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Gravitational Potential Energy (Extended)

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Newton's Law of Universal GravitationPotential Energy: Gravitational and Elastic+1 moreOrbital 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 ZeroThe Number ZeroCounting to FiveCounting to 10Counting to 20Counting a Set of Objects Up to 20Cardinality: The Last Number CountedMatching Numerals to QuantitiesSubitizing Small QuantitiesAddition Within 10Number Bonds to 10Addition Within 20Doubles and Near DoublesDoubles Facts Within 10Near Doubles Facts Within 20Mental Math Strategies for AdditionMental Math: Adding and Subtracting TensAddition Within 100Repeated Addition as MultiplicationMultiplication as Equal GroupsMultiplication: ArraysBasic Multiplication Facts (0s, 1s, 2s, 5s, 10s)Multiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Multiplication and Division Fact FamiliesRelationship Between Multiplication and DivisionDivision Facts as Inverse of MultiplicationRemainders and Quotients in DivisionDivision Word ProblemsMulti-Step Word ProblemsSolving Multi-Step Word ProblemsMultiplication Word ProblemsDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueIntegers and the Number LineComparing and Ordering IntegersAbsolute ValueAdding IntegersSubtracting IntegersMultiplying IntegersDividing IntegersUnit RatesProportionsPercent ConceptConverting Between Fractions, Decimals, and PercentsOperations with Rational NumbersTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionSine, Cosine, and Tangent RatiosTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIndefinite IntegralsBasic Integration RulesRiemann SumsDefinite Integral DefinitionDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsWork Done by a ForcePotential Energy: Gravitational and ElasticGravitational Potential Energy (Extended)

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