Page 185 - Biomass Gasification, Pyrolysis And Torrefaction Practical Design and Theory
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162                          Biomass Gasification, Pyrolysis and Torrefaction


               Temperature has a major influence on the product of pyrolysis. The
            carbon dioxide yield is high at lower temperatures and decreases at higher

            temperatures. The release of hydrocarbon gases peaks at around 450 C and
            then starts decreasing above 500 C, boosting the generation of hydrogen.

               Hot char particles can catalyze the primary cracking of the vapor released
            within the biomass particle and the secondary cracking occurring outside the
            particle but inside the reactor. To avoid cracking of condensable gases and
            thereby increasing the liquid yield, rapid removal of the condensable vapor
            is very important. The shorter the residence time of the condensable gas in
            the reactor, the less the secondary cracking and hence the higher the liquid
            yield.
               Some overlap of the stages in the pyrolysis process is natural. For example,
            owing to its low thermal conductivity (0.1 0.05 W/m K), a large log of wood
            may be burning outside while the interior may still be in the drying stage, and
            water may be squeezed out from the ends. During a forest fire, this phenome-
            non is often observed. The observed intense flame comes primarily from the
            combustion of the pyrolysis products released from the wood interior rather
            than from the burning of the exterior surface.


            5.4.2 Chemical Aspects

            As mentioned earlier, a typical biomass has three main polymeric compo-
            nents: (i) cellulose, (ii) hemicellulose, and (iii) lignin. These constituents
            have different rates of degradation and preferred temperature ranges of
            decomposition.


            5.4.2.1 Cellulose
            Decomposition of cellulose is a complex multistage process. A large number
            of models have been proposed to explain it. The Broido Shafizadeh model
            (Bradbury et al., 1979) is the best known and can be applied, at least qualita-
            tively, to most biomass (Bridgwater et al., 2001).
               Figure 5.9 is a schematic of the Broido Shafizadeh model, according to
            which the pyrolysis process involves an intermediate prereaction (I) followed
            by two competing first-order reactions:
              Reaction II: dehydration (dominates at low temperature and slow heating
               rates)
              Reaction III: depolymerization (dominates at fast heating rates).
               Reaction II involves dehydration, decarboxylation, and carbonization
            through a sequence of steps to produce char and noncondensable gases
            like water vapor, carbon dioxide, and carbon monoxide. It is favored at low
            temperatures, of less than 300 C (Soltes and Elder, 1981, p. 82) and slow

            heating rates (Reed, 2002, p. II-113).
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