River-spring connectivity and hydrogeochemical interactions in a shallow fractured rock formation. The case study of Fuensanta river valley (Southern Spain)

• Published in: Journal of hydrology (Amsterdam) Vol. 547; pp. 253 - 268
• Main Authors: Barberá, J.A., Andreo, B.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-04-2017
• Subjects: Fractured rock formation; Fuensanta river valley; Hydrogeochemical processes; Surface water-groundwater interaction; Tracing experiments; Fuensanta river valley; Surface water-groundwater interaction; Tracing experiments; Fractured rock formation; Hydrogeochemical processes
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2017.01.046

•Flow dynamics within a shallow and fractured rock formation is analyzed.•Groundwater flow is substantially influenced by river hydrology and chemistry.•Hydrodynamic and tracing techniques proved local river-spring connectivity.•Mixing and calcite dissolution mainly control Fuensanta spring hydrochemistry.•The proposed model permits a rough quantification of mixing water fractions.
In upland catchments, the hydrology and hydrochemistry of streams are largely influenced by groundwater inflows, at both regional and local scale. However, reverse conditions (groundwater dynamics conditioned by surface water interferences), although less described, may also occur. In this research, the local river-spring connectivity and induced hydrogeochemical interactions in intensely folded, fractured and layered Cretaceous marls and marly-limestones (Fuensanta river valley, S Spain) are discussed based on field observations, tracer tests and hydrodynamic and hydrochemical data. The differential flow measurements and tracing experiments performed in the Fuensanta river permitted us to quantify the surface water losses and to verify its direct hydraulic connection with the Fuensanta spring. The numerical simulations of tracer breakthrough curves suggest the existence of a groundwater flow system through well-connected master and tributary fractures, with fast and multi-source flow components. Furthermore, the multivariate statistical analysis conducted using chemical data from the sampled waters, the geochemical study of water-rock interactions and the proposed water mixing approach allowed the spatial characterization of the chemistry of the springs and river/stream waters draining low permeable Cretaceous formations. Results corroborated that the mixing of surface waters, as well as calcite dissolution and CO2 dissolution/exsolution, are the main geochemical processes constraining Fuensanta spring hydrochemistry. The estimated contribution of the tributary surface waters to the spring flow during the research period was approximately 26–53% (Fuensanta river) and 47–74% (Convento stream), being predominant the first component during high flow and the second one during the dry season. The identification of secondary geochemical processes (dolomite and gypsum dissolution and dedolomitization) in Fuensanta spring waters evidences the induced hydrogeochemical changes resulting from the allogenic recharge. This research highlights the usefulness of an integrated approach based on river and spring flow examination, dye tracing interpretation and regression and multivariate statistical analysis using hydrochemical data for surface water-groundwater interaction assessment in fractured complex environments worldwide, whose implementation becomes critical for an appropriate groundwater policy.