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Water and salt diffusion during cheese ripening : effect of the external and internal resistances to mass transfer

机译:奶酪成熟过程中的水和盐分扩散:内部和内部阻力对传质的影响

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摘要

High humidities of drying medium lead to lower drying rates, and both external or internal conditions determine the drying rate. Thus, a diffusional model has been developed assuming that the external resistance to mass transfer could not be neglected in these cases and solved by a finite difference method. The external mass transfer coefficient was estimated from the literature. This mathematical model was used to identify water and salt effective diffusivity coefficients by using experimental data of ripening experiments carried out on parallelepipedal Mahon cheeses of 0.14 m × 0.14 m × 0.09 m edges kept at 12℃ and 85/100 RH. Using these identified values, 7.8 × 10~-12 m~2/s for moisture diffusion and 5.3 × 10~-10 m~2/s for salt diffusion, average moisture content and water and salt profiles during the ripening of 0.20 m × 0.20 m × 0.10 m cheeses ripened at 12℃ and two different relative humidities, 70/100 and 80/100 RH, were accurately simulated.
机译:干燥介质的高湿度导致干燥速率降低,并且外部或内部条件都决定了干燥速率。因此,假设在这些情况下不能忽略对传质的外部阻力,并通过有限差分法求解,则建立了扩散模型。外传质系数是根据文献估计的。该数学模型通过使用在0.14 m×0.14 m×0.09 m边缘的平行六面体Mahon干酪在12℃和85/100 RH下进行的熟化实验的实验数据来识别水和盐的有效扩散系数。使用这些确定的值,水分扩散时为7.8×10〜-12 m〜2 / s,盐扩散时为5.3×10〜-10 m〜2 / s,平均水分为0.20 m×精确模拟了在12℃和两种不同的相对湿度70/100和80/100 RH时成熟的0.20 m×0.10 m奶酪。

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