Research on Deep-Site Failure Mechanism of High-Steep Slope under Active Fault Creeping Dislocation

The reverse thrust in the deep site causes the upward propagation of stress and displacement in the overlying soil. The displacement ﬁeld around the fault zone is maximum. As the spatial location becomes shallower, the soil displacement gradually becomes smaller. The deformation of the overlying soil is mainly aﬀected by the vertical dislocation of the fracture zone. The monitoring curve showed no abrupt change value, indicating that the top surface of soil did not rupture, and only the inﬂuence of fault on the displacement transfer of the top surface of the soil. When a creeping dislocation occurs in the bottom fracture zone, the maximum principal stress of the upper boundary of the deep site is dominated by compressive stress. The maximum principal stress of the soil on both sides of the fracture zone has a maximum value, and the soil on the right side of the fracture zone has a signiﬁcant compression eﬀect. The maximum principal stress monitoring curve varies greatly, indicating the plastic failure development of soil, which is the same as the research results of the plastic failure zone in the following paper. When the bottom fracture zone starts to move, the plastic zone ﬁrst appears at the junction area between the front end of the bottom fracture zone and the overlying soil. As the amount of dislocation of the fracture zone increases, the plastic zone continues to extend into the inner soil. The left and right sides of the fracture zone show tensile failure and compression failure, respectively. The development of the upper envelope curve in the plastic zone of the overlying soil satisﬁes the Boltzmann equation with a ﬁrst-order exponential growth, while the development of the lower envelope curve satisﬁes the Gauss equation with a second-order exponential growth. The development curve equation of the plastic zone is veriﬁed according to the residual ﬁgures of the ﬁtting result and the correlation parameters.


Introduction
e stability of the slope under the action of earthquake has always been a research hotspot in slope engineering disaster prevention and mitigation. Dislocation of faults during earthquake will cause huge damage to the slope, induce secondary disasters such as landslides and collapses, and cause huge economic losses [1]. With the deepening of research, slope stability gradually formed some classic calculation theories and methods, such as Bishop method [2], limit analysis method [3], and transfer coefficient method [4]. In addition, some experts and scholars have introduced new research methods for the study of slope stability, such as reliability analysis method [5] and grey theory analysis method [6]. At present, experts on slope stability research methods have done a lot of research based on model tests and finite element analysis. Sun and Yao [7] summarized the typical failure geological models of rock slopes in China and revealed the deformation failure mechanism of slopes. Soto [8] used the bottom friction theory to carry out the slope rock mass toppling deformation test to study the stability of the rock slope. Bray and Goodman [9] conducted a theoretical analysis on the bottom friction test and concluded that the rock mass is in the limit equilibrium state and the model is similar to the gravity field. Adhykary et al. [10] studied slope dumping and arc shear failure theory through centrifuge tests. Sun et al. [11] combined numerical simulation and laboratory tests to study the influence of normal fault on the Urumqi subway tunnel and found that the results of numerical simulation and laboratory tests were basically consistent. Ji et al. [12] developed a more complete set of laboratory test equipment based on the advantages and disadvantages of domestic and foreign test devices and verified the reliability of the device. e research results showed that the device was stable and reliable, which could provide a new model test method and research means for future research. Abe et al. [13,14] used three-dimensional discrete element numerical simulation to describe the improved evolution law of fault gouge, and the results showed that the shape of fault gouge fragments and the resulting interaction determined the friction strength of the fault. Lunn et al. [15] proposed a conceptual model of fault development and numerically simulated the time and space development of geometrically complex fault linkage structures with finite element software. e results showed that the geometry was affected by three key factors: stress ratio, original joint geometry, such as contraction or expansion configuration, and the direction of principal stress. Luan et al. [16] used the strength reduction finite element method to propose a plastic zone criterion for slope instability, which was applied in actual slope engineering. Zheng et al. [17][18][19] used the strength reduction method to perform finite element calculations on the slope and obtained the failure process of the slope, which provided a new idea for the study of slope stability. Li et al. [20] simulated the entire process of slope instability through real examples and developed a RFPA system based on the strength reduction method.
e above-mentioned research has important guiding significance for the construction of slope engineering, but it has not obtained a reliable index for how the fault dislocation caused by earthquake affects the stability of the slope and the degree of influence. e failure mode and instability conditions of the slope under fault dislocation need to be further studied. In this paper, based on the finite element analysis software ABAQUS, a calculation model for the deep site of the high-steep slope under the dislocation of the 30°dip angle fracture zone is established. From the deformation propagation of the soil, the distribution of the maximum principal stress of the overlying soil, and the development of the plastic zone during the dislocation of the fracture zone, the failure mechanism of the deep site is studied. According to the range of the plastic zone under the maximum dislocation, the distribution equation of the plastic zone is proposed in order to provide a reference for the instability mechanism of high-steep slopes under fault dislocation.

Establishment of the Three-Dimensional Finite Element Model
Fault dislocation is divided into creeping dislocation and stick-slip dislocation. e stick-slip dislocation is a kind of rapid fracture movement. e entire process takes a short time and the soil layer is not fully deformed. e creeping dislocation is a slow motion that gradually deforms over time. e creeping dislocation gives the soil time to fully deform [21]. Relevant studies have shown [22] that the creeping dislocation has more significant damage than stickslip dislocation.
e dislocation of the bottom fracture zone propagates through the deep site to the slope, which leads to the instability of the slope. is paper takes the deep site at the bottom of the slope toe as the research object to study the failure mode of the deep site under the creep of the fracture zone. Combined with previous studies on the accuracy of slope stability safety factor [23]; after many trial calculations, the overall size of the calculation model is 400 m (length) × 50 m (width) × 105 m (height), which is composed of overlying soil and bottom bedrock. e overlying soil is divided into three parts with thicknesses of 20 m, 30 m, and 50 m from top to bottom. e thickness of the bottom bedrock is 5 m, the fracture zone is located in the middle of the bedrock, whose width is 100 m and dip angle is 30°. e schematic diagram of the calculation model is shown in Figure 1.
e main failure mode of the soil under the dislocation of the fracture zone is shear failure, and the deformation during the whole process will show certain nonlinear characteristics. In order to accurately reflect the elastoplastic constitutive relationship of the stress and strain characteristics of the soil layer, the yield criterion is the Drucker-Prager yield criterion. e bottom bedrock is made of mudstone, and the overlying soil is divided into three layers and superimposed by two materials. e three layers of soil are round gravel soil, silty clay, and round gravel soil from top to bottom. e detailed soil parameters are shown in Table 1.
e calculation of the model is divided into two steps: the initial ground stress balance and the application of displacement in the bedrock fracture zone. In the initial ground stress balance calculation, the bottom and side boundary conditions of the calculation model are all normal constraints, and the upper boundary is a free boundary. e contact between the fracture zone and the overlying soil is set as frictional contact, and the initial ground stress predefined field of the soil itself is obtained by applying gravity. After the initial ground stress is balanced, the normal constraint of the fracture zone is released, and the dislocation is realized by applying the displacement load on the bottom fracture zone. e dislocation direction of the fracture zone is X-direction and Z-direction. e displacement load is mainly applied in the Z-direction, and the maximum displacement is 4.0 m. In this paper, considering the influence of the most adverse conditions, the initial dislocation rate of the fracture zone is set to 0.05 m/s. After a certain displacement due to the activity of the fault zone, the dislocation rate is gradually increased until the displacement reaches 4.0 m, and the overlying soil is fully deformed [24,25]. e displacement load is applied to the meshing nodes of the fracture zone, and the composite direction of the displacement load is consistent with the dip angle. e displacement loading boundary conditions are shown in Figure 2.
Since the model in this paper is an ideal homogeneous soil model, the general static analysis step is iteratively used to determine the solution of the nonlinear problem during the initial ground stress balance, which can improve the solution efficiency. After applying the displacement of the fracture zone, the dynamic implicit algorithm can reach the convergence faster. In order to make the calculation converge faster and make the soil deformation caused by fault action closer to the actual situation, the numerical simulation adopted normal constraints around and under the surface, and no constraints were imposed on the top surface.
Due to the relatively regular shape of the calculation model, the overlying soil and the bottom bedrock are all homogeneous materials. e model is divided by eight-node hexahedral structured elements. e meshing diagram of the model is shown in Figure 3.

Analysis of the Destruction Mechanism of Deep Site under Active Fault
Creeping Dislocation e dislocation of the fracture zone at the bottom of the model is essentially the dislocation of a thrust fault, and the thrust fault is a low-angle fault with large displacement. When the fault movement, it will show significant compression and fragmentation. After the dislocation, fracture structures such as breccia and granular rock will be formed [26], and the displacement value is difficult to obtain in actual engineering. In order to obtain more accurate calculation results, the dislocation range of the fracture zone is set to 0.1∼4.0 m in this paper, and a large number of monitoring points are selected from the displacement distribution, stress distribution, and plastic zone distribution of the soil to reveal the failure mechanism of the deep site under the fault dislocation.

Analysis of the Displacement Response of the Deep Site under the Creeping Dislocation of the Active Fault.
e area closely related to the deep site and the slope is the upper boundary of the overlying soil.
is paper selects the monitoring points of the upper boundary to study the damage of the upper soil through the displacement distribution. e displacement load of the fracture zone is a combination of two directions, so the X-and Z-direction displacement distributions are used for analysis. Figure 4 is the vertical displacement cloud diagram when the fracture zone is displaced by 0.1 m and 4.0 m, and Figure 5 is the displacement distribution curve of the monitoring points on the upper boundary of the deep site in the X-direction and Zdirection under different displacements.
When creeping dislocation occurs in the bottom bedrock fracture zone, the X-direction displacement curve of the overlying soil on the deep site under different displacements is centered symmetrically with a center point of 150 m, and the center point is roughly located in the middle of the fracture zone. e deformation value on the left side of the overlying soil is negative, and the maximum value is approximately at the interface between the front of the fracture zone and the bedrock at 100 m. e deformation value of the soil on the right is positive and the maximum deformation is roughly located at the interface between the back of the fracture zone and the bedrock at 200 m. e distribution range of negative deformation is roughly 0∼150 m, the distribution range of positive deformation is roughly

Shock and Vibration
150∼300 m, and the deep-site deformation within 300∼400 m is basically zero. When the fracture zone is displaced by 0.1 m, the deep-site displacement is mainly distributed in the range of 50∼300 m. With the increase of the displacement amount of the fracture zone, the displacement curve gradually rises, and the slope of the curve at the center point gradually increases.
e Z-direction displacement curve is symmetrically distributed with the axis of symmetry at 150 m. e overall deformation is positive, and the maximum deformation is located at the axis of symmetry. e distribution range of the deformation along the longitudinal direction is roughly 0∼300 m, and the deformation of the soil within the range of 300∼400 m is basically 0, which is consistent with the distribution of the X-direction displacement curve along the longitudinal direction. When the fracture zone is displaced by 0.1 m, the maximum deformation value of the overlying soil on the deep site is 0.05 m. With the increase of the dislocation displacement of the fracture zone, the shape of the curve gradually becomes steeper, and the amount of soil deformation gradually increases. When the fracture zone is displaced by 4.0 m, the deformation value of the upper soil is   the largest, which is 1.75 m, and the deformation range reaches the maximum value.
In summary, the deformation range of the overlying soil along the longitudinal length of the deep site during the dislocation of the fracture zone is roughly distributed in the 100 m area before and after the fracture zone, and the upper soil has the most severe deformation. e negative displacement of the X-direction deformation curve may be due to the forward movement of the left soil body under the pressure of the upper soil body during the dislocation process of the fracture zone.
e Z-direction overall deformation is tensile deformation, and the Z-direction deformation is larger than the X-direction deformation under different displacement amounts. With the increase of the dislocation amount of the fracture zone, the maximum displacement in the X-direction at the boundary of the overlying soil layer is 0.45 m, and the maximum displacement in the Z-direction is 1.75 m. It can be inferred that the propagation of the fracture zone displacement to the overlying soil layer is mainly determined by the vertical displacement.

Analysis of the Stress Response of the Deep Site under the Creeping Dislocation of the Active Fault.
For the upper boundary of the overlying soil, the maximum principal stress distribution is used to measure the damage of its surface. Figure 6 shows the maximum principal stress distribution curve along the longitudinal direction of the upper boundary of the fracture zone with different displacements.
Comprehensive analysis of the maximum principal stress distribution curve of the upper boundary in the above figure shows that the maximum principal stress of the overlying soil is dominated by compressive stress. When the fracture zone just started to move, the maximum principal stress of the soil along the longitudinal length direction increased negatively, and the compressive stress gradually increased. In the area near 100 m, the compressive stress begins to decrease, showing a tendency of tension, but the maximum principal stress value does not show a positive value, and the soil is still in a compressed state. With the increase of the longitudinal distance, the compressive trend becomes more obvious and reaches the maximum compressive stress near 250 m. When the dislocation amount of the fracture zone is 0.1∼1.0 m, the shape of the maximum principal stress distribution curve does not change significantly, but as the displacement amount of the fracture zone increases, the value of the maximum principal stress increases as a whole. When the fracture zone is displaced by 1.5 m, the curve changes greatly. e maximum principal stress value of the soil in the area of 100∼200 m appears to be a plateau, and its value does not change significantly with the increase of the displacement amount of the fracture zone, while the maximum principal stress on both sides of the fracture zone increases significantly. e fracture zone is displaced to the upper right part of the overlying soil at a dip angle of 30°, and the lower right area of the deep site has a significant compression effect. When the dislocation amount is 2.0 m, 3.0 m, and 4.0 m, it can be seen that the variation trend of the maximum principal stress curve has a great change. e analysis reason is mainly due to the plastic failure development situation caused by the influence of fault on the soil, which changes in the soft soil layer. e following will focus on the analysis of this change.

Analysis of the Development of Plastic Zone under the Creeping Dislocation of the Active Fault.
Related research [27] shows that when calculating slope stability and studying slope instability conditions, the equivalent plastic strain penetration from the toe to the slope can be used as an important criterion for slope instability. e distribution of the plastic zone of the overlying soil layer under the dislocation of the bedrock fracture zone indicates the specific damage range of the soil and the development process of the damage. Since there are many working conditions of the model built, the working conditions with a significant development range of the plastic zone are selected for analysis and research. e development cloud diagrams of the plastic zone of the overlying soil under the creeping dislocation of the bedrock fracture zone show that when the bottom fracture zone starts to move, the plastic zone first appears at the boundary between the front end of the fracture zone and the overlying soil. With the increase of the displacement amount of the fracture zone, the plastic zone of the overlying soil begins to develop inside the overlying soil at an angle of 45°. When the fracture zone is displaced by 0.6 m, plastic deformation occurs in the boundary area between the rear end of the fracture zone and the overlying soil, and it extends into the soil with the increase of the displacement of the fracture zone. e plastic zone at the front end of the fracture zone begins to extend inner in a horizontal direction, and the plastic strain is concentrated in the boundary area between the front end of the fracture zone and the overlying soil and gradually decreases inward in a disc-shaped during the whole process. e reason for this phenomenon may be due to the fact that the soil on the left side of the fracture zone mainly bears the tensile force, and the right side mainly bears the pressure during the dislocation process. e compressive strength of soil is much better than its own tensile strength. With the increase of displacement, the soil on the left is gradually damaged, and the soil on the right is gradually crushed. During the whole dislocation process of the bottom fracture zone, the plastic zone development law of the overlying soil is obvious. erefore, it can be inferred that there is a certain connection between the development of the plastic strain of the overlying soil and the dislocation of the fracture zone. As the amount of fault dislocation continues to increase, the soil layer contains a soft clay layer, and a plastic failure zone develops laterally, which is mainly caused by the silty clay layer's soft texture, large cohesive force, and small friction angle, which is easy to be destroyed.

Quantitative Analysis of the Development of Rupture Traces in Deep Site under Active Fault Creeping Dislocation
e development of the plastic zone of the overlying soil is regular in the dislocation process of the fracture zone at the bottom of the deep site. Studying the development of the plastic zone in the dislocation process of fracture zone will provide an important reference for engineering construction and engineering disaster prevention and mitigation [28]. e study in Section 3 of this paper shows that the plastic strain develops more significantly in the area between the overlying soil and the left side of the fracture zone during the fault movement. In order to explore the development law of the plastic zone of the overlying soil, this paper establishes a calculation model for the overlying soil of the uniform round gravel soil and selects the trace of the plastic zone on the left side of the fracture zone under the displacement amount of 4.0 m for quantitative regularity research. Figure 8 shows the cloud diagram of the development of the plastic zone.
When the bottom fracture zone is displaced 4.0 m, the plastic strain in the boundary area between the overlying soil and the front end of the fracture zone is more concentrated. e development area of the plastic zone is divided into an upper envelope and a lower envelope, which is divided into two parts for research.

Development Law of the Upper Envelope Curve of the Plastic Zone.
When the fracture zone is displaced 4.0 m, the development range of the plastic zone is roughly 0∼50 m. According to the approximate range of the upper envelope when the fracture zone is displaced 4.0 m, some suitable reference points are selected and fitted to obtain the upper envelope. e fitting result is shown in Figure 9, and the fitting curve equation and related parameters are shown in Table 2.
e fitting function of the envelope curve on the plastic zone selects Boltzmann equation. Boltzmann extended the Maxwell distribution to Maxwell-Boltzmann distribution, and it has been widely used in engineering practice [29,30]. After bringing the data into the equation, the fitting curve formula of the envelope curve on the plastic zone is obtained: (1) After the fitting curve is obtained, it is determined whether the curve has a good degree of fit according to the residuals and correlation coefficients. e residual figures of the fitting curve are shown in Figure 10.
It can be seen from the fitting curve related parameter table and the fitting curve residual graph that the correlation coefficient R 2 of the fitting curve is 0.9995, and the fitting degree of the reference points and the upper envelope curve is better. e points in the residual graph are distributed on a horizontal band with the origin as the center, and the distribution of scattered points along the horizontal direction is the same, indicating that the residuals are random and the selected regression model is reasonable. erefore, it can be inferred that the development of the upper envelope curve on the plastic zone of the overlying soil during the fracture zone dislocation process satisfies the Boltzmann equation and exhibits a first-order exponential growth.   Shock and Vibration 7

Development Law of the Lower Envelope
upper envelope curve of the plastic zone, reference points are selected for curve fitting according to the range of the lower envelope curve when the fracture zone is displaced 4.0 m. Figure 11 shows the lower envelope curve fitting curve graph, and the relevant parameters of the fitting curve are shown in Table 3. e fitting function of the lower envelope curve in the plastic zone selects the Gauss equation. After bringing the data into the equation, the fitting curve formula of the lower envelope curve in the plastic zone is obtained. After putting the data into the equation, the following formula is obtained:      e residual diagram of the lower envelope fitting curve is shown in Figure 12.
e correlation coefficient R 2 of the lower envelope curve fitting curve is 0.9976, and the fitting degree of the reference points and the lower envelope fitting curve of the plastic zone is better. e points in the residual graph are distributed on a horizontal band with the origin as the center, and the distribution of scattered points along the horizontal direction is the same, indicating that the residuals are random and the selected regression model is reasonable. erefore, it can be inferred that the development of the lower envelope of the plastic zone in the process of fracture zone dislocation satisfies the Gauss equation and exhibits a second-order exponential growth.

Conclusion
is paper uses the finite element analysis software ABAQUS to establish a three-dimensional finite element deep-site calculation model and studies the dynamic response of the deep site through the displacement distribution, stress distribution, and plastic zone distribution of the upper boundary of the overlying layer on the deep site along the longitudinal direction. At the same time, the contours of the plastic zone in the overlying soil are analyzed and fitted, and the failure mechanism of the deep site under the fault creeping dislocation is revealed. e conclusions are as follows: (1) When creeping dislocation occurs in the bottom bedrock fracture zone, the X-direction deformation curve of the overlying soil is centered symmetrically at about 150 m, and the center point is roughly located in the middle of the fracture zone. As the bottom fracture zone is squeezed to the right, the soil on the right side of the overlying layer is deformed negatively, and the soil on the left side is positively deformed. With the increase of the dislocation amount of the fracture zone, the development range of soil deformation continues to increase and finally stabilizes in the range of 0∼300 m. e Z-direction deformation curve is approximately symmetrically distributed around 150 m as the axis of symmetry, and the dislocation of the bottom fracture zone drives the overall positive deformation of the soil. As the amount of displacement of the fracture zone increases, the amount of deformation and the deformation range of the overlying soil continue to increase and stabilize in the range of 0∼300 m. Due to the large distance between the upper boundary and the bottom fracture zone, the amount of deformation gradually decreases in a disc-shaped form as the deformation propagates upward. e maximum displacement in the Z-direction is greater than the maximum displacement in the X direction, and the deformation of the overlying soil is mainly affected by the vertical displacement of the fracture zone. e monitoring curve showed no abrupt change value, indicating that the top surface of soil did not rupture, only the influence of fault on the displacement transfer of the top surface of the soil. (2) When creeping dislocation occurs in the bottom fracture zone, the maximum principal stress of the upper boundary of the overlying soil layer on the deep site is dominated by compressive stress. e maximum principal stress of the soil on both sides of the fracture zone has a negative maximum value. Because the entire fracture zone is displaced to the upper right at a dip angle of 30°, the compression effect of the soil on the right side is significant. When the displacement of the fracture zone is less than 1.5 m, the platform range of the maximum principal stress curve is roughly the same as the range of the fracture zone. When the displacement is greater than 1.5 m, the range of the platform expands to 100∼250 m. e maximum principal stress monitoring curve shows a great change, indicating the development of plastic failure of soil, which is the same as the result of the plastic failure zone studied later.
(3) When the bottom fracture zone started to move, the plastic zone first appears at the junction area between the front end of the fracture zone and the overlying soil. With the increase of the amount of dislocation of the fracture zone, the plastic zone of the overlying soil begins to develop inside the overlying soil at an angle of 45°. After the fracture zone is displaced for a certain distance, a plastic zone begins to appear in the boundary area between its rear end and the overlying soil and extends to the upper part of the soil with the increase of the dislocation of the fracture zone, while the plastic zone at the front end extends horizontally inward. e soil on the left side of the fracture zone mainly bears the tensile force, and the right side mainly bears the pressure. e compressive strength of the soil is greater than the tensile strength, so the size of the plastic strain is concentrated in the boundary area between the front end of the fracture zone and the overlying soil and gradually decreases inward in a disc-shaped form. With the increase of the displacement amount of the fracture zone, the soil on the left shows tensile failure, and the soil on the right shows compression failure. As the amount of fault dislocation continues to increase, the soil layer contains a soft clay layer, and a plastic failure zone develops laterally, which is mainly caused by the soft clay layer's soft texture, large cohesive force, and small friction angle, which is easy to be destroyed.

Data Availability
All the data in this paper are available from the corresponding author upon request.

Conflicts of Interest
e authors declare that they have no conflicts of interest.