In this study, ash
transformation during fixed-bed combustion of
different agricultural opportunity fuels was investigated with a special
focus on potassium (K) and phosphorus (P). The fuel pellets were combusted
in an underfed fixed-bed pellet burner. Residual ashes (bottom ash
and slag) and particulate matter were collected and characterized
by scanning electron microscopy–energy-dispersive X-ray spectroscopy,
X-ray diffraction, inductively coupled plasma, and ion chromatography.
The interpretation of the results was supported by thermodynamic equilibrium
calculations. For all fuels, almost all P (>97%) was found in residual-/coarse
ash fractions, while K showed different degrees of volatilization,
depending on fuel composition. During combustion of poplar, which
represents Ca–K-rich fuels, a carbonate melt rich in K and
Ca decomposed into CaO, CO2, and gaseous K species at sufficiently
high temperatures. Ca5(PO4)3OH was
the main P-containing crystalline phase in the bottom ash. For wheat
straw and grass, representing Si–K-rich fuels, a lower degree
of K volatilization was observed than for poplar. P was found here
in amorphous phosphosilicates and CaKPO4. For wheat grain
residues, representing P–K-rich fuels, a high degree of both
K and P retention was observed due to the interaction of K and P with
the fuel-bed constituents, i.e., char, ash, and slag. The residual
ash was almost completely melted and rich in P, K, and Mg. P was found
in amorphous phosphates and different crystalline phases such as KMgPO4, K2CaP2O7, K2MgP2O7, and K4Mg4(P2O7)3. In general, the results therefore
imply that an interaction between ash-forming elements in a single
burning fuel particle and the surrounding bed ash or slag is important
for the overall retention of P and K during fuel conversion in fixed-bed
combustion of agricultural biomass fuels.