Integrate gravitational work with a defensible reference
Recover inverse-square potential and distinguish an exact radial transfer from a local constant-field approximation.
Learning outcome: Compare final radii 3 and 8 for m=2. Reconstruct the definite integral and both work signs, then express the relative change of g. Propose how a small-height comparison would test the approximation without claiming a launch experiment.
Starting recap
Derive the integral or derivative, preserve the system boundary, and reject physically inaccessible continuations.
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For m=2,ri=2,rf=4, potential rises from −20 to −10 J; gravity work is −10 J and quasistatic external work +10 J. The initial-g linear estimate gives 20 J, twice the exact difference.
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Why does the initial-g approximation overestimate this outward potential increase?
Experiment
Compare final radii 3 and 8 for m=2. Reconstruct the definite integral and both work signs, then express the relative change of g. Propose how a small-height comparison would test the approximation without claiming a launch experiment.
Integrate an inverse-square interaction
Worked teaching model · synthetic values · Stipulated fixed central source GM=20 m³/s², initial radius 2 m. Both endpoints external to a spherical source. Compare quasistatic outward work and constant-initial-g approximation; no actual orbit or launch.
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External gravitational potential
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.
External gravitational potential: numerical coordinates
| radius (m) | potential (J) |
|---|---|
| 2 | -20 |
| 2.05 | -19.5122 |
| 2.1 | -19.0476 |
| 2.15 | -18.6047 |
| 2.2 | -18.1818 |
| 2.25 | -17.7778 |
| 2.3 | -17.3913 |
| 2.35 | -17.0213 |
| 2.4 | -16.6667 |
| 2.45 | -16.3265 |
| 2.5 | -16 |
| 2.55 | -15.6863 |
| 2.6 | -15.3846 |
| 2.65 | -15.0943 |
| 2.7 | -14.8148 |
| 2.75 | -14.5455 |
| 2.8 | -14.2857 |
| 2.85 | -14.0351 |
| 2.9 | -13.7931 |
| 2.95 | -13.5593 |
| 3 | -13.3333 |
| 3.05 | -13.1148 |
| 3.1 | -12.9032 |
| 3.15 | -12.6984 |
| 3.2 | -12.5 |
| 3.25 | -12.3077 |
| 3.3 | -12.1212 |
| 3.35 | -11.9403 |
| 3.4 | -11.7647 |
| 3.45 | -11.5942 |
| 3.5 | -11.4286 |
| 3.55 | -11.2676 |
| 3.6 | -11.1111 |
| 3.65 | -10.9589 |
| 3.7 | -10.8108 |
| 3.75 | -10.6667 |
| 3.8 | -10.5263 |
| 3.85 | -10.3896 |
| 3.9 | -10.2564 |
| 3.95 | -10.1266 |
| 4 | -10 |
| Quantity | Value | Unit |
|---|---|---|
| Potential at initial radius | -20 | J |
| Potential at final radius | -10 | J |
| Increase in potential | 10 | J |
| Work by gravity | -10 | J |
| Quasistatic external work | 10 | J |
| Initial-g linear estimate | 20 | J |
| Marginal escape kinetic energy at start | 20 | J |
Integrating inverse-square force fixes the sign and exposes the limits of a constant-g approximation.
Use zero potential at infinity. Outward gravity work is negative; a quasistatic external agent supplies the opposite work. The fixed-source approximation omits source recoil. Marginal escape approaches zero speed only asymptotically at infinity.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
Integrating inverse-square force fixes the sign and exposes the limits of a constant-g approximation.
Use zero potential at infinity. Outward gravity work is negative; a quasistatic external agent supplies the opposite work. The fixed-source approximation omits source recoil. Marginal escape approaches zero speed only asymptotically at infinity.
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What changes if the external transfer is rapid rather than quasistatic?
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