A spherical mass density gives projected surface density . On the positive half of the line of sight, substitute to obtain the displayed Abel transform. Spherical symmetry is essential: a general three-dimensional density cannot be reconstructed uniquely from one projection.
The strip density is the mass per unit projected Cartesian coordinate : . It is even in . For , changing variables to projected radius gives . Alternatively integrate the three-dimensional mass density over the plane of coordinates to obtain the displayed expression. Consequently for .
For an isolated spherical distribution, shell assembly gives gravitational potential energy . Use and to write . A second integration by parts gives the displayed negative quadratic functional. The boundary terms and must vanish; finite-mass regular profiles with finite binding energy satisfy the usual sufficient decay conditions.
Put and . Then . Composing this Abel transform with itself and exchanging convergent integrals gives , because the inner integral from to is . Differentiate after writing to obtain . Substituting yields the displayed reconstruction. Decay and regularity sufficient for the exchanges and derivatives are required.
For and , the projected profile has the displayed spherical Abel transform inverse. Indeed its composed transform is , with . Differentiate in , divide by , and use the Gamma function recurrence to obtain the coefficient. The same kernel reconstructs tracer number density or isotropic random pressure from their respective projected profiles.
For a spherical, nonstreaming stellar population with isotropic velocity dispersion, each component of the random pressure tensor equals . The observed second stellar velocity moment satisfies . Composing this Abel transform with itself gives the displayed inverse under sufficient decay and regularity. The Spherical Jeans equation then gives , with gravitational acceleration . The Poisson equation for Newtonian gravity recovers total gravitating mass density, not just the tracer density. Without velocity isotropy the same projected moment also contains anisotropic stresses.

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