Coal Moisture Evaporation Model Reference

The Coal Moisture Evaporation model allows the H2O component of the coal particle to lose its mass through a quasi-steady evaporation process.

The coal particle is assumed to be initially coated with moisture so that a single-component evaporation treatment is appropriate. The driving force for evaporation of this layer is the departure from equilibrium of the liquid-vapor system. In coal combustion, the moisture evaporation is usually heat-transfer limited and takes place rapidly. The devolatilization and char oxidation reactions occur after the moisture has evaporated.

The formulation is that of the Quasi-Steady Single-Component Droplet Evaporation model as applied to a water droplet, and the associated Sherwood and Nusselt numbers are calculated using the Ranz-Marshall correlation.

Table 1. Coal Moisture Evaporation Model Reference
Theory See Droplet Evaporation
Provided By [Lagrangian Phase] > Models > Moisture Evaporation
Example Node Path [physics continuum] > Models > Lagrangian Multiphase > Lagrangian Phases > [Phase 1] > Models > Coal Moisture Evaporation
Requires In the continuous phase, either:
  • Material: Gas
  • Flow: any
  • Optional Models: Lagrangian Multiphase
  • Material: Multi-Component Gas
  • Reaction Regime: Non-reacting
  • Flow: any
  • Optional Models: Lagrangian Multiphase
Then, in a Lagrangian phase:
  • Particle Type: Material Particles
  • Material: Multi-Component Coal
  • Mass Transfer: Coal Combustion
Activates Field Functions Coal Moisture Latent Heat of Vaporization (H2O), Coal Moisture Saturation Pressure (H2O). See Field Functions.

Field Functions

Coal Moisture Latent Heat of Vaporization (H2O)
Coal Moisture Saturation Pressure (H2O)