∫ ∫ lpdS = ∫ ∫ ∫ρX dx dy dz,

(1)

where l, m, n denote the direction cosines of the normal drawn outward of the surface S.

But by Green’s transformation

∫ ∫ lp dS = ∫ ∫ ∫ dpdx dy dz,
dx

(2)

thus leading to the differential relation at every point

dp= ρX,   dp= ρY,   dp= ρZ.
dx dydz

(3)

The three equations of equilibrium obtained by taking moments round the axes are then found to be satisfied identically.