Thermo-Hydro-Mechanical Coupling in Fractured Rock:
(4). The next three papers extend these views by taking a closer look on parameters that govern hydraulic diffusivity in sandstones and other types of rocks. Specific targets addressed are the influence of differential stress on permeability (5), imaging of the fracture geometry (6), and pressure in...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Basel
Birkhäuser Basel
2003
|
| Schriftenreihe: | Pageoph Topical Volumes
|
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | (4). The next three papers extend these views by taking a closer look on parameters that govern hydraulic diffusivity in sandstones and other types of rocks. Specific targets addressed are the influence of differential stress on permeability (5), imaging of the fracture geometry (6), and pressure induced variations in the pore geometry (7). Contributions no. 8 to 10 cover investigations of permeability-porosity relationships during rock evolution (8), of the formation, propagation, and roughness of fractures in a plexi-glass block (9), and pressure oscillation effects of two-phase flow under controlled conditions (10). The subsequent four articles focus on diverse modeling approaches. Issues considered are how the geometry and the mechanical behavior of fractures can be characterized by mathematical expressions (11), how the evolution of permeability in a microcracking rock can be expressed by an analytical model (12), deviations from the cubic law for a fracture of varying aperture (13), and the numerical simulation of scale effects in flow through fractures (14). Three further papers refer to in situ observations, being related to topics as the assessment of in situ permeability from the spatio temporal distribution of an aftershock sequence (15), to the scale dependence of hydraulic pathways in crystalline rock (16), and to the significance of pore pressure - stress coupling in deep tunnels and galleries (17) |
| Beschreibung: | 1 Online-Ressource (VI, 354 p. 70 illus) |
| ISBN: | 9783034880831 |
| DOI: | 10.1007/978-3-0348-8083-1 |
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| 520 | |a (4). The next three papers extend these views by taking a closer look on parameters that govern hydraulic diffusivity in sandstones and other types of rocks. Specific targets addressed are the influence of differential stress on permeability (5), imaging of the fracture geometry (6), and pressure induced variations in the pore geometry (7). Contributions no. 8 to 10 cover investigations of permeability-porosity relationships during rock evolution (8), of the formation, propagation, and roughness of fractures in a plexi-glass block (9), and pressure oscillation effects of two-phase flow under controlled conditions (10). The subsequent four articles focus on diverse modeling approaches. Issues considered are how the geometry and the mechanical behavior of fractures can be characterized by mathematical expressions (11), how the evolution of permeability in a microcracking rock can be expressed by an analytical model (12), deviations from the cubic law for a fracture of varying aperture (13), and the numerical simulation of scale effects in flow through fractures (14). Three further papers refer to in situ observations, being related to topics as the assessment of in situ permeability from the spatio temporal distribution of an aftershock sequence (15), to the scale dependence of hydraulic pathways in crystalline rock (16), and to the significance of pore pressure - stress coupling in deep tunnels and galleries (17) | ||
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Datensatz im Suchindex
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| spelling | Thermo-Hydro-Mechanical Coupling in Fractured Rock edited by Hans-Joachim Kmpel Basel Birkhäuser Basel 2003 1 Online-Ressource (VI, 354 p. 70 illus) txt rdacontent c rdamedia cr rdacarrier Pageoph Topical Volumes (4). The next three papers extend these views by taking a closer look on parameters that govern hydraulic diffusivity in sandstones and other types of rocks. Specific targets addressed are the influence of differential stress on permeability (5), imaging of the fracture geometry (6), and pressure induced variations in the pore geometry (7). Contributions no. 8 to 10 cover investigations of permeability-porosity relationships during rock evolution (8), of the formation, propagation, and roughness of fractures in a plexi-glass block (9), and pressure oscillation effects of two-phase flow under controlled conditions (10). The subsequent four articles focus on diverse modeling approaches. Issues considered are how the geometry and the mechanical behavior of fractures can be characterized by mathematical expressions (11), how the evolution of permeability in a microcracking rock can be expressed by an analytical model (12), deviations from the cubic law for a fracture of varying aperture (13), and the numerical simulation of scale effects in flow through fractures (14). Three further papers refer to in situ observations, being related to topics as the assessment of in situ permeability from the spatio temporal distribution of an aftershock sequence (15), to the scale dependence of hydraulic pathways in crystalline rock (16), and to the significance of pore pressure - stress coupling in deep tunnels and galleries (17) Earth Sciences Geology Classical Continuum Physics Earth sciences Continuum physics 1\p (DE-588)1071861417 Konferenzschrift gnd-content Kmpel, Hans-Joachim edt Erscheint auch als Druck-Ausgabe 9783764302535 https://doi.org/10.1007/978-3-0348-8083-1 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Thermo-Hydro-Mechanical Coupling in Fractured Rock Earth Sciences Geology Classical Continuum Physics Earth sciences Continuum physics |
| subject_GND | (DE-588)1071861417 |
| title | Thermo-Hydro-Mechanical Coupling in Fractured Rock |
| title_auth | Thermo-Hydro-Mechanical Coupling in Fractured Rock |
| title_exact_search | Thermo-Hydro-Mechanical Coupling in Fractured Rock |
| title_full | Thermo-Hydro-Mechanical Coupling in Fractured Rock edited by Hans-Joachim Kmpel |
| title_fullStr | Thermo-Hydro-Mechanical Coupling in Fractured Rock edited by Hans-Joachim Kmpel |
| title_full_unstemmed | Thermo-Hydro-Mechanical Coupling in Fractured Rock edited by Hans-Joachim Kmpel |
| title_short | Thermo-Hydro-Mechanical Coupling in Fractured Rock |
| title_sort | thermo hydro mechanical coupling in fractured rock |
| topic | Earth Sciences Geology Classical Continuum Physics Earth sciences Continuum physics |
| topic_facet | Earth Sciences Geology Classical Continuum Physics Earth sciences Continuum physics Konferenzschrift |
| url | https://doi.org/10.1007/978-3-0348-8083-1 |
| work_keys_str_mv | AT kmpelhansjoachim thermohydromechanicalcouplinginfracturedrock |