Laboratory Thin-Layer Drying Wind Tunnel
Insulated aerodynamic duct delivering precisely controlled temperature, velocity, and humidity.
Investigate the forced-air thin-layer drying kinetics of agricultural cereal grain, determine moisture ratio decay over time, and evaluate Page model drying parameters. Explore interactive farm machinery simulation, irrigation hydraulics, and agricultural engineering telemetry.
Ready to sample with ln(Time t) = 3.4012 ln(min).
Adjust ln(Time t), then execute agricultural trial.
Agricultural engineering telemetry and biosystems states are evaluated rigorously using 64-bit IEEE 754 precision. Residuals reflect ordinary least-squares regression across successive observations. Continuous data structures support high-fidelity agricultural and environmental modeling.
Page's model is purely empirical; its parameters n_p and k_p do not directly represent fundamental physical transport properties like Fickian diffusivity. Evaluated using rough paddy rice (initial moisture 24.5% d.b., equilibrium moisture 9.2% d.b.) dried under forced air at 50°C and 1.2 m/s face velocity.
Insulated aerodynamic duct delivering precisely controlled temperature, velocity, and humidity.
Suspends the grain tray inside the air duct, recording mass loss every 10 seconds without stopping airflow.
Maintains drying air temperature at exactly 50.0°C within ±0.2°C precision.
Holds a single layer of grain kernels (300 g) with 85% open mesh area for unrestricted airflow.
Measures face air velocity entering the grain layer with 0.05 m/s precision.
Logs drying air psychrometric properties at the test section inlet.
Investigate the forced-air thin-layer drying kinetics of agricultural cereal grain, determine moisture ratio decay over time, and evaluate Page model drying parameters. Standardized parameter settings: 2.3026, 2.7081, 3.2189, 3.6889, 4.0943, 4.4998 ln(min).
Turn on the tunnel blower and PID heater, setting airflow to 1.2 m/s and air temperature to 50.0°C, allowing the empty duct to reach steady thermal equilibrium for 20 minutes.
Determine initial grain moisture content M_0 via rapid moisture tester (24.5% d.b.). Tare the suspended perforated tray on the continuous balance.
Evenly spread 300.0 g of moist paddy rice in a single kernel layer across the tray, immediately inserting it into the drying air stream and zeroing the timer at t = 0.
Log instantaneous tray mass m(t) at 10, 15, 25, 40, 60, and 90 minutes as moisture evaporates into the conditioned air stream.
Convert instantaneous mass into dry-basis moisture M_t, calculate Moisture Ratio MR = (M_t - M_e) / (M_0 - M_e), and compute the double logarithm ln[-ln(MR)].
Plot ln[-ln(MR)] against ln(t), perform linear regression, and extract Page's drying exponent n_p and drying rate constant k_p.
Points are your recorded observations. The solid regression line validates Thin-Layer Drying Kinetics mathematical scaling.
| # | Logarithm of Drying Time ln(t) (ln(min)) | Double Logarithm ln(-ln(MR)) (transformed) | ln(Drying time t in min) | ln(-ln(Moisture ratio MR)) | Remove |
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