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Joint inversion of navigation and resistivity using a fixed transmitter and a towed receiver array: a transient marine CSEM model study

2011· article· en· W2123006473 on OpenAlexafffundabout
Andrei Swidinsky, R. N. Edwards

Bibliographic record

VenueGeophysical Journal International · 2011
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeophysical and Geoelectrical Methods
Canadian institutionsUniversity of Toronto
FundersNatural Sciences and Engineering Research Council of CanadaUniversity of TorontoCommonwealth Scientific and Industrial Research Organisation
KeywordsTransmitterGeologyInversion (geology)Transient (computer programming)Joint (building)GeodesyElectrical resistivity and conductivityAcousticsGeophysicsRemote sensingSeismologyComputer scienceTelecommunicationsPhysicsElectrical engineeringEngineering

Abstract

fetched live from OpenAlex

A typical marine controlled-source electromagnetic system consists of an electric dipole
\ntransmitter and one or more electric dipole receivers. The objective of a survey is to determine
\nthe seafloor resistivity by recording the electromagnetic transients, which diffuse through the
\nearth from the transmitter to the receivers. Accurate knowledge of system geometry is crucial
\nfor proper interpretation; errors in the position and orientation of the transmitter and/or the
\nreceivers propagate into errors in the predicted seafloor resistivity. We show theoretically
\nthat for certain multireceiver set-ups and crustal electrical profiles that the geometry and the
\nseafloor resistivity may be determined independently. A specific example is an experiment
\nproposed in association with NEPTUNE Canada. Here, we have already deployed an electric
\ndipole transmitter with a known orientation in a known location. A cabled streamer of receivers
\nmay be towed by a survey vessel in the vicinity of the transmitter on a known heading. For this
\nconfiguration, an eigenparameter analysis of two seafloor models consisting of (1) a halfspace
\nand (2) a resistive layer buried within a halfspace shows that the resistivity structure of the
\nseafloor can be independently resolved from the cable location. Further studies of these two
\nmodels also indicate that the position of the streamer must be roughly known in advance on
\nthe order of a hundred metres to be used as a suitable starting model in a non-linear inversion.
\nThe crucial information is contained in the parts of the pulse which travel through the seawater
\nand which act as a calibration path. Such information is absent for a static DC method.

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: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.790
Threshold uncertainty score0.396

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 head0.052
GPT teacher head0.255
Teacher spread0.203 · 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 designObservational
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

Citations9
Published2011
Admission routes3
Has abstractyes

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