Journal
JOURNAL OF HYDROLOGY
Volume 593, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.jhydrol.2020.125859
Keywords
Karst aquifer; Hydrochemistry; Hydrodynamic; Source-mixing calculation; Conceptual model
Funding
- Region Occitanie
- Conseil Departemental du Lot
- Commissariat a l'Energie Atomique et auxenergies alternatives
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This study aims to understand the hydrodynamical and geochemical variations at the outflow of karst systems, using a multi-proxy approach to trace water origins, evaluate mixing phenomena, and consider contributions from both autogenic and allogenic recharge sources. The research conducted in the Ouysse karst system in western France showcases how water-mixing processes in binary karst systems can be studied and analyzed using global water chemistry, hydrograph and chemograph analysis, and source-mixing calculation during a flood event. The information obtained can be valuable for forecasting and management actions related to water resource management.
On the edge of sedimentary basins, karst aquifers can be fed by several water origins from both autogenic and allogenic recharge. In some cases, water origin assessment is difficult and issues in water management may arise. The main goal of this study is to understand what controls hydrodynamical and geochemical variations at the outflow of a quite complex and large karst system. More precisely, this study illustrates how a consistent observational setup can be developed, based on a multi-proxy approach that can be used for tracing water origins, evaluating mixing phenomena, and contributions in karst aquifers considering both autogenic and allogenic recharge. The Ouysse karst system (650 km(2)), located in western France, provides the opportunity of studying water-mixing processes in binary karst systems fed by allogenic and autogenic recharges. Global water chemistry, hydrograph and chemograph analysis during a flood event, and source-mixing calculation were used to evaluate groundwater-flow origins and the contribution of each water type during the studied flood event: (i) karstic water; (ii) evaporite water; (iii) water from igneous-metamorphic rock aquifers. In terms of resource management, the information obtained can be used as a basis of forecasting and management actions.
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