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Record W3012301793

Physical Properties of Gas Hydrate Related Sediments, Offshore Vancouver Island

2002· article· en· W3012301793 on OpenAlexaboutno aff
Ivana Novosel, G. D. Spence, R. D. Hyndman

Bibliographic record

VenueAGUFM · 2002
Typearticle
Languageen
FieldEnvironmental Science
TopicMethane Hydrates and Related Phenomena
Canadian institutionsnot available
Fundersnot available
KeywordsSubmarine pipelineClathrate hydrateGeologyOceanographyHydratePetroleum engineeringChemistry
DOInot available

Abstract

fetched live from OpenAlex

A gas hydrate vent field on the South Vancouver Island continental slope was the target of a series of seafloor core sampling programs in years 2000 and 2001. The vent structures had been previously imaged on the Cascadia accretionary margin as prominent blank zones in seismic reflection data. In 2000, 26 piston cores, with maximum recovered lengths of approximately 8 m, were collected in the vent field region. Extensive physical property measurements were carried out on these cores. The objectives of the analyses were to: (1) provide ground-truth calibrations for seismic impedance and electrical resistivity remote surveys, and (2) examine the effect of high methane fluxes on the physical, chemical, and mineralogical character of sediments within the region of a vent field. Gas hydrate was recovered in 4 cores located within the most prominent seismic blank zone (Blank Zone I). Cores located within the blank zones contained low magnetic susceptibility authigenic pyrite, rather than high magnetic susceptibility magnetite and thus created a low magnetic zone within the vent. Leather clams (genus acharax) were recovered in several cores located inside the vent, indicating an environment high in sulfide. Increased seismic reflection coefficients and sample thermal conductivity values within the topmost sediments of Blank Zone 1 correlated with the presence of authigenic carbonate. All observations are consistent with high methane fluxes from seafloor sediments within a cold seep environment. The comparison of core measured porosity, thermal conductivity, and velocity with physical properties from deeper in the stratigraphy from the Ocean Drilling Program (ODP) clearly indicates that within ~ 10 m of the seafloor sediment compaction is distinctly different from that indicated by deeper trends. Within these cored sediments porosity decreases from as much as 75% at the seafloor to 55% at 8 m below; in contrast, the porosities over this depth range extrapolated from the deeper ODP trends are consistently 60%. Thermal conductivity, being highly dependent on density and porosity, also increases dramatically within the top few metres of the sediment. However, no decrease in sample seismic velocity is observed over the same depth range. This particular behaviour of shallow sediments may be significant for: 1) heat flow studies.

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)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.614
Threshold uncertainty score0.768

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.012
GPT teacher head0.189
Teacher spread0.177 · 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 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

Citations4
Published2002
Admission routes1
Has abstractno

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