The size and fractal dimension of
asphaltene aggregates were investigated
for two Western Canadian bitumens diluted with n-heptane
at concentrations above the onset of precipitation. Asphaltene aggregate
size distributions were measured over time using focused beam reflectance
and micrographic methods in a series of batch experiments at different n-heptane contents and shear rates. The fractal dimensions
of the aggregates were determined from the volume of the settled aggregates.
The asphaltenes formed approximately log-normal size distributions
with volume mean diameters of tens to hundreds of micrometers, depending
mainly upon the n-heptane content. The distributions
were established in less time than the first measurement could be
obtained (about 30 s) and changed relatively little afterward. The
average aggregate size increased with an increasing n-heptane content but reached a plateau value at 70–80 wt % n-heptane. The fractal dimension reached a maximum at a
similar n-heptane content. Micrographic images and
fractal dimensions indicated that, near the onset of precipitation,
compact linear and planar aggregate structures dominated. At higher n-heptane contents up to approximately 75 wt % n-heptane, the aggregates remained compact but became more three-dimensional.
At higher n-heptane contents, larger, looser structures
were formed that could be broken under sufficient shear but did not
reaggregate. The results were consistent with simultaneous nucleation,
growth, and flocculation processes, where the precipitating material
was initially sticky but lost its stickiness over time. The loss in
stickiness was confirmed with surface force adhesion measurements.