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Equilibrium Moisture Content (EMC) in Drying. Muanmai Apintanapong. Moisted air. At equilibrium : determine Moisture content Temperature RH EMC : Loss of water = desorption Gain of water = adsorption. Constant T, RH. sample. Heated air. Ideally Desorption and Adsorption. Desorption.
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Equilibrium Moisture Content (EMC)in Drying MuanmaiApintanapong
Moisted air • At equilibrium : determine • Moisture content • Temperature • RH • EMC : • Loss of water = desorption • Gain of water = adsorption Constant T, RH sample Heated air
Ideally Desorption and Adsorption Desorption EMC Time Adsorption
Practically Desorption and Adsorption Desorption EMC Time Adsorption
Relationship between EMC and RH • EMC Isotherms EMC Desorption Adsorption RH
Relationship between EMC, T and RH Low Temp High Temp
Types of Equations (Models) used to represent EMC Data or Isotherm • 3 variables : RH, MC and T • MC = f (RH, T) • EMC = f (ERH, T) at equilibrium • RH = f (MC, T)
Henderson’s equation • Use in grain and food materials 1 – RH = exp(-c.T.Mn) Where c, n = constant RH = relative humidity in decimal M = moisture content in %db T = temperature in Rankin
Modified Henderson’s equation • For desorption isotherms (drying) 1 – RH = exp[-K.(T+C)(100.M)N] Where c, n = constant RH = relative humidity in decimal M = moisture content in %db T = temperature in Rankin
Chung’s equation • For desorption isotherms (drying) RH = exp[-A/(T+c) exp(-B.M)]