ArticleScientific reports2026
Morphological evolution indicates the transformation of stress interference in parallel fractures.
Article in Scientific reports, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
What it found
Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.
The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.
Who cites it
0 citing papers in PubMed.
No citing paper in PubMed yet.
Corrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
Authors and funding
7 authors.
Funding
Abstract
Fracture propagation is ubiquitous in natural strata and geological engineering, influencing key processes such as engineering stability assessment and design optimization. While prior studies have investigated the propagation of individual fractures through gelatin experiments, stress interference between fractures has been less considered. This study presents an innovative mirror-symmetric dual-fracture experiment that dynamically correlates fracture morphology with stress interference. Using light attenuation, we quantified the morphological evolution and identified distinct propagation regions governed by different degrees of stress interference. The results indicate that a regional transition occurs when the fracture radius approaches the fracture spacing. We defined a stress interference factor (β) to quantitatively characterize the interaction and derived an analytical model for β, which shows satisfactory agreement with experimental data. Through energy balance analysis during stagnation events, we revealed that the partitioning between elastic energy storage and viscous dissipation varies with fracture radius, explaining the observed differences in stagnation frequency and duration at different propagation stages.
Indexed as
Identifiers
What OpenQuestion holds
Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.