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DOI: 10.1094/CC-82-0683
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ARTICLE
Thermal Properties of Starch from Exotic-by-Adapted Corn (Zea mays L.)
Lines Grown in Four Environments.
E. Lenihan (1,2), L. Pollak (3), and P. White
(1,4). (1) Graduate student and professor, respectively, 2312 Food Sciences
Building, Department of Food Science and Human Nutrition and Center for Crops
Utilization Research, Iowa State University, Ames, IA 50011. (2) Currently, Food
Technologist, Tate and Lyle, Decatur, IL 62525. (3) Research geneticist,
USDA-ARS, Corn Insects and Crop Genetics Research Unit, Department of Agronomy,
Iowa State University, Ames, IA 50011. (4) Corresponding author. Phone: (515)
294-9688. Fax: (515) 294-8181. E-mail: <pjwhite@iastate.edu> Cereal Chem.
82(6):683-689. Accepted June 21, 2005. Copyright 2005 AACC International, Inc.
The effect of four growing environments (two at Ames, IA; one at Clinton, IL;
and one at Columbia, MO) on the thermal properties of starch from five
exotic-by-adapted corn inbred lines (Chis37, Cuba34, Cuba38, Dk8, Dk10) and two
control lines (B73 and Mo17) were studied using differential scanning
calorimetry (DSC). The variations in thermal properties within environments were
similar for the exotic-by-adapted lines and control lines. Missouri was the
warmest environment and generally produced starch with the greatest
gelatinization onset temperature (T(oG)), the narrowest range of
gelatinization (R(G)), and the greatest enthalpy of gelatinization (DeltaH(G)).
Illinois was the coolest environment and generally resulted in starch with the
lowest T(oG), widest R(G), and lowest DeltaH(G). These
differences were attributed to higher temperatures in Missouri during
grain-filling months either increasing the amount of longer branches of
amylopectin or perfecting amylopectin crystalline structure. The Ames 1
environment produced starch with thermal properties most similar to those of
Illinois, whereas the Ames 2 environment produced starch with thermal properties
most similar to those of Missouri. Ames 2, located near a river bottom where
temperatures tend to be warmer, likely had temperatures most similar to those
found in Missouri during grain filling.
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