Estudio geotécnico in Villaviciosa

In Villaviciosa, the predominant subsoil corresponds to formations of low or very low permeability, which limits infiltration and the formation of aquifers except in very shallow areas. The soil types identified, mainly fine sands and silts in a small proportion, do not usually present significant problems in terms of bearing capacity; however, it is essential to study their distribution and the presence of soft zones, since they affect the type of foundation recommended depending on the load to be transmitted.

Seismic activity in Villaviciosa is very low, with only one event recorded in 30 years and a maximum magnitude of 1.7; therefore, seismicity does not represent a relevant constraint for structural design. On the other hand, the fact that the subsoil is not clayey rules out any risk associated with expansive soils. However, it is essential to check for the presence or absence of karstic phenomena before carrying out any foundation works, since karst can lead to instabilities or the existence of cavities that critically condition the safety and feasibility of the project.