The transformation of sodium to particulate matter (PM)
during
lignite combustion has been widely investigated, while the importance
of Ca, Mg, S, and Fe in low-rank coal has been recently revealed.
In this study, three kinds of Zhundong lignites (ZD, YH, and HSY)
rich in Na, Mg, Ca, S, and Fe were selected and the combustion was
conducted in an entrained flow reactor with a furnace temperature
of 1473 K. PM was sampled by a Deakti low-pressure impactor (DLPI),
and the components were analyzed by scanning electron microscopy equipped
with energy-dispersive X-ray spectrometry (SEM–EDS), with the
PM number concentration measured by a scanning mobility particle sizer
(SMPS). The characteristics of PM under air and oxy-fuel (Oxy21, Oxy30,
and Oxy40) atmospheres were compared. The results show that the comparable
O2 concentration is related to coal properties and located
between 30 and 40% for Zhundong lignite. It is acceptable to take
the PM10 mass yield as a reference to reflect the combustion
intensity. An oxy-fuel atmosphere has more effect on PM1–10 than PM1. The participation of Na in PM1 is
highest under Oxy21 combustion, which is enhanced through S and Cl.
An increasing O2 concentration will intensify the fragmentation
and decomposition of Ca-, Mg-, Fe-, and Si-bearing minerals, which
contribute mostly to the production of PM1–10. The
contents of Si–Al-bearing minerals in raw coal significantly
affect the contribution of Fe and S on PM1–10 through
eutectic formation. Besides, the vaporization of inorganic elements
(mostly Ca, Mg, Fe, and Si) will also be enhanced under oxy-fuel combustion
at a higher O2 concentration, increasing the PM1 production and moving the number-based particle size distribution
(NPSD) toward a larger particle size.