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Book DOI: 10.21467/abstracts.93 water repellent". So, in the geological section of well No1 in the Victory Park (Cheboksary), within one “aquiferous complex of the Tatar Paleozoic sediments,” there were up to 4-5 independent stratal and interstratal aquifers, which play their own role in the stability of the Volga slope. Based on the foregoing, for the design of reclamation of waterlogged and landslide slopes, we use the following series of types of GW or aquifer: 1 soil water; 2 – top water; 3 – ground water; 4 – interstratal water; 5 low pressure stratal GW; 6 high-pressure interstratal water (artesian); 7 – micro-interstratal water. Of the seven listed GWs, the content of the first three and the 6th GW is interpreted in the literature more or less unambiguously. The other three are defined below. Interstratal GW 4 groundwater is between water-resistant strata, non-pressure the GW power is less than the capacity of the water-containing stratum. Aquifer GW 5 differs from GW 4 in that the water completely fills the water-containing stratum (layer) and may have a low pressure. Micro-interstratal GW 7 confined to the strata of thin alternation (intercalation) of clays, siltstones and fine sands, bounded by water-resistant rocks below and above. The horizon is poorly developed; in the unloading zones on the slopes it feeds the swamp (frontal feeding). Horizons 3, 4 and 5 can be unloaded on slopes, in ravines, within the walls of landslide disruptions in the form of descending (horizons 3, 4) and ascending (horizons 5, 6) springs. The above types of GW are simultaneously considered as types of underground water supply of the swamp, wells and landslides. In addition to them, surface water due to precipitation can also participate in the swamping of land. As factors of waterlogging and by their role in slope processes, atmospheric waters are subdivided into internal, falling directly onto the object, and external (alluvial), falling onto the object (waterlogging site, landslide, and ravine) from the side.

Landslide Hazardous Slope Arrays and their Hydrogeological Features