2022
DOI: 10.1029/2021wr031793
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Pumping Optimization Under Uncertainty in an Island Freshwater Lens Using a Sharp‐Interface Seawater Intrusion Model

Abstract: Island groundwater resources often form freshwater lenses overlying saline groundwater. When water is withdrawn from a freshwater lens by a pumping well, saline groundwater migrates upwards toward the well. This vertical seawater intrusion process, also called saltwater upconing, is a major concern when managing well fields. Freshwater lenses of island aquifers have been described as being more vulnerable than continental coastal aquifers, since vertical migration distances associated with upconing are shorter… Show more

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Cited by 11 publications
(17 citation statements)
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“…Deterministic parameter estimation and SLP, FOSM-based OUU were previously implemented on Grande Entrée Island to 85 determine maximum pumping rates avoiding well salinization, considering parameter and observation uncertainty and current climate conditions (Coulon et al, 2021;Coulon et al, 2022). This study details the implementation of the ensemble-based approach for history matching and multi-objective (MO) OUU, and the incorporation of climate uncertainty (specifically, sea level and recharge uncertainty) into the pumping optimization.…”
Section: Study Area 80mentioning
confidence: 99%
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“…Deterministic parameter estimation and SLP, FOSM-based OUU were previously implemented on Grande Entrée Island to 85 determine maximum pumping rates avoiding well salinization, considering parameter and observation uncertainty and current climate conditions (Coulon et al, 2021;Coulon et al, 2022). This study details the implementation of the ensemble-based approach for history matching and multi-objective (MO) OUU, and the incorporation of climate uncertainty (specifically, sea level and recharge uncertainty) into the pumping optimization.…”
Section: Study Area 80mentioning
confidence: 99%
“…1), along with Quaternary sand dunes and glacial sediments (mostly fine sand). A spatially distributed recharge representative of the period 1989-2019 was generated for the Magdalen Islands archipelago by Lemieux et al (2022), using a SWB2 groundwater recharge model (Soil-Water-Balance-2, Westenbroek et al, 2018). A spatial average of 524 mm/year was determined for the whole archipelago, and of 559 mm/year for Grande-Entrée Island specifically.…”
Section: Study Area 80mentioning
confidence: 99%
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