The azimuthal momentum equation with isHence the slow radial drift isSubstitution into mass conservation, , gives the nonlinear diffusion equationIt describes slow axisymmetric viscous spreading while the velocity remains close to the imposed Kepler shear. It omits epicyclic and acoustic waves, rapid transients, self-gravity, nonaxisymmetric structure, and edge dynamics for which the assumed shear and secular force balance fail.
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