Abstract
Research that has been conducted has made it possible to establish changes with respect to depth and time in the physical properties of clayey soils isolated in the roof of the moraine horizon of the Moscow stage of glaciation. The dependencies of shearing load on flow index, and compression modulus on permeability also suggest variation in strength and deformation indices with time. The variations have their own characteristic features in all isolated layers. In the median and lower layers, which reside in the zone of influence of structures, the minimum values of the indices of physic-mechanical properties are recorded during the fall, and the maximum in the winter.
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