Tracing groundwater discharge in the floodplain of the parana river, argentina: implications for its biological communities

• Published in: River research and applications 2014-02, Vol.30 (2), p.166-179
• Main Authors: Marchetti, Z. Y, Carrillo‐Rivera, J. J
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; aquatic environment; Biological and medical sciences; Communities; Discharge; ecosystems; floodplain; floodplains; flow systems; forests; Fresh water ecosystems; Freshwater; Fundamental and applied biological sciences. Psychology; General aspects; grasslands; Ground-water flow; Groundwater; groundwater discharge; groundwater flow; intermediate flow; Local flow; Piezometers; rain; Rivers; Signatures; surface water; surface water and groundwater interaction; Synecology; wells
• ISSN: 1535-1459; 1535-1467
• DOI: 10.1002/rra.2629

Groundwater discharge can be an important determinant of the functioning of aquatic environments and their associated biological communities. However, the presence and the importance of groundwater have not been considered in the Parana River floodplain owing to the large quantity of surface water. The present study aimed to identify groundwater discharge conditions in a sector of the middle of the floodplain of the Parana River by studying groundwater flow systems. Eight piezometers were installed to record groundwater movement in the vertical plane weekly for 2 years. Water samples were collected in piezometers, domestic wells, the river and other water bodies to study the groundwater flow systems. Rising of the water level during piezometer installation and recording suggested that the study zone represents groundwater discharge conditions. Residence time proxy allowed identification of local flows and intermediate flows. Local rainfall (in Santa Fe) showed an isotopic signature (δD and δ¹⁸O) similar to some local flows detected in the study zone, and this suggested local recharge. The chemical characteristics of an intermediate flow suggest that water would have travelled from a recharge area ~30 km from the study zone. Local rainfall and the intermediate flow have different isotopic signature. Results suggest that the willow forest is associated with the recharge area of a local flow, which plurispecific‐canopy forest is related to a transit area of a semi‐intermediate flow, and that tall grassland and marshy community colonize discharge areas of local and intermediate flows, respectively. Copyright © 2012 John Wiley & Sons, Ltd.