The constant-coefficient one-dimensional advection-diffusion equation is
Translation to coordinates moving at speed reduces it to the heat equation.
For a passive scalar on a half-line, impose constant total solute flux at its inlet, with initially zero concentration and constant positive advection speed and mass diffusivity . A Laplace transform in time gives
With , and , its inverse is
The complementary error function describes the smeared front. This is a flux boundary condition, not the constant-concentration inlet solution. At large axial Péclet number, both have the leading advancing front .
The half-line solution of with initially zero concentration, unit inlet concentration for positive time, and decay at infinity at fixed time. Both complementary error functions are needed to satisfy the inlet exactly. A Laplace transform gives . A finite layer requires an additional downstream boundary condition.
For the advection-diffusion equation , the multiplication gives . A Dirichlet boundary condition remains a prescribed value, multiplied by at the endpoint. This real exponential conjugation removes the first derivative without changing a bounded spatial interval.
After the Dirichlet gauge transform for constant drift, put . The Dirichlet Green function of is
The original unweighted resolvent kernel is . Its poles are . The kernel is even in , so the apparent square-root branch point is removable.
On , consider with , zero scalar flux at the endpoints for , and unit initial impulse at the origin. Put and . The normalized similarity solution is
The ansatz gives . Endpoint decay sets this integrated constant to zero and hence ; the gamma function normalizes its integral to one. Its scale is , so it converges weakly to a unit impulse as . Its gamma distribution shape is , its maximum occurs at , and its expected value is . For width proportional to , the associated horizontally averaged plume concentration is proportional to : its interior maximum is when , its supremum occurs at the origin when , and it is singular there when . The physical finite source regularizes this ideal-origin behaviour.
Writing transforms into . A prescribed coordinate derivative at an endpoint becomes there. Thus a Neumann boundary condition becomes a Robin boundary condition. The signs are coordinate-derivative signs at both endpoints; outward normal derivatives require a sign change at the left endpoint.
On , the differential operator with homogeneous Neumann boundary conditions is self-adjoint in the weighted inner product with weight . Its eigenfunctions and nonnegative decay rates are
Their squared norms are and . The Sturm-Liouville eigenfunction expansion gives
This kernel acts against the measure , not Lebesgue measure alone. It is symmetric in ; the transition density against Lebesgue measure is .
For , constant and , on put , with the principal square root, and
These satisfy and the left and right homogeneous Neumann boundary conditions, respectively. The weighted Wronskian gives
The first derivative jumps by , so the resolvent integrates against . Its time Laplace transform interpretation is . The factor records the zero eigenvalue and constant stationary eigenfunction.
For with and , two applications of integration by parts against a Neumann eigenfunction give the boundary forcing . Solving the resulting modal linear differential equation gives
The endpoint derivatives are interior limits: the short-time singularity prevents evaluating each homogeneous boundary derivative before the time integral and infinite sum. The constant eigenfunction gives the weighted-mass law .
The Cauchy problem with initial value has
The homogeneous Dirichlet boundary condition kernel for on . Here is the heat kernel. The exponential reflection weight makes . Gaussian decay makes its initial-data integral convergent even when the exponentially weighted initial data are not integrable separately.

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