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Record W4415978702 · doi:10.1016/j.jhydrol.2025.134553

Numerical investigation of offshore freshened groundwater dynamics in a changing marine environment

2025· article· en· W4415978702 on OpenAlexafffundabout
Shengchao Yu, Barret L. Kurylyk, Holly A. Michael, Vittorio Maselli, M. R. Nedimović, Irena Schulten, Fernando Córdoba-Ramírez

Bibliographic record

VenueJournal of Hydrology · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGroundwater and Isotope Geochemistry
Canadian institutionsDalhousie University
FundersAlliance de recherche numérique du CanadaCanada First Research Excellence FundOcean Frontier InstituteCanada Research Chairs
KeywordsGroundwater rechargeGroundwaterSubmarine pipelineGroundwater flowHydrology (agriculture)HydrogeologyDepression-focused rechargeAquifer

Abstract

fetched live from OpenAlex

Offshore freshened groundwater (OFG) is a potential alternative water resource for coastal populations facing water insecurity caused by high population density, pollution, or converging stressors from atmospheric and oceanic climate change. However, OFG systems are globally less explored than terrestrial groundwater systems, and no prior studies have been conducted on the Canadian continental shelf. Recent observations from two boreholes in the Gulf of St. Lawrence, Canada indicate a salinity decrease from 30 g/L to 20 g/L and 26 g/L, respectively, within the uppermost 5 m of marine sediment. To investigate the mechanisms driving OFG formation in the region, we conducted three-dimensional numerical simulations of coupled variable-density groundwater flow and salt transport, incorporating detailed analyses of the region’s topography, stratigraphy, and geological structures. Our findings indicate that sub-ice-sheet recharge and meteoric recharge are the primary processes responsible for OFG emplacement since the Last Glacial Maximum. The modeled OFG volume is 57,950 km 3 , while the total submarine groundwater discharge across the entire Gulf is estimated at 1.15 km 3 /year. Anisotropy in geological formations facilitates hydraulic connections between onshore and offshore aquifers, promoting active recharge of OFG. This onshore-offshore connectivity is reinforced by lower hydraulic conductivity, thicker unconsolidated marine sediments, greater anisotropy, and interlayered aquitards. Sensitivity analysis demonstrates that the system’s behavior varies across the range of plausible geologic connectivity, transitioning from active flow dynamics in highly connected settings to a more passive regime in less connected configurations. This study highlights how geological and hydrological factors influence the distribution and availability of OFG resources in the region. Understanding the existence and function of the OFG system could inform the potential development of an alternative freshwater resource for the province of Prince Edward Island that is entirely groundwater reliant and faces competing water demands from domestic water users and the intensive agricultural industry.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.057
Threshold uncertainty score0.113

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.000
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0020.001
Insufficient payload (model declined to judge)0.0020.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.005
GPT teacher head0.187
Teacher spread0.181 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designSimulation or modeling
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations2
Published2025
Admission routes3
Has abstractyes

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