In most studies, the properties of dust-acoustic solitons are derived from
the first integral of the Poisson equation, in which the shape of the pseudopotential
determines both the conditions in which a soliton may exist and its amplitude. Here
this first integral is interpreted as conservation of total momentum, which, along
with the Bernoulli-like energy equations for each species, may be cast as the structure
equation for the dust (or heavy-ion) speed in the wave. In this fluid-dynamic
picture, the significance of the sonic points of each species becomes apparent. In the
wave, the heavy-ion (or dust) flow speed is supersonic (relative to its sound speed),
whereas the protons and electrons are subsonic (relative to their sound speeds),
and the dust flow is driven towards its sonic point. It is this last feature that limits
the strength (amplitude) of the wave, since the equilibrium point (the centre of
the wave) must be reached before the dust speed becomes sonic. The wave is characterized
by a compression in the heavies and a compression (rarefaction) in the
electrons and a rarefaction (compression) in the protons if the heavies have positive
(negative) charge, and the corresponding potential is a hump (dip). These features
are elucidated by an exact analytical soliton, in a special case, which provides the
fully nonlinear counterpoint to the weakly nonlinear sech2-type solitons associated
with the Korteweg–de Vries equation, and indicates the parameter regimes in which
solitons may exist.