Abstract

The article discusses nanosized powdery ice-forming reagents, which are supposed to be used in the works on active action on clouds in order to regulate precipitation and hail suppression, as well as to dissipate supercooled fog. These ice-forming reagents have been obtained by the levilite method, in which a layer of silver iodide is deposited on the surface of nanosilica particles. Description of the methodology for studying the effectiveness of nanosized powdery ice-forming reagents, as well as the results of laboratory studies of their effectiveness obtained in different organizations is given. The results of studies of ice-forming reagents carried out at laboratories of RPA “Typhoon”, High-Mountain Geophysical Institute, JSC “Cheboksary production association n.a. V.I. Chapaev” and ANO “Agency of atmospheric technologies” have shown that the efficiency of these reagents differs significantly from those obtained earlier in the Central Aerological Observatory. It has been suggested that the low efficiency of nanosized ice-forming reagents is due to the high aggregation of the original nanosilicum particles, resulting from the high surface activity of these particles. Possible ways to reduce the degree of aggregation of powders by modifying the surface of the original nanoparticles aimed at decreasing the high activity of the nanosilica particles surface are discussed.

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