UDC 544.723We have used low-temperature 1 H NMR spectroscopy to determine the thermodynamic characteristics of water bound to OX-50 nanosilica (S BET ≈ 50 m 2 /g) in different media: aqueous, air, chloroform medium, and gaseous methane. We demonstrate the difference between the hydration parameters of silica OX-50 on going from an aqueous suspension to a hydrated powder. We present the water cluster size distributions in the studied systems, calculated from the Gibbs-Thomson equation. We found that the average water cluster size in suspension is considerably larger than the cluster sizes in hydrated powders.Introduction. Highly dispersed silicas, synthesized by means of high-temperature hydrolysis of silicon tetrachloride in the flame of a hydrogen/oxygen torch, are widely used in many areas of technology as polymer fillers, thixotropic additives, adsorbents effectively binding organic materials of medium and high molecular weight, etc.[1-3]. Highly dispersed silicas have a rather complex structural hierarchy: protoparticles (<1 nm), primary particles (5-100 nm), aggregates of primary particles (<1 μm, secondary particles), agglomerates of aggregates (1-50 μm, tertiary particles), and visible particles. Secondary particles of highly dispersed silica, with high specific surface area, are often rather stable in aqueous medium and cannot be broken down (or reformed) to individual primary particles even with high-intensity sonication [4]. Aggregation of primary particles of highly dispersed silica is responsible for the presence of textured porosity: voids between the primary particles in the aggregates and agglomerates [4][5][6][7]. Highly dispersed silica is a hydrophilic material, capable of binding a large amount of water in a liquid medium. The amount of bound water depends on the characteristic features of the interparticle interactions, i.e., on the nature of the textured porosity, the surface charge density on the nanoparticles, the composition of the dispersion medium, and the temperature. If there are significant electrostatic repulsion forces between the particles (at a pH far from the zero charge point), then even concentrated suspensions may not go to the gel-like state and may have a viscosity close to the viscosity of water. However, formation of a three-dimensional network of interparticle bonds (a continuous cluster) at low surface charge density leads to rapid gel formation in the system, in which a significant part of the water is found in the bound state [4,8]. On the other hand, powders of nanosilicas, not in contact with liquid water, absorb a relatively small amount of water from the air. Under normal conditions (293 K and relative air humidity 70%), the moisture content of silicas is no greater than 2-5%, i.e., interaction of highly dispersed silicas with water is determined not only by the presence of a significant concentration of primary adsorption centers (OH groups) but also by the relative positions of the primary silica particles, their surface roughness, and also the medium in which th...