Hydrogeological interactions between fault zones and alluvial aquifers in regional flow systems

Albert Folch, Josep Mas-Pla

    Research output: Contribution to journalArticleResearchpeer-review

    37 Citations (Scopus)


    The hydrological influence of fault zones in tectonic areas is usually difficult to depict from field data. Numerical simulation allows representation of such flow systems and an estimation of flow lines and rates. This paper reports on simulations of the groundwater flow in a range-and-basin area affected by a regional fault zone, which may drain or recharge an overlaying alluvial aquifer. Different hydraulic conductivity values for the range rocks, the fault-zone, and the sedimentary infill of the basin are considered, as well as different fault-zone widths and boundary conditions. Results show that upward and downward fluxes develop in the upper part of the fault zone, controlled by the action of the alluvial aquifer, influencing the recharge of the sedimentary basin. This paper shows the hydrological efficiency of fault zones as preferential flow; it also analyses the constraints that determine groundwater recharge to the surrounding basins. These results contribute to the understanding of hydrogeological dynamics in tectonic areas. Copyright © 2008 John Wiley & Sons.
    Original languageEnglish
    Pages (from-to)3476-3487
    JournalHydrological Processes
    Issue number17
    Publication statusPublished - 15 Aug 2008


    • Alluvial aquifer
    • Fractured rocks
    • Numerical flow modelling
    • Recharge


    Dive into the research topics of 'Hydrogeological interactions between fault zones and alluvial aquifers in regional flow systems'. Together they form a unique fingerprint.

    Cite this