Stressed state of gas-saturated rock mass around an elliptical excavation

1984 ◽  
Vol 20 (2) ◽  
pp. 153-157
Author(s):  
R. M. Israfilov
Keyword(s):  
Rock Mass ◽  
Stressed State ◽  
Saturated Rock

Investigation of the stressed state of a gas-saturated rock mass near an ellipsoidal working

1980 ◽  
Vol 16 (9) ◽  
pp. 760-767
Author(s):  
Yu. N. Podil'chuk ◽  
V. V. Lyakh
Keyword(s):  
Rock Mass ◽  
Stressed State ◽  
Saturated Rock

scholarly journals Thermo-hydro-mechanical processes in fractured rock formations during a glacial advance

2015 ◽  
Vol 8 (7) ◽  
pp. 2167-2185 ◽  
Author(s):  
A. P. S. Selvadurai ◽  
A. P. Suvorov ◽  
P. A. Selvadurai
Keyword(s):  
Rock Mass ◽  
Fractured Rock ◽  
Fluid Pressure ◽  
Computational Modelling ◽  
Fracture Zones ◽  
Saturated Rock ◽  
Rock Formations ◽  
Geological Formation ◽  
High Level Nuclear Waste ◽  
High Level

Abstract. The paper examines the coupled thermo-hydro-mechanical (THM) processes that develop in a fractured rock region within a fluid-saturated rock mass due to loads imposed by an advancing glacier. This scenario needs to be examined in order to assess the suitability of potential sites for the location of deep geologic repositories for the storage of high-level nuclear waste. The THM processes are examined using a computational multiphysics approach that takes into account thermo-poroelasticity of the intact geological formation and the presence of a system of sessile but hydraulically interacting fractures (fracture zones). The modelling considers coupled thermo-hydro-mechanical effects in both the intact rock and the fracture zones due to contact normal stresses and fluid pressure at the base of the advancing glacier. Computational modelling provides an assessment of the role of fractures in modifying the pore pressure generation within the entire rock mass.

scholarly journals Influence of unloading slots on the stressed state and creep of a rock mass in the vicinity of an excavation

2011 ◽  
Vol 4 (2) ◽  
pp. 110-118 ◽  
Author(s):  
V.M. Pestrenin ◽  
I.V. Pestrenina ◽  
P.P. Kostromina
Keyword(s):  
Rock Mass ◽  
Stressed State

Natural Convection in Water-Saturated Rock Mass under Artificial Freezing

2020 ◽  
Vol 56 (2) ◽  
pp. 297-308
Author(s):  
M. A. Semin ◽  
L. Yu. Levin ◽  
M. S. Zhelnin ◽  
O. A. Plekhov
Keyword(s):  
Rock Mass ◽  
Natural Convection ◽  
Saturated Rock ◽  
Artificial Freezing ◽  
Water Saturated

Stressed state of the rock mass during excavation of the underground machine gallery for the Inguri hydroelectric plant

1978 ◽  
Vol 12 (2) ◽  
pp. 118-123
Author(s):  
S. A. Yufin ◽  
T. G. Chincharauli
Keyword(s):  
Rock Mass ◽  
Stressed State ◽  
Hydroelectric Plant ◽  
Machine Gallery

Effect of excavation on the stressed state of a rock mass in the vicinity of a preparatory working

1972 ◽  
Vol 8 (5) ◽  
pp. 498-501
Author(s):  
I. A. Gorovykh ◽  
P. V. Akimochkin
Keyword(s):  
Rock Mass ◽  
Stressed State ◽  
Preparatory Working

Strength of gas-saturated rock mass around preparatory excavation

1982 ◽  
Vol 18 (11) ◽  
pp. 982-986 ◽  
Author(s):  
R. M. Israfilov
Keyword(s):  
Rock Mass ◽  
Saturated Rock

scholarly journals Thermo-hydro-mechanical processes in fractured rock formations during glacial advance

2014 ◽  
Vol 7 (6) ◽  
pp. 7351-7394 ◽  
Author(s):  
A. P. S. Selvadurai ◽  
A. P. Suvorov ◽  
P. A. Selvadurai
Keyword(s):  
Rock Mass ◽  
Fractured Rock ◽  
Fluid Pressure ◽  
Computational Modelling ◽  
Fracture Zones ◽  
Saturated Rock ◽  
Rock Formations ◽  
Geological Formation ◽  
High Level Nuclear Waste ◽  
High Level

Abstract. The paper examines the coupled thermo-hydro-mechanical (THM) processes that develop in a fractured rock region within a fluid-saturated rock mass due to loads imposed by an advancing glacier. This scenario needs to be examined in order to assess the suitability of potential sites for the location of deep geologic repositories for the storage of high-level nuclear waste. The THM processes are examined using a computational multiphysics approach that takes into account thermo-poroelasticity of the intact geological formation and the presence of a system of sessile but hydraulically interacting fractures (fracture zones). The modeling considers coupled thermo-hydro-mechanical effects in both the intact rock and the fracture zones due to contact normal stresses and fluid pressure at the base of the advancing glacier. Computational modelling provides an assessment of the role of fractures that can modify the pore pressure generation within the entire rock mass.

Stressed state of a rock mass around a working with a relief cavity

1992 ◽  
Vol 60 (1) ◽  
pp. 1270-1273
Author(s):  
S. A. Kaloerov ◽  
A. A. Levshin ◽  
V. A. Polukhin
Keyword(s):  
Rock Mass ◽  
Stressed State
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