Estudio geotécnico in Ripollet

In Ripollet, fine sands and silts predominate, which make up the great majority of the soils present in the area, with a smaller proportion of materials such as sandstones, conglomerates and flysch. These characteristics generally provide favourable bearing capacity for buildings, although this may vary depending on the degree of compactness and moisture. Given the presence of extensive aquifers, it is essential to study the groundwater table in detail and its seasonal behaviour, as very high permeability can influence both the choice of foundation type and potential risks of destabilisation due to undermining or subsidence.

The seismicity recorded in Ripollet is very low, with no need for special considerations in structural design, since the maximum magnitude values are low and the number of events is scarce. An assessment of expansivity rules out risks arising from expansive clays because the substrate is not clayey. In conclusion, the main factor to consider in geotechnical studies in Ripollet lies in the high permeability of the ground, which requires particular attention to the management and drainage of groundwater during and after construction.