The razor-thin disk approximation replaces a disk's vertical density profile by . It is useful for horizontal dynamics on scales much longer than the disk thickness.
At an abruptly truncated razor-thin disk with nonzero edge surface density of a disk, the midplane radial force diverges logarithmically. Locally, mass occupies a half-plane and the inward force contains a nonzero angular factor multiplying . The opposite exterior half-plane is absent, so its cancellation does not occur. Finite thickness or a taper taking the edge density to zero regularizes the force. Therefore a finite-edge galaxy rotation curve requires more than the ideal scale-free Mestel disk normalization.
A two-dimensional disk equation with pressure acceleration requires an equation of state for vertically integrated pressure in terms of surface density of a disk . A barotropic fluid closure is , with linear enthalpy perturbation . Merely giving for a volume density does not close the two-dimensional equations unless a vertical conversion is specified. Positive gives ordinary pressure restoration of an inertial-acoustic wave.
For a horizontal Fourier mode of wavenumber , the midplane gravitational potential of a razor-thin disk is
For an isolated razor-thin disk, define the two-dimensional Fourier transform by . At , the razor-thin disk Poisson kernel gives the displayed inversion. Since the transform of is , inversion also gives . The forward relation is . An additive potential constant is irrelevant; a uniform infinite sheet and scale-free divergent potentials require separate zero-mode or potential-difference treatment rather than an arbitrary decaying boundary condition.
For , horizontal Fourier transform gives . Decay and continuity give an exponential on each side; its derivative jump fixes the coefficient. The uniform mode needs a separate linear vertical solution and a potential reference.
The vertical field of a disk has kernel . The triangle inequality therefore bounds a signed-surface density field by the field of its absolute surface density. If that surface density is everywhere smaller than a nonnegative comparison surface density, their vertical fields satisfy the displayed strict comparison, provided the integrals exist and the strict bound holds on positive measure. This is useful when comparing gravity-equivalent magnetic surface density with actual disk mass.
Articles by others on the same topic
There are currently no matching articles.