advanced30 min studyLesson 55 in Physics

Einstein’s equations and the Newtonian limit

Relate matter to curvature, separate constraints from evolution, and recover Poisson’s equation in a controlled weak-field limit.

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What you’ll understand

  • Identify the geometric and matter terms in Einstein’s equation.
  • Explain how the Bianchi identity supports local stress conservation.
  • Recover Newtonian acceleration and Poisson’s equation in the appropriate limit.

The metric governs clocks, light cones, and free fall. Einstein’s equations add the missing rule: how matter and boundary or initial conditions determine that metric. Their compact notation hides a coupled nonlinear system with coordinate freedom and constraints. We will read the structure before taking a controlled limit in which familiar Newtonian gravity emerges, rather than assuming that a gravitational potential can be inserted into any relativistic formula unchanged.

A local field equation with consistency built in

Keep the earlier Riemann convention and (+,−,−,−)(+,-,-,-) signature. Define Gμν=Rμν−Rgμν/2G_{\mu\nu}=R_{\mu\nu}-Rg_{\mu\nu}/2. With zero cosmological constant, Einstein’s equation is Gμν=8πGTμν/c4G_{\mu\nu}=8\pi G T_{\mu\nu}/c^4. Curvature has units of inverse length squared, so the coupling converts energy density into the same units. The equation relates tensor components at one event, while its solutions depend on data across a region.

The contracted Bianchi identity gives ∇μGμν=0\nabla^\mu G_{\mu\nu}=0, making ∇μTμν=0\nabla^\mu T_{\mu\nu}=0 a consistency requirement. This is a local conservation statement, not an extra coordinate choice. A cosmological term proportional to the metric can also be included consistently because the metric’s covariant derivative vanishes. We set it to zero in this weak-field derivation; the cosmology lesson will state its positive-expansion convention separately to avoid signature-dependent ambiguity.

Gμν≡Rμν−12Rgμν=8πGc4Tμν,∇μGμν=0G_{\mu\nu}\equiv R_{\mu\nu}-\frac12Rg_{\mu\nu}=\frac{8\pi G}{c^4}T_{\mu\nu},\qquad \nabla^\mu G_{\mu\nu}=0
This displayed equation sets the cosmological term to zero. G without indices is Newton’s constant, whereas G with two indices is the Einstein tensor.↔ Scroll wide equations horizontally.

Weak, slow, and almost static are separate assumptions

For a weak static field with negligible anisotropic stress, use ds2≃(1+2Φ/c2)c2dt2−(1−2Φ/c2)dx2ds^2\simeq(1+2\Phi/c^2)c^2dt^2-(1-2\Phi/c^2)d\mathbf x^2. Small ∣Φ∣/c2|\Phi|/c^2 controls the metric expansion. A slowly moving test particle additionally has v/c≪1v/c\ll1, and a nearly stationary source lets us neglect time derivatives of the field. None of these assumptions follows automatically from either of the others.

The leading spatial geodesic equation becomes d2xi/dt2≃−c2Γ00i=−∂iΦd^2x^i/dt^2\simeq-c^2\Gamma^i_{00}=-\partial_i\Phi. For a pressureless source, T00≃ρc2T_{00}\simeq\rho c^2, where rho is rest-mass density. The leading time-time field equation then recovers ∇2Φ=4πGρ\nabla^2\Phi=4\pi G\rho. A relativistic fluid, fast-moving compact binary, or rapidly changing geometry requires terms discarded in this limit, so the recovery of Newtonian gravity is a consistency check with a stated domain.

Γ00i≃∂iΦc2,G00≃2∇2Φc2,∇2Φ=4πGρ\Gamma^i_{00}\simeq\frac{\partial_i\Phi}{c^2},\qquad G_{00}\simeq\frac{2\nabla^2\Phi}{c^2},\qquad \nabla^2\Phi=4\pi G\rho
Use x zero equal to ct and a spatially nearly Cartesian chart. The matter approximation neglects pressure compared with rest-energy density.↔ Scroll wide equations horizontally.

A solution needs more than a density profile

The metric has ten independent symmetric components in four dimensions, but coordinate freedom and differential identities mean they are not ten independent unconstrained wave equations. A spacelike initial slice carries geometric data that must satisfy constraint equations. A coordinate or gauge prescription then organizes the evolution. Giving an arbitrary density field without matter velocities, consistent geometric data, and boundary conditions does not uniquely specify a relativistic spacetime.

Even in Newtonian gravity, Poisson’s equation needs boundary conditions: adding a harmonic function changes the solution without changing the local density. In general relativity, gravitational waves can enter through initial or boundary data even in vacuum. “Matter tells spacetime how to curve” is therefore a useful mnemonic, provided it does not conceal free gravitational degrees of freedom or the role of global conditions. The next lessons study exact exterior geometry and propagating perturbations separately.

A uniform sphere in the weak-field limit

Consider a static sphere of uniform mass density ρ\rho in Newtonian weak-field gravity. Inside it, spherical symmetry gives (r2Φ′)′=4πGρr2(r^2\Phi')'=4\pi G\rho r^2. Find the acceleration at radius R when Gρ=0.03 s−2G\rho=0.03\,\mathrm{s^{-2}} and R=2 mR=2\,\mathrm m.

  1. Integrate from the center: r2Φ′=4πGρr3/3+Cr^2\Phi'=4\pi G\rho r^3/3+C. Regularity at the center sets C=0C=0, excluding a hidden point mass.

  2. Divide by r2r^2 to obtain Φ′=4πGρr/3\Phi'=4\pi G\rho r/3, so the radial acceleration is ar=−4πGρr/3a_r=-4\pi G\rho r/3.

  3. At R the magnitude is 4π(0.03)(2)/3=0.08π≃0.251 m s−24\pi(0.03)(2)/3=0.08\pi\simeq0.251\,\mathrm{m\,s^{-2}}. Its direction is inward; its linear dependence on r differs from the exterior inverse-square law.

The result

The center condition and density jointly determine the interior acceleration. Matching the potential to an exterior solution fixes its remaining additive constant once a reference at infinity is chosen.

Explore the model

Interactive lab

Interactive lab · fields

A field picture with explicit limits

Vary q and Ω in the softened planar source field q r/(r² + ε) + Ω(−y, x). Compare radial arrows with circulation and notice that a vector field contains direction information beyond a single scalar readout.

A field picture with explicit limitsThe softened illustration is q·r/(r² + 0.2) + Ω(−y, x). Moving markers indicate local direction, not integrated particle paths or a Maxwell solution. Current readings: Fx at (1, 0): 0.833; Fy at (1, 0): 0.5; Field magnitude there: 0.972. All parameters are adjustable with the labeled controls below.−3.2−1.601.63.2−1.5−0.7500.751.5xyq = 1
Local field directionSource strength
Fx at (1, 0)
0.833
Fy at (1, 0)
0.5
Field magnitude there
0.972
t = 0 s

The softened illustration is q·r/(r² + 0.2) + Ω(−y, x). Moving markers indicate local direction, not integrated particle paths or a Maxwell solution. Parameter changes pause playback and recompute the model at the current elapsed time. Reset restores both parameters and returns time to zero. Playback starts paused. Adjust either parameter, then choose Play or Step.

Look forThis model is neither a Newtonian inverse-square solution nor an Einstein-equation solver. Use it only as an analogy for inspecting a field, then apply the written equations for quantitative gravity.

Check your understanding

Which conditions support the Newtonian limit used in this lesson?

Try it yourself

Outside a spherical weak-field source, let Φ=−GM/r\Phi=-GM/r and GM/(Rc2)=10−6GM/(Rc^2)=10^{-6} at a chosen radius R. Find the leading g00g_{00} there and the inward acceleration in terms of c2/Rc^2/R.

Take a moment to make a prediction or work it out on paper. Open a hint when you need one.

Give me a hint

Use the coefficient of the time-time metric term and differentiate the potential; do not interpret the potential itself as an acceleration.

Compare with the solution

The metric coefficient is g00≃1+2Φ/c2=1−2×10−6=0.999998g_{00}\simeq1+2\Phi/c^2=1-2\times10^{-6}=0.999998. The inward acceleration magnitude is GM/R2=10−6c2/RGM/R^2=10^{-6}c^2/R. The potential is dimensionless only after division by c2c^2, whereas the acceleration contains another inverse length. The small potential controls the local metric expansion; a slow test-body speed is still a separate requirement for Newtonian motion.

Take it with you

  • Einstein’s equations couple tensorial curvature to energy, momentum, and stress.
  • Recovering Newtonian gravity requires several explicit approximations, not just a small test body.
  • Constraints, coordinate freedom, and boundary or initial data are part of a gravitational solution.

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