17 | 0.68 |
| -0.16 | 0.64 |
| -0.15 | 0.6 |
| -0.14 | 0.56 |
| -0.13 | 0.52 |
| -0.12 | 0.48 |
| -0.11 | 0.44 |
| -0.1 | 0.4 |
| -0.09 | 0.36 |
| -0.08 | 0.32 |
| -0.07 | 0.28 |
| -0.06 | 0.24 |
| -0.05 | 0.2 |
| -0.04 | 0.16 |
| -0.03 | 0.12 |
| -0.02 | 0.08 |
| -0.01 | 0.04 |
| 0 | 0 |
| 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 |
| Quantity | Value | Unit |
|---|---|---|
| Single effective stiffness | 8 | N/m |
| Single vertical equilibrium extension | 2.5 | m |
| Single angular frequency | 2 | rad/s |
| Single period | 3.14159 | s |
| Parallel effective stiffness | 16 | N/m |
| Parallel vertical equilibrium extension | 1.25 | m |
| Parallel angular frequency | 2.82843 | rad/s |
| Parallel period | 2.22144 | s |
| Series effective stiffness | 4 | N/m |
| Series vertical equilibrium extension | 5 | m |
| Series angular frequency | 1.41421 | rad/s |
| Series period | 4.44288 | s |
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.
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What would fail if one series connector had a significant accelerating mass?
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