Ec. Sanford et al., RESIDUUM HYDROCRACKING WITH SUPPORTED AND DISPERSED CATALYSTS - STABLE HYDROGEN AND CARBON-ISOTOPE STUDIES ON HYDROGENATION AND CATALYST DEACTIVATION, Energy & fuels, 9(5), 1995, pp. 928-935
The generally accepted mode of action of Ni- or Co-Mo/Al2O3 catalysts
during hydrocracking of residua is that the catalyst participates in t
he hydrogenation of aromatics which results in heteroatom removal and
CCR conversion. Earlier studies have shown that under hydrocracking co
nditions with residua, the catalyst loses the ability to hydrogenate a
romatics within hours, and thereafter catalysis proceeds by a differen
t mechanism. The established techniques of stable isotope analyses hav
e been used to provide additional support for the proposed mechanism.
The isotope studies showed that in the absence of a catalyst, there wa
s no incorporation of gaseous hydrogen into the residuum fraction and
only a small amount into the distillates. With a fresh catalyst, hydro
gen was incorporated into all fractions initially but hydrogenation of
residuum lasted for only 4 h. When bitumen residuum was hydrogenated
under mild conditions, the added hydrogen was not lost under hydrocrac
king conditions, Addition of gaseous hydrogen to the residuum was depe
ndent on the concentration of catalyst for dispersed catalysts, and ca
talysts previously used under mild conditions in the pilot plant did n
ot show any hydrogen transfer from the gas phase to the residuum fract
ion. In all cases, carbon-to-carbon bond breaking was correlated with
the incorporation of gaseous hydrogen.