General relativity §
General relativity (GR) is the geometric theory of gravity: mass-energy curves spacetime, and free bodies follow the straightest possible paths (geodesics) in that curved geometry. It is needed whenever gravity is strong ( not negligible), when precision matters (GPS time correction, pulsar timing), or when the source is not just matter but any stress-energy, including pressure, radiation, and the field’s own energy. It is the parent theory of every other page in the Gravity topic: Newtonian gravitation is its weak-field limit, and Gravitational waves, Compact objects, and Cosmological gravity are its radiative, strong-field stationary, and homogeneous-isotropic solution families.
Authoritative sources
The equivalence principle §
Definition. Locally, the effects of a gravitational field are indistinguishable from those of an accelerated frame: a freely falling body follows a path independent of its mass and composition, and in a small enough laboratory free fall feels like zero gravity.
Details
- Weak equivalence principle. Inertial mass equals gravitational mass, so all bodies fall with the same acceleration. Eötvös-type experiments verify this to . Newtonian gravity assumes it; GR builds the theory on it.
- Einstein equivalence principle. In a freely falling frame, all non-gravitational physics reduces to special relativity. Gravity is therefore not a force in the usual sense: it is the geometry that remains after you remove every local effect.
- Consequences. Gravitational time dilation: clocks deeper in a potential well run slow by . GPS satellites gain about 38 μs/day net (GR slows them by 45 μs/day at altitude, special relativity speeds them up by 7 μs/day from orbital speed); without correction, GPS positions would drift by kilometers per day.
Example. An astronaut in a windowless capsule in orbit floats because the capsule and the astronaut are both in free fall — the equivalence principle in action, not the absence of gravity.
The Einstein field equations §
Definition. Ten coupled nonlinear equations relating spacetime curvature to stress-energy:
Details
- Left side: geometry. is the metric (the machine that converts coordinate separations into proper times and distances); and are its curvatures. The Einstein tensor is divergence-free, automatically conserving energy-momentum.
- Right side: matter. packages density, momentum flux, pressure, and shear. Crucially, pressure gravitates: radiation-dominated matter () pulls three times harder than dust. This is why the early universe’s expansion decelerated faster, and why pressure can make collapse inevitable inside Compact objects.
- Nonlinearity. Gravity gravitates: the field’s own energy is a source. This makes exact solutions rare and is the technical root of why quantizing gravity is hard (see the Gravity overview).
- Weak-field limit. With , the field equations reduce to Poisson’s equation — Newton’s theory reappears, which is why the Newtonian page works so well on Earth.
Example. The Schwarzschild solution ( outside a spherical mass) yields light deflection of at impact parameter — twice the Newtonian prediction, confirmed by Eddington in 1919.
Geodesic motion and classic tests §
Definition. Free bodies follow geodesics of the metric; the three classical tests are perihelion precession, light deflection, and gravitational redshift.
Details
- Geodesic equation. , where (Christoffel symbols) encode how the coordinate basis twists and stretches. In the weak field this reduces to Newton’s plus small corrections.
- Perihelion precession. The relativistic correction to the orbit equation is per orbit — 43″/century for Mercury, and minutes of arc per orbit for binary pulsars.
- Gravitational redshift. Light climbing out of a potential well loses frequency: . Pound–Rebka (1959) measured it over a 22.5 m tower.
- Modern tests. Shapiro time delay, Gravity Probe B frame dragging, and Event Horizon Telescope shadow imaging all confirm GR in regimes spanning 15 orders of magnitude in field strength.
Example problem. How much slower does a clock run at Earth’s surface compared to far away?
Solution
.
Numerator: . Denominator: .
: a surface clock loses about 22 ms per year relative to a clock at infinity (partially offset by Earth’s rotation for a real observer).
Example problem §
Why does GPS need both special-relativistic and general-relativistic corrections?
How to solve it
Satellite clocks tick faster because they are higher in Earth’s gravitational potential (GR effect: , about +45 μs/day) but slower because they move at ~3.9 km/s (special relativity: , about −7 μs/day). The net is +38 μs/day, and since light travels ~300 m per μs, ignoring it would corrupt positions by ~11 km/day. Both effects are of the same order of magnitude (), so neither can be neglected.