Gravitational Potential Energy (Extended)

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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

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication 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 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-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 IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble 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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