The
aging of alkali-bromide-containing ash deposits was studied
by applying premixed alkali bromide–alkali sulfate mixtures
on a laboratory-scale temperature gradient probe. The probe temperature
was kept at 500 °C, while the furnace air temperature was measured
to be 800 °C, simulating a heat exchanger ash deposit temperature
profile. Deposits of ∼5 mm thick were aged in the furnace for
2–8 h and subsequently rapidly cooled to room temperature.
The deposit cross-sections were analyzed and characterized using SEM/EDX.
The deposits were observed to form multilayered structures, where
the furnace-facing region was dense and sintered, while the steel-facing
region was porous. Within the porous region, a gas phase migration
of alkali bromides toward the colder temperature was observed. The
alkali bromide migration toward the colder steel temperature observed
in the experiments was quantified and compared to modeling results.
The modeling results were calculated by modifying an existing temperature-gradient-driven
alkali chloride intradeposit migration model for alkali bromides.
The model is in agreement with the experimental results, validating
an enrichment mechanism for alkali bromides. Because of their relatively
high saturation pressures, alkali bromide migration was observed to
be significantly faster than the earlier reported migration of alkali
chlorides. Enrichment of alkali bromides in colder temperatures in
boiler deposits could lead to significant changes in the local composition
of the deposit, possibly leading to an enhanced corrosion rate of
the tube material and/or densification of the deposit structure.