Structural-State Closure of the Full Stick–Slip Cycle: Reproducing the Inter-Slip Locked Phase and Delineating Its Boundary from Rate-and-State Friction

Statistical studies of stick–slip (the published PES companion [1]) describe the avalanche endpoint: event-size distributions, precursory signals, and critical slowdown. What remains unresolved is the full time course: during the long inter-slip (locked) loading period, how does the contact network of the frictional interface evolve continuously, and can a closed model reproduce the complete sequence and delimit its boundary against the continuous state-evolution equations of rate-and-state friction (RSF)? This paper develops a structural-state closure in which two unresolved interfacial coordinates carry the dynamics: a sliding-generated structure s (relaxing at a loading-rate-independent time \(\tau_{N}=1 / b\) ), and a contact maturation m (Dieterich ageing). A high-speed liquid-lubrication floor closes the slip phase and renders the free block–spring selfsustaining. Three results follow. (i) \(T 1\) exact reduction: on the PES-validated speed branch the steady-state of the closure is identical to the published two-component ice-friction law of Pan [1] to a maximum deviation of \(3.0 ×10^{-8}\) , and the free slider produces repeated stick– slip (153 events; mean recurrence 25.4; mean stress drop 0.302). (ii) Locked-phase two-channel divergence: during loading the structure softens (s relaxes) while maturation hardens (m ages), so the static strength is non-monotone (strength dip 0.071 at \(t ~eq 19.9\) ), with slip nucleating near \(t ~eq 688\) . A single-state RSF law predicts monotone ageing only and cannot reproduce this dip. (iii) Testable predictions: (P2) the non-monotone dip of Dillavou and Rubinstein [5] is reproduced, but the experimental memory scaling \(T_{min } \propto T_{W}\) requires upgrading the structure channel to a power-law relaxation spectrum with logarithmic maturation — then the closure reproduces \(T_{min }=0.59 T_{W}\) against the AOI value \(0.30 T_{W}\) ; (P1) the precursory time span shortens with load-point velocity, consistent with the loading-rate series of Wang and Dresen [7]. We delineate the boundary: RSF performs well in monotone-aging and velocity-strengthening regimes, whereas the closure compensates for non-monotone recovery and memory scaling. All model results are reproducible from the enclosed reduced equations; experimental numbers are distinguished from model demonstrations throughout.

Authors

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-10-30
DOI
https://doi.org/10.5281/zenodo.23789450
Primary Topic
earthquake and tectonic studies
Type
preprint
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
preprint

Structural-State Closure of the Full Stick–Slip Cycle: Reproducing the Inter-Slip Locked Phase and Delineating Its Boundary from Rate-and-State Friction

Guojun Pan
Zenodo (CERN European Organization for Nuclear Research)
earthquake and tectonic studies
preprint

Structural-State Closure of the Full Stick–Slip Cycle: Reproducing the Inter-Slip Locked Phase and Delineating Its Boundary from Rate-and-State Friction

Guojun Pan
preprint en

Abstract

Statistical studies of stick–slip (the published PES companion [1]) describe the avalanche endpoint: event-size distributions, precursory signals, and critical slowdown. What remains unresolved is the full time course: during the long inter-slip (locked) loading period, how does the contact network of the frictional interface evolve continuously, and can a closed model reproduce the complete sequence and delimit its boundary against the continuous state-evolution equations of rate-and-state friction (RSF)? This paper develops a structural-state closure in which two unresolved interfacial coordinates carry the dynamics: a sliding-generated structure s (relaxing at a loading-rate-independent time \(\tau_{N}=1 / b\) ), and a contact maturation m (Dieterich ageing). A high-speed liquid-lubrication floor closes the slip phase and renders the free block–spring selfsustaining. Three results follow. (i) \(T 1\) exact reduction: on the PES-validated speed branch the steady-state of the closure is identical to the published two-component ice-friction law of Pan [1] to a maximum deviation of \(3.0 ×10^{-8}\) , and the free slider produces repeated stick– slip (153 events; mean recurrence 25.4; mean stress drop 0.302). (ii) Locked-phase two-channel divergence: during loading the structure softens (s relaxes) while maturation hardens (m ages), so the static strength is non-monotone (strength dip 0.071 at \(t ~eq 19.9\) ), with slip nucleating near \(t ~eq 688\) . A single-state RSF law predicts monotone ageing only and cannot reproduce this dip. (iii) Testable predictions: (P2) the non-monotone dip of Dillavou and Rubinstein [5] is reproduced, but the experimental memory scaling \(T_{min } \propto T_{W}\) requires upgrading the structure channel to a power-law relaxation spectrum with logarithmic maturation — then the closure reproduces \(T_{min }=0.59 T_{W}\) against the AOI value \(0.30 T_{W}\) ; (P1) the precursory time span shortens with load-point velocity, consistent with the loading-rate series of Wang and Dresen [7]. We delineate the boundary: RSF performs well in monotone-aging and velocity-strengthening regimes, whereas the closure compensates for non-monotone recovery and memory scaling. All model results are reproducible from the enclosed reduced equations; experimental numbers are distinguished from model demonstrations throughout.

Zenodo (CERN European Organization for Nuclear Research)
earthquake and tectonic studies
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Laika access coming soon