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Self-affine rock joint profiles

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F17%3APU125610" target="_blank" >RIV/00216305:26110/17:PU125610 - isvavai.cz</a>

  • Result on the web

    <a href="https://sgemworld.at/sgemlib/spip.php?article9115" target="_blank" >https://sgemworld.at/sgemlib/spip.php?article9115</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5593/sgem2017/12/S02.091" target="_blank" >10.5593/sgem2017/12/S02.091</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Self-affine rock joint profiles

  • Original language description

    The two-dimensional profile curves created by Barton are often used in geotechnics for the determination of the rock joint coefficients. These two-dimensional profiles of solid surfaces show self-affine properties, i.e. they are scaled differently in x- and y- directions. Similarly, the three-dimensional reliefs (3D) of solid surfaces are scaled differently in z-direction in comparison to x- or y-directions. Therefore, the vertical sections of surface reliefs (two-dimensional profiles) are self-affine curve (self-affine fractals) whereas the horizontal sections (horizontal contours) correspond to self-similar fractals. The two-dimensional self-affine profiles require a special treatment when their fractal dimensions are computed. Many papers devoted to the fractal properties of these profiles were published in the past but only a few of those papers employed a convenient computational method that would have guaranteed a sound value of that dimension. As a consequence, anomalously low dimensions were presented. This paper briefly describes one of the possible way of performing fractal analysis of the 2D self-affine profiles of rock joints whose fractal dimensions are occasionally used for classification of joint rock coefficients. These coefficients enters the formula of shear strength of inclined rock joints and in this way they assist to evaluate mechanical stability of rocky terrains.

  • Czech name

  • Czech description

Classification

  • Type

    D - Article in proceedings

  • CEP classification

  • OECD FORD branch

    10504 - Mineralogy

Result continuities

  • Project

    <a href="/en/project/GA13-03403S" target="_blank" >GA13-03403S: Morphology analysis of fracture surfaces and its consequences for stability of large civil engineering constructions</a><br>

  • Continuities

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

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Article name in the collection

    17th International multidiciplinary scientific geoconference SGEM 2017

  • ISBN

    978-619-7105-99-5

  • ISSN

    1314-2704

  • e-ISSN

  • Number of pages

    6

  • Pages from-to

    713-718

  • Publisher name

    STEF92 Technology Ltd.

  • Place of publication

    Bulharsko

  • Event location

    Albena

  • Event date

    Jun 27, 2017

  • Type of event by nationality

    WRD - Celosvětová akce

  • UT code for WoS article