PHASE-TRANSITIONS OF THE STARCH-WATER SYSTEM

被引:794
作者
DONOVAN, JW
机构
[1] Western Regional Research Center, Agricultural Research Service, Usda, Berkeley, California
关键词
D O I
10.1002/bip.1979.360180204
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
When purified potato starch granules are heated in the presence of limited amounts of water (less than 1.5 H2O: starch, w/w), two endothermic transitions are observed by differential scanning calorimetry. The lower temperature endotherm is always observed at a fixed temperature, 66°C; it is the only endotherm observed when excess water is present. The higher temperature endotherm is observed at increasing temperatures as the water content is decreased. The size of this endotherm decreases with water content. The appearance of the higher temperature endotherm allows the determination of the stoichiometry for full hydration of starch, 14 H2O/hexose unit. The shift of the higher temperature endotherm is interpreted as the lowering of the melting point of starch crystallites by solvent water. Copyright © 1979 John Wiley & Sons, Inc.
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页码:263 / 275
页数:13
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