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Record W4242977585 · doi:10.4133/1.2923658

Delineation of Water Inflow in an Underground Potash Mine with 3‐D Electrical Resistivity Imaging

2006· article· en· W4242977585 on OpenAlexaff
Robert A. Eso, Michael Maxwell, Douglas W. Oldenburg, John Unrau

Bibliographic record

VenueSymposium on the Application of Geophysics to Engineering and Environmental Problems 2006 · 2006
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeophysical and Geoelectrical Methods
Canadian institutionsPotashCorp (Canada)Golder Associates (Canada)University of British Columbia
Fundersnot available
KeywordsPotashInflowBoreholeMining engineeringGeologyElectrical resistivity and conductivityInversion (geology)Electrical resistivity tomographyAquiferDrillingResistive touchscreenGroundwaterGround-penetrating radarGeotechnical engineeringEngineeringStructural basinElectrical engineeringGeomorphologyMaterials scienceMechanical engineeringRadar

Abstract

fetched live from OpenAlex

Delineating water inflow in underground potash mining environments has routinely been done using conventional mining methods, seismic techniques and recently GPR as a useful non‐invasive tool. The combination of highly resistive dry salt and highly conductive wet salt makes these water inflow areas a good candidate for Electrical Resistivity Imaging (ERI). Mosaic Potash, Golder Associates Ltd., and the University of British Columbia's Geophysical Inversion Facility (UBC‐GIF) have worked to develop and apply ERI techniques for the underground environment. Because of the 3‐D distribution of current and potential electrodes and the 3‐D nature of the targets, full 3‐D forward modeling and inversion of the data are required. The nature of underground mining limits the placement of electrodes to existing underground drifts and this severely restricts the available electrode geometry. By placing additional electrodes in boreholes, a survey geometry with enough information to constrain the 3‐D inversion can be deployed. We present a case study of the delineation of a water inflow in a potash mine using 3‐D ERI. The resulting inversion models of electrical conductivity have helped to focus drilling and mitigation efforts and have provided the geotechnical engineers and mine personnel with valuable information about the underground water distribution.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.718
Threshold uncertainty score0.302

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

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 head0.004
GPT teacher head0.170
Teacher spread0.167 · 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 teacher head, 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

Citations3
Published2006
Admission routes1
Has abstractyes

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