Methods
of experimental research and quantum chemical calculation
were combined to study the effect of kaolin on ash melting characteristics
of Zhundong high alkali coal and the mineral evolution law during
ash melting processes. Furthermore, the behavior mechanism of kaolin
capturing alkali metal was also studied from the perspective of mineral
microstructure features. The results show that the melting temperature
of Zhundong high alkali coal ash have rapid rise first and then gradually
decreased with the amounts of kaolin increasing. When the adding proportion
of kaolin is greater than 10%, the improving efficiency on the ash
melting temperature become weakened. Once kaolin was added in Zhundong
high alkali coal, anorthite, anhydrite, albite, and muscovite would
be generated among the temperature range from 1000 to 1200 °C,
Na+ or K+ that easy to volatile and form eutectics
have been captured by the Si–Al system, some mullite generated
among the temperature range from 1200 to 1300 °C. Investigating
the capture mechanism, it indicates that O (26) and O (22) have electrophilic
reaction with Na+ and K+ easily, which would
promote the rupture of aluminum–oxygen bonds. The O2– of alkali metal or alkaline earth metal oxide would easily have
nucleophilic reaction with Si (6) and Si (8) and prompt the rupture
of bridging oxygen bonds (Si–O–Si). Kaolinite would
be transformed into high melting point minerals that contain Na+ or K+ which have trend to form eutectics or evaporate
into the flue gas easily, and the degree of fouling and slagging on
the heating surface can be reduced based on the two easiest reaction
paths.