Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 40 1 i Solution Created 2026-10-03 Updated 2026-10-06
Use the Minkowski metric , , and . The Proca field has nonzero mass . Vary its action, using the fact that the gauge field strength is an antisymmetric second-rank tensor:The integration by parts discards a boundary term, with the variation fixed at the boundary. Thus the Euler-Lagrange field equation is the Proca equationThe minus sign on is required by the chosen Minkowski metric; after imposing the constraint below, the plane waves have positive energy .
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 40 1 vi Solution Created 2026-10-03 Updated 2026-10-06
There are two closely related objects to distinguish. Inverting the quadratic Proca action gives the usual covariant Proca propagator. After integration by parts, its kernel isThe matrix inverse with the Feynman i-epsilon prescription givesMultiplication by gives in the distributional limit. The numerator agrees with the polarization sum for a massive vector boson at the poles, but is not a transverse linear projection at arbitrary four-momentum.
For the literal canonical time-ordered product of and , the nondynamical component produces the Proca time-ordering contact term. In the chosen time coordinate the full answer isTo see the local term directly, the three physical polarization vectors give . The canonical two-point correlation function therefore has Fourier transformBy contrast, , so the covariant expression contains an additional . The mixed and spatial components have no additional contact term. ThusIf is used to mean covariant time ordering, commonly denoted , the conventional answer is instead just . Both conventions have the same propagating poles and agree away from coincidence; explicitly separating them respects the printed definition as an ordinary time-ordered product.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 44 2 c Solution Created 2026-10-03 Updated 2026-10-06
It is useful to regulate the number of modes first, so the functional integral identities reduce to ordinary integration by parts. Let be the Gaussian covariance, , and put a dot for . The matrix identity givesThe second field derivative of the Gaussian isHence, after two integrations by parts,The imposed flow makes the bracket vanish. The remaining trace is independent of the fields and only changes the Gaussian normalization. Since the free Gaussian normalization is , . ThereforeEquivalently, is cutoff independent after discarding the stated overall rescaling. This is the Gaussian covariance differentiation identity behind the Polchinski equation.
With the Fourier convention above and functional derivatives satisfying , contraction with becomes . Thus the numerator in the printed flow is consistent with this derivative convention; it must not be changed independently of the convention.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 5 2 f Solution Created 2026-10-03 Updated 2026-10-06
Use unit speed and write the Cauchy data as , . For finite-energy data define the wave energy estimate quantityMultiply by and use integration by parts. With compact support or sufficient decay the boundary flux is zero, soFor general finite-energy solutions, cutoff or approximation arguments justify this identity; equivalently the local estimate below, applied in both time directions and with radii tending to infinity, gives the same equality. Arbitrary smooth data need not have finite global energy; then the global bound with an infinite right side is uninformative, while the local estimate remains useful.
If and , the fundamental theorem of calculus and the wave energy estimate further giveTogether these yield an a priori bound for on each bounded time interval. No existence assumption is proved by the estimate itself; it controls any sufficiently regular solution.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 5 3 a iii Solution Created 2026-10-03 Updated 2026-10-06
There is a normalization error in the PDF. With the printed unnormalized integral, testing a constant function equal to one would give a left side and a right side zero. Thus that formulation fails whenever .
Use instead the average . The Poincare-Wirtinger inequality, also called the Neumann-Poincare inequality, isIf no exists, subtract the average and normalize a violating sequence to obtain with , , and . This sequence is bounded in the Sobolev space . The Rellich-Kondrachov compactness theorem supplies a subsequence converging strongly in to .
For every compactly supported test function , integration by parts and these convergences give . Thus has zero weak gradient. The Sobolev function with zero weak gradient result and connectedness make constant. Strong convergence preserves its zero integral, so . It also preserves its norm one, a contradiction. This proves the correctly normalized Neumann-Poincare inequality.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 5 3 b ii Solution Created 2026-10-03 Updated 2026-10-06
The difference of two weak solutions lies in the clamped second-order Sobolev space. Testing with yields , so . Since , integration by parts givesThe Poincare inequality for zero boundary values now implies . The clamped biharmonic problem has at most one weak solution. Unlike the Neumann Poisson problem, no additive constant is allowed by these boundary traces.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 5 4 a ii Solution Created 2026-10-03 Updated 2026-10-06
Multiply the viscous scalar conservation law by , rather than estimating after differentiating. Integration by parts yieldsThus . Applying the Gronwall inequality givesOnly the assumed bound on is used; a global bound on is not needed for this energy estimate.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 5 4 a i Solution Created 2026-10-03 Updated 2026-10-06
Let . The sharper energy estimate uses the divergence structure of the viscous scalar conservation law. Multiply by and integrate over the line. With ,because the decay makes tend to zero at both ends. Integration by parts in the diffusion term therefore givesOne may take , uniformly in . This does not require .
If a bound explicitly involving and is desired, retaining the transport term and using the Cauchy-Schwarz inequality and the elementary inequality givesThe Gronwall inequality then gives the valid but weaker choice . The exact cancellation explains why its divergence is unnecessary.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 55 1 Solution Created 2026-10-03 Updated 2026-10-06
For a spherical stellar polytrope in hydrostatic equilibrium, combine with to eliminate the enclosed mass:For , put , , and . Since , chooseThe Lane-Emden equation is thenA regular center requires and , with positive chosen central mass density and pressure. Locally . The stellar surface is the first positive zero , where the idealized external pressure is zero; retain the positive solution before it. Thus and the Lane-Emden mass formula isThe surface condition selects where to stop a centrally regular solution, rather than replacing its central regularity conditions.
For a polytrope of index zero, the density is constant and . Regularity givesThe pressure is and , so . Index zero is the structural incompressible limit: the expression is not itself defined at .
For a polytrope of index one, set . The equation becomes , while central regularity requires , . HenceThe mass is , so it can change with central mass density while the radius stays fixed.
The moment of inertia of a polytropic star about any axis through its center follows by integrating over spherical shells:For constant mass density this gives . For index one, integration by parts gives , and thereforeThese are axial moments of inertia, not the scalar second mass moment .
For a finite-radius centrally regular stellar polytrope with and , eliminate from and . The resulting polytropic mass-radius relation isHere are dimensionless functions of . At no such single-valued mass-as-a-power-of-radius relation exists at fixed : the radius is fixed instead. At the exponent is zero and is independent of central mass density. For the incompressible case, at fixed mass density. Regular solutions have no finite zero-pressure surface, so the finite-radius formula does not apply to them.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 64 1 ii Solution Created 2026-10-03 Updated 2026-10-07
Use a bounded BV extension operator for the bounded Lipschitz domain. Extend to , supported in one fixed compact set, with . Such an extension is obtained by reflection in Lipschitz boundary charts, a partition of unity and a fixed cutoff function. A naive zero extension must also charge its boundary-trace jump; it cannot discard that contribution.
Let bound these norms and let be their mollifications. The BV mollification error estimate givesThe variation measure here is on . The printed lemma's needs this correction unless it also assumes all the derivative mass lies in : a nonconstant bump supported outside disproves its literal wording. The correct estimate follows by averaging the BV translation estimate over a mollifier supported in .
For each fixed , convolution gives uniform boundsThe mollifications have common compact support and are uniformly equicontinuous. The Arzela-Ascoli theorem supplies a uniformly convergent subsequence at each scale . A diagonal subsequence converges at every one of those scales. For two late members of that subsequence,First choose large , then late ; the sequence is a Cauchy sequence in . Its limit belongs to the BV space because the total variation seminorm on a domain is sequentially lower semicontinuous. Uniform derivative bounds and integration by parts give . Restriction to proves the required weak-star convergence in BV.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 64 1 i Solution Created 2026-10-03 Updated 2026-10-07
The bounded-variation space carries the norm . Its weak-star convergence in BV is characterized byThe second condition means convergence of the vector measure pairings against every . Equivalently, strong convergence in together with suffices: integration by parts identifies the limit on smooth compactly supported tests, and uniform approximation extends this to tests.
The bounded-variation compactness theorem says thatguarantees a subsequence convergent in weak-star convergence in BV on a bounded Lipschitz domain. This is the uniform criterion for relative sequential compactness. If asking only for the existence of one convergent subsequence, the exact condition is the existence of a BV-bounded subsequence, equivalently . The entire sequence need not be bounded: alternating zero functions and constants tending to infinity gives a simple example. Conversely, a convergent subsequence has bounded norm and bounded total variation seminorm by the Uniform boundedness principle for its derivative-measure pairings.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 64 3 i Solution Created 2026-10-03 Updated 2026-10-07
The structure theorem for functions of bounded variation is the measure representation of the distributional derivative: for there is a unique finite vector Radon measure withfor every . It also has a polar decomposition of a vector measure with for -almost every point.
To prove it, let . The test-function definition of total variation seminorm, applied to both signs, gives . Compactly supported smooth vector fields are uniformly dense in , so extends uniquely to a bounded functional there. The Riesz-Markov-Kakutani representation theorem, applied componentwise, gives the unique vector measure . The operator norm of is exactly the defining variation supremum; the vector-measure dual norm is , proving equality. Conversely any finite measure satisfying the identity bounds that supremum, so this also characterizes membership in the BV space.
The Radon-Nikodym theorem applied to the components relative to gives ; the definition of the variation measure forces almost everywhere. If is smooth, ordinary integration by parts gives . Compact support of the test field removes any boundary contribution; no boundary regularity is needed for this representation statement.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 66 1 a Solution Created 2026-10-03 Updated 2026-10-06
Take real and use the L2 norm on the spatial interval. Existence, uniqueness and continuous dependence are the three requirements of Hadamard well-posedness. An energy method supplies the decisive estimate. For a smooth solution with homogeneous Dirichlet boundary conditions, integration by parts givesThe drift contributes only a boundary term, which vanishes. The Poincare inequality further givesApply the same argument to the difference of two solutions to obtain uniqueness and continuous dependence on the initial data.
For existence, use the Dirichlet gauge transform for constant drift: satisfies with zero boundary values. Expanding in its Fourier sine series givesFor the series defines a solution continuous in down to and smooth for positive time; multiplication by the fixed bounded exponentials preserves this interpretation. Its energy estimate follows by approximation with smooth initial data. For a classical solution at the initial corners, require the usual smoothness and boundary compatibility instead. The problem is well posed in , with a contraction estimate independent of the initial data.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 66 7 Solution Created 2026-10-03 Updated 2026-10-06
The finite element method replaces an infinite-dimensional variational problem by a finite-dimensional one, usually using functions that are polynomial on small mesh elements. Ritz method and Galerkin method describe how the discrete equations are selected; neither intrinsically requires piecewise polynomials, though those spaces make assembly local and sparse.
For a concrete realization of the two-point problem, choose homogeneous Dirichlet boundary conditions at both endpoints of . The differential expression alone is not a complete boundary value problem, so this boundary choice is an explicit assumption. Let with , with , and . Use the zero-boundary Sobolev space with norm . By the Poincare inequality this is equivalent to its full first-order Sobolev norm. Multiplying by a test function and applying integration by parts givesThe endpoint terms vanish by the essential boundary condition. The form is a symmetric bilinear form, bounded byand it is a coercive bilinear form:The load is a bounded linear functional. The Lax-Milgram theorem gives a unique weak solution and a bound . Under the stated coefficient regularity it solves the differential equation in the usual weak sense.
The Ritz method minimizes the energyover , or over a conforming finite-dimensional subspace . Its first variation is ; symmetry and coercivity make the functional strictly convex. In fact, if is the weak solution,Thus the energy minimizer is exactly the weak solution. The Galerkin method instead directly asks for with for all . For this symmetric coercive problem, Ritz-Galerkin equivalence for a symmetric coercive form shows that the discrete minimizer and Galerkin solution coincide. For a nonsymmetric problem, a Galerkin formulation can still apply but the same quadratic minimization generally cannot represent its full bilinear form; appropriate coercivity or inf-sup conditions must then justify the chosen spaces.
Subtract the continuous and discrete weak equations to obtain Galerkin orthogonality . Since defines the energy norm , the Pythagorean identity givesIn a general reference norm, the Céa lemma yieldsThe proof uses together with coercivity and continuity. Dense approximation spaces therefore imply convergence; the estimate reduces a numerical error problem to an approximation problem.
For implementation, partition the interval by nodes . Choose continuous piecewise-linear functions and the interior piecewise-linear hat functions as a basis, with the two boundary coefficients prescribed. Write . The coefficients satisfyThe stiffness matrix is symmetric positive definite: for nonzero interior coefficients. The local supports make it tridiagonal in this one-dimensional linear-element case.
On an element of length , for constant element coefficients , the two-node matrix and constant-load vector areFor variable coefficients, integrate against the same shape functions rather than silently replacing them by constants. Element contributions are added at shared nodes, and boundary values are eliminated or lifted into the right side. A sparse direct solve or a suitable iterative method gives the nodal coefficients. Numerical quadrature should preserve the required accuracy and, with positive coefficients and weights, the positive energy structure.
A finite element interpolation estimate gives for these elements, where is the largest element size and the solution has the stated regularity. The Céa lemma then gives first-order energy error. If the dual elliptic problem has regularity, the Aubin–Nitsche duality argument gives second-order error: for , solve , then use to gain one further factor of . Higher-order elements improve rates when the solution is sufficiently smooth.
Nonzero Dirichlet data are handled by a boundary lifting and an affine trial space. Neumann boundary conditions enter naturally through the integrated boundary term; Robin terms modify both the form and the load. With pure Neumann conditions and , constants lie in the kernel: existence needs the load/flux compatibility condition, uniqueness needs a mean constraint, and the preceding Dirichlet coercivity argument cannot simply be reused. Conforming approximation, boundary conditions and coercivity are the ingredients connecting the finite-element construction to a justified Ritz or Galerkin solution.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 67 2 Solution Created 2026-10-03 Updated 2026-10-06
For , choose a cutoff function on a neighborhood of its support. Its extension to smooth functions makesindependent of the choice of cutoff. For real frequency, the definition of the distributional Fourier transform gives : interchange the pairing with the integral of a Schwartz function, using the finite-order estimate on the cutoff's compact support. On each compact set of complex frequencies the exponential and all its derivatives have uniformly convergent power series. Continuity of the distribution allows termwise differentiation, withConsequently is entire on .
For the precise exponential type, a fixed enlarged support would give an unnecessarily enlarged radius. Instead use the shrinking-cutoff exponential-type estimate. On one fixed compact neighborhood of the closed radius- ball, has finite order of a distribution . Choose near that ball, supported in the radius- ball, with for . The finite-order estimate givesTake . Its extra exponential is bounded by , while the derivative cost is polynomial. ThusThe entire function was defined with a fixed cutoff; only its bound uses a frequency-dependent cutoff, so no holomorphic dependence is lost. This proves the required estimate with some without enlarging .
For the converse, set . Its restriction to real frequencies has polynomial growth. Define the inverse tempered distribution byRapid decay of the Schwartz function transform proves convergence and continuity, and Fourier inversion gives on real frequencies.
We prove its support directly by contour shifting, rather than assuming the support conclusion of the Paley–Wiener–Schwartz theorem. Let be a real unit vector and take a test function supported in for some . For every integer , integration by parts in the real-frequency Fourier integral givesIndeed, move from the oscillatory exponential to ; its derivatives supply at most powers of .
The product is entire. Rotate coordinates so that is the first coordinate vector and apply Cauchy integral theorem to a rectangle in that one complex coordinate, integrating the remaining real coordinates afterwards. For fixed , choose ; the displayed decay estimate, uniformly on the intervening imaginary segment, makes the vertical faces vanish as the real rectangle width tends to infinity. The horizontal integrals are absolutely convergent. HenceUsing and the growth hypothesis bounds this pairing byIt tends to zero as , so the pairing vanishes. Every point outside the closed radius- ball lies in such a separating half-space; a finite partition of unity for the support of a test function outside the ball proves .
Translate this compactly supported distribution by : define . The Translation property of the Fourier transform givesThe compact-support entire extension agrees with everywhere by the identity theorem, applied successively in the complex coordinates. Fourier inversion also gives uniqueness. This completes both directions of the ball version of the Paley–Wiener–Schwartz theorem.
For the wave equation, take a real constant . The Fourier transform method for the wave equation givesThis inverse tempered distribution is twice differentiable in : time derivatives introduce polynomial frequency factors, still integrable against every Schwartz function. It has the specified initial displacement and zero initial velocity and satisfies the equation distributionally.
To apply the support theorem, replace the real norm by the entire wave cosine multiplierThis series is entire and equals regardless of the square-root choice. Write and . Since ,Together with , this yields . The forward estimate for the translated initial support now givesThe converse therefore proves finite propagation with the stated speed:In particular, itself need not be entire; it is the even cosine series that provides the required entire extension.
For completeness this construction identifies the distributional Cauchy solution even without initially assuming spatial temperedness. The zero-displacement wave multiplier is , entire with bound . Given a compactly supported smooth and final time , the backward solution is smooth, has support in one compact ball for by the same support theorem, and satisfies , . For the difference of two distributional solutions with zero initial data,All pairings use compactly supported test functions. The expression vanishes initially and equals finally. Hence , establishing uniqueness in the usual time-differentiable distributional solution class.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 68 1 Solution Created 2026-10-03 Updated 2026-10-06
A one-dimensional Sobolev representative is absolutely continuous. For , the fundamental theorem of calculus and Holder inequality giveThus has a representative in . The qualification about representatives matters because a Sobolev space element is an almost-everywhere equivalence class.
In two dimensions, the Sobolev fundamental theorem of calculus on lines and Fubini's theorem imply that almost every horizontal and vertical slice belongs to and has this one-dimensional Hölder continuity. The slice seminorm depends on the slice; this does not give one uniform pointwise estimate on the square. For , Morrey's inequality additionally gives a globally Hölder continuous representative of exponent . For , global continuity need not hold. For example, with a smooth cutoff around an interior point, lies in when , but is unbounded. At , the cutoff version of is unbounded while its gradient has finite squared integral, sinceThese examples distinguish Sobolev slicing and planar continuity from a false two-dimensional application of the interval exponent.
Put . A BV space is a function whose distributional derivative is a finite vector-valued Radon measure. Equivalently its total variation seminorm is finite:The BV space has norm . For , integration by parts against the compactly supported field gives . Conversely the measurable choice on nonzero gradients attains the pointwise bound. Approximating this bounded field by smooth fields, using interior cutoffs and the finite measure , justifies the supremum and givesIt is a norm of the derivative measure, rather than a pointwise derivative at jump discontinuities.
There is a genuine mismatch in the printed definition of the next functional. Its constraints on and are independent. Hence its stated supremum, denoted , separates asThe scalar supremum is , by cutoffs approaching one, and the vector supremum is the variation. For an affine image signal with , this gives , whereas the displayed square-root area would give . The intended relaxed graph-area functional instead uses the coupled pointwise constraint , givingwhere is the singular part of . Both readings have a minimizer, but their equations are different.
Here is the direct method in the calculus of variations for either reading. Let be the literal or the corrected , and define the energy on , assigning infinity elsewhere. A minimizing sequence has bounded energy by comparison with . Both , so its variation is bounded, and the fidelity bounds , hence also and . By bounded-variation compactness, a subsequence converges strongly in to , and after another subsequence almost everywhere. Fatou's lemma provesThe regularizer is a supremum of affine functionals continuous in , since the test-field divergence is bounded. It is therefore lower semicontinuous. Combining the two lower bounds proves existence of a minimizer. In fact the convex regularizer and the strictly convex squared fidelity make the minimizer unique up to null sets. This does not assert that the minimizer must belong to .
For the intended graph area, conditionally assume that the minimizer is in . For , differentiate at . The derivative of the integrand is bounded by , so dominated convergence applies. The weak equation isthat is,This is the graph-area Euler-Lagrange equation. Compactly supported variations impose no boundary condition in this statement.
For the literal printed supremum, the constant drops out and one obtains total variation denoising. Its total variation calibration form isThe distributional equation means . In particular wherever the gradient is nonzero; writing this quotient without handling zero gradients would be incomplete. Formally the one-sided derivative of isMinimality in the directions and bounds the remaining linear functional by the second integral. The Hahn-Banach theorem extends it on that zero-gradient set to a bounded vector field of magnitude at most one, furnishing and the displayed weak equation. Thus the literal definition has a nonsmooth subgradient equation, not the square-root equation above.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 69 1 iv Solution Created 2026-10-03 Updated 2026-10-06
The partial differential equation. Each term in is a translated heat kernel and satisfies for . The same holds for , either by direct differentiation or because it is . For , and its derivatives vanish faster than any power as . Therefore differentiating the boundary convolution creates no extra upper-endpoint term. Gaussian domination justifies differentiating both integrals on compact subsets of , proving the advection-diffusion equation.
The initial condition. For fixed , the first Gaussian in is an approximate identity centered at . Its integral tends to . The reflected Gaussian is exponentially small as , because its center lies outside the half-line. The boundary convolution also tends to zero for . Thus .
The Dirichlet boundary condition. The identityshows that , so the initial-data contribution vanishes at zero. The boundary contribution must be evaluated as a limit, not by substituting inside its singular integral. The positive kernel satisfiesfor every . Hence it is a one-sided approximate identity at zero time, and continuity of givesThe mass formula follows from the Gaussian Laplace integral, or from the decaying solution of the corresponding constant-coefficient ordinary differential equation. Compatibility gives the continuous corner value. These arguments also verify the equivalent contour solution in (iii). In the decaying energy class the solution is unique: the difference of two solutions has zero data and for real solutions, with the analogous modulus identity for complex solutions.
The unheaded sine transform question. The direct classical Fourier sine transform does not close on . Ifthen integration by parts givesThe drift introduces an unknown cosine transform; the usual scalar sine-transform solution of the heat equation is therefore unavailable directly.
A Dirichlet gauge transform for constant drift does provide a qualified alternative. Set . Then , with and . If these weighted data have the decay needed for an ordinary Fourier sine transform, it solves the transformed problem and produces exactly the kernel above. Mere decay of does not ensure this weighted integrability. Thus not directly by the classical sine transform of ; yes after a gauge transformation when the required weighted-transform hypotheses hold, or after a justified cutoff/limit argument.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 7 2 d Solution Created 2026-10-03 Updated 2026-10-06
Interpret the given velocity regularity in the stated Sobolev space sense. Repeated integration by parts, or the Fourier transform of a derivative in distributions, givesThe usual one-dimensional one-dimensional Sobolev representative or a smooth approximation justifies this identity without imposing extra decay of classical derivatives at specific boundary points. The transform of an integrable function has absolute value at most its norm. ThereforeSetting and taking the supremum gives the required uniform weighted bound. The term on the left is zero; there is no division by that frequency in this argument.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 76 1 i Solution Created 2026-10-03 Updated 2026-10-06
For the long-wave convection equation with broken Boussinesq symmetry, use a sufficiently smooth real temperature field. To make the spatial average and integrations meaningful, take a periodic pattern, or an existing long-interval average with bounded derivatives and vanishing averaged endpoint fluxes. Boundedness of the temperature alone does not guarantee all those averaging properties. Multiply the evolution equation by and average. Integration by parts givesand . Thus the energy method yieldsThe energy square completion for long-wave convection starts fromPut . The energy identity becomesSince pointwise,Therefore excludes growth of the mean-square temperature, for arbitrary amplitude within this smooth averaging class. This is a nonlinear energy-stability criterion, not a proof of pointwise monotonicity at each position. A spatially constant component instead decays through the term. The criterion is sufficient; it need not coincide with the linear instability threshold.
Past exam of the mathematics course of the University of Cambridge 2014 iii Paper 78 3 Solution Created 2026-10-03 Updated 2026-10-07
The imposed pressure gradient and Darcy's law give a linear velocity profile. Use as the mean pore velocity in the contaminant advection-diffusion equation; thenThe last conditions express zero transverse solute flux under the standard closed-layer interpretation. Transverse exchange through the layer boundaries would change this cell problem and requires additional boundary data. If the prescribed mean speed is a Darcy velocity, its corresponding pore velocity is that speed divided by porosity.
The given parameter is the ratio of transverse mixing time to travel time:Thus transverse dispersion mixes the contaminant across the layer many times during its passage along the long layer. Different fluid speeds still matter: repeated exchange between slow and fast portions produces Taylor dispersion, rather than transport solely at each parcel's original speed. The averaged description applies after and on longitudinal scales large compared with the distance travelled during that mixing time.
Write and, to leading correction order, , with . Taking in the local equation gives the cell problemWith , its solution isAveraging the local advection-diffusion equation now yields . An integration by parts in the cell problem gives . Since , the effective equation isThis is Taylor dispersion in a linear porous-layer velocity profile. For a localized pulse away from the inlet and outlet, its mean position advances at and its longitudinal variance grows as .
For the inlet step, use the semi-infinite inlet approximation , , and as at fixed . The resulting constant-concentration inlet solution isOne derivation is to Laplace transform in time: . Inverting gives the two complementary error functions. Their sum is one at ; for fixed both terms vanish as , and substitution verifies the averaged equation. Retaining only the first term gives the familiar moving error-function front far from the inlet when longitudinal advection dominates diffusion, but does not satisfy the inlet condition exactly.
For a literal finite layer , a downstream boundary condition is also needed once the outlet influences the solution. The PDF's step-inlet request specifies only the initially clean region , so the formula above is the semi-infinite/long-layer solution, not a claim of a unique finite-interval solution with unspecified outlet data.