The distribution of water in native starch granules—a multinuclear NMR study

Abstract

The microscopic distribution and dynamic state of water in native potato, maize and pea starch granules are investigated with NMR relaxometry and diffusometry. Besides extra-granular water, three water populations can be identified inside native potato starch granules. These are assigned to water in the amorphous growth rings; water in the semi-crystalline lamellae and “channel water”, which is located in the hexagonal channels within the B-type amylopectin crystals. The first two water populations are orientationally disordered and exchange with each other on a millisecond timescale at 290 K. NMR diffusometry shows that the water in packed granule beds is undergoing translational diffusion in a 2-dimensional space, either in thin layers between granules and/or in amorphous growth rings within the granules. The “channel water” is uniquely characterised by a 1 kHz deuterium doublet splitting and is in slow exchange with water in the other compartments on the NMR timescale. In the smaller maize granules all intra-granular water populations are in fast exchange and there is no evidence for “channel water” in the A-type crystal lattice. The NMR water proton and deuterium data for pea starch are consistent with a composite A and B-type crystal structure.