Since the late 1960s,
differential scanning calorimetry (DSC) has
been used to characterize petroleum bitumen, in particular, for the
determination of the crystallized fraction (CF) content. This procedure
is based on the construction of a baseline after identifying the CF
dissolution endotherm on the heating curve. However, many bitumens
commonly exhibit double-peak endotherms during a DSC heating scan.
In this case, the task of constructing the corresponding baseline
does not have a unique solution because the interpretation of the
heat flow profile is ambiguous. Several interpretations have been
proposed earlier to explain the origins of the double-peak endotherm.
However, the double-peak endotherm is currently still not fully understood,
and a comprehensive consensus has not been achieved. If the determination
of the baseline location is incorrect, the CF content can be over-
or underestimated by 20–30%. In the current work, double-peak
endotherm behavior was investigated by temperature modulation DSC.
All of the earlier explanations were critically considered. The origin
of the double-peak endotherm was discussed in detail, and a probable
descriptive model for the formation of the double-peak endotherm was
suggested. The endotherm pattern is assumed to be governed by three
overlapping thermal events: a broad endothermic background and a twin
“recrystallization exotherm–dissolution endotherm”
pair. The onset of the recrystallization exotherm and the intensity
of both events depend on the annealing temperature and time. The study
promotes a better understanding of the relationship between the thermal
effects on the DSC curves and the structural changes of bitumen. A
correct interpretation of the double-peak endotherm can provide a
more exact determination of the CF content in bitumen.