Estudio geotécnico in Socuéllamos

In Socuéllamos, the soils are predominantly formed by limestones, dolomites, and marbles, often accompanied by gypsum, anhydrite and salts, in addition to the occasional presence of shales, schists, gravels and compacted sands. These materials usually show acceptable strength for foundation works, although the frequent occurrence of gypsum and salts implies a potential risk of dissolution, which requires detailed studies before carrying out deep or shallow foundations. The permeability levels are usually low at the surface, although aquifers may occur at greater depths, which affects the choice of foundation system and the management of groundwater.

The seismicity in the area is notable, with 55 events recorded over 30 years, albeit of low magnitude (Mmax 3.3). Seismic hazard should preferably be taken into account in sensitive projects. On the other hand, the existence of karst-related phenomena associated with the carbonate formations and the presence of gypsum makes the mandatory verification of karst conditions before building essential, as it can generate voids and sinkholes that would compromise structural safety. As the substrate is non-clayey, there is no risk of expansivity. The main geotechnical constraint in Socuéllamos is the presence of karst and the associated risk of dissolution linked to gypsum; these factors require a thorough and specific geotechnical study before starting any construction project.