The most monuments of the Kyiv-Pechersk reservation are built on loessial soils. Deformation of loessial soils and the stability of architectural monuments depend on the superficial run-off and the outflow from waterpipes, sewerage, and heat networks. These factors often result in the formation of perched groundwater, rise of a level of groundwaters, underflooding of cellars, damping and deformations of the constructions of buildings. In order to study these processes and their consequences, we used hydrophysical and geophysical observations and the simulation of test problems for unsaturated porous media.

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