The flow field generated by axial oscillations of a finite-length cyli
nder in an incompressible viscous fluid is described by the unsteady S
tokes equations and computed with a first-kind boundary-integral formu
lation. Numerical calculations were conducted for particle oscillation
periods comparable with the viscous relaxation time and the results a
re contrasted to those for an oscillating sphere and spheroid. For hig
h-frequency oscillations, a two-term boundary-layer solution is formul
ated that involves two, sequentially solved, second-kind integral equa
tions. Good agreement is obtained between the boundary-layer solution
and fully numerical calculations at moderate oscillation frequencies.
The flow field and traction on the cylinder surface display several fe
atures that are qualitatively distinct from those found for smooth par
ticles. At the edges, where the base joins the side of the cylinder, t
he traction on the cylinder surface exhibits a singular behaviour, cha
racteristic of steady two-dimensional viscous flow. The singular tract
ion is manifested by a sharply varying pressure profile in a near-fiel
d region. Instantaneous streamline patterns show the formation of thre
e viscous eddies during the decelerating portion of the oscillation cy
cle that are attached to the side and bases of the cylinder. As decele
ration proceeds, the eddies grow, coalesce at the edges of the particl
e, and thus form a single eddy that encloses the entire particle. Subs
equent instantaneous streamline patterns for the remainder of the osci
llation cycle are insensitive to particle geometry: the eddy diffuses
outwards and vanishes upon particle reversal; a simple streaming flow
pattern occurs during particle acceleration. The evolution of the visc
ous eddies is most apparent at moderate oscillation frequencies. Quali
tative results are obtained for the oscillatory flow field past an arb
itrary particle. For moderate oscillation frequencies, pathlines are e
lliptical orbits that are insensitive to particle geometry; pathlines
reduce to streamline segments in constant-phase regions close to and f
ar from the particle surface.