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Physics I course sequence · Problem studio

Gravitation problem studio

Most wrong answers in gravitation come from the right law applied to the wrong quantity. This studio drills the choice — a vector field or a scalar potential, surface g or the g where the craft actually is, one orbit's numbers or a ratio between two — and then makes every orbit change pay its way in energy.

UPI-13.07 · Lesson 7 of 7 in this unit. Position is not a completion score.
Starting model: Gravitation problem studioEnergy per kilogram against distance from Earth's centre, from the surface to 7 Earth radii, with zero energy on the top line. Lower curve U/m = −GM/r, upper curve the circular-orbit total E/m = −GM/(2r). From r₁ = 1.1 to r₂ = 6.6 Earth radii the burns supply 23.70 MJ/kg, U changes by 47.40 MJ/kg and K by -23.70 MJ/kg.EUr₁ = 1.1 REr₂ = 6.6 REE = U/2 = −GMm/(2r), K = −Edashed: mgh using g at r₁○ transfer: burn 1 = 86% of ΔEv₁ = 7.54 → v₂ = 3.08 km/s
Start with a picture. Change the model in the lab below.
1

Build the model

Pick the quantity before the equation: vector pulls or scalar energies.

The key idea

Solving a gravitation problem means choosing which of four linked quantities carries the question — force, field, potential energy or total orbital energy — and moving between them with g = F/m, F = −dU/dr and mv²/r = GMm/r².

Example. At r = 2RE the field is g = 2.46 m s⁻², a quarter of the surface value; a 100 kg satellite there has U = −3.13 × 10⁹ J, half its surface value, and in circular orbit moves at v = 5.59 km s⁻¹ with E = −1.56 × 10⁹ J.

The complete physical model and assumptions

Every problem in this section runs on one law, F = GMm/r², valid for point masses and for uniform spheres outside their surfaces, and on one decision: which of its four faces carries the question. Force and field are vectors that fall as 1/r² and superpose by components. Potential energy and potential are scalars that fall as 1/r and superpose as signed numbers, with zero set at infinite separation. A circular orbit ties the two families together, because mv²/r = GMm/r² forces K = −E = −U/2 at every radius. That relation makes energy the natural currency for satellites: a burn changes E, E fixes the orbit's size, and speed and period follow as powers of r that compare cleanly by ratio. The familiar mgh is not a rival model but the tangent to −GMm/r at the surface, good to the fraction h/R. The framework fails where its idealisations do: Earth's equatorial bulge and upper-atmosphere drag perturb low orbits; a second body of comparable mass makes both bodies move, so the static neutral point between Earth and Moon is not the L1 balance point of the rotating system; and precise timing, as in GPS, needs general relativity's corrections to Newton.

1Name the quantity before you write an equation

The four quantities in this section share one law and behave differently. Force F = GMm/r² and field g = GM/r² are vectors falling as 1/r². Potential energy U = −GMm/r and potential V = −GM/r are scalars falling as 1/r. A circular orbit adds E = −GMm/(2r), from mv²/r = GMm/r². So read the question for what it asks. A direction or an acceleration wants a vector sum. A speed, a fuel budget or an escape wants energy, because the force changes along the path and the constant-force W = F ⋅ d no longer applies. A comparison between two orbits wants a ratio. One point, r = 3RE, shows why the choice matters: there g = 1.09 m s⁻², a ninth of its surface value; U/m = −20.9 MJ kg⁻¹, a third; and a circular orbit has E/m = −10.4 MJ kg⁻¹ and v = 4.57 km s⁻¹. Carry the wrong quantity and the power of r is wrong before the arithmetic begins.

2Add fields head to tail and potentials as numbers

With several bodies, find each contribution alone, then combine. Fields are vectors: point each GMᵢ/rᵢ² from the field point toward body i, resolve, and add components. Potentials are signed scalars, V = −Σ GMᵢ/rᵢ, with no angles at all. The two sums can tell very different stories. On the Earth–Moon line the pulls cancel where GME/x² = GMM/(d − x)². With ME/MM = 81.3 and d = 3.84 × 10⁸ m, x = d/(1 + 1/√81.3) = 3.46 × 10⁸ m, 90% of the way to the Moon. The field there is zero, yet V = −1.15 MJ kg⁻¹ − 0.13 MJ kg⁻¹ = −1.28 MJ kg⁻¹, so a probe at rest there is still bound to the pair. Along the line V is at its maximum at that point: it is a ridge a craft must cross, not a place where gravity has switched off.

3Retire mgh once h is a fair fraction of R

mgh treats g as constant over the climb, which makes it the tangent line to U = −GMm/r at the surface. The exact change is ΔU = GMm(1/R − 1/(R + h)), which rearranges to mg₀h × R/(R + h). So mg₀h overstates the gain by the factor 1 + h/R: 0.16% for a 10 km airliner climb, 6.3% for a climb to the ISS's 400 km, twice the true value at h = R, and 6.6 times at geostationary altitude. The field shrinks by the square of the same factor, g = g₀R²/(R + h)². At 400 km it is 8.69 m s⁻², still 89% of g₀ = 9.82 m s⁻², which is why the claim that there is no gravity in orbit is wrong: the crew is in free fall, with gravity supplying exactly the centripetal acceleration. The working rule is to compare h/R with the precision you need, and switch to the 1/r form as soon as h/R is the larger.

4Compare orbits by ratio so G and M cancel

Around one central body, v = √(GM/r), T = 2π√(r³/GM), K = GMm/(2r) and E = −GMm/(2r). Divide one orbit's value by another's and the constants vanish: v₂/v₁ = (r₁/r₂)¹⁄², T₂/T₁ = (r₂/r₁)³⁄² and E₂/E₁ = r₁/r₂. The ISS circles at r = 6.771 × 10⁶ m with T = 92.4 min and v = 7.67 km s⁻¹. A geostationary satellite orbits at 4.216 × 10⁷ m, 6.23 times farther out, so its period is 6.23³⁄² = 15.5 times longer, 23.9 h, and its speed is 1/√6.23 = 0.401 times as large, 3.07 km s⁻¹, all without G or ME. Its total energy is 6.23 times smaller in magnitude, and less negative means more energy, which is what the trip has to pay for. Ratios also expose slips: if a larger orbit comes out faster, or a period scales as r², a step is wrong, whatever the calculator says.

5Budget every orbit change in total energy

Thrusters do work equal to the change in E, not in K or U. Between circular orbits ΔE = (GMm/2)(1/r₁ − 1/r₂), and because U = 2E and K = −E at every radius, ΔU = 2ΔE and ΔK = −ΔE. Raising a 1000 kg satellite from the ISS radius to geostationary radius needs ΔE = 2.47 × 10¹⁰ J: U rises by 4.94 × 10¹⁰ J while K falls by 2.47 × 10¹⁰ J, because gravity's negative work on the climb is twice what the burns supply. One burn cannot do the job, since an orbit changed by a single impulse still passes through the point where the impulse happened. The standard route is two burns joined by a transfer ellipse tangent to both circles, with semi-major axis a = (r₁ + r₂)/2 and energy Eₜ = −GMm/(2a). Burn 1 lifts E from −GMm/(2r₁) to Eₜ, burn 2 from Eₜ to −GMm/(2r₂), and the first burn carries the fraction r₂/(r₁ + r₂) of the total: 86% for this transfer.

6Finish with escape, limits and signs

Every energy here is measured from zero at infinite separation, so bound orbits have E < 0 and escape needs E ≥ 0. Setting ½mv² − GMm/r = 0 gives vesc = √(2GM/r) = √2 vcirc at the same radius: from the ISS orbit, escape takes 10.85 km s⁻¹ against 7.67 km s⁻¹ in orbit, an extra 3.18 km s⁻¹ if the burn is along the motion. Then make each result pass the checks it owes you. As h → 0, GMm(1/R − 1/(R + h)) must reduce to mg₀h. As r₂ → r₁, ΔE must vanish. As r → ∞, v, K, U and E must all go to zero while T grows without limit. Signs come last and catch the most: raising a circular orbit must give ΔE > 0, ΔU > 0 and ΔK < 0 together. Units close the loop: GM/r carries m² s⁻², a speed squared, so √(GM/r) is a speed and GMm/r is an energy in joules.

2

Key equations

Read the units, assumptions and limits before substituting.

Superposition of field and potential

g⃗ = Σ (GMᵢ/rᵢ²) r̂ᵢ · V = −Σ GMᵢ/rᵢ

Fields add by components and can cancel; potentials add as signed numbers and never cancel, so g = 0 does not mean V = 0.

g in N kg⁻¹ (m s⁻²), V in J kg⁻¹, rᵢ in m; r̂ᵢ points from the field point toward body i

Field at altitude

g(h) = GM/(R + h)² = g₀ R²/(R + h)²

At the ISS's 400 km, g is 8.69 m s⁻², still 89% of g₀: an orbiting crew is falling, not beyond gravity.

g₀ = GM/R² = 9.82 m s⁻² for Earth, R = 6.371 × 10⁶ m, h in m above the surface

Potential-energy change on a climb

ΔU = GMm(1/R − 1/(R + h)) = mg₀h × R/(R + h)

mg₀h overstates ΔU by the factor 1 + h/R: 0.16% at 10 km, 6.3% at 400 km, double at h = R.

U in J, m in kg; U = 0 at infinite separation; exact outside a spherical body

Circular orbits compared by ratio

v₂/v₁ = (r₁/r₂)¹⁄² · T₂/T₁ = (r₂/r₁)³⁄² · E₂/E₁ = r₁/r₂

G and M cancel: an orbit 6.23 times farther out has 15.5 times the period and 0.401 times the speed.

from v = √(GM/r) and T = 2π√(r³/GM); r in m from the centre; one central mass

Energy split on a circular orbit

K = GMm/(2r) · U = −GMm/r · E = −GMm/(2r), so ΔU = 2ΔE and ΔK = −ΔE

Thrusters supply ΔE while U climbs by twice that, so the difference comes out of K and a raised satellite ends slower.

energies in J; r from the centre, not the altitude; E < 0 on every bound orbit

Transfer ellipse and escape

Eₜ = −GMm/(2a), a = (r₁ + r₂)/2 · vesc = √(2GM/r) = √2 vcirc

Because a is the mean of the two radii, Eₜ sits between the two circular energies; pushing a towards infinity sends Eₜ to zero, which is the escape condition.

a is the semi-major axis in m; the transfer ellipse touches both circular orbits
3

Interactive lab

Predict first. Explore the model. Compare the result.

Explore the model

1.1 RE
1.1 to 7 RE; steps of 0.1.
6.6 RE
1.1 to 7 RE; steps of 0.1.

Try this. From the start, r₁ = 1.1 to r₂ = 6.6 (near geostationary), the burns supply 23.70 MJ per kg, U rises by twice that and the speed falls from 7.54 to 3.08 km/s. Drag r₂ below r₁: energy leaves and the craft speeds up. The dashed mgh tangent always gives r₂/r₁ times the true ΔU.

Live results

ΔE/m SUPPLIED BY BURNS
23.70 MJ kg⁻¹
ΔU/m
47.40 MJ kg⁻¹
ΔK/m
-23.70 MJ kg⁻¹
mgh ÷ TRUE ΔU
6.00

Results follow this lesson’s model and assumptions. Displayed values are rounded.

Interactive Physics I modelEnergy per kilogram against distance from Earth's centre, from the surface to 7 Earth radii, with zero energy on the top line. Lower curve U/m = −GM/r, upper curve the circular-orbit total E/m = −GM/(2r). From r₁ = 1.1 to r₂ = 6.6 Earth radii the burns supply 23.70 MJ/kg, U changes by 47.40 MJ/kg and K by -23.70 MJ/kg.EUr₁ = 1.1 REr₂ = 6.6 REE = U/2 = −GMm/(2r), K = −Edashed: mgh using g at r₁○ transfer: burn 1 = 86% of ΔEv₁ = 7.54 → v₂ = 3.08 km/s
Energy per kilogram against distance from Earth's centre, from the surface to 7 Earth radii, with zero energy on the top line. Lower curve U/m = −GM/r, upper curve the circular-orbit total E/m = −GM/(2r). From r₁ = 1.1 to r₂ = 6.6 Earth radii the burns supply 23.70 MJ/kg, U changes by 47.40 MJ/kg and K by −23.70 MJ/kg.

Predict → change one variable → check

Plan a change before running it. Every other input stays at the saved baseline.

Saved baseline. Starting orbit radius r₁: 1.1 RE; Final orbit radius r₂: 6.6 RE

Baseline 1.1; choose 1.1 to 7, in steps of 0.1.
4. Compared with the saved baseline, this result will…

This experiment is kept only while this page is open. It does not change saved course progress.

4

Catch the common trap

“Air drag slows a satellite down.” Drag pushes against the motion at every instant, yet a satellite on a nearly circular orbit ends up faster. Drag removes total energy, and on a circular orbit E = −K, so each joule of total energy lost is a joule of kinetic energy gained: the satellite sinks to a smaller r, where v = √(GM/r) is larger. The bookkeeping is exact. If drag dissipates 1.0 MJ, U falls by 2.0 MJ and K rises by 1.0 MJ, because gravity does 2.0 MJ of positive work on the inward-spiralling craft while drag does 1.0 MJ of negative work. The same error run backwards says a raised satellite has lost energy because it ends up slower. It has gained energy: U rises by twice the gain while K falls by the gain itself. Judge an orbit change by E, never by speed.

5

Problem-solving studio

3 authored examples. Make an attempt, then reveal the reasoning one step at a time.

EasyExample 1

A sounding rocket carries a 45.0 kg instrument package straight up to a highest point 1500 km above Earth's surface. Find g at that height and the package's gain in gravitational potential energy, and say by how much the constant-g estimate mg₀h overstates that gain. Use GME = 3.986 × 10¹⁴ m³ s⁻² and RE = 6.371 × 10⁶ m.

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 4 steps revealed.

MediumExample 2

A binary asteroid is modelled as two fixed uniform spheres: A, 3.00 × 10¹² kg, centred at the origin, and B, 1.20 × 10¹² kg, centred at (6.00 km, 0). A 40.0 kg probe is momentarily at rest at P = (3.00 km, 4.00 km). Find the net gravitational field at P, the probe's gravitational potential energy, and the speed it needs at P to escape the pair. Use G = 6.674 × 10⁻¹¹ N m² kg⁻².

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 6 steps revealed.

HardExample 3

A 1200 kg satellite is left in a circular parking orbit of radius r₁ = 6.671 × 10⁶ m, 300 km up, and must reach a circular orbit of radius r₂ = 2.656 × 10⁷ m by a two-burn transfer ellipse. Find the energy the burns supply, in total and at each burn, the speed change at each burn, and the time spent coasting between them. Use GME = 3.986 × 10¹⁴ m³ s⁻².

Sketch your answer or reasoning, then compare it with the authored solution. Your writing is not automatically graded or saved.

0 of 6 steps revealed.

6

Quick check

Select an answer and explain it before checking.

A satellite of mass m circles a planet of mass M and radius R at orbital radius 2R. Its thrusters move it to a circular orbit of radius 4R. Ignoring the mass of fuel burned, how much work do the thrusters do in total?
7

Review & continue

Solving a gravitation problem means choosing which of four linked quantities carries the question — force, field, potential energy or total orbital energy — and moving between them with g = F/m, F = −dU/dr and mv²/r = GMm/r².

  • Explain the relationship without looking at the equation.
  • Check a sign, a unit and a model assumption in your working.
  • Return to the lab or worked example if a step is still unclear.

Optional supporting lessons

These chapter resources can help with earlier ideas; they are not additional required Physics I completion tasks.

Extra challenging questions

Connect several ideas, explore supplied data, and compare your reasoning with a worked solution.