The Influence of the Mutual Relationship between Dilatancy and Fluid Flow on the Strength of Localized Shear Bands in Permeable Rocks

Bibliografski detalji
Parent link:AIP Conference Proceedings
Vol. 1909 : Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2017 (AMHS’17).— 2017.— [020193, 4 p.]
Glavni autor: Shilko E. V. Evgeny Viktorovich
Autor kompanije: Национальный исследовательский Томский политехнический университет (ТПУ) Институт физики высоких технологий (ИФВТ) Кафедра физики высоких технологий в машиностроении (ФВТМ)
Daljnji autori: Dimaki A. V. Andrey Viktorovich, Psakhie S. G. Sergey Grigorievich
Sažetak:Title screen
The paper is devoted to the numerical study of the influence of the mutual relationship between dilatancy of solid skeleton and pore fluid inflow on the value of shear strength of shear bands in rocks. We show that this influence has a nonlinear and nonmonotonic character and strongly depends on the degree of confinement of a shear band. The results of the study broaden the understanding of possible limits of the change in the strength of localized shear bands and are relevant for solving the problem of estimating the conditions for the onset of an accelerated relative slip of structural blocks in rock massifs.
Режим доступа: по договору с организацией-держателем ресурса
Jezik:engleski
Izdano: 2017
Teme:
Online pristup:https://doi.org/10.1063/1.5013874
Format: Elektronički Poglavlje knjige
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=657174
Opis
Sažetak:Title screen
The paper is devoted to the numerical study of the influence of the mutual relationship between dilatancy of solid skeleton and pore fluid inflow on the value of shear strength of shear bands in rocks. We show that this influence has a nonlinear and nonmonotonic character and strongly depends on the degree of confinement of a shear band. The results of the study broaden the understanding of possible limits of the change in the strength of localized shear bands and are relevant for solving the problem of estimating the conditions for the onset of an accelerated relative slip of structural blocks in rock massifs.
Режим доступа: по договору с организацией-держателем ресурса
Digitalni identifikator objekta:10.1063/1.5013874