Sentence examples for binding of water from inspiring English sources

Hydration (i.e., the binding of water) may also occur at the hydroxyl (−OH) groups of serine and threonine or at the amide (−CONH2) groups of asparagine and glutamine.

The binding of water molecules to either charged or polar (partly charged) groups is explained by the dipolar structure of the water molecule; that is, the two positively charged hydrogen atoms form an angle of about 105°, with the negatively charged oxygen atom at the apex.

For examples, the highly conserved residues P906, G930, N941, R971, and G1010 (Fig. S1) are either directly involved in the formation of the proton-transfer wires, or facilitate binding of water molecules.

LEA proteins have been considered to play roles in maintaining membrane structures, binding of water, and acting as molecular chaperones [ 36].

As the meat pH value was higher than the pI values of myofibrillar proteins, this can also increase the binding of water molecules.

In contrast, the binding of water to the Fe center causes only a modest perturbation to the original Fe ligand bonds, as expected considering that water is a weak field ligand.

MIP syntheses in aqueous solutions may lead to higher selectivity and stronger binding of water-soluble target molecules.

Quasielastic neutron scattering (QENS) has been used to investigate the binding process of water molecules in pastes of calcium geopolymer prepared with low and high calcium fly ash contents, and at two different NaOH molarities, 10 and 14 M.

The maximum dimensions, the shape, and the internal structure of aggregates found at El Chichón and Ilamatepec are similar to those of aggregates formed by the binding action of water.

Alleviation of the effects of soaking injury as a result of the increase in the moisture content of seeds before imbibition is related to the reduced binding energy of water molecules and the appearance of respiratory activity (Vertucci and Leopold, 1984; Ishida et al., 1988 b ).

Particles larger than 1 mm are instead common inside aggregates found at Poás, El Chichón, and Ilamatepec volcanoes; at El Chichón and Ilamatepec, they occur also in the most external rims, which are instead characteristically made of particles only tens of microns in size in pellets formed by the binding action of water.