MétaCan
Menu
Back to cohort
Record W2981727086 · doi:10.4095/288040

Aquatic soft sediment sampling methods: freeze coring and grab/hand coring

2011· report· en· W2981727086 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.

Bibliographic record

Venuenot available
Typereport
Languageen
FieldEngineering
TopicFreezing and Crystallization Processes
Canadian institutionsNatural Resources Canada
Fundersnot available
KeywordsCoringSampling (signal processing)SedimentGeologyEnvironmental scienceComputer scienceEngineeringPaleontologyComputer vision

Abstract

fetched live from OpenAlex

To obtain reliable cores of shallow aquatic sediments requires a pragmatic marriage of the substrate type that you will be coring to the research goals that you wish to achieve. Aquatic sediment substrates vary from extremely "soupy" to well compacted. The goals can vary from climate histories to geotechnical to geochemical, each of which may require specific sampling techniques. The resolution required in the study commonly dictates the type of substrate and the type of coring method required. The highest resolution lake coring, with also the best preservation of geotechnical properties, is freeze coring. When properly deployed this technique preserves sediment stratigraphy in hard to very soft substrates with sediment disturbance reduced to virtually nil either during or post sampling. Freeze cores can be transported back to the lab for detailed stratigraphic study, with resolution at millimetre scales possible through microtoming and X-Ray examination. Freeze coring is logistically difficult, requiring transport of dry ice into the field, and the maintenance of frozen conditions subsequent to sampling. The amount of sediment can also be relatively small in freeze cores, especially for the sediment-water interface. Freeze coring of marine substrates is the same as for fresh water. Other soupy sediment techniques include gravity coring (Sam Alpay) and hand coring. Hand cores can be used delicately and precisely, and hence can be effective coring devices in the softest of substrates. Hard substrates can cause as many problems as soft substrates, but are advantageous in that they are resistant to disturbance and thus can be relatively easily transported back to the lab. Many gravity corers are unsuited to these kinds of substrates due to a lack of penetration, no matter how good the operator or how heavy the weight used. Hand coring is a good option in these substrates, and can yield long and well preserved cores, although depth penetration can be limited by the amount of weight one can use to push the corer into the substrate (a sharp-ended coring nose is preferable). Short (<30cm) cores of hard substrates can also be obtained by coring the sediment retrieved in a box corer or large grab sampler. This technique provides large sediment volumes with easily correlated core depths. Lake or marine cores >1-2 metres generally require vibracoring or piston coring techniques, which are logistically difficult unless significant lifting capabilities are available. Small piston and vibracorers can be deployed off small vessels but the depth penetration of these systems is often limited by substrate layers or lift capacity. These techniques can disturb the uppermost 0.5-1 m and so need to be used in conjunction with gravity or other coring techniques that better capture the sediment-water interface (if that is of importance). Stratigraphy from different coring techniques can generally be spliced using radiometric dating and/or proxy data measurements.

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.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Methods · Consensus signal: Methods
Teacher disagreement score0.861
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
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 head0.094
GPT teacher head0.322
Teacher spread0.229 · 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

Quick stats

Citations0
Published2011
Admission routes1
Has abstractyes

Explore more

Same topicFreezing and Crystallization ProcessesFrench-language works237,207