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Analysis of the internal structure of Brenna sandstone samples with respect to the differences in measured quasi‑elastic moduli

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F24%3A00585109" target="_blank" >RIV/68145535:_____/24:00585109 - isvavai.cz</a>

  • Result on the web

    <a href="https://link.springer.com/article/10.1007/s00603-024-03828-3" target="_blank" >https://link.springer.com/article/10.1007/s00603-024-03828-3</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00603-024-03828-3" target="_blank" >10.1007/s00603-024-03828-3</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Analysis of the internal structure of Brenna sandstone samples with respect to the differences in measured quasi‑elastic moduli

  • Original language description

    The Young’s modulus and Poisson’s ratio determined for the rocks under uniaxial or triaxial loading conditions represent necessary input parameters for solving many geotechnical tasks. However, these effective stiffness moduli, particularly the Poisson’s ratios, measured on different samples sometimes substantially differ, even for visually compact and macroscopically homogeneous rock. This has been observed for Brenna sandstone, especially under conditions of conventional triaxial extensions. The aim of this study was, thus, to reveal differences in rock structure that could cause such behavior. Several complementary methods were used to investigate the structure of this sandstone: X-ray computed tomography (CT), visual analysis using optical scanning and stereo-microscopy, and a new method combining water jet erosion with these visualization techniques. Analyses of this structure revealed mechanically more resistant compact thick and adjacent thin weak layers. In rock samples, these layers have different patterns and orientations. To demonstrate the influence of layer orientation on effective stiffness moduli measured under different loading conditions, FEM calculations were performed for idealized structural models. The outcomes of this numerical analysis are in qualitative agreement with the results of the loading experiments and the layered structure revealed in the samples. The ability of the proposed method using water erosion to analyze the rock structure in detail was verified. The method offers an interesting alternative to standard visual and X-ray CT techniques. The numerical calculations indicate the importance of latent layered defects in sedimentary rocks for fine measurements of stiffness moduli (especially the Poisson’s ratios) used as inputs for geotechnical applications.n

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10302 - Condensed matter physics (including formerly solid state physics, supercond.)

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Rock Mechanics and Rock Engineering

  • ISSN

    0723-2632

  • e-ISSN

    1434-453X

  • Volume of the periodical

    57

  • Issue of the periodical within the volume

    8

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    22

  • Pages from-to

    5913-5934

  • UT code for WoS article

    001198584400003

  • EID of the result in the Scopus database

    2-s2.0-85189624583