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Record W2125478980 · doi:10.1785/0120060242

Rate Dependence of Acoustic Emissions Generated during Shear of Simulated Fault Gouge

2007· article· en· W2125478980 on OpenAlexaff
Karen Mair, Chris Marone, R. P. Young

Bibliographic record

VenueBulletin of the Seismological Society of America · 2007
Typearticle
Languageen
FieldEarth and Planetary Sciences
Topicearthquake and tectonic studies
Canadian institutionsUniversity of Toronto
FundersRoyal SocietyNational Science Foundation
KeywordsShear (geology)Fault gougeGeologySeismologyAcoustic emissionFault (geology)Geotechnical engineeringAcousticsPetrologyPhysics

Abstract

fetched live from OpenAlex

Abstract Earthquake systems are commonly described using rate and state dependent fault models; however, the connection between rate and state friction parameters and specific microprocesses remains a challenge. We present new laboratory observations using modern ultrasonic techniques to reveal dynamic processes operating during frictional sliding. Granular layers were sheared under constant normal stress for a range of loading rates. During experiments, we monitored high-frequency acoustic emissions (AE) generated by grain fracture and friction using an array of piezoelectric transducers surrounding the layers. Complete waveforms and event information were collected for thousands of microearthquakes. Perturbations in imposed load point velocity (V) produced a friction response consistent with previous work. For a given V, AE per sec decreased with accumulated slip, suggesting sensitivity to gouge layer evolution. Step increases in V led to immediate and sustained increases in AE per sec; the converse was true for V decreases. The positive rate dependence of AE per second is unsurprising because more slip is covered per unit time at higher V; however, AE per unit slip decreases with increasing V, indicating a deficit of acoustic activity at a faster slip rate. Assuming that AE result mainly from grain contact sliding, acoustic activity is proportional to the real area of contact between sliding particles. Our results qualitatively agree with previous experiments carried out on bare rock surfaces and support ideas that the frictional contact junction area is reduced at increased sliding velocity. We highlight a new way to visualize micromechanical contact processes important in frictional mechanics and highly relevant to earthquake physics.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.664
Threshold uncertainty score0.999

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 studies0.0000.001
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.015
GPT teacher head0.227
Teacher spread0.211 · 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.

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

Citations36
Published2007
Admission routes1
Has abstractyes

Explore more

Same venueBulletin of the Seismological Society of AmericaSame topicearthquake and tectonic studiesFrench-language works237,207