Soil Springs for Sloped Ground Movement in Saturated Soil
Bibliographic record
Abstract
Abstract Pipelines buried in sloping ground have not previously incorporated adequately defined soil-springs to represent the reality of forces applied on sloping ground. The soil-spring representation, with its three mutually orthogonal spring pairs, has been developed and defined first by ASCE (1984), and subsequently built on by others. These guidelines were based on physical modelling experiments conducted in the 1970’s and 80’s, and were composed of straight sections of rigid pipe. Those experiments saw the pipe translated relative to the soil in single directions under monotonic movement. The soils studied were largely laboratory (clean sand) and manufactured clays. These experiments define the soil springs for horizontal ground only, and do not necessarily represent the interaction occurring on sloping ground. Physical modelling in a geotechnical centrifuge has been undertaken to study the direct soil-pipe interaction in landslides. Centrifuge modelling recreates scale models in an accelerated gravity field such that the forces, stresses, and physical dimensions are multiplied representing the full-scale equivalent environment. A model pipe representing an NPS 18, ∼X52 line pipe has been designed to allow axial and bending response equivalent to the real-world pipe. Landslides were initiated by elevated pore water pressure, representing above mean seasonal rainfall in upland areas. Pipe strain was monitored using fiber optics and subsurface imaging was used to capture the strain demand (soil displacement) provided by the landslide. Pipe strain was decomposed into bending moment, as well as axial and orthogonal structural forces representing the soil loading on the pipe. Results of the pipe-soil experiments give new insight into the strain transfer between the sloping ground and the pipe. Results show that the peak bending moments shift downslope as the landslide movement progresses. A comparison of American Petroleum Institute (API), DNV, and other industry guidance for springs is made to the pipe-slide interaction results from the physical experiments.
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How this classification was reachedexpand
Full frame machine prediction
Teacher imitationNot 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.
Distilled classifier scores by category (both heads)
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.001 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.003 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.
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".