| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 239282 | Powder Technology | 2007 | 8 Pages |
This paper describes a numerical investigation of heat and moisture transfer in a bed of porous polycrystalline potash pellets. In this study a non-equilibrium mathematical model of temperature and moisture distribution within the bed was developed. Simulations were performed for a bed of potash pellets that is subjected to flows of humid air on the upper boundary and a cold impermeable surface on the lower boundary. The numerical predictions are in good agreement with the experiments and within the experimental uncertainty bounds. The model predicts that beds of porous potash pellets will contain less moisture than other types of potash fertilizer beds that are exposed to the same environmental conditions. The predictions also indicate that most of the accumulated moisture will be located in the top 10% of the bed and that the pore space relative humidity will be much greater than the supply air relative humidity.
Graphical abstractThis paper describes a model of moisture and heat transfer in through beds of polycrystalline, porous particles that are exposed to flow across the top of the bed and a cold impermeable bottom plate. The numerical predictions are in good agreement with the experimental measurements and it was predicted that most moisture adsorption will occur in the top part of the beds.Figure optionsDownload full-size imageDownload as PowerPoint slidePredicted moisture accumulation profile for T∞ = 22 °C, ϕ∞ = 70%, Tc = 0 °C, ReD = 4000, t = 12h. Mass fraction basis. Position (m) = 0 is the bed bottom.
