Estudio geotécnico in Huévar del Aljarafe

In Huévar del Aljarafe, the predominant geotechnical substrate is made up mainly of limestones, dolomites and marbles, indicating the presence of soils of a competent nature and good bearing capacity for shallow or semi-deep foundations. Compact gravels and sands, although infrequent, also provide favourable performance in terms of stability and settlements, and the overall permeability is low, although there may be layers with some potential for shallow aquifers, which requires identification during the field investigation.

Seismicity in the municipality is very low, with only one event recorded with low magnitude (Mmax 1.7) over the last 30 years, so its influence on structural designs is minimal. With regard to expansive behaviour, although the clays do not show significant expansivity and are not dispersed, a risk of expansivity is indicated in certain areas, so the presence of local clayey layers must be verified before defining the foundation. The main limiting factor is determined by the need to rule out expansive clays and to pay attention to impermeability and possible the presence of groundwater.