Počet záznamů: 1  

Rate-dependency of residual shear strength of soils: implications for landslide evolution

  1. 1.
    SYSNO ASEP0572535
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevRate-dependency of residual shear strength of soils: implications for landslide evolution
    Tvůrce(i) Duque, J. (CO)
    Loche, Marco (USMH-B) ORCID, RID
    Scaringi, G. (CZ)
    Celkový počet autorů3
    Zdroj.dok.Geotechnique Letters - ISSN 2049-825X
    Roč. 13, č. 2 (2023), s. 105-112
    Poč.str.8 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovalandslide ; residual shear strength ; shear-rate effect ; velocity strengthening ; velocity weakening
    Obor OECDEnvironmental and geological engineering, geotechnics
    CEPSS02030023 GA TA ČR - Technologická agentura ČR
    Způsob publikováníOmezený přístup
    Institucionální podporaUSMH-B - RVO:67985891
    UT WOS000987679900001
    EID SCOPUS85160347537
    DOI10.1680/jgele.23.00004
    AnotaceShear-rate weakening or strengthening behaviours can effectively control landslide runouts, defining sudden runaway sliding or years-long slow-creep phases. These behaviours are partly controlled by the properties of the basal material. Understanding its stress-strain-time response is crucial in physically-based assessments of landslide dynamics and the associated risk. We investigate the frictional resistance of a calcium bentonite, a kaolin and a quartz sand by means of a conventional ring-shear apparatus under normal stresses representative of landslide shear zones. Results for the fine-grained soils, in line with literature on pure clays, indicate important velocity strengthening, whereas small shear-rate effects were observed in sand. As long as effective stresses remain constant, a velocity strengthening response can exert a feedback that, under certain conditions, counteracts perturbations in boundary conditions and prevents fast runouts on pre-existing shear zones. Accordingly, we argue that specifically testing for shear-rate-dependency and incorporating observed behaviours in model formulations can be beneficial for better predicting landslide fates.
    PracovištěÚstav struktury a mechaniky hornin
    KontaktIva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216
    Rok sběru2024
    Elektronická adresahttps://doi.org/10.1680/jgele.23.00004
Počet záznamů: 1  

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