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Shaking Table Test of Geogrid Reinforced Soil Slope with Gabion Surface Protection

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ABSTRACT Gabions are one of the important slope protection forms for reinforced soil slopes. However, the seismic performance of this type of reinforced soil slope has not been clearly investigated. In this study, a scaled shaking table test was conducted on a reinforced soil slope model with gabions as surface protection under different seismic waves. The acceleration response, slope deformation, earth pressure, and tensile force distribution in the geogrid of the slope model were systematically studied to evaluate its performance under seismic action. The results showed that under the action of Wenchuan (WC) and EI Centro (EI) waves, the height-dependent amplification and surface-amplification phenomena coexisted in the reinforced soil slope, while the WC wave exerted a stronger influence on the acceleration response. Both peak and residual horizontal displacements of the slope surface increased with rising input peak ground acceleration (PGA) and elevation. Larger displacements accompanied by a relatively weaker recovery capability were observed in the slope under the WC wave compared to the EI wave. The slope crest settlement exhibited nonlinear dynamic responses with four distinct stages. The final slope top contour line presented an arc-shaped distribution and the EI wave-induced settlement trends aligned with WC wave behaviors. The dynamic vertical earth pressure responses across the slope exhibited a consistent pattern as the input PGA and seismic waves changed. The tensile force growth trend across geogrid positions displayed three stages based on the input PGA. Additionally, the tensile force induced by the WC wave exceeded that induced by the EI wave.

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The southwestern mountainous region of China is tectonically active and characterized by high, steep anti-dip rock slopes with weak intercalations. Under seismic action, the dynamic response characteristics of these slopes are complex, and the mechanisms of deformation and damage remain unclear, hindering effective disaster risk prevention and control. Based on extensive investigations of high and steep slopes in the upper reaches of the Jinsha River, a conceptual geological model is developed. It examines the dynamic response characteristics and deformation failure of the slopes under varying conditions of peak ground acceleration(<italic>PGA</italic>), seismic wave frequency, and loading direction through large-scale shaking table model tests. The results indicate pronounced nonlinear dynamic response characteristics of weak interlayer anti-dip rock slopes under seismic action, exhibiting significant height and surface effects. As the<italic> PGA</italic> increases, these two dynamic amplification effects become more prominent. The vertical dynamic response of slopes within the range of 1/3<italic>h</italic> to 2/3<italic>h</italic> demonstrates a surface effect when subjected to sinusoidal waves. As the frequency of sinusoidal waves increases, the region exhibiting a greater dynamic response gradually shifts from 1/3<italic>h</italic> to 2/3<italic>h</italic> towards the foot of the slope. When <italic>PGA</italic>≥0.4 <italic>g</italic>, under the action of a 2 Hz sinusoidal wave, the dynamic response in the damage area at the top of the slope shows signs of decay. Under the influence of the Wenchuan wave, the horizontal dynamic response at the slope<italic>'</italic>s top and surface is significantly weaker than the vertical dynamic response. However, under the effect of high peak ground acceleration(<italic>PGA</italic>≥0.4 <italic>g</italic>) seismic waves, an opposing pattern is observed. The vertical dynamic response in the upper range of 1/2<italic>h</italic> to 5/6<italic>h</italic> of the slope is stronger when loading occurs simultaneously in the <italic>x</italic> and <italic>z</italic> directions compared to loading the Wenchuan wave solely in the <italic>x</italic> direction. The deformation and failure process of the slope model can be categorized into five stages: the tiny damage stage, the cracking stage at the slope top, the failure stage at the slope shoulder, the evolution stage of the sliding surface, and the instability stage of the sliding surface.

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Load transformation from the yielding part of the soil to the adjacent part is known as the soil arching effect, which plays an important role in the design of various geotechnical infrastructures. Terzaghi’s trapdoor test was an important milestone in the development of theories on soil arching. The research on earth pressure of the trapdoor problem is presented in this paper using the three-dimensional (3D) discrete element method (DEM). Five 3D trapdoor models with different heights are established by 3D DEM software PFC 3D. The variation of earth pressure on the trapdoor with the downward movement of the trapdoor, the distribution of vertical earth pressure along the horizontal direction, the distribution of vertical earth pressure along the vertical direction, the distribution of lateral earth pressure coefficient along the depth direction, the magnitude and direction of contact force chain are studied, respectively. Related research results show that the earth pressure on the trapdoor decreases rapidly after the downward movement of the trapdoor, and then reaches the minimum earth pressure. After that, the earth’s pressure will rise slightly, and whether this phenomenon occurs depends on the depth ratio. For the bottom soil, due to the stress transfer caused by the soil arching effect, the ratio of earth pressure in the loose area decreases, while the ratio of earth pressure in the stable area increases. With the trapdoor moving down, the vertical earth pressure along the depth in the stable zone is basically consistent with the initial state, which shows an approximate linear distribution. After the trapdoor moves down, the distribution of earth pressure along with the depth in the loose area changes, which is far less than the theoretical value of vertical earth pressure of its self-weight. Because of the compression of the soil on both sides, the lateral earth pressure coefficient of most areas on the central axis of the loose zone is close to the passive earth pressure coefficient Kp. The existence of a ‘soil arch’ can be observed intuitively from the distribution diagram of the contact force chain in the loose zone.

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Early adjusting damping force for sloped rolling-type seismic isolatorsbased on earthquake early warning information
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By means of installing sloped rolling-type seismic isolators (SRI), the horizontal acceleration transmitted to the to-be-protected object above can be effectively and significantly reduced under external disturbance. To prevent the maximum horizontal displacement response of SRI from reaching a threshold, designing large and conservative damping force for SRI might be required, which will also enlarge the transmitted acceleration response. In a word, when adopting seismic isolation, minimizing acceleration or displacement responses is always a trade-off. Therefore, this paper proposes that by exploiting the possible information provided by an earthquake early warning system, the damping force applied to SRI which can better control both acceleration and displacement responses might be determined in advance and accordingly adjusted in a semi-active control manner. By using a large number of ground motion records with peak ground acceleration not less than 80 gal, the numerical results present that the maximum horizontal displacement response of SRI is highly correlated with and proportional to some important parameters of input excitations, the velocity pulse energy rate and peak velocity in particular. A control law employing the basic form of hyperbolic tangent function and two objective functions are considered in this study for conceptually developing suitable control algorithms. Compared with the numerical results of simply designing a constant, large damping factor to prevent SRI from pounding, adopting the recommended control algorithms can have more than 60% reduction of acceleration responses in average under the excitations. More importantly, it is effective in reducing acceleration responses under approximately 98% of the excitations.

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