K Nn mK - Amecamex.org.mx
K Nn mK - Amecamex.org.mx
K Nn mK - Amecamex.org.mx
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product quality needs to be taken into<br />
account during food processing.<br />
Sorption isotherms. Figure 3 shows<br />
the sorption isotherms at 15, 25 and<br />
35C. The figure indicates that there is<br />
a great influence of temperature on<br />
the isotherm sorption. Data are<br />
exponentially distributed as shown in<br />
other high starch products (Chen,<br />
2002).<br />
Water content (g H2O/g d.m)<br />
0.8<br />
0.6<br />
0.4<br />
0.2<br />
15°C<br />
25°C<br />
35°C<br />
0<br />
0.2 0.4 0.6<br />
Aw<br />
0.8 1<br />
Figure 3 Sorption isotherm of Tejate at 15,<br />
25 and 35 C<br />
The Chung-Pfost equation was<br />
linerized to calculate the constant<br />
values<br />
ln<br />
⎛<br />
( − ln Aw ) = ⎜ln<br />
+ ( − b)<br />
M ⎟<br />
⎝ T ⎠<br />
a<br />
where: a=C1/R and b=C2<br />
and also Henderson equation<br />
[ − ln(<br />
1−<br />
A ) ] = ln aT b ln M<br />
ln w +<br />
a=C1 and b=C2.<br />
Table 1 shows the constant values<br />
and the correlation coefficient (r 2 ) for<br />
Chung-Pfost and Henderson models.<br />
The accuracy of models at the<br />
studied temperatures is the same for<br />
both equations. They represent<br />
⎞<br />
isotherm behavior but they were more<br />
accurate at low temperatures than at<br />
high temperatures. Chung-Pfost and<br />
Henderson models have been used<br />
to predict sorption isotherms for<br />
cereals or starchy products (Sun<br />
D.W., 1998, Silakul and Jindal, 2002,<br />
Chen, 2002). Both equations have<br />
been modified to increase their<br />
accuracy. Chung-Pfost equation has<br />
been recommended to use in rice<br />
products and mushroom (Durakova<br />
and Mendkov, 2004, Shivhare et al.,<br />
2004). Figure 4 fits both equations<br />
and experimental results at 15 C.<br />
There is a region between 0.7 and<br />
0.95 of Aw where the isotherm was<br />
not well described by the models.<br />
Table 1. Values of constants and r 2 of<br />
Chung-Pfost and Henderson equations for<br />
Tejate.<br />
Chung-Pfost<br />
a= 668.84<br />
b= 8.5224<br />
Henderson<br />
a= 0.0243<br />
b= 1.1473<br />
r 2<br />
15C 25C 35C<br />
0.9841<br />
0.9851<br />
Water content (g water/g d.m.)<br />
0.6<br />
0.5<br />
0.4<br />
0.3<br />
0.2<br />
0.1<br />
Experimental<br />
Chung-Pfost<br />
Henderson<br />
0.9650<br />
0.9718<br />
0<br />
0 0.2 0.4 0.6 0.8 1<br />
0.9343<br />
0.9469<br />
Aw<br />
Figure 4. Experimental and predicted<br />
absorption isotherms by Chung-Pfost and<br />
Henderson models at 15C