Formation of NOx and SOx precursors during the pyrolysis of coal and biomass. Part III. Further discussion on the formation of HCN and NH3 during pyrolysis

The formation of HCN and NH3 from the pyrolysis of coal (and biomass) is di scussed based on our experimental data as well as the data in the literatur e, including the pyrolysis of N-containing pyrrolic and pyridinic model com pounds reported in the literature. The pyrolysis of the model compounds and the thermal cracking of coal pyrolysis volatiles appear to he in good qual itative agreement in terms of the onset decomposition temperature, the main intermediates and the final N-containing product (HCN). The formation of N H3 requires the presence of condensed phase(s) of carbonaceous materials ri ch in hydrogen. Direct hydrogenation of the N-sites by the H radicals gener ated in situ in the pyrolysing solid is the main source of NH3 from the sol id. The initiation of the N-containing heteroaromatic ring by radical(s) is the first step for the formation of both HCN and NH3. While the thermally less stable N-containing structures are mainly responsible for the formatio n of HCN, the thermally more stable N-containing structures may be hydrogen ated slowly by the H radicals to NH3. The formation of NH3 and the formatio n of HCN are controlled by the local availability of radicals, particularly the H radicals, in the pyrolysing solid. The increased yield of NH3 (and H CN) with increasing heating rate can he explained by the rapid generation o f the H radicals at high heating rates, favouring the formation of NH3 (and HCN) over the combination of N-containing ring systems within the coal/cha r matrix. The size of the N-containing heteroaromatic ring systems and the types of substitutional groups also play important roles in the formation o f HCN and NH3. (C) 2000 Elsevier Science Ltd. All rights reserved.