Part E · curved space · spine
Two covariant derivatives fail to commute, and the failure is a tensor. That tensor is what no change of coordinates can remove — and, component for component, it is unit 05's tidal tensor.
needs 32, 05~3½ h slides + 7 h problemsproblems: ./mr problems 33
33 · overview
$[\nabla_\mu,\nabla_\nu]$ is not zero, and is not a differential operator: it is multiplication by a tensor. That tensor is the Riemann curvature tensor.
Four symmetries cut $n^4$ components to $n^2(n^2-1)/12$: twenty in four dimensions, six in three, one in two.
The angle a vector turns through when carried round a loop, and — Gauss — a quantity no bending of the surface in space can alter.
Two freely falling particles accelerate apart at a rate that is curvature. In the Newtonian limit that rate is $\partial_i\partial_j\Phi$.
A dotted underline is a glossary term: click it. G lists every term, N opens the notes, where the long proofs live. The round sphere of radius $a$, solid-underlined like that, runs through all five sections; its octant triangle and two of its meridians do the work.
section 1
Second derivatives that refuse to commute, and the tensor that measures by how much.
33 · definition
Unit 32's normal coordinates at $p$ gave $g_{\mu\nu}(p) = \eta_{\mu\nu}$ and $\partial_\lambda g_{\mu\nu}(p) = 0$, hence $\Gamma^\rho_{\mu\nu}(p) = 0$ — and could not be pushed to the second derivatives. Count why:
Order by order in the Taylor expansion about $p$: the derivatives of $g$ to be set to their flat values (purple) against the coefficients a change of chart offers (orange). Enough at orders 0 and 1 — exactly enough at order 1 — and $20$ short at order 2.
At second order the chart runs out of freedom by $100 - 80 = 20$. Twenty numbers at each point cannot be set to zero, and this unit is about those twenty.
It says something survives; it does not say what, nor that the survivor is a tensor. Both have to be produced. The honest route is not to count but to find an operator that is manifestly coordinate-free and see what it contains.
The numbers: $g$ symmetric in $n=4$ gives $10$; its first derivatives $10\times4 = 40$; its seconds $10\times10 = 100$ using Clairaut in the two derivative slots. A chart change $x \mapsto x'$ has $4\times4 = 16$ first coefficients, $4\times10 = 40$ second, $4\times20 = 80$ third.
33 · definition
Mathematics first. Let $\nabla$ be unit 32's Levi-Civita connection on a manifold $M$, and let $\mathfrak X(M)$ be its vector fields.
$R : \mathfrak X(M)^3 \to \mathfrak X(M)$,
$$R(X,Y)Z := [\nabla_X,\nabla_Y]Z - \nabla_{[X,Y]}Z ,$$where $[\nabla_X,\nabla_Y]Z = \nabla_X\nabla_YZ - \nabla_Y\nabla_XZ$.
Every term is a vector field, so $R(X,Y)Z$ is one, with no coordinates anywhere. The bracket term is unit 31's Lie bracket, and it is there to remove the part of the failure that is merely the two flows not commuting.
"How much the surface bends in space" is not available: a spacetime sits in nothing. Any definition of curvature this course can use must be built from $g$ and $\nabla$ alone. Section 3 proves — Gauss — that nothing is lost.
The next slide draws what the commutator compares, and why the bracket term has to be there.
33 · definition
Unit 32 made $\nabla$ the derivative that compares a vector here with a vector transported from there. Carrying $Z$ along $X$ then $Y$, against $Y$ then $X$, compares two transports round the two sides of a parallelogram. The difference is the failure of parallel transport to be path-independent — which is what "curved" is supposed to mean.
If the flows of $X$ and $Y$ do not commute, the two routes do not even end at the same point: the gap is $[X,Y]$, and part of the mismatch in $Z$ is just $Z$ changing across that gap. The term $-\nabla_{[X,Y]}Z$ subtracts exactly that part.
Two routes from $p$, each with $Z$ carried along it. They end a gap $[X,Y]$ apart (exaggerated here), and the two carried copies of $Z$ disagree. Close the gap and what remains of the disagreement is $R(X,Y)Z$, times the area enclosed.
33 · definition
$R(X,Y)Z$ is $C^\infty(M)$-linear in each of $X$, $Y$, $Z$: for every smooth $f$, $R(fX,Y)Z = R(X,fY)Z = R(X,Y)(fZ) = f\,R(X,Y)Z$. Hence $R$ is a $(1,3)$-tensor field: its value at $p$ depends on $X,Y,Z$ only through $X_p, Y_p, Z_p$.
$\nabla_X\nabla_Y(fZ) = \nabla_X\big(f\nabla_YZ + (Yf)Z\big)$ $= f\nabla_X\nabla_YZ + (Xf)\nabla_YZ + (Yf)\nabla_XZ + (XYf)Z$.
Subtract the same with $X \leftrightarrow Y$: the two middle terms are symmetric and cancel, leaving $f[\nabla_X,\nabla_Y]Z + (XYf - YXf)Z$. And $XYf - YXf = [X,Y]f$, which is exactly what $-\nabla_{[X,Y]}(fZ)$ subtracts. $\square$
$\nabla_XZ$ alone is not $C^\infty$-linear in $Z$ — the Leibniz term $(Xf)Z$ is the whole point of a connection. Only in the antisymmetrised pair does it cancel. Curvature is a second derivative of the metric that behaves like a tensor, and nothing weaker does.
full proof in the notes — the $X$ and $Y$ slots, and the lemma that turns $C^\infty$-linearity into pointwise dependence.
33 · components
Take $X = \partial_\mu$, $Y = \partial_\nu$ — coordinate fields, so $[X,Y] = 0$ and the bracket term drops. Writing $R(\partial_\mu,\partial_\nu)\partial_\sigma = R^\rho{}_{\sigma\mu\nu}\,\partial_\rho$ defines the components, and expanding gives
Equivalently, acting on any vector field — the Ricci identity:
Read $\partial\Gamma - \partial\Gamma + \Gamma\Gamma - \Gamma\Gamma$ with the last two lower slots antisymmetrised, and the differentiated $\Gamma$ carrying the other two. It is a mnemonic for these conventions only: swap any sign convention of unit 32 and it changes.
On a function, $[\nabla_\mu,\nabla_\nu]f = \nabla_\mu\partial_\nu f - \nabla_\nu\partial_\mu f = -(\Gamma^\lambda_{\mu\nu}-\Gamma^\lambda_{\nu\mu})\partial_\lambda f = 0$: torsion-free means scalars never see curvature. Curvature needs something with an index to rotate.
33 · example
On $S^2_a$, unit 32's Christoffel symbols are $\Gamma^\theta_{\phi\phi} = -\sin\theta\cos\theta$ and $\Gamma^\phi_{\theta\phi} = \Gamma^\phi_{\phi\theta} = \cot\theta$; every other one vanishes. Compute $R^\theta{}_{\phi\theta\phi}$, taking $\rho = \theta$, $\sigma = \phi$, $\mu = \theta$, $\nu = \phi$:
$$R^\theta{}_{\phi\theta\phi} = \underbrace{\partial_\theta\Gamma^\theta_{\phi\phi}}_{\text{(i)}} - \underbrace{\partial_\phi\Gamma^\theta_{\theta\phi}}_{\text{(ii)}} + \underbrace{\Gamma^\theta_{\theta\lambda}\Gamma^\lambda_{\phi\phi}}_{\text{(iii)}} - \underbrace{\Gamma^\theta_{\phi\lambda}\Gamma^\lambda_{\theta\phi}}_{\text{(iv)}}$$(i) $\partial_\theta(-\sin\theta\cos\theta) = \sin^2\theta - \cos^2\theta$. (ii) $\Gamma^\theta_{\theta\phi} = 0$, so this is $0$. (iii) $\Gamma^\theta_{\theta\lambda} = 0$ for both $\lambda$, so this is $0$. (iv) the only surviving $\lambda$ is $\phi$: $\Gamma^\theta_{\phi\phi}\Gamma^\phi_{\theta\phi} = (-\sin\theta\cos\theta)(\cot\theta) = -\cos^2\theta$.
$$R^\theta{}_{\phi\theta\phi} = \sin^2\theta - \cos^2\theta - 0 + 0 + \cos^2\theta = \sin^2\theta$$Lower the first index: $R_{\theta\phi\theta\phi} = g_{\theta\theta}R^\theta{}_{\phi\theta\phi} = a^2\sin^2\theta$.
Dimensions. $[R_{\theta\phi\theta\phi}] = \mathrm L^2$ because $\theta,\phi$ are angles; the invariant $R_{\theta\phi\theta\phi}/(g_{\theta\theta}g_{\phi\phi}) = 1/a^2$ has $\mathrm L^{-2}$ ✓ — curvature is an inverse area.
Limit $a\to\infty$. $1/a^2 \to 0$: a sphere of huge radius is locally flat ✓. Limit $\theta\to0$. $R_{\theta\phi\theta\phi}\to0$, but so does $g_{\phi\phi}$; the ratio stays $1/a^2$ ✓ — the pole is a coordinate singularity, not a curvature one, exactly as unit 31 warned.
$n = 2$ gives $2^4 = 16$ components, and we computed one. Section 2 proves that in two dimensions all sixteen are determined by that one — so this is the curvature of the sphere, finished.
33 · transport
Parallel-transport $V$ round the coordinate parallelogram with edges $\delta a^\mu$ and $\delta b^\nu$ — along $\delta a$, then $\delta b$, then back. The vector returns changed by
$$\Delta V^\rho = -R^\rho{}_{\sigma\mu\nu}\,V^\sigma\,\delta a^\mu\,\delta b^\nu + O(\delta^3) .$$So curvature is not merely like path-dependence of transport: it is its leading coefficient, per unit coordinate area. A vanishing $R$ makes transport path-independent on a simply connected region (cited in the notes), and a vector field defined by transporting from one point is then well defined — which is what "flat" means.
$\delta a^\mu\delta b^\nu$ enters only through its antisymmetric part, $R$ being antisymmetric in $\mu\nu$. Curvature is indexed by planes: it answers "go round this two-dimensional loop", never "go in this direction".
Out along $\delta a$, along $\delta b$, back and back, carrying $V$ the whole way (the turn is exaggerated). The mismatch $\Delta V$ on return is proportional to the enclosed area $\delta a\wedge\delta b$: halve both edges and it drops by four.
33 · transport
On an oriented surface, parallel transport once round the positively oriented boundary of a region $S$ that is a topological disc rotates every tangent vector by the same angle
$$\Delta\alpha = \int_S K\,\mathrm dA ,$$where $K := R_{1212}/\det g$ is the Gaussian curvature. Worked example 1 found it on the sphere: $R_{\theta\phi\theta\phi}/(g_{\theta\theta}g_{\phi\phi}) = 1/a^2$. Section 3 proves it is chart-independent and is the surface's whole curvature.
Additivity does the rest: a big region is a union of small ones, each turning $V$ by $K\,\delta A$ (the previous slide), and the internal edges are traversed twice in opposite senses and cancel.
Cut $S$ into small cells and go round each one anticlockwise. Every inner edge is walked once each way, so its contributions cancel; what survives is one trip round the boundary $\partial S$, with $S$ on the left.
33 · transport
Metric compatibility (unit 32) says transport preserves $g$, so the holonomy of a loop is an isometry of the tangent plane fixing the origin: an element of $\mathrm O(2)$. Transport along the loop up to time $t$ has a determinant, measured in oriented bases, that is continuous in $t$, equal to $\pm1$, and $1$ at $t=0$; so it stays $1$, and the holonomy lies in $\mathrm{SO}(2)$ — a rotation, by an angle.
Reverse the loop and $\Delta\alpha$ changes sign. "Positively oriented boundary" means the region is on the left. Get this wrong and a sphere appears to have negative curvature.
So all a surface's holonomy can say about a loop is one signed angle, the same for every vector carried round it.
33 · example
Take $a = 1$ and embed to keep the bookkeeping honest: $A = (1,0,0)$, $B = (0,1,0)$ on the equator, $N = (0,0,1)$. Traverse the octant $A\to B\to N\to A$, which is positively oriented. Start with $V = \hat y$ at $A$ — due east. On a great circle the travel direction is itself parallel-transported, and transport preserves the angle to it; that is all we need.
Leg $A\to B$ (equator, a geodesic). $V = \hat y$ is the travel direction, so it stays tangent: at $B$ the travel direction is $-\hat x$, so $V = -\hat x$.
Leg $B\to N$ (meridian $\phi = \tfrac\pi2$, in the $yz$-plane). Travel direction at $B$ is $\hat z$; $V = -\hat x$ is perpendicular to it and perpendicular to the plane of the great circle, so it is unmoved along the whole leg. At $N$, $V = -\hat x$.
Leg $N\to A$ (meridian $\phi = 0$, in the $xz$-plane). Travel direction at $N$ is $+\hat x$, so $V = -\hat x$ is anti-parallel to it and stays so. At $A$ the travel direction is $-\hat z$, hence $V = +\hat z$ — due north.
Schematic. Flat paper cannot hold a triangle with three right angles unless its sides bend — here by $30^\circ$ each. Along each side $V$ keeps its angle to the side, exactly the rule used on the sphere, so it turns with the sides: $3\times30^\circ = 90^\circ$, east to north.
33 · example
Holonomy. East $\to$ north is a rotation by $+\pi/2$ in the outward-normal orientation ✓.
Integral. $\displaystyle\int_\triangle K\,\mathrm dA = \frac{1}{a^2}\cdot\frac{4\pi a^2}{8} = \frac{\pi}{2}$ ✓. Independent of $a$, as the angle must be.
Angle excess. Three right angles: $\tfrac{3\pi}{2}-\pi = \tfrac\pi2$ ✓, the same number a third way.
Gauss's own survey triangle, Hoher Hagen–Brocken–Inselsberg, sides $69$, $85$, $107$ km, area $2929\ \mathrm{km^2}$: excess $A/R_\oplus^2 = 7.22\times10^{-5}$ rad $= 14.9''$. Small, and larger than his instruments' error.
The octant's excess is $\pi/2$ on a sphere of any radius; Gauss's triangle has $14.9''$ only because it covers $2929/(4\pi R_\oplus^2)$ of the Earth, about $5.7\times10^{-6}$ of it. Excess is $K$ times area.
section 2
Four symmetries, one count, and the two identities that everything later leans on.
33 · symmetries
Work with all indices down, $R_{\rho\sigma\mu\nu} = g_{\rho\lambda}R^\lambda{}_{\sigma\mu\nu}$.
S1 $\;R_{\rho\sigma\mu\nu} = -R_{\rho\sigma\nu\mu}$
S2 $\;R_{\rho\sigma\mu\nu} = -R_{\sigma\rho\mu\nu}$
S3 $\;R_{\rho[\sigma\mu\nu]} = 0$, the first Bianchi identity
S4 $\;R_{\rho\sigma\mu\nu} = R_{\mu\nu\rho\sigma}$, pair symmetry
S1 is the definition ($R(X,Y) = -R(Y,X)$). S4 is not independent: it follows from S1–S3.
Apply the Ricci identity to the metric itself. For a $(0,2)$-tensor, $[\nabla_\mu,\nabla_\nu]T_{\rho\sigma} = -R^\lambda{}_{\rho\mu\nu}T_{\lambda\sigma} - R^\lambda{}_{\sigma\mu\nu}T_{\rho\lambda}$. Put $T = g$. Metric compatibility gives $\nabla g = 0$, so the left side is zero: $$0 = -R_{\sigma\rho\mu\nu} - R_{\rho\sigma\mu\nu} . \;\square$$
S1 and S3 hold for any torsion-free connection. S2 needs $\nabla g = 0$ — so a connection that is not metric has a curvature with more independent components than the counting theorem allows.
33 · symmetries
Both sides of S3 are tensors, so it is enough to prove it at one arbitrary point $p$ in one chart. Choose unit 32's normal coordinates at $p$, where $\Gamma^\rho_{\mu\nu}(p) = 0$ but $\partial\Gamma(p)$ need not vanish. There the $\Gamma\Gamma$ terms drop and
$$R^\rho{}_{\sigma\mu\nu}\big|_p = \partial_\mu\Gamma^\rho_{\nu\sigma} - \partial_\nu\Gamma^\rho_{\mu\sigma}.$$Sum cyclically over $(\sigma,\mu,\nu)$:
$$\begin{aligned}&\big(\partial_\mu\Gamma^\rho_{\nu\sigma} - \partial_\nu\Gamma^\rho_{\mu\sigma}\big) + \big(\partial_\nu\Gamma^\rho_{\sigma\mu} - \partial_\sigma\Gamma^\rho_{\nu\mu}\big)\\ &\quad + \big(\partial_\sigma\Gamma^\rho_{\mu\nu} - \partial_\mu\Gamma^\rho_{\sigma\nu}\big) = 0,\end{aligned}$$every term cancelling its partner because $\Gamma^\rho_{\mu\nu} = \Gamma^\rho_{\nu\mu}$ — torsion-freeness, and nothing else. $\square$
"Tensor equation, so prove it in normal coordinates at a point" is the standard move and it is valid: if two tensors agree at $p$ in one basis they agree at $p$ in every basis, and $p$ was arbitrary. It will prove the second Bianchi identity in the same three lines.
Only for equations between tensors. Setting $\Gamma(p) = 0$ inside an expression that is not tensorial — $\partial_\mu\Gamma$ on its own, say — proves nothing, because the conclusion would not transport to another chart.
33 · symmetries
Write the cyclic identity S3 four times, once with each of $\rho,\sigma,\mu,\nu$ held in the first slot; add two of them and subtract the other two. Terms cancel in pairs by S1 and S2, and what survives, after relabelling, is
$$2R_{\rho\sigma\mu\nu} - 2R_{\mu\nu\rho\sigma} = 0 .$$full proof in the notes — the bookkeeping is the whole content, and it is worth doing once.
Think of $R$ as a map $\Lambda^2 \times \Lambda^2 \to \mathbb R$, eating two planes: $R(u\wedge v,\,x\wedge y) := R_{\rho\sigma\mu\nu}u^\rho v^\sigma x^\mu y^\nu$. S1 and S2 say it is well defined on planes; S4 says it is symmetric in them. Curvature is a symmetric bilinear form on the space of planes — which is the sentence the counting theorem turns into a number.
$\Lambda^2$ here just means antisymmetric pairs, written $u\wedge v$; unit 34 gives the wedge its algebra. Nothing on this slide needs more than the index pattern.
33 · counting
In $n$ dimensions, a tensor with S1–S4 has exactly
$$\frac{n^2(n^2-1)}{12}$$independent components.
Let $N = \binom n2 = \tfrac{n(n-1)}2$ be the number of index pairs $[\rho\sigma]$. By S1, S2 and S4, $R$ is a symmetric bilinear form on an $N$-dimensional space: $\tfrac{N(N+1)}2$ numbers. Given those, S3 says exactly that the totally antisymmetric part $R_{[\rho\sigma\mu\nu]}$ vanishes, and every totally antisymmetric tensor occurs as such a part, so S3 removes exactly $\binom n4$:
$$\frac{N(N+1)}{2} - \binom{n}{4} = \frac{n^2(n^2-1)}{12}. \;\square$$The algebra, and why S3 is exactly $\binom n4$ conditions, are in the notes.
$n = 4$, so $N = 6$ index pairs. S1 and S2 make $R$ a $6\times6$ matrix indexed by pairs, S4 makes it symmetric: $21$ entries. S3 is then a single linear relation, tying the three entries whose pairs share no index.
33 · counting
| $n$ | $\tfrac{N(N+1)}2$ | Riemann | Ricci | Weyl |
|---|---|---|---|---|
| 2 | 1 | 1 | — | — |
| 3 | 6 | 6 | 6 | 0 |
| 4 | 21 | 20 | 10 | 10 |
| 5 | 55 | 50 | 15 | 35 |
The last two columns look ahead to section 5. Ricci is the one trace of Riemann, a symmetric tensor with $\tfrac{n(n+1)}2$ components; Weyl is the part of Riemann the trace does not see, so its count is Riemann minus Ricci.
Twenty in four dimensions — the same twenty the chart-counting slide could not remove. Two arguments with nothing in common, one answer.
$n^2(n^2-1)/12$ grows like $n^4$: one number at $n = 2$, where the sphere has lived so far, and twenty at $n = 4$. Pictures from surfaces carry over plane by plane — section 3 — but never all at once.
33 · counting
Lowered and with S4, equivalently $\nabla_{[\lambda}R_{\rho\sigma]\mu\nu} = 0$.
Both sides are tensors; work at $p$ in normal coordinates, where $\Gamma(p) = 0$, so $\nabla_\lambda$ acting on $R$ at $p$ is $\partial_\lambda$, and the $\Gamma\Gamma$ terms in $R$ contribute nothing to a single derivative at $p$ (each is a product of two factors, one of which vanishes). Hence at $p$
$$\nabla_\lambda R^\rho{}_{\sigma\mu\nu} = \partial_\lambda\partial_\mu\Gamma^\rho_{\nu\sigma} - \partial_\lambda\partial_\nu\Gamma^\rho_{\mu\sigma} .$$Sum cyclically over $(\lambda,\mu,\nu)$: six terms, which cancel in pairs because partial derivatives commute (Clairaut, unit 03). $\square$
S1–S4 are algebra at a point; the second Bianchi identity is the only differential constraint, and it is not optional or approximate — it holds for every metric whatsoever. Contract it twice and it says $\nabla^\mu G_{\mu\nu} = 0$ identically, which is section 5, and which is why unit 35's field equation can be consistent with $\nabla^\mu T_{\mu\nu} = 0$.
The derivative index cycles with one antisymmetric pair — either one, by S4. Cycling it with one index from each pair gives a false statement.
section 3
Sectional curvature, Gauss's theorem, and why no flat map of the Earth is possible.
33 · sectional
For a plane $\Pi \subset T_pM$ spanned by independent $X, Y$,
$$K(\Pi) = \frac{R_{\rho\sigma\mu\nu}X^\rho Y^\sigma X^\mu Y^\nu}{\;|X|^2|Y|^2 - \langle X,Y\rangle^2\;} .$$The denominator is the squared area of the parallelogram on $X,Y$ (Gram determinant), positive whenever $X,Y$ are independent and $\Pi$ is spacelike. Under a change of basis of $\Pi$ both numerator and denominator are multiplied by the square of its determinant, so $K$ depends on $\Pi$ alone.
The sectional curvatures of all planes determine $R$ completely — a polarisation argument, like recovering a symmetric bilinear form from its quadratic form. So "curvature" can be thought of as a function on planes, which is how Riemann thought of it and how a physicist should picture it.
The next slide: what happens when every plane at every point gives the same number.
33 · sectional
If $K(\Pi) = K$ for all $\Pi$ at all points, then $R_{\rho\sigma\mu\nu} = K\,(g_{\rho\mu}g_{\sigma\nu} - g_{\rho\nu}g_{\sigma\mu})$, the only tensor with S1–S4 built from $g$ alone. The sphere, hyperbolic space and flat space are the model cases; unit 39 needs this for cosmology.
Schematic. One geodesic triangle on each model surface. Its angle excess is $\int K\,\mathrm dA$ — the transport theorem of section 1 — so its sign is the sign of $K$; and the same sign decides whether geodesics that start parallel close up or spread, as section 4 will show.
33 · sectional
A surface has a single tangent plane at each point, so a single sectional curvature — a function, the Gaussian curvature $K(p)$. Consistently with the counting theorem's answer of $1$:
full proof in the notes; problem P2 does it again with the indices out.
$R_{\theta\phi\theta\phi} = a^2\sin^2\theta$, $\det g = a^4\sin^2\theta$, so $K = 1/a^2$ ✓ — and $K$ is the same at every point, including where $\sin\theta$ is nearly zero.
For a conformally flat surface metric $g = e^{2\varphi}(\mathrm dx^2+\mathrm dy^2)$,
$$K = -e^{-2\varphi}\,\Delta\varphi,$$with $\Delta = \partial_x^2+\partial_y^2$ the flat Laplacian.
Every surface metric is locally of this form (isothermal coordinates, cited), so this computes any $K$ with no Christoffel symbols at all.
Stereographic: $e^{2\varphi} = 4a^2/(1+r^2)^2$, $r^2 = u^2+v^2$, so $\varphi = \ln(2a) - \ln(1+r^2)$ and $\Delta\varphi = -\tfrac1r\partial_r\!\big(\tfrac{2r^2}{1+r^2}\big) = -\tfrac{4}{(1+r^2)^2}$. Hence $K = \tfrac{(1+r^2)^2}{4a^2}\cdot\tfrac{4}{(1+r^2)^2} = \tfrac{1}{a^2}$ ✓.
33 · intrinsic
For a surface $\Sigma \subset \mathbb R^3$, the product of the principal curvatures $\kappa_1\kappa_2$ — defined by how $\Sigma$ bends in space — equals the Gaussian curvature $K$ computed from the induced metric alone. Hence $K$ is intrinsic: it is unchanged by any bending that does not stretch.
Cited: the equality $\det(\mathrm{II}) = R_{1212}$ is Gauss's equation, proved in do Carmo, Curves and Surfaces, §4-3. It needs the second fundamental form, which this course does not build — it has no use for a surrounding space.
If $F : (M,g) \to (M',g')$ is an isometry, then $K' \circ F = K$. Immediate: $K$ was defined from $R$, $R$ from $\nabla$, $\nabla$ from $g$ — and $F^*g' = g$ carries each construction to the next. $\square$
No region of the sphere is isometric to any region of the plane, because $1/a^2 \ne 0$. Every flat map of the Earth distorts lengths — not through the cartographer's incompetence but because $K$ is an invariant. Mercator preserves angles and ruins areas; Peters preserves areas and ruins shapes; nothing preserves both.
33 · example
The cylinder of radius $a$, with coordinates $z$ along the axis and angle $\phi$ round it, has $g = \mathrm dz^2 + a^2\mathrm d\phi^2$.
Every component is constant, so every $\partial g = 0$, every $\Gamma$ vanishes, and $R = 0$: $K = 0$ everywhere.
Yet the cylinder is visibly bent in $\mathbb R^3$: round it the principal curvature is $\kappa_1 = 1/a$, along it $\kappa_2 = 0$. Product zero ✓, as Gauss says it must be.
A sheet of paper rolls into a cylinder without tearing; it will not wrap a ball.
Rolling the sheet bends it in space but stretches nothing, so every length and angle drawn on it survives: the triangle still has angle sum $\pi$. Bending in one direction only — one principal curvature zero — is what makes that possible.
section 4
Two freely falling particles, and the equation that says curvature is the tidal force.
33 · deviation
Let $\gamma(\tau, s)$ be a smooth one-parameter family of geodesics: for each fixed $s$, $\tau \mapsto \gamma(\tau,s)$ is a geodesic with affine parameter $\tau$. Put
$$u = \frac{\partial\gamma}{\partial\tau}, \qquad \xi = \frac{\partial\gamma}{\partial s} .$$$\xi$ points from one geodesic to its neighbour. $u$ and $\xi$ are coordinate fields of the chart $(\tau,s)$ on the surface swept out, so $[u,\xi] = 0$ — unit 31's statement that coordinate fields commute. Torsion-freeness then gives $\nabla_u\xi = \nabla_\xi u$.
Both facts are used once each, in the proof of the geodesic deviation equation, and nothing else is needed.
The family as a chart on the surface it sweeps: geodesics are the lines of constant $s$, and $u$ and $\xi$ are the two coordinate directions. Each small cell of the $(\tau, s)$ grid closes up — the shaded one, for instance — and that is $[u,\xi] = 0$.
33 · deviation
There is no such thing without a convention: the two worldlines are not at the same time in any absolute sense. $\xi$ is defined by the family, and it is a genuine vector field along each geodesic. What is physical is $\xi$ measured in the freely falling observer's own orthonormal frame — which is what the Newtonian limit will make explicit.
The freedom to reparametrise $s$ rescales $\xi$; the freedom to shift $\tau$ by a function of $s$ adds a multiple of $u$ to $\xi$. Neither changes anything that follows, because $R$ is antisymmetric in the relevant slots.
Shifting where each neighbour's clock starts joins my point to a different point of the same neighbour's worldline: $\xi$ becomes $\xi + f\,u$. The curvature term cannot tell the difference, since $R(u,u) = 0$.
33 · deviation
where $\mathrm D/\mathrm d\tau = \nabla_u$ is unit 32's covariant derivative along the curve.
$\nabla_u\nabla_u\xi = \nabla_u\nabla_\xi u$ (torsion-free, with $[u,\xi] = 0$)
$\phantom{\nabla_u\nabla_u\xi} = \nabla_\xi\nabla_u u + R(u,\xi)u$ (definition of $R$, with $[u,\xi]=0$)
$\phantom{\nabla_u\nabla_u\xi} = R(u,\xi)u$ (each curve is a geodesic: $\nabla_uu = 0$)
and $R(u,\xi)u$ has components $R^\rho{}_{\sigma\mu\nu}u^\sigma u^\mu\xi^\nu = -R^\rho{}_{\sigma\mu\nu}u^\sigma\xi^\mu u^\nu$ by S1. $\square$
No first derivative of the metric, no $\Gamma$, no acceleration, no force. Both particles are in free fall and feel nothing; the only thing that appears is curvature. If $R = 0$ the separation is linear in $\tau$ — Euclid's parallel postulate, as a differential equation.
Dimensions. $[\mathrm D^2\xi/\mathrm d\tau^2] = \mathrm{L\,T^{-2}}$; $[R]=\mathrm L^{-2}$, $[u] = \mathrm{L\,T^{-1}}$, so the right side is $\mathrm{L^{-2}}\cdot\mathrm L\cdot\mathrm{L^2T^{-2}} = \mathrm{L\,T^{-2}}$ ✓.
Special case $\xi \parallel u$: right side vanishes by S1 ✓ — no relative acceleration along the direction of motion, as it must be.
33 · example
On $S^2_a$, the meridians $\gamma(s,\phi_0)$ run north from the equator, $s$ arc length, $\phi_0$ the family parameter: $u = \partial_s$, $\xi = \Delta\phi\,\partial_{\phi_0}$ for two of them $\Delta\phi$ apart.
In two dimensions $R_{\rho\sigma\mu\nu} = K(g_{\rho\mu}g_{\sigma\nu} - g_{\rho\nu}g_{\sigma\mu})$. Take $\xi \perp u$ and write $\xi$ for the length of $\xi$. Then
$$-R^\rho{}_{\sigma\mu\nu}u^\sigma\xi^\mu u^\nu = -K\big(\xi^\rho (u\!\cdot\!u) - u^\rho(u\!\cdot\!\xi)\big) = -K\,\xi^\rho$$using $u\cdot u = 1$ (arc length) and $u\cdot\xi = 0$. Hence
$$\xi'' = -K\xi = -\frac{\xi}{a^2}, \qquad \xi(s) = a\,\Delta\phi\,\cos(s/a),$$taking $\xi(0) = a\,\Delta\phi$ at the equator and $\xi'(0) = 0$ (the meridians leave parallel).
Two meridians $\Delta\phi$ apart (exaggerated), drawn from the equator. They leave it parallel, never turn, and the gap between them shrinks as $\cos(s/a)$ until they meet at the pole.
33 · example
$\xi$ vanishes at $s = \pi a/2$: a quarter of a great circle, the pole. Two paths that start parallel, never turn, and meet. That is a tidal force, with no force in it.
Direct check: at colatitude $\theta$ the separation is $a\sin\theta\,\Delta\phi$, and $s = a(\tfrac\pi2-\theta)$, so $a\sin\theta = a\cos(s/a)$ ✓ — the ODE reproduces plane trigonometry on the sphere.
Limit $a\to\infty$: $\xi \to a\Delta\phi$, constant — parallel lines stay parallel ✓. Dimensions: $[K] = \mathrm L^{-2}$, $[\xi''] = \mathrm{L^{-1}}$ ✓.
On the Earth, meridians $1$ km apart at the equator are $1000\cos 45^\circ = 707$ m apart at latitude $45^\circ$. A flat map says $1000$ m.
The same equation $\xi'' = -K\xi$ for three signs of $K$, all starting parallel. Positive $K$ closes the gap ($0.707$ at latitude $45^\circ$, zero at the pole); zero keeps it; negative $K$ opens it exponentially.
33 · Newton
Unit 32 fixed the weak, static, slow-motion regime: with $x^0 = ct$,
$$g_{00} = -\Big(1 + \frac{2\Phi}{c^2}\Big), \qquad g_{ij} = \delta_{ij}, \qquad g_{0i} = 0,$$with $|\Phi|/c^2 \ll 1$ and $\partial_t \Phi= 0$, and showed the geodesic equation becomes $\ddot{\vec x} = -\nabla\Phi$. The only Christoffel symbol that survives at this order is
$$\Gamma^i_{00} = -\tfrac12 g^{ij}\partial_j g_{00} = \frac{1}{c^2}\,\partial_i\Phi .$$A freely falling observer has $u^\mu \approx (c, \vec v)$ with $|\vec v| \ll c$, so $u^0 \approx c$ dominates, and $\mathrm d\tau \approx \mathrm dt$.
$\partial_i\Phi$ means $\partial\Phi/\partial x^i$ with $x^i$ a length, while $\partial_0 = c^{-1}\partial_t$. Keeping $c$ explicit in every step is tedious and is the only way the factors come out right; the identification on the next slide is worthless with a stray $c^2$.
Unit 05 derived, from Newton alone, $\ddot\xi_i = -(\partial_i\partial_j\Phi)\,\xi_j$ — the tidal deviation equation. The geodesic deviation equation must reduce to exactly that, or the whole construction is wrong.
33 · example
Step 1 — the component. To first order in $\Phi/c^2$ the $\Gamma\Gamma$ terms are second order and drop:
$$R^i{}_{0j0} = \partial_j\Gamma^i_{00} - \partial_0\Gamma^i_{j0} = \partial_j\Big(\frac{\partial_i\Phi}{c^2}\Big) - 0 = \frac{\partial_i\partial_j\Phi}{c^2}.$$($\Gamma^i_{j0}$ vanishes for a static field, and $\partial_0$ of anything static is zero.)
Step 2 — the deviation equation. With $u^\mu \approx (c,\vec 0)$ and $\xi^\mu \approx (0,\vec\xi)$, only $\sigma = \nu = 0$ and $\mu = j$ survive:
$$\begin{aligned}\frac{\mathrm D^2\xi^i}{\mathrm d\tau^2} &= -R^i{}_{0j0}\,u^0\xi^j u^0 = -c^2\cdot\frac{\partial_i\partial_j\Phi}{c^2}\,\xi^j\\ &= -\big(\partial_i\partial_j\Phi\big)\xi^j .\end{aligned}$$Step 3 — compare. The left side is $\ddot\xi_i$ at this order. This is unit 05's equation, character for character.
Dimensions: $[\partial_i\partial_j\Phi] = \mathrm{T^{-2}}$, over $c^2$ gives $\mathrm L^{-2}$ ✓ — curvature is an inverse area, and the conversion factor is $c^2$.
Trace: $R^i{}_{0i0} = \nabla^2\Phi/c^2 = 4\pi G\rho/c^2$, zero in vacuum ✓ — the trace-free tidal tensor of unit 05, and the seed of unit 35's field equation.
Limit $\Phi \to$ const: no tidal field, $R^i{}_{0j0} = 0$ ✓ — a uniform gravitational field is no curvature at all, which is unit 30's equivalence principle.
33 · example
$$\boxed{\;R^i{}_{0j0} = \frac{\partial_i\partial_j\Phi}{c^2}\;}$$
For a point mass, $\partial_i\partial_j\Phi = \tfrac{GM}{r^3}(\delta_{ij}-3n_in_j)$: eigenvalues $(-2,1,1)\,GM/(c^2r^3)$, stretch along $\hat n$, squeeze across. The two tidal bulges of unit 05 are two components of the Riemann tensor.
Relative acceleration is $\ddot\xi_i = -c^2R^i{}_{0j0}\,\xi^j$: along $\hat n$, $+2GM/r^3$ times the offset, outward; across, $GM/r^3$ times it, inward.
A ring of particles falling freely with an observer, a mass $M$ off to the left. Each arrow is $-c^2R^i{}_{0j0}\xi^j$ at that particle: twice as long outward along $\hat n$ as inward across it. Left alone, the ring becomes the ellipse (exaggerated) — the two tidal bulges.
33 · Newton
| unit 05, Newton | unit 33, geometry |
|---|---|
| $\ddot\xi_i = -(\partial_i\partial_j\Phi)\xi_j$ | $\mathrm D^2\xi^\rho/\mathrm d\tau^2 = -R^\rho{}_{\sigma\mu\nu}u^\sigma\xi^\mu u^\nu$ |
| $T_{ij} = \partial_i\partial_j\Phi$ | $c^2R^i{}_{0j0}$ |
| $\operatorname{tr}T = 4\pi G\rho$ | $c^2R_{00}$, and hence unit 35 |
| trace-free in vacuum | Weyl carries vacuum tides |
| eigenvalues $(-2,1,1)\tfrac{GM}{r^3}$ | the same, over $c^2$ |
Both equations are second-order linear ODEs for the same physical separation, with the same solutions and the same eigenvalues. They are not analogous: they are the same computation, written in two notations, one of which happens to survive a Lorentz boost.
Not that the metric is determined — that needs a field equation. Not that $R^i{}_{0j0}$ exhausts $R$ — it is $6$ of the $20$, the "electric" part; the rest shows up in unit 38's waves. Not that $\Phi$ exists in general — it does not; only the weak static limit has one.
33 · Newton
Two balls dropped $1$ m apart horizontally, falling $100$ m: they converge by $\tfrac12(GM_\oplus/R_\oplus^3)\,\xi\,t^2$ with $t = 4.52$ s, that is $15.7\ \mu$m. Small, real, and entirely a statement about the curvature of spacetime.
Each ball falls straight at the Earth's centre, so the two lines of fall meet $R_\oplus$ below. Over a fall of $h$ they close by $\xi h/R_\oplus = (1\ \mathrm m)(100)/(6.378\times10^6) = 15.7\ \mu$m ✓ — the same number with no curvature in sight, as it must be: the squeeze eigenvalue $GM/r^3$ is exactly what converging radial lines give.
Not to scale: the lines of fall really converge $6378$ km below. Horizontal neighbours squeeze together — the $+1$ eigenvalue — just as the two meridians did on the sphere.
section 5
Ricci, scalar, Weyl, Einstein — and the identity that makes a field equation possible.
33 · traces
Contract $\rho$ with $\mu$: $R_{\sigma\nu}$. With $\nu$: $-R_{\sigma\mu}$, by S1. With $\sigma$: $R^\rho{}_{\rho\mu\nu} = g^{\rho\lambda}R_{\lambda\rho\mu\nu} = 0$, by S2. A trace of two lower indices uses $g^{-1}$: over $\mu\nu$ it is zero by S1, and over $\sigma\mu$ or $\sigma\nu$ it is $\pm$ the Ricci trace again by S4. So up to sign there is exactly one. $\square$
$R_{\sigma\nu}$ is symmetric: $R_{\sigma\nu} = g^{\rho\lambda}R_{\lambda\sigma\rho\nu} = g^{\rho\lambda}R_{\rho\nu\lambda\sigma}$ (S4) $= R_{\nu\sigma}$.
Ricci: a small ball of dust released at rest has $\ddot V/V = -R_{\mu\nu}u^\mu u^\nu$ — the trace of the deviation equation, so the trace of the tidal tensor, which unit 05 said is $4\pi G\rho$. Scalar: $R$ measures how the volume of a small geodesic ball falls short of the Euclidean one (cited, in the notes).
$R_{\mu\nu} = \tfrac{1}{a^2}g_{\mu\nu}$ and $R = \tfrac{2}{a^2}$. Check: $R = g^{\mu\nu}(g_{\mu\nu}/a^2) = 2/a^2$ ✓, and in two dimensions $R = 2K$ always. Positive, as a sphere must be with these conventions.
33 · traces
Counting already told us: at $n=3$, Riemann has $6$ components and the symmetric Ricci tensor has $\tfrac{3\cdot4}{2} = 6$. Equal counts do not by themselves prove determination — but here the map is explicit.
Check by tracing. Contract with $g^{\rho\mu}$, using $g^{\rho\mu}g_{\rho\mu} = 3$: the five terms give $3R_{\sigma\nu} + g_{\sigma\nu}R - R_{\sigma\nu} - R_{\sigma\nu} - \tfrac R2(3-1)g_{\sigma\nu} = R_{\sigma\nu}$ ✓.
In three dimensions, $R_{\mu\nu} = 0$ forces $R_{\rho\sigma\mu\nu} = 0$: vacuum is flat. A universe with two space dimensions and one of time has no gravitational waves, no Schwarzschild solution, no orbits — gravity exists only where matter is. In four dimensions $20 - 10 = 10$ components are left free by the trace, and those ten are everything this course has left to study.
Three-dimensional gravity is locally trivial, not globally: a point mass produces a cone, flat everywhere but with a deficit angle — exactly the cone of section 3. Curvature concentrated where the matter is, holonomy round it, and no field outside.
33 · traces
the unique combination with S1–S4 and every trace zero: $g^{\rho\mu}C_{\rho\sigma\mu\nu} = 0$.
So Riemann splits: $\;20 = 10 \;(\text{Ricci}) + 10\;(\text{Weyl})$ in four dimensions, $6 = 6 + 0$ in three, and at $n=2$ the split does not exist.
$C$ is conformally invariant: rescaling $g \to e^{2\omega}g$ leaves $C^\rho{}_{\sigma\mu\nu}$ unchanged (Wald, General Relativity, App. D). And for $n \ge 4$, $C = 0$ on an open set iff the metric is conformally flat there (Weyl 1918, Schouten 1921).
33 · traces
Unit 35's field equation will fix Ricci algebraically from the matter at each point. Weyl is what is left over, and it is what propagates: in vacuum $R_{\mu\nu} = 0$ and $C = R$, so the tides you feel in empty space are Weyl. The Moon's pull on the oceans, light bending near the Sun, and the gravitational waves of unit 38 are all Weyl curvature.
Schematic, exaggerated: a ball of dust released at rest. The trace of the tidal tensor — Ricci, $\ddot V/V = -R_{\mu\nu}u^\mu u^\nu$ — changes its volume and only where there is matter. The trace-free part changes its shape at fixed volume; in vacuum that part is all there is, and it is Weyl.
33 · Bianchi
Start from $\nabla_\lambda R_{\rho\sigma\mu\nu} + \nabla_\rho R_{\sigma\lambda\mu\nu} + \nabla_\sigma R_{\lambda\rho\mu\nu} = 0$ and contract with $g^{\lambda\mu}$. Using $\nabla g = 0$ to move the inverse metric through, and $R_{\sigma\nu} = g^{\rho\lambda}R_{\lambda\sigma\rho\nu}$:
$$\nabla^\mu R_{\rho\sigma\mu\nu} - \nabla_\rho R_{\sigma\nu} + \nabla_\sigma R_{\rho\nu} = 0 .$$Now contract with $g^{\sigma\nu}$. The first term becomes $\nabla^\mu R_{\rho\mu}$, the second $-\nabla_\rho R$, the third $\nabla^\nu R_{\rho\nu}$:
$$2\nabla^\mu R_{\rho\mu} - \nabla_\rho R = 0 . \;\square$$The last line rearranges the proof: $\nabla^\mu(R_{\rho\mu} - \tfrac12 g_{\rho\mu}R) = \tfrac12\nabla_\rho R - \tfrac12\nabla_\rho R = 0$.
Local conservation of energy and momentum is $\nabla^\mu T_{\mu\nu} = 0$ for any matter (unit 35 sets up $T_{\mu\nu}$). A field equation $(\text{geometry})_{\mu\nu} = \kappa\,T_{\mu\nu}$ is therefore inconsistent unless the left side is identically divergence-free. $R_{\mu\nu} = \kappa T_{\mu\nu}$ fails. $G_{\mu\nu} = \kappa T_{\mu\nu}$ cannot fail. Unit 35 has almost no freedom left.
33 · closing the example
| object | on $S^2_a$ |
|---|---|
| $R_{\theta\phi\theta\phi}$ | $a^2\sin^2\theta$ |
| $K$ | $1/a^2$ |
| $R_{\mu\nu}$ | $g_{\mu\nu}/a^2$ |
| $R$ | $2/a^2$ |
| $G_{\mu\nu}$ | $g_{\mu\nu}/a^2 - \tfrac12(2/a^2)g_{\mu\nu} = 0$ |
| holonomy of $\triangle$ | $\pi/2 = \int_\triangle K\,\mathrm dA$ |
| deviation of two meridians | $\xi = a\Delta\phi\cos(s/a)$ |
$G_{\mu\nu} \equiv 0$ on every two-dimensional manifold, because $R_{\mu\nu} = \tfrac12 Rg_{\mu\nu}$ identically there. So the Einstein equation in two dimensions reads $0 = \kappa T_{\mu\nu}$: it permits no matter at all. Gravity, as a field theory, does not exist below three dimensions — and, by the $n=3$ slide, has no vacuum degrees of freedom below four.
$n=2$: $G \equiv 0$, no theory. $n=3$: $G$ determines $R$ entirely, no waves, no exterior field. $n=4$: ten components of $G$ fixed by matter, ten of Weyl left free to propagate. The next five units are about those ten.
33 · checkpoint
Covariant derivatives fail to commute by a tensor; no chart removes it, it is the tidal tensor, and one identity makes its trace-reversed trace conserved for free.
Unit 34 rewrites all of it with forms, and unit 35 writes down the field equation that the last slide of section 5 has already almost forced.
Twelve problems, about seven hours: ./mr problems 33. When the four items above are true: ./mr done 33.