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Joint International Conference on Long-term Experiments ...

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During the chemical changes the pore structure is opened up and becomes c<strong>on</strong>tinuous. In<br />

this new pore system the water is more free to move. As can be seen from the results, the<br />

measured water c<strong>on</strong>tent in the centre starts to increase at approximately 70±5 0 C, which<br />

c<strong>on</strong>firms the theory that the water is not free to move until the structural change occurred.<br />

The partial water vapour pressure gradient caused by the temperature gradient attempts to<br />

reduce itself.<br />

Figure 3: Typical diagram of the changes in water c<strong>on</strong>tent under the top crust of the loaf.<br />

The decrease in water c<strong>on</strong>tent during the first period in the oven is a measured decrease<br />

<strong>on</strong>ly, not an actual decrease. When the temperature has reached 70±5 0 C the water<br />

c<strong>on</strong>tent increases with approximately 3 g water/100 g bread and then slowly decreases<br />

with approximately 13 g water/100 g bread<br />

The water vapour therefore starts to move towards the centre and towards the surface. As<br />

can be seen in Figure 2 the water c<strong>on</strong>tent appears to increase in the centre when the<br />

temperature has reached 70±5 0 C, and appears to decrease 1 cm from the bottom surface. At<br />

1 cm under the top crust, Figure 3, the results show an increase in the measured water<br />

c<strong>on</strong>tent immediately after the temperature has reached 75 0 C. This is probably due to the<br />

transport of water vapour towards the colder parts being prevented by the dough. Only when<br />

the interior has changed to bread can the water move freely. Part of the rise could also be<br />

due to compressi<strong>on</strong> of the crumb near the surface, as the crust has started to form and the<br />

interior is still rising. Part of the rise could therefore be a measured rise <strong>on</strong>ly and not an<br />

actual rise. Figure 4 shows the cross secti<strong>on</strong> of a loaf with a rough divisi<strong>on</strong> into regi<strong>on</strong>s of<br />

increasing and decreasing water c<strong>on</strong>tent, at the time point when the loaf is removed from the<br />

oven. The water c<strong>on</strong>tents of the regi<strong>on</strong>s have been estimated as a mean value from the<br />

measured water c<strong>on</strong>tents. The water c<strong>on</strong>tent of the dough was 41.8 g waterr100 g dough.<br />

The crust is set at 0 g water/100 g bread, the regi<strong>on</strong> below the top crust, DV10 decreasing<br />

417

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