In analysing fluid forces on a moving body, a natural approach is to seek a
component due to viscosity and an inviscid' remainder. It is also attractive to decompose the velocity field into irrotational and rotational parts, and apportion the force resultants accordingly. The irrotational’ resultants can
then be identified as classical added mass', but the remaining, rotational’,
resultants appear not to be consistent with the physical interpretation of the
rotational velocity field (as that arising from the fluid vorticity with the
body stationary). The alternative presented here splits the inviscid resultants
into components that are unquestionably due to independent aspects of the
problem: convective' and accelerative’. The former are associated with the
pressure field that would arise in an inviscid flow with (instantaneously) the
same velocities as the real one, and with the body’s velocity parameters —
angular and translational — unchanging. The latter correspond to the pressure
generated when the body accelerates from rest in quiescent fluid with its given
rates of change of angular and translational velocity. They are reminiscent of
the added-mass force resultants, but are simpler, and closer to the standard
rigid-body inertia formulae, than the developed expressions for added-mass
force and moment. Finally, the force resultants due to viscosity also include a
contribution from pressure. Its presence is necessary in order to satisfy the
equations governing the pressure field, and it has previously been recognised
in the context of `excess’ stagnation-point pressure. However, its existence
does not yet seem to be widely appreciated.

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