F. Sahbaz et al., Moisture sorption and the applicability of the Brunauer-Emmet-Teller (BET)equation for blanched and unblanched mushrooms, NAHRUNG, 43(5), 1999, pp. 325-329
Moisture sorption isotherms of blanched and unblanched mushrooms over 0.11-
0.75 a(w) were determined at 27 degrees C and 37 degrees C by using the sta
tic gravimetric method. Adsorption and desorption behaviors of blanched and
unblanched mushrooms were compared. The unblanched material adsorbed more
water than that of the blanched. In desorption isotherms, the equilibrium m
oisture contents of the unblanched material were found to be higher than th
ose of the blanched throughout the entire a, range. The BET equation was te
sted to fit the experimental moisture sorption data over the 0.11-0.43 a(w)
, 0.11-0.55 a(w), 0.11-0.64 a(w) and 0.11-0.75 a(w). Nonlinear regression a
nalysis was used for the determination of the parameters in the equation. T
he quality of the fit of the BET model over each a, range was judged from t
he value of the relative percent root mean square (% RMS). The moisture sor
ption behavior over 0.11-0.43 a(w) of mushrooms has indicated that the BET
equation is applicable generally up to 0.43 a(w). Monolayer moisture conten
ts and C constants in the BET equation obtained for each a(w) interval were
reported. The water activities corresponding to the monolayer values have
been determined and discussed related to mushroom storage.
The net isosteric hears of adsorption and desorption were estimated from eq
uilibrium sorption data, using the integrated form of the Clausius-Clapeyro
n equation. The heats of adsorption/desorption decreased with increase in m
oisture content and approached to a constant value. It was, concluded that
moisture adsorption/desorption occurred by physical mechanisms at high mois
ture contents,but at low moisture contents, besides physical adsorption, ch
emisorption was also observed.