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Record W4322209946 · doi:10.5194/egusphere-egu23-14159

Evolving concepts and communication: what do we need to evaluate better regional groundwater flow?

2023· preprint· en· W4322209946 on OpenAlexaff
Judit Mádl‐Szőnyi, John Molson, Okke Batelaan, J.M. Verweij, Xiao-Wei Jiang, José Joel Carrillo-Rivera, Ádám Tóth

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicGroundwater and Isotope Geochemistry
Canadian institutionsUniversité Laval
Fundersnot available
KeywordsGroundwater flowAquiferGroundwaterHydrogeologyStructural basinGeologyGroundwater modelHydrology (agriculture)Earth scienceGeomorphologyGeotechnical engineering

Abstract

fetched live from OpenAlex

The theory of regional groundwater flow is sixty years old in 2023, which has made it possible to evaluate groundwater flow systems and evolution in sedimentary basins. Recently, the approach has been extended to different environments in the Earth's crust. By applying regional groundwater flow theory, we can solve groundwater issues on a larger scale than for single aquifers. Application of the concept contributes to all practical aspects of groundwater topics, including the UN’s Sustainable Development Goals for water.However, the developed terms related to groundwater flow evaluation need to be more strictly defined and clarified for interpreting complex hydrogeological flow systems. The presentation summarizes the results of discussions among RGFC-IAH board members on this topic and tries to provide some necessary frameworks for the future application of the concept.At regional scales, groundwater flow evaluation should include the concept of aquifer systems. The term artesian basin has become obsolete because it implies impermeable layers in natural environments; groundwater basin is preferred instead. Sedimentary basin is a broader term which can contain more than one groundwater basin. For the goals of flow system evaluation, the term groundwater basins can be used, which are characterized by siliciclastic basin fill and basement aquifer systems. The full-groundwater basin is required for 2D and 3D interpretations, because half- (or symmetric-) basin assessment can provide misleading results. Hydraulic continuity is a fundamental principle in groundwater flow evaluation, it can be assumed in groundwater basins across multiple aquifers, aquitards and faults, as long as one has no contradicting evidence. Conceptual groundwater flow models need to be tested with specific field data, numerical simulations and groundwater flow-related manifestations.The presentation aims to initiate a discussion on improving the application of regional groundwater flow theory. The conference presentation is supported by the National Multidisciplinary Laboratory for Climate Change, RRF-2.3.1- 21-2022-00014 project.

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)0.044
metaresearch head score (Gemma)0.111
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Theoretical or conceptual · Consensus signal: none
GenreCandidate signal: Review · Consensus signal: none
Teacher disagreement score0.044
Threshold uncertainty score0.233

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0440.111
Meta-epidemiology (narrow)0.0020.001
Meta-epidemiology (broad)0.0020.001
Bibliometrics0.0060.007
Science and technology studies0.0030.016
Scholarly communication0.0230.064
Open science0.0040.005
Research integrity0.0070.006
Insufficient payload (model declined to judge)0.0140.004

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 head0.045
GPT teacher head0.275
Teacher spread0.230 · 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 designTheoretical or conceptual
Domainnot available
GenreReview

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

Citations0
Published2023
Admission routes1
Has abstractyes

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