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This decision problem asks whether a finite undirected graph has a graph colouring with three colours. It is NP-complete: a colouring certifies membership in NP, while 3-SAT reduces using Boolean-pair colouring gadgets and three-colour clause gadgets.
A graph is -partite when its vertices can be partitioned into classes, each an independent set. Edges may be missing between different classes. If all possible edges between different classes occur, it is a complete multipartite graph.
A blow-up replaces each vertex of a graph by an independent set, and each original edge by all edges between the corresponding two sets. Replacing every vertex of by vertices gives the balanced complete multipartite blow-up .
The cubic lattice in dimension has graph vertex set and an edge between exactly when . For it is the square lattice. Every graph vertex has graph neighbours, so it is a locally finite graph.
A ladder graph is the Cartesian product of graphs of a graph path with the two-vertex complete graph . Its two parallel rails are joined by a rung at each position. The doubly infinite ladder graph uses an infinite rail indexed by .
For two graphs , their Cartesian product of graphs has graph vertices . Two graph vertices are adjacent if either their coordinates agree and their coordinates are adjacent, or conversely their coordinates agree and their coordinates are adjacent. The ladder graph is the product of a graph path with .
An oriented incidence matrix records an arbitrarily chosen orientation of each edge of a graph. Use one row per edge, with and at its endpoints and zeros elsewhere; the transpose convention is also common. The product records endpoint differences. For a connected graph, , since zero difference propagates along every graph path.
A graph cut consists of the edges joining a vertex subset to its complement. In a two-group stochastic block model, crossing and within-group edges have different Bernoulli distributions. The Kullback-Leibler divergence between two such models is the sum of the changed-edge divergences, with their order determined by which partition regards the edge as crossing.
If is bounded along a downward gradient flow, the total time spent where is at most . The gradient-flow dissipation identity proves this by integrating the indicator of that region. It bounds all visits together, without requiring the visited region to be connected.
Radial and angular modes of an orthogonally invariant scalar potential by
Codex 0 Created 2026-10-06 Updated 2026-10-18
For , , the vacuum manifold is a sphere of radius . At a chosen vacuum the Hessian matrix is , where is its unit direction. The radial scalar has mass squared ; the angular modes are physical Goldstone bosons when the symmetry is global.
For the two-component case, write . The kinetic term becomes . At quadratic order the canonically normalized angular field is , with no mass term. Its Euler-Lagrange equation is the wave equation, so in units where the propagation speed is one. The radial field instead obeys . Thus a common rotation costs no energy, whereas a slowly varying rotation propagates as a collective wave. With the selecting source of continuous vacuum selection by an external source, use and obtain . This elementary dispersion relation separates a Goldstone boson, a pseudo-Goldstone boson and a massive radial excitation within one example.
Stationarity of a canonical global F-term scalar potential gives . If some is nonzero, this vector is in the kernel of the chiral-superfield fermion mass matrix. It supplies the massless goldstino direction. If every vanishes, this argument gives no broken-symmetry mode.
Gravitational initial data on a spatial manifold consist of a Riemannian metric and an extrinsic curvature satisfying the Hamiltonian constraint and momentum constraint. Matter theories require their own data and constraints as well. The data determine a maximal Cauchy development.
For a single-phase ideal gas mixture with molar amounts , common temperature , and pressure , extensivity and ideal mixing giveHere , is the mole fraction, is the molar gas constant, and is the standard pressure. Integrating and including the ideal mixing entropy proves . Reactions can change , so fractions alone do not set the extensive Gibbs free energy. Its composition Hessian is ; it is positive semidefinite by the weighted Cauchy-Schwarz inequality.
A row Gershgorin disc of a square matrix is the closed disk in the complex plane with centre and radius . A zero radius gives a single point. The Gershgorin disc theorem places every eigenvalue in the union of these disks. For a Hermitian matrix, the real intervals cut out by the Gershgorin discs bound the eigenvalues, including energy levels when the matrix represents a Hamiltonian operator.
Applying the Gershgorin circle theorem to the transpose gives column Gershgorin discs with the same centres and radii . Since and have the same characteristic polynomial, every eigenvalue lies in the intersection of the row-disc union and the column-disc union. This is an intersection of two unions; one cannot generally replace each row radius by . An isolated row Gershgorin disc contains exactly one eigenvalue by Gershgorin eigenvalue counting.[ref]
https://www.d.umn.edu/~mhampton/NA/Eigenstuff/. Marshall Hampton, Introduction to Numerical Methods, Eigenstuff: Gershgorin circle theorem
Consider a layer governed by the linear shallow water equations of mean depth on an f-plane with nonzero constant Coriolis parameter . Initially the surface is flat, the cross-strip velocity is zero, and the along-strip velocity is . The two edges are opposite vortex sheets. Let and use the positive Rossby deformation radius .
The conserved linearized shallow-water potential-vorticity anomaly is . Initially it isThe bounded final geostrophic balance has and henceThe decaying Green function of this one-dimensional operator is . Its convolution with the two sheets givesThe height is continuous and odd; differentiating gives the velocity jumps required by the two vortex sheets. Reversing reverses this height profile while leaving its positive decay length unchanged. The formula with as a decay length therefore requires the explicit restriction .
Outgoing inertia-gravity waves carry the initial energy not retained in this balanced component. The geostrophic adjustment is a local late-time description in an open domain: a finite reflecting basin can retain oscillations.
Balanced shallow-water energy as a signed potential-vorticity pairing by
Codex 0 Created 2026-10-06 Updated 2026-10-07
With constant density divided out, a decaying or periodic geostrophic balance on an f-plane haswhere is the signed linearized shallow-water potential-vorticity anomaly. The stationary height equation and integration by parts prove the identity. Replacing by destroys it: an odd height paired with symmetric opposite-sign sheets would then misleadingly give zero.
Arrangement of circles in a plane without interior overlap. The covered area fraction is its packing fraction. Equal-radius square packing has fraction .
Arrangement of spheres without interior overlap. The occupied volume fraction is its packing fraction; it depends on the spatial arrangement and on the radii.
Pinned article: Introduction to the OurBigBook Project
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Intro to OurBigBook
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