All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Assessing the Efficiency of Thermochemical Pressurization in the Jiweishan Rockslide

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F23%3A10476851" target="_blank" >RIV/00216208:11310/23:10476851 - isvavai.cz</a>

  • Result on the web

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=94x9jewk71" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=94x9jewk71</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00603-023-03639-y" target="_blank" >10.1007/s00603-023-03639-y</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Assessing the Efficiency of Thermochemical Pressurization in the Jiweishan Rockslide

  • Original language description

    Thermochemical pressurization is a possible weakening mechanism that could explain the hypermobility of large landslides in carbonate rock. However, the factors controlling the efficiency of this mechanism in generating hypermobility have not been elucidated. Here, we use mass and energy conservation equations - accounting for the thermal decomposition of carbonate and a thermoporoelastic mechanism - to evaluate the efficiency of thermochemical pressurization in the 2009 Jiweishan rockslide event in China. We consider distinct permeability functions for the shear zone and the rock wall, controlled by distinct mechanical processes, and explore the sensitivity of the model to changes in the values of the key parameters. We evaluate that a combination of pore pressure increase and the endothermic nature of the chemical reaction may effectively limit frictional heating. We observe that the increase in pore pressure is controlled by the permeability of the rock wall rather than by that of the shear zone and its thickness. We also find that the permeability of the damaged rock wall is the key factor controlling the energy ratio-a measure of efficiency. We conclude that the comparatively low velocity and small thickness of the sliding body, and the relatively high permeability of the formation in which the Jiweishan landslide developed may have limited the effect of thermal decomposition.

  • 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

    10505 - Geology

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

    2023

  • 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

    2

  • Country of publishing house

    AT - AUSTRIA

  • Number of pages

    14

  • Pages from-to

    793-806

  • UT code for WoS article

    001101725500001

  • EID of the result in the Scopus database

    2-s2.0-85176812802