Manifestaciones hidrológicas e hidroquímicas de flujos subterráneos procedentes de formaciones poco permeables del terciario en el Somontano de Huesca
DOI:
https://doi.org/10.3989/egeol.88445-6560Keywords:
Hydrogeology, Hidrochemistry, humid areas, saline soils, sodic soils, Ebro basin, Huesca, SpainAbstract
Presence of groundwater flow in the «somontano Oscense» area, proceeding from low permeability detritic tertiary rocks, is considered. It's given a grounwater flow model for these tertiary rocks. This model explains both water flow through them and water chemical characteristics. Groundwater flow has clear surface manifestations: it causes wet-areas (which are called «paules» in the area) with sodic waters; it makes appear saline, sodic or alkaline soils; and it modifies, too, water chemical composition of rivers in Somontano.
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