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Record W110941357

Seismic Microzonation of Great Toronto Area and Influence of Building Resonances on Measured Soil Responses

2011· article· en· W110941357 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.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueScholarship@Western (Western University) · 2011
Typearticle
Languageen
FieldEngineering
TopicGeotechnical and Geomechanical Engineering
Canadian institutionsnot available
Fundersnot available
KeywordsSeismic microzonationSeismologyGeology
DOInot available

Abstract

fetched live from OpenAlex

A pilot seismic microzonation of the Greater Toronto Area (GTA) is used to establish the conditions and limitations of geophysical methods for site response investigations in city conditions. Maps of fundamental soil resonant frequencies, amplifications at these frequencies and interpolated average shear wave velocity of top 30 m of soil profile (VS- 30) used in soil classification were compared to the maps of drift thickness and surficial geology for the GTA. The non-applicability of the interpolated VS-30 map for site classification between measured test points is indicated. It is also shown that the soil response cannot be estimated properly using VS-30 values only. In order to enhance the capability of the horizontal-to-vertical-spectral-ratio (HVSR) method to resolve the fundamental soil resonances, a procedure and a computer program were developed for separation of ambient vibrations from nearby traffic as well as distant sources using the recorded waveforms before calculating the HVSR. A portable seismic station was developed for field HVSR waveforms recordings. It was also used for identification of building vibration modes. The influence of building vibrations on the HVSR result was investigated considering a benchmark building before construction started and after its completion. This influence is expressed as suppression or split-up of HVSR resonance if the building and soil resonances are close. This effect spreads out to distances comparable to the maximum dimension of the building. The experimentally obtained building resonant frequency at first vibration mode was found to be significantly higher than that calculated using empirical equations proposed by building codes, while the damping factor was less than the prescribed value. Additionally, the concept of using the HVSR inside a building to identify its resonances was examined using recorded waveforms, but the results did not confirm applicability of the HVSR for this purpose. The limitations and initial conditions that are necessary for successful implementation of refracted shear wave seismic profiling (SH-profiling) and multi-channel-analysis-ofsurface- waves (MASW) methods for application in urban areas are discussed. The problems with interlaying low velocity soil layer are pointed out. The soil response functions obtained from the microzonation studies using low intensity seismic sources differ from the response during an earthquake. An approach to estimate the changes of soil response in relation with expected Peak Ground Velocity (PGV) and Intensity of Modified Mercalli Scale (IMM) is proposed. The results were found to be in agreement with strong motion data from the epicentral area of a strong earthquake. It was concluded that the results from seismic microzonation studies should be considered in conjunction with models that simulate the change in dynamic characteristics of soil and buildings during expected earthquake events.

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)0.000
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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.260
Threshold uncertainty score0.852

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 communication0.0000.001
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 head0.064
GPT teacher head0.251
Teacher spread0.187 · 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