Abstract
It is recommended to use the given relationships when designing dikes of reservoirs operated under conditions similar to the conditions of the Kiev PSS reservoir [3–5]. To refine a number of the foregoing assumptions and proposed relationships, it is expedient to continue hydrophysical investigations of the dynamics of formation of the structure and mechanical strength of the layered ice prism on the slopes of the dike of the Kiev PSS reservoir. The materials presented and also the data of on-site observations can serve as grounds for developing as a first approximation a method of designing revetments of dike slopes of PSS reservoirs for the effect of ice.
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