The chemical reactions and mass transfer processes occurring within a single coal particle during high temperature hydropyrolysis are described mathematically and the model is tested using extant experimental data. A significant feature of the model is the treatment of bulk flow due to the evolution of volatiles and the resulting balance between diffusion, bulk flow, and chemical reaction. Predictions of the variations in conversion due to changes in total pressure, hydrogen partial pressure, and particle size agree quantitatively with experimental data. The objectives of this study were to develop a model of the chemical reactions and transport processes taking place within a small coal particle after exposure to hot hydrogen at high pressures and to test the predictions using extant experimental data. Such a model provides a means for understanding the effects of process variables (principally temperature, pressure, particle size, and residence time) on the yields from a given coal. Previous work on single-particle models focuses on the various chemical reaction rates and either ignores mass transport processes completely or lumps the resistance into a film coefficient. Although such models can often be adjusted to fit data for a given particle size, the sharp increase in yield observed as particle size is decreased appears to be beyond their predictive capabilities. To illustrate the role of mass transfer by bulk flow and diffusion, the kinetics of the devolatilization process and the time temperature history of the particle have been simplified by assuming a single first-order devolatilization reaction, instantaneous heatup to an isothermal state, and a long reaction time.
CONCLUSIONS AND SIGNIFICANCEA theory has been developed to describe the chemical reactions and mass transfer processes occurring in a single coal particle during hydropyrolysis. The particle is assumed to maintain a porous structure throughout decomposition, with volatiles transported by diffusion and hydrodynamic flow. Chemical reactions are described in terms of the weight loss kinetics developed by previous workers and include the primary devolatilization of the coal, secondary reactions of free radicals, and direct hydrogenation of char. Order of magnitude estimates are used to show that bulk flow and the combination of free radicals with hydrogen are rapid compared to devolatilization, while diffusion is generally slow. The corresponding mathematical simplifications in the conservation equations lead to analytical solutions for the instantaneous rate of evolution of volatiles. Total yields obtained by integrating over an idealized temperature history agree closely with experimental data for variations in pressure, hydrogen partial