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Record W3211709779

The importance of characterizing slope damage in rock slopes

2019· article· en· W3211709779 on OpenAlexaboutno aff
Davide Donati, D. Stead

Bibliographic record

VenueArchivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna) · 2019
Typearticle
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyRockfallWater damageLandslideGeotechnical engineeringGeographyCartographyAsphalt
DOInot available

Abstract

fetched live from OpenAlex

The stability of high rock slopes is controlled by many geological factors including the orientation, size, and location of geological structures, lithology, rock mass strength, hydrogeological setting, and slope topography. Together, these “inherited” factors often control the location, the extent, and the volume of the potential rock mass involved in a rock slope failure. Rock slopes can remain stable for many thousands of years before a de-stabilizing event or “trigger”, causes the slope to fail. However, often the failure of a rock slope is the final outcome of a slow and progressive degradation of the rock mass causing a gradual reduction in slope stability. Many authors have investigated the role of so-called “exogenic” and “endogenic” factors on the evolution of rock slope stability. Exogenic factors may lead to damage in the rock mass at the surface of rock slopes (i.e. weathering, erosion, etc.). Conversely, endogenic factors cause the weakening of the rock mass from within the Earth’s crust (earthquakes, volcanism, etc.). The action of the above factors, extending over thousands of years, and the interaction with the aforementioned inherited factors, causes the formation of rock slope damage features such as tension cracks, rock mass dilation and brittle fracture resulting in “progressive failure” of the slope. In the course of this research, several landslide sites were visited, both in North America (the Downie Slide and the Hope Slide, British Columbia, Canada) and Italy (San Leo landslide). At each site, slope damage was investigated using an integrated remote sensing and numerical modelling approach. It was noted that the accumulation of slope damage was driven and controlled by a complex interaction of factors and geomorphic processes, including glacial and fluvial erosion, steepening and undermining of the slope, debuttressing, slope deformations and fatigue. In this paper we provide clear evidence of how mapping and characterization of slope damage features using state-of-the-art remote sensing methods can provide new insights on the style of slope deformation and the factors that control the stability and failure of rock slopes. Finally, it is recommended that the analysis of rock slope damage should be an important component in the workflow to ensure comprehensive rock slope characterization.

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)0.002
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 score0.009
Threshold uncertainty score0.017

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0030.002
Science and technology studies0.0000.000
Scholarly communication0.0010.001
Open science0.0010.000
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0010.001

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 head0.008
GPT teacher head0.200
Teacher spread0.193 · 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

Citations0
Published2019
Admission routes1
Has abstractyes

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