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SCIENCE · INVESTIGATE AND EXPLAIN

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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Try

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.

Open the experiment

Predict

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.

Reset keeps your prediction, captures and practice history.

External gravitational potential

potential (J)radius (m)240-20

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
Calculated values under the declared model
QuantityValueUnit
Potential at initial radius-20J
Potential at final radius-10J
Increase in potential10J
Work by gravity-10J
Quasistatic external work10J
Initial-g linear estimate20J
Marginal escape kinetic energy at start20J

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.

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

Understand

Integrate force along the radial coordinate

Outside a spherical source, radial gravitational force is −GMm/r², with positive r outward. The work from ri to rf is the integral of this force, GMm(1/rf−1/ri). Since potential change is minus conservative work, choosing U=0 at infinity gives U=−GMm/r. Negative potential does not mean negative kinetic energy.

Compare external work under a stated process

For a quasistatic outward displacement, an external agent supplies a force balancing gravity and transfers work ΔU. Gravity supplies the opposite signed work. If the object instead accelerates, external work also changes kinetic energy; the quasistatic result cannot be reused without that qualification. The workbench fixes the source and neglects recoil.

Test the local approximation

With GM=20, ri=2 and test mass m, initial g=5 m/s². A constant-initial-g estimate gives ΔU≈5m(rf−2), while the exact result is 20m(1/2−1/rf). The linear estimate overstates the required outward energy because the field decreases with radius. For a small height h, expanding 1/(ri+h) recovers the leading m g_i h term.

Count interaction pairs once

For several separated spherical bodies in the Newtonian point approximation, total gravitational potential sums −G mi mj/rij over distinct unordered pairs. Three objects have three pairs, not six; summing each object’s interaction with every other object and then adding without a one-half correction double counts. This potential describes the configuration, not one object’s isolated property.

Use escape energy without claiming a finite endpoint

For fixed-source radial escape, marginal total energy zero gives initial K=GMm/ri. The speed approaches zero only as r tends to infinity, not at a finite stop. Positive total energy permits a nonzero limiting speed under this isolated model; negative energy is bound. Real launch dynamics, atmosphere and source motion are outside this calculation.

Worked original case

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.

Investigation

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.

Public numerical transfer practice

Try a new practice case

With GM=20 m³/s², mass 3 kg and initial radius 2 m, what marginal escape kinetic energy is required in joules?

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 teaching, values and calculations, checked 30 October 2026 against the official calculus-based Mechanics framework and OpenStax work and kinetic energy. The numerical packets are supplied or generated, not measured apparatus records. No physical launch, machinery, loading or field intervention is requested. Public feedback and virtual captures do not establish independent mastery or supervised laboratory participation.

Apply

Why does the initial-g approximation overestimate this outward potential increase?

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

What changes if the external transfer is rapid rather than quasistatic?

Continue

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