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Gravitational Potential Energy (Extended)

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Newton's Law of Universal GravitationPotential Energy: Gravitational and Elastic+1 more→→Orbital Energy and Escape VelocityTidal Forces and Orbital Evolution
gravitation potential-energy energy orbits

Core Idea

Gravitational potential energy between two masses is U(r) = −G m₁ m₂ / r (with U = 0 at r = ∞). Unlike the near-Earth approximation U = mgh (linear in height), the true gravitational PE is inversely proportional to distance and negative, indicating an attractive interaction. Total mechanical energy E = KE + U is conserved in gravitational systems, determining whether orbits are bound (E < 0) or unbound (E ≥ 0).

Explainer

You already know potential energy as stored energy associated with position in a force field: the closer you are to Earth's surface, the lower your gravitational PE (taking the surface as reference). And from Newton's law of gravitation you know the force law: F = −G m₁ m₂ / r², always attractive, falling off as 1/r². The extended potential energy formula is just what you get when you integrate that force law over all possible separations, using infinity as the natural zero point.

The formula U(r) = −G m₁ m₂ / r has two features that initially surprise students. First, it is always negative. This is because gravity is attractive: to pull two masses apart from their natural tendency to fall together, you must add energy. Starting at infinity (U = 0), any finite separation is *below* the natural reference — you're in an energy well. The deeper you are (smaller r), the more negative U is, and the more energy you would need to supply to reach r = ∞. Second, it is inversely proportional to r (not r²): the *force* falls off as 1/r², but integrating that gives a 1/r potential. At twice the distance, the potential energy is halved in magnitude (U doubles toward zero), while the force is reduced to one-quarter.

The near-Earth approximation U = mgh is the limit of this formula for small height h above Earth's surface. If you expand −GMm/(R + h) around h = 0, the first correction is +GMmh/R² = mgh (since g = GM/R²). For h ≪ R, the approximation is excellent; for satellite orbits or interplanetary trajectories, you must use the full 1/r formula. The crossover happens roughly at heights comparable to Earth's radius (~6400 km).

The most powerful consequence is the energy classification of orbits. Total mechanical energy E = ½mv² − GMm/r is conserved (no friction, no thrust). If E < 0, the object is bound: it lacks enough kinetic energy to escape to infinity. The orbit is an ellipse (or circle), and the object endlessly returns. If E = 0, the object is on a parabolic escape trajectory — just barely able to reach infinity with zero velocity remaining. If E > 0, the orbit is hyperbolic — the object escapes with kinetic energy to spare. Escape velocity is simply the v that sets E = 0: v_esc = √(2GM/r). For Earth's surface, v_esc ≈ 11.2 km/s. The sign of total energy is the single most important quantity in orbital mechanics.

Practice Questions 5 questions

Prerequisite Chain

Understanding Zero → The Number Zero → Counting to Five → Counting to 10 → Counting to 20 → Counting a Set of Objects Up to 20 → Cardinality: The Last Number Counted → Matching Numerals to Quantities → Subitizing Small Quantities → Addition Within 10 → Number Bonds to 10 → Addition Within 20 → Doubles and Near Doubles → Doubles Facts Within 10 → Near Doubles Facts Within 20 → Mental Math Strategies for Addition → Mental Math: Adding and Subtracting Tens → Addition Within 100 → Repeated Addition as Multiplication → Multiplication as Equal Groups → Multiplication: Arrays → Basic Multiplication Facts (0s, 1s, 2s, 5s, 10s) → Multiplication Facts Within 100 → Division as Equal Sharing → Division as Grouping (Measurement Division) → Division: Grouping (Repeated Subtraction) Model → Division: Fair Sharing Model → Division as Equal Sharing → Division as Grouping → Basic Division Facts → Division Facts Within 100 → Multiplication and Division Fact Families → Relationship Between Multiplication and Division → Division Facts as Inverse of Multiplication → Remainders and Quotients in Division → Division Word Problems → Multi-Step Word Problems → Solving Multi-Step Word Problems → Multiplication Word Problems → Division Word Problems → Introduction to Long Division → Factors and Multiples → Prime and Composite Numbers → Equivalent Fractions → Relating Fractions and Decimals → Decimal Place Value → Integers and the Number Line → Comparing and Ordering Integers → Absolute Value → Adding Integers → Subtracting Integers → Multiplying Integers → Dividing Integers → Unit Rates → Proportions → Percent Concept → Converting Between Fractions, Decimals, and Percents → Operations with Rational Numbers → Two-Step Equations → Solving Multi-Step Equations → Equations with Variables on Both Sides → Angle Pairs: Complementary, Supplementary, and Vertical → Parallel Lines and Transversals → Corresponding Angles → Alternate Interior Angles → Triangle Angle Sum Theorem → Exterior Angle Theorem → Triangle Inequality Theorem → Similar Triangles: AA Similarity → Similar Triangles: SSS and SAS Similarity → Proportions in Similar Triangles → Right Triangle Trigonometry Introduction → Sine, Cosine, and Tangent Ratios → Trigonometric Ratios Review → Radian Measure → Converting Between Degrees and Radians → The Unit Circle → Graphing Sine and Cosine → Graphing Tangent and Reciprocal Trigonometric Functions → Derivatives of Trigonometric Functions → Antiderivatives → Indefinite Integrals → Basic Integration Rules → Riemann Sums → Definite Integral Definition → Double Integrals: Definition and Setup → Iterated Integrals and Fubini's Theorem → Double Integrals over Rectangular Regions → Double Integrals over General Regions → Applications of Double Integrals: Area, Mass, and Moments → Work Done by a Force → Potential Energy: Gravitational and Elastic → Gravitational Potential Energy (Extended)

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