Estudio geotécnico in Mejorada del Campo

In Mejorada del Campo, the geotechnical setting is characterised mainly by the presence of water bodies, which cover more than 60% of the area, together with occasional outcrops of limestones, dolomites and compact gravels. The existence of Gypsum, Anhydrite and Salts in the ground introduces the risk of dissolution, which necessitates a thorough analysis of the susceptibility to collapse or subsidence, particularly when the foundation coincides with these materials. In addition, the high permeability of the aquifers suggests a significant potential for fluctuations in the groundwater level, which affects both bearing capacity and the choice of the most suitable foundation type.

As regards seismicity, few events are recorded over a period of 30 years and the maximum magnitude reaches M3, which places the local seismic hazard at a very low level. However, the possibility of karsitic development associated with the carbonate and gypsum materials requires rigorous checks before defining the foundation for any structure. Likewise, the localised presence of expansive clays requires special attention due to the risk posed by their seasonal volumetric behaviour, particularly in continental climate zones. In this context, detailed characterisation of the ground in search of karstic cavities and the assessment of clay expansion are the main geotechnical constraints in the municipality.