Estudio geotécnico in Aguadulce

In Aguadulce, a substrate composed mainly of sandstones, conglomerates and flysch predominates; these materials usually provide good stability and adequate bearing capacity for most structures. The occasional presence of fine sands and silts, as well as of limestones, dolomites and marbles, may influence the choice of foundation type in specific areas, particularly in those sectors where the finer soils may reduce strength. The permeability characteristics observed usually condition the drainage of water, so it will be essential to consider the possibility of superficial aquifers during the geotechnical study.

With regard to associated risks, seismicity in Aguadulce is very low, since only 1 event has been recorded in 30 years with a low maximum magnitude of 1.7, so the seismic influence on structural design is practically negligible. However, it is relevant to note the possibility of karstification in areas with limestones, dolomites and marbles; this aspect must be carefully verified before any foundation is carried out in order to avoid stability problems. Expansive clays are only locally present or in areas not predisposed to their development, so the associated risk is low, with the main limiting factor being the potential presence of karst cavities.