(95a) Analysis of Upstream Creeping Reaction Zones in Catalytic Monolith Reactors
AIChE Annual Meeting
Monday, November 14, 2016 - 8:00am to 8:20am
of Upstream Creeping Reaction Zones in Catalytic Monolith Reactors
Tian Gu and Vemuri Balakotaiah
of Chemical and Biomolecular Engineering, University of Houston, TX-77204
reactors are widely used in catalytic after-treatment systems (e.g. TWC, DOC,
LNT and SCR). One major challenge in exhaust after-treatment is reducing cold
start emissions which accounts for a significant fraction of the total
emissions. Recent developments in advanced combustion strategies such as low
temperature combustion (LTC) make abating cold start emissions and meeting
environmental regulations even more challenging.
During a cold
start, ignition can occur at the front-end, in the middle or at the back-end of
the reactor. After the reactor is ignited, it is desired that the reaction zone
is maintained close to the inlet so that when small excursions in gas velocity,
inlet temperature and concentrations do not quench the reactor. This can be achieved
if front-end ignition is possible (which requires high precious metal loading
and/or high inlet temperature and/or high adiabatic temperature rise). While front-end
ignition is technologically possible, it may be economically impractical. In
such cases, back-end ignition followed by a fast upstream creeping reaction
zone provides a feasible way to reduce cold start emissions.
In this work,
the upstream creeping reaction zone is investigated in detail using a modeling
approach. The effects of various design parameters (e.g. solid thermal conductivity,
heat capacity, etc.) and operating conditions (gas velocity, inlet
temperature/concentrations) on the creep velocity are determined and summarized
as a correlation. Analytical criteria for reaction zones to creep upstream are also
presented. These criteria can provide guidance for both design and control of
catalytic after-treatment systems.
Fig.2 Creep velocity as a function
of the gas velocity with different adiabatic temperature rise.