globalchange  > 气候变化与战略
DOI: 10.5194/hess-24-5655-2020
论文题名:
Hydraulic and geochemical impact of occasional saltwater intrusions through a submarine spring in a karst and thermal aquifer (Balaruc peninsula near Montpellier; France)
作者: Petre M.-A.; Ladouche B.; Seidel J.-L.; Hemelsdaël R.; De Montety V.; Batiot-Guilhe C.; Lamotte C.
刊名: Hydrology and Earth System Sciences
ISSN: 1027-5606
出版年: 2020
卷: 24, 期:11
起始页码: 5655
结束页码: 5672
语种: 英语
Scopus关键词: Aquifers ; Exploratory geochemistry ; Groundwater resources ; Hydrogeology ; Landforms ; Offshore oil well production ; Rare earths ; Salt water intrusion ; Submarines ; Tracers ; Water management ; Discharge features ; Geochemical data ; Groundwater management ; Hydraulic heads ; Hydrogeological ; Mediterranean coasts ; Rare earth elements (REEs) ; Thermal aquifers ; Hydrochemistry ; aquifer characterization ; geochemical survey ; hydraulic conductivity ; karst hydrology ; saline intrusion ; salinity ; spring (hydrology) ; water quality ; France
英文摘要: Submarine springs are a common discharge feature of the karst aquifers along the Mediterranean coast. In some instances, occasional and localized saltwater intrusions can occur through the submarine spring and negatively impact the quality of the groundwater resource. The hydraulic and geochemical behaviour of a submarine spring discharging into the Thau Lagoon just offshore of the Balaruc peninsula near Montpellier, France, has been characterized to determine the impacts of such phenomena to better understand the dynamics of a regional karst aquifer and improve its groundwater management. This work is based on both historical and new hydrogeological and geochemical data, illustrating six occasional saltwater intrusion events (from 1967 to 2014) in the Thau Lagoon area (southern France). Hydraulic perturbation of the aquifer is propagated instantly within the Balaruc-les-Bains peninsula and reaches a distance of about 5 km upgradient within 9 d. Comparison of hydraulic heads during seawater intrusion events in 2010 and 2014 indicates an aggravation of the phenomenon with an increase in hydraulic head variations. In contrast, isotopic tracers (87Sr=86Sr, D/H, 18O=16O) and rare earth elements (REEs) demonstrate that the geochemical impact of these inversac events is only observed at the local scale but is still perceptible several years after the event. For example, some of the thermal wells had not recovered their initial geochemical state 20 and 40 months after the last two inversac events (2010 and 2014, respectively), suggesting a geochemical legacy of this phenomenon within the complex karst system. By contrast, an adjacent deep karst compartment located south of the study area is not affected by the saltwater intrusion and is characterized by distinctly different hydrodynamic behaviour. Overall, this work on occasional and localized saltwater intrusions constitutes a key step in understanding the dynamics of this complex karstic and thermal aquifer and will support the management of the groundwater resource. © 2020 Author(s).
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被引频次[WOS]:7   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162536
Appears in Collections:气候变化与战略

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作者单位: Petre, M.-A., HydroSciences Montpellier, Montpellier University, CNRS, IRD, Montpellier, France, North Carolina State University, Marine, Earth, and Atmospheric Sciences Department, Raleigh, NC 27695, United States; Ladouche, B., BRGM, Montpellier University, Montpellier, France; Seidel, J.-L., HydroSciences Montpellier, Montpellier University, CNRS, IRD, Montpellier, France; Hemelsdaël, R., Geosciences Montpellier, Montpellier University, CNRS, Montpellier, France; De Montety, V., HydroSciences Montpellier, Montpellier University, CNRS, IRD, Montpellier, France; Batiot-Guilhe, C., HydroSciences Montpellier, Montpellier University, CNRS, IRD, Montpellier, France; Lamotte, C., BRGM, Montpellier University, Montpellier, France

Recommended Citation:
Petre M.-A.,Ladouche B.,Seidel J.-L.,et al. Hydraulic and geochemical impact of occasional saltwater intrusions through a submarine spring in a karst and thermal aquifer (Balaruc peninsula near Montpellier; France)[J]. Hydrology and Earth System Sciences,2020-01-01,24(11)
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