Oxygen
consumption and deposition measurements of model fuel mixtures
and real fuels are used to explore the roles that heteroatomic fuel
species and their interactions play during fuel autoxidation. A range
of temperatures, oxygen consumption regimes, and flow environments
are employed to provide results applicable over a wide range of fuel
autoxidative conditions. The quartz crystal microbalance (QCM) provides
a low temperature (140 °C) batch reactor environment for long
reaction times (minutes to hours) with oxygen consumption and sensitive,
in situ deposition measurements. The JFTOT system provides a flowing
environment at higher temperatures (260 to 300 °C) and short
residence times (seconds) which is modified with both an outlet oxygen
sensor and with quantitative deposition measurements via ellipsometry.
These techniques are used to study model systems (Exxsol D80 with
added heteroatom species) and real jet fuels to determine the role
of heteroatomic species in jet fuel autoxidation and deposition. The
QCM results demonstrate that nitrogen and sulfur species (e.g., indoles/anilines
and sulfides) interact during jet fuel autoxidation to encourage deposit
formation. The further addition of phenol species, which occur naturally
in most petroleum-derived jet fuels, facilitates even greater deposit
production. This behavior is confirmed in the JFTOT via addition of
nitrogen and sulfur-containing species to medium and low sulfur jet
fuels. These results, along with gas chromatographic (GC) analysis
of samples collected during autoxidation in the QCM, show rapid sulfur
autoxidation followed by a slower reaction of the nitrogen species
to form deposit precursors, implying a stepwise reaction of sulfur
oxidation products with nitrogen species to form deposit precursors.
These results have important implications for fuel production strategies
and mitigation of thermal stability degradation during fuel pipeline
transport, storage, and use.