The interaction between rock joints and seismic waves is critical in rock engineering when rock mass is suffered from human-induced or natural earthquakes. Stress wave propagation across rock joints is usually dependent on the seismic response of the joints. Wave propagation may cause joints close or open under the in situ stress. In this paper, the seismic response for wave propagation with an arbitrary incident angle impinging on joints is studied. Both reflection and transmission usually occurring at the two interfaces of the joint are considered, respectively. Wave propagation equations with equally and unequally close-open behaviours are deduced firstly, which can be applied for the general cases of arbitrary incident P- or S-wave. The...
Incident energy gets transmitted, reflected and absorbed across an interface in jointed rock mass le...
Rock joints have significant effects on wave propagation. When the joints are filled with saturated ...
Different methods are presently available for the analysis of wave propagation across jointed rock ...
Due to the presence of joints, waves are greatly attenuated when propagating across rock masses. Zhu...
The propagation of stress waves in filled jointed rocks involves two important influencing factors: ...
Knowledge of wave propagation across rock joints is necessary for understanding distinctions between...
Rock masses are distinguished from other engineering materials by the existence of joints. When a wa...
This paper presents a numerical study on wave transmission across jointed rock masses with UDEC, whe...
The presence of nonlinear discontinuities in a rockmass makes the stress wave propagation rules in a...
AbstractSeismic wave interaction with a slippery rock joint with an arbitrary impinging angle is ana...
Joints are an important mechanical feature of rock masses. Their effect on wave propagation is signi...
The present study essentially employs a thin-layer interface model for filled rock joints to analyze...
Experiments were conducted to study the relationship between the transmission ratio (TR) and normal ...
Rock joints are often filled with weak medium, for example, saturated clay or sand, of viscoelastic ...
When the point under consideration is not near to the source of vibration, the strains developed in ...
Incident energy gets transmitted, reflected and absorbed across an interface in jointed rock mass le...
Rock joints have significant effects on wave propagation. When the joints are filled with saturated ...
Different methods are presently available for the analysis of wave propagation across jointed rock ...
Due to the presence of joints, waves are greatly attenuated when propagating across rock masses. Zhu...
The propagation of stress waves in filled jointed rocks involves two important influencing factors: ...
Knowledge of wave propagation across rock joints is necessary for understanding distinctions between...
Rock masses are distinguished from other engineering materials by the existence of joints. When a wa...
This paper presents a numerical study on wave transmission across jointed rock masses with UDEC, whe...
The presence of nonlinear discontinuities in a rockmass makes the stress wave propagation rules in a...
AbstractSeismic wave interaction with a slippery rock joint with an arbitrary impinging angle is ana...
Joints are an important mechanical feature of rock masses. Their effect on wave propagation is signi...
The present study essentially employs a thin-layer interface model for filled rock joints to analyze...
Experiments were conducted to study the relationship between the transmission ratio (TR) and normal ...
Rock joints are often filled with weak medium, for example, saturated clay or sand, of viscoelastic ...
When the point under consideration is not near to the source of vibration, the strains developed in ...
Incident energy gets transmitted, reflected and absorbed across an interface in jointed rock mass le...
Rock joints have significant effects on wave propagation. When the joints are filled with saturated ...
Different methods are presently available for the analysis of wave propagation across jointed rock ...