Pith Number

pith:DLTHOOBK

pith:2026:DLTHOOBKFDCRHN62HXYTX6LX2C

not attested not anchored not stored refs resolved

Three dimensional simulation of fluid-driven frictional and tensile ruptures on existing discontinuities

Alexis S\'aez, Ankit Gupta, Antareep Sarma, Brice Lecampion, Regina Fakhretdinova, Sylvain Brisson

An implicit coupled solver simulates three-dimensional fluid-driven ruptures combining frictional slip and tensile opening on intersecting discontinuities.

arxiv:2605.14397 v1 · 2026-05-14 · physics.geo-ph · cs.NA · math.NA · physics.comp-ph · physics.flu-dyn

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\usepackage{pith}
\pithnumber{DLTHOOBKFDCRHN62HXYTX6LX2C}

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Record completeness

1 Bitcoin timestamp

2 Internet Archive

3 Author claim open · sign in to claim

4 Citations open

5 Replications open

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The bundle contains the canonical record plus signed events. A mirror can host it anywhere and recompute the same current state with the deterministic merge algorithm.

Claims

C1strongest claim

The proposed framework simultaneously captures frictional slip, dilatancy, permeability evolution, and tensile opening.

C2weakest assumption

The rock matrix is linearly elastic and impermeable, with failure governed by a poro-elastoplastic cohesive zone interface law.

C3one line summary

A new implicit fully-coupled hydro-mechanical solver simulates 3D fluid-driven frictional slip and tensile opening on arbitrary intersecting fractures using combined boundary element and finite element methods.

References

300 extracted · 300 resolved · 1 Pith anchors

[1] Kato, A. and Sakai, S. and Iidaka, T. and Iwasaki, T. and Hirata, N. , date-added =. Non-volcanic seismic swarms triggered by circulating fluids and pressure fluctuations above a solidified diorite in 2010

[2] Ross, Z. E. and Rollins, C. and Cochran, E. S. and Hauksson, E. and Avouac, J-P. and Ben-Zion, Y. , date-added =. Aftershocks driven by afterslip and fluid pressure sweeping through a fault-fracture m 2017

[3] The deep Basel-1 geothermal well: an attempt assessing the predrilling hydraulic and hydrochemical conditions in the basement of the Upper Rhine Graben , volume = 2022

[4] Duration of hydraulic fracture containment by tougher bounding layers , year =

[5] Faults simulations for three-dimensional reservoir-geomechanical models with the extended finite element method , volume = 2016

Receipt and verification

First computed	2026-05-17T23:39:07.540168Z
Builder	pith-number-builder-2026-05-17-v1
Signature	Pith Ed25519 (`pith-v1-2026-05`) · public key
Schema	pith-number/v1.0

Canonical hash

1ae677382a28c513b7da3df13bf977d0bf00a21596d824ff94e8692a1d239487

Aliases

arxiv: 2605.14397 · arxiv_version: 2605.14397v1 · doi: 10.48550/arxiv.2605.14397 · pith_short_12: DLTHOOBKFDCR · pith_short_16: DLTHOOBKFDCRHN62 · pith_short_8: DLTHOOBK

Agent API

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Verify this Pith Number yourself

curl -sH 'Accept: application/ld+json' https://pith.science/pith/DLTHOOBKFDCRHN62HXYTX6LX2C \
  | jq -c '.canonical_record' \
  | python3 -c "import sys,json,hashlib; b=json.dumps(json.loads(sys.stdin.read()), sort_keys=True, separators=(',',':'), ensure_ascii=False).encode(); print(hashlib.sha256(b).hexdigest())"
# expect: 1ae677382a28c513b7da3df13bf977d0bf00a21596d824ff94e8692a1d239487

Canonical record JSON

{
  "metadata": {
    "abstract_canon_sha256": "7f1012f9819f58bf4e8d0f4d84f2843fc5ea35f2040e4a1ac2ff8d1f49556f12",
    "cross_cats_sorted": [
      "cs.NA",
      "math.NA",
      "physics.comp-ph",
      "physics.flu-dyn"
    ],
    "license": "http://creativecommons.org/licenses/by-nc-sa/4.0/",
    "primary_cat": "physics.geo-ph",
    "submitted_at": "2026-05-14T05:25:28Z",
    "title_canon_sha256": "e13abfce7d12fe26b2cd5ae8585dbecda242f1d59561ae028e21eb37c6d135fe"
  },
  "schema_version": "1.0",
  "source": {
    "id": "2605.14397",
    "kind": "arxiv",
    "version": 1
  }
}