Skip to main navigation Skip to search Skip to main content

Numerical study of rock failure due to the pre-existing crack initiation and propagation and hydraulic fractures interaction

  • S. Y. Wang
  • , K. C. Lam
  • , S. K. Au
  • , Li-Jun Su
  • , X. Q. Yang

    Research output: Chapters, Conference Papers, Creative and Literary WorksRGC 32 - Refereed conference paper (with host publication)peer-review

    Abstract

    Rock is a very heterogeneous material, containing various types of weaknesses such as gain boundaries, pores, and cracks and other defects. When rock is subjected to surrounding loading or the increase of hydraulic pressure due to rainstorm, the pre-existing fractures will initiate or propagate at the point of least resistance, which may cause failure of the entire structure of slope, dam and so on. By using Flow-Rock Failure Process Analysis code, F-RFPA2D. Firstly, a numerical simulation and similar materials experiment on rock samples with two pre-existing cracks without hydraulic pressure were conducted to investigate the initiation, propagation, coalescence of cracks and failure mechanism of rock considering the heterogeneity of rock; secondly, another sample with two pre-existing cracks subjected to hydraulic pressure under the loading conditions of different k0 is used to investigate the behavior of hydraulic fractures evolution, and their coupling action. Numerical results reproduce the process of pre-existing cracking evolution process which agreed with the experimental results.
    Original languageEnglish
    Title of host publicationGeotechnical Special Publication
    Pages268-275
    DOIs
    Publication statusPublished - 2006
    EventSoil and Rock Behavior and Modeling - Shanghai, China
    Duration: 6 Jun 20068 Jun 2006

    Publication series

    Name
    ISSN (Print)0895-0563

    Conference

    ConferenceSoil and Rock Behavior and Modeling
    PlaceChina
    CityShanghai
    Period6/06/068/06/06

    Fingerprint

    Dive into the research topics of 'Numerical study of rock failure due to the pre-existing crack initiation and propagation and hydraulic fractures interaction'. Together they form a unique fingerprint.

    Cite this