PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
July 10, 2026Acta Geotechnica0 citationsOpen Access

A coupled variational phase-field and multiphase flow model for hydraulic fracturing in quasi-brittle materials

HLHui LiSWShanyong Wang

Key Points

  • This research aims to develop and validate a model for simulating hydraulic fracturing in quasi-brittle materials by incorporating multiphase flow dynamics and fracture mechanics.
  • Developed a coupled variational phase-field and multiphase flow model for unsaturated porous media.
  • Utilized finite element method and staggered Newton–Raphson scheme for discretization and solving.
  • Model verified against analytical benchmarks and then applied to study non-wetting pressure effects on fracture interactions.
  • High non-wetting pressure enhances the propagation of natural fractures when intersecting hydraulic fractures.
  • Model outcomes signify differences compared to single-phase simulations in saturated media, providing new insights into hydraulic fracturing behavior.

Abstract

Abstract This study presents a novel coupled variational phase-field and multiphase flow model for simulating quasi-brittle hydraulic fracturing in unsaturated porous media. The multiphase flow is governed by mass and momentum conservation, incorporating a modified Darcy–Poiseuille law to consistently describe wetting and non-wetting fluid transport in both porous matrix and fracture domains. Capillary effects are captured via the van Genuchten retention model. The fluid pressure field is coupled with a phase-field regularized cohesive zone model to simulate fluid-driven crack initiation and propagation. The coupled system is discretised using the finite element method and solved with a staggered Newton–Raphson scheme. Model verification is conducted against analytical benchmarks, followed by application to investigate the influence of non-wetting pressure on fracture interaction. Simulated results show that high non-wetting pressure promotes propagation of natural fractures upon intersection with hydraulic fractures, through the combined effects of pre-opening of natural fractures and the sustained high effective pressure within the connected fracture network. This observed phenomenon differs from single-phase simulation results in saturated-media, providing a novel perspective on hydraulic fracturing mechanisms. The capacity of the proposed model to simulate complex unsaturated hydraulic fracturing is well validated.

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

Li et al. (2026) studied this question.

synapsesocial.com/papers/6a508df96eeac72a437a11a6https://doi.org/10.1007/s11440-026-03058-7
Ask AI
Helpful
Bookmark
Share
View Full Paper

Also Consider

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1A Fully Coupled Hydro-Mechanical Phase-Field Model for Hydraulic Fracture Initiation and Complex Propagation in Porous Rock Media2026
  2. 2Phase-Field Modeling of Hydraulic Fracture in Porous Media with In Situ Stresses2024 · 1 citations
  3. 3Numerical Simulation of Hydraulic Fracturing in the Phase Field from Dynamic Adaptive and Fully Unstructured Gridding2025
  4. 4Phase field modelling of the hydro-mechanical coupling failure mechanisms of fissured rock masses2025
  5. 5Numerical Simulation of Hydraulic Fracture Vertical Propagation in Bedded Shale by Phase-Field Method2024