Starch Granule Hydration—A MAS NMR Investigation

Abstract

Starch is the most important energy resource in human diet, and starch is used extensively as a food ingredient to manipulate the quality of our food. In both applications, starch functionality is intimately related to its hydration level. This paper aims at elucidating the starch granule hydration by investigating genotype-specific differences for native wheat, maize, and potato starches by 1H high-resolution (HR) magic angle spinning (MAS) nuclear magnetic resonance (NMR) spectroscopy. The preparations as analyzed in D2O suspensions at room temperature provided NMR spectra with large differences in signal-to-noise (S/N) ratio ranging over several orders of magnitude. It was possible to assign a wide range of components including anomeric α-1,4 and α-1,6-protons from reducing and non-reducing ends, respectively. We utilized the effect that only mobile protons (e.g, dissolved or partially hydrated) are observed using 1H HR-MAS spectroscopy, whereas immobile protons (e.g., in water-inaccessible regions) of the starch granule are not observed due to strong homonuclear interactions to verify the hypothesis that the variations in signal intensities between the different starches are caused by genotype-specific variations in assembly of the starch granules and that the signal intensity, thus, indicates the extent of accessible granule hydration surfaces. Moreover, events taking place during thermal starch granule hydration (gelatinization) were investigated for ten representative starches. NMR spectra of suspended samples were acquired at 30, 45 and 70 °C and again after cooling at 30 °C. A substantial increase in NMR signal intensity occurs above the gelatinization temperature due to extensive proton mobilization in the starch granule assembly. The relative integrated spectral intensities at 30 °C before and after gelatinization at 70 °C showed differences in gain factors between 4 and 193. Also, 31P MAS NMR spectra displayed a similar significant intensity gain upon gelatinization. The results showed that the phosphate groups in the starch granule are mobilized concomitantly with the protons and thus deeply “buried” in the immobile (water inaccessible) domains.