A platform for research: civil engineering, architecture and urbanism
A rotating block method is developed to calculate the rotational displacement of slopes of saturated clay under seismic loading. The method is similar to the pseudo-static sliding block method of Newmark and is quite easy to use in design calculations. When the threshold acceleration for rotation is exceeded, the slope will start to rotate until the angular velocity for rotation is reduced to zero. Rotational displacement will be accumulated each time the threshold acceleration is exceeded during ground vibration. The influence of ground motion characteristics on the computed slope deformation is evaluated. Implications for design are discussed.
A rotating block method is developed to calculate the rotational displacement of slopes of saturated clay under seismic loading. The method is similar to the pseudo-static sliding block method of Newmark and is quite easy to use in design calculations. When the threshold acceleration for rotation is exceeded, the slope will start to rotate until the angular velocity for rotation is reduced to zero. Rotational displacement will be accumulated each time the threshold acceleration is exceeded during ground vibration. The influence of ground motion characteristics on the computed slope deformation is evaluated. Implications for design are discussed.
Rotating Block Method for Seismic Displacement of Slopes of Saturated Clay
Second International Conference on Geotechnical and Earthquake Engineering ; 2013 ; Chengdu, China
IACGE 2013 ; 27-36
2013-10-09
Conference paper
Electronic Resource
English
Rotating Block Method for Seismic Displacement of Slopes of Saturated Clay
British Library Conference Proceedings | 2013
|Seismic Stability Analysis of Saturated and Unsaturated Soil Slopes Using Permanent Displacement
DOAJ | 2018
|Seismic response of saturated cohesionless slopes
British Library Online Contents | 2000
|Seismic response of saturated cohesionless slopes
British Library Conference Proceedings | 2000
|Seismic response of saturated cohesionless slopes
Online Contents | 2000
|