Benchtop Recirculating Tunnel Tray Dryer
Insulated drying duct with variable-speed blower and 3.0 kW electrical finned air heaters.
Determine drying rate curves for a wet porous granular slab in a convective hot-air tray dryer, evaluate the constant drying rate R_c as a function of air velocity v_a, and identify critical moisture content X_c. Explore interactive transport phenomena, unit operations simulation, and chemical engineering telemetry.
Ready to sample with Air Velocity v_a = 3.0 m/s.
Adjust Air Velocity v_a, then execute chemical process trial.
Chemical and process engineering telemetry is evaluated rigorously using 64-bit IEEE 754 precision. Residuals reflect ordinary least-squares regression across successive observations. Continuous data structures support high-fidelity transport phenomena and unit operations modeling.
The transport and thermodynamic models apply within the specified calibrated operating window (1.0 to 6.0 m/s). Evaluated using a 200 mm × 200 mm tray (active area A = 0.040 m^2, dry sand mass L_s = 1.20 kg, initial moisture X_0 = 0.25 kg/kg) in a 50.0 °C drying tunnel. Linear regression models constant drying rate R_c versus (v_a)^0.8 to extract S = 0.6500 kg/(m^2·h)/(m/s)^0.8.
Insulated drying duct with variable-speed blower and 3.0 kW electrical finned air heaters.
Continuously records total tray mass in real-time with 0.01 g precision during drying.
200 mm × 200 mm × 15 mm stainless steel tray (area 0.040 m^2) insulated on sides and bottom.
Measures parallel air sweep velocity v_a from 0.5 to 8.0 m/s with 0.05 m/s precision.
Measures inlet and outlet air dry-bulb temperature (50.0 °C) and wet-bulb temperature (28.0 °C).
Oven dries final solids at 105 °C to establish absolute dry solid mass L_s = 1.200 kg.
Determine drying rate curves for a wet porous granular slab in a convective hot-air tray dryer, evaluate the constant drying rate R_c as a function of air velocity v_a, and identify critical moisture content X_c. Standardized parameter settings: 1.0, 2.0, 3.0, 4.0, 5.0, 6.0 m/s.
Set air heater to 50.0 °C and blower to moderate speed; circulate air for 20 minutes until dry-bulb (50.0 °C) and wet-bulb (28.0 °C) steady state is achieved.
Mix 1.200 kg of dry quartz sand with 300 g of water (X_0 = 0.250 kg/kg); pack into the tray flush with the rim and place onto the balance cradle.
Adjust blower speed to establish air velocity v_a = 1.0 m/s across the tray surface; record initial mass at t = 0.
Log tray mass every 60 seconds over 40 minutes; compute moisture content X(t) and instantaneous drying rate flux R = -(L_s/A) · (dX/dt).
Repeat tests with fresh identical wet slabs at air velocities v_a = 2.0, 3.0, 4.0, 5.0, and 6.0 m/s, recording the constant drying rate plateau R_c for each run.
Plot R versus X to locate critical moisture X_c, plot R_c versus (v_a)^0.8, and fit a linear regression through the origin to determine S.
Points are your recorded observations. The solid regression line validates Convective Tray Drying Kinetics mathematical scaling.
| # | Hot Air Drying Velocity v_a (m/s) | Constant Drying Flux R_c (kg/(m^2·h)) | Air velocity factor (v_a)^0.8 ((m/s)^0.8) | Constant drying rate flux R_c (kg/(m^2·h)) | Remove |
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Drying of moist solids is an energy-intensive simultaneous heat and mass transfer unit operation in chemical engineering, encompassing the manufacturing of pharmaceuticals, pigments, fertilizers, catalysts, polymers, and food products. In convective tray drying, hot dry air sweeps across exposed wet granular slabs placed in shallow trays. Heat conducts and convects from the air stream to the wet solid surface, providing the latent heat required to evaporate moisture, while evaporated water vapor diffuses across the hydrodynamic boundary layer into the bulk air. Plotting the drying rate flux R = - (L_s / A) · (dX / dt) against moisture content X (dry basis, kg water/kg dry solid) reveals characteristic drying periods. In the initial constant-rate drying period (X > X_c), the solid surface is completely saturated with free liquid water, and vaporization proceeds at a constant rate R_c governed purely by external boundary layer heat and mass transfer. Because convective mass transfer across a flat plate scales with air velocity as v_a^0.8 (Reynolds analogy), the constant drying rate follows: R_c = S · v_a^0.8. When moisture drops to the critical moisture content X_c, capillary action can no longer replenish surface water, dry spots appear, and drying enters the falling-rate period where internal moisture diffusion governs drying. In this laboratory investigation, a wet sand slab is dried in a benchtop tunnel tray dryer across air velocities from 1.0 to 6.0 m/s at 50.0 °C to determine the constant drying rate scaling slope S and identify critical moisture content X_c.
Evaluated using a 200 mm × 200 mm tray (active area A = 0.040 m^2, dry sand mass L_s = 1.20 kg, initial moisture X_0 = 0.25 kg/kg) in a 50.0 °C drying tunnel. Linear regression models constant drying rate R_c versus (v_a)^0.8 to extract S = 0.6500 kg/(m^2·h)/(m/s)^0.8.