Geomorphologically Host is on the Transnistrian elevated position within the Kiev plateau. The relief gully is flat. Stream Vita khots is divided into two parts, there are two lakes. Before field work experts go to inspect the area. Planned places will be a drilled well. Is estimated Geology khots – are studied outcrops, ponds, surface manifestations of natural hazards. Set the water level in nearby wells.
set of works: Geology + topographic survey + the removal of borders on price 10 900 UAH
Surveying khots at the initial stage includes the definition of plot on the ground. Topographical survey khots required to pre-project construction. Before the drilling is done surveying, removed all structures, communications. After the digital version of topoplan apply all of the designed building, communications, planned to drill wells. the Removal of borders khots you need to plan well to make the axis of buildings, objects. In the next phase, when the drilling team arrives, surveying the khots is to take away the terrain projected wells. After processing all data, you may have to change the location of buildings, structures. Then again you will need the removal of the boundaries of the khots.
Survey khots also allows more detailed reference to work with Geology. Tectonically the study area is located on the Northern slope of the Ukrainian shield within the maximum distribution of the glacier. Geological section Hotova, starting at the top:
- soil-vegetative layer – 1.5 m
- Sands of Pleistocene fluvioglacial deposits – up to 10m;
- variegated Neogene clay approximately 10m.
- Neogene Poltava clay – 15-20m
- Kiev Paleogene clay is about 30m.
On human map in Hostave common aaloo-sandy deluvial sediments. To the East, closer to the river Dnieper, spread granular alluvial sand, loam, silt, marl. the Geology khots is characterized by the fact that the modern relief was formed as a result of the glacier activity, erosion and deluvial processes. As a result of geological study clarifies Geology, hydrogeology, properties of rocks.
Hydrogeology are characterized by two nearest water horizons:
- Poltava - at a depth of 20-40m
- Bucha – at a depth of 50-80m.
in Addition, when there is a waterproof clay loam – forms a Bank. During drilling operations at a depth up to 6 meters of groundwater were detected. As a result of observations it was found that the average depth of frost penetration silty, fine sand, sandy loam – Maximum 0.8 m – 1.2 m. According to the regulations the study site is not potentially flood prone areas. For seismic conditions the area placed in the third category on a five point scale. On engineering-geological conditions of the area belongs to the first category of complexity. As a result, field surveys have not been found dangerous geotechnical phenomena: karst, erosion, suffusion. However, note that after the glacier remained loess-like soils. When moisture increases their settling.
Engineering-geological properties of soils can vary even on a relatively short distance. Geology you can enjoy in the company LLC "Guild Engineering".