Guelph Food Research Centre, Canada.
Ann N Y Acad Sci. 2010 Feb;1189:55-61. doi: 10.1111/j.1749-6632.2009.05200.x.
Wheat starch gels containing 56.0% of water were obtained during thermal gelatinization under isobaric conditions at different pressures ranging from 0.5 to 100 MPa. Thermogravimetric analysis allowed determination of pressure influence on water behavior in gel matrix. The vaporization rate indicated that water is released in two main steps. The first step corresponds to the diffusion of the water fraction (so-called nonbound water) from the porous structure of the amylose gel located between partially swollen starch granules. However, the second step that appears at higher temperature is related to the desorption of water molecules (bound water), included in the swollen granules. It was observed that the most important influence of pressure on water partitioning in the starch gel took place over a pressure range from 0.5 to 10 MPa. The results obtained indicate that pressure is a thermodynamical parameter, which stabilizes the native state of starch granules.
在等压条件下,不同压力(0.5-100 MPa)下的热凝胶化过程中得到了含有 56.0%水的小麦淀粉凝胶。热重分析允许确定压力对凝胶基质中水分行为的影响。蒸发速率表明水是分两步释放的。第一步对应于水(所谓的非结合水)从位于部分溶胀淀粉颗粒之间的直链淀粉凝胶的多孔结构中扩散。然而,在较高温度下出现的第二步与包括在溶胀颗粒中的水分子(结合水)的解吸有关。观察到压力对淀粉凝胶中水分分配的最重要影响发生在 0.5-10 MPa 的压力范围内。所得结果表明,压力是热力学参数,它稳定了淀粉颗粒的天然状态。