The precipitation and redissolution of asphaltenes upon the addition and re
moval of solvent were investigated for Athabasca and Cold Lake bitumens usi
ng a flow-loop apparatus. The presence of precipitate was detected through
an increase in pressure drop across an in-line filter. These solvent-revers
ibility experiments were conducted at 40 and 60 degreesC with n-heptane sol
vent. A significant hysteresis was observed for Athabasca bitumen while lit
tle or no hysteresis was observed for Cold Lake bitumen. In both cases, the
precipitation could be completely reversed. Temperature-reversibility was
also investigated with n-dodecane solvent at temperatures ranging from 40 t
o 160 degreesC. A hysteresis was observed for both bitumens and only partia
l reversibility was achieved. Benchtop solvent-reversibility experiments we
re also conducted on the two bitumens at room temperature. In this case, th
e precipitate was recovered by centrifugation. The benchtop results were in
good agreement with the flow-loop experimental results. Two heavy oils wer
e also tested and both exhibited hysteresis and complete reversibility. Pre
cipitation and redissolution in n-heptane were measured over time for the A
thabasca bitumen. Precipitation increased over time reaching an apparent eq
uilibrium after 8 days. Redissolution experiments reached virtually the sam
e equilibrium position in less than 1 day. The slow kinetics of precipitati
on suggests rate-limiting nucleation, growth, or flocculation of the asphal
tenes. Redissolution experiments with their more rapid kinetics are better
suited for obtaining equilibrium solubility data.