General Relativity

Einstein's Masterpiece: Gravity is the curvature of spacetime. Mass-energy tells spacetime how to curve, and spacetime tells mass-energy how to move.

Part III: Einstein Field Equations

Einstein's field equations relate the curvature of spacetime to the distribution of matter and energy. This is the core of general relativity: "Matter tells spacetime how to curve, and spacetime tells matter how to move."

Part Overview

The Einstein field equations are where is the Einstein tensor (geometry) and is the stress-energy tensor (matter/energy). These 10 coupled nonlinear partial differential equations determine how spacetime curves in response to matter. We derive them from the equivalence principle and the Einstein-Hilbert action, explore their limits, and learn to solve them.

Key Topics

  • • Equivalence principle: gravity = acceleration locally
  • • Einstein field equations:
  • • Stress-energy tensor: energy density, momentum density, stress
  • • Einstein-Hilbert action and variational derivation
  • • Weak field limit: recovering Newtonian gravity
  • • Post-Newtonian approximations and experimental tests

6 chapters | The heart of GR | From principle to equations

Chapters

Chapter 1: Equivalence Principle

The foundation of GR: locally, gravity is indistinguishable from acceleration. Weak equivalence principle (universality of free fall). Einstein's gedankenexperiment: the elevator. Why gravity must curve spacetime. Strong equivalence principle: all local physics is the same in freely falling frames. Experimental tests.

Equivalence PrincipleFree FallCurved Spacetime

Chapter 2: Einstein Field Equations

The field equations: where is the Einstein tensor and is the cosmological constant. Why this form? Consistency with energy-momentum conservation. Structure: 10 equations for 10 metric components, but gauge freedom reduces independent equations.

Field EquationsEinstein TensorCosmological Constant

Chapter 3: Stress-Energy Tensor

encodes energy density, momentum density, momentum flux, and stress. Perfect fluid: . Electromagnetic field: . Vacuum energy: . Conservation: .

Stress-EnergyPerfect FluidConservation

Chapter 4: Einstein-Hilbert Action

Deriving the field equations from the action principle. The Einstein-Hilbert action: . Varying with respect to the metric gives the field equations. The Gibbons-Hawking-York boundary term. Action principle unifies GR with quantum field theory formalism.

Action PrincipleVariational DerivationBoundary Terms

Chapter 5: Weak Field Limit

Linearized gravity: where . The linearized field equations become wave equations. Recovering Newtonian gravity: where . Gravitational waves as ripples in spacetime. Gauge choices: harmonic gauge, transverse-traceless gauge.

Weak FieldsLinearizationNewtonian Limit

Chapter 6: Newtonian Limit

The rigorous derivation of Newtonian gravity from GR. Assumptions: weak fields, slow velocities (), static sources. The geodesic equation reduces to . Post-Newtonian corrections: perihelion precession, light bending, Shapiro delay. Experimental verification of GR.

Newtonian GravityPost-NewtonianExperimental Tests

Course Navigation

Prerequisites: