Detection of anomalies such as ice lenses, vein ice in frost cracks in dispersed soils, etc.
Result
The surface layer is in a thawed state.
Below the level of the boundary of cooled soils, the conductivity drops sharply, there are numerous anomalies of increased resistance, having an irregular or lens shape - zones of increased ice content and changes in the composition of rocks 2-7 meters in size horizontally.
No extended ice wedges were found.
Value
Choosing the depth of piles for resting on frozen soils based on actual data
Optimization of the location of buildings and structures.
