Hydrogeomorphic Relations Among Soil Pipes, Flow Pathways, and Soil Detachments Within A Permafrost Hillslope
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.
Bibliographic record
Abstract
Abstract Soil pipes have been cited as preferential flow features within permafrost hillslopes. However, there has been limited discussion on their mechanisms of formation and relation to other hillslope process such as slope stability and the development of preferential flow pathways. On an organic-covered permafrost-underlain subarctic slope in Yukon Territory, Canada, pipe formation and development processes were studied in an attempt to ascertain their larger role in the hillslope hydrogeomorphic framework. Pipes are widespread on the study slope, conveying water during the snowmelt period when the water table is at or near the surface. During snowmelt, excess pore pressures generated at the heterogeneous thaw front reduce soil strength, increasing the potential for thaw-zone detachment failures. Upon failure, seepage erosion at the interface between organic and mineral soils induces pipe formation. Pipes, which are closely associated with rills and other zones of preferential flow, then become integrated into the larger hillslope drainage network. Drainage within preferential flow pathways advects heat, leading to local increases in thaw and encouraging ground subsidence where the permafrost is ice-rich. In this way, a positive-feedback occurs whereby preferential flow pathways reinforce their influence on the drainage network through subsidence. Keywords: soil pipingpermafrosthillsloperunoffsubarctic
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 imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.001 |
| 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 | 0.001 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it