Three-Dimensional Wave-Field Characteristics of Earth-Rock Dams with Different Hidden Hazards

,e three-dimensional wave-field characteristics of dangerous earth-rock dams are the premise and foundation to identify the hidden hazards of the earth-rock dams via wave test method. Based on the equivalent elastic wave theory in isotropic mediums, the three-dimensional wave field of earth-rock dams with different defects was calculated using the finite element numerical simulation method. ,e characteristic and regularity of the three-dimensional wave field was explored. ,e result of the analysis shows that the size and position of the defects are closely related with the wave-field information received on the dam surface.,e elasticity modulus and density of the defects have great effect on the wave field, and alternately, Poisson’s ratio of the defects has little effect on the wave field. ,e greater the difference between the wave velocity of the hazardous materials and the dam body is, the stronger the energy of the scattered wave will be, which in turn will produce clearer lineups of the scattered wave on the timehistory profile. For a single wave movement signal, the dominant frequency amplitude is exponentially correlated with the longitudinal wave velocity of the hazardous materials. ,erefore, in the process of wave detection for earth-rock dam hazards, the effect of the elasticity modulus, density, and wave velocity on the test signal should be taken into account.,e dominant frequency amplitude can serve as one of the control parameters for interpretation of dam hazards by the analysis of the wave test signal.


Introduction
Geophysical exploration techniques is an important tool for studying the Earth's nonuniform structural and dynamic processes, and seismic tomography is one of the most widely used methods [1,2].According to the wave field's characteristic parameters such as kinetic and kinematics, the range and position of any abnormalities can be obtained.e wave-field characteristics can be utilized for the inversion imaging of a particular medium or anomaly.Seismic wave detection technology has been widely used in geotechnical engineering applications, boasting fast, lossless, and simple operation [3][4][5].Scholars have studied the application of seismic wave detection technology for earth-rock dams. is method was initially used for the geological exploration of the dam and then was gradually utilized for detection of the hidden hazards [6][7][8].Research shows that although the wave signals on the dam surface contain abundant information of the dam's internal structure, it is difficult to improve its inversion accuracy using wave velocity parameters.
erefore, a key application of wave detection technology has become determining how to extract the information about hidden hazards from the test signal.It is necessary to analyze the wave-field distribution characteristics of the dam in order to effectively extract the information of the hidden hazard from the test signal.
e wave equation numerical simulation method is an effective means of studying the wave propagation law and analyzing the internal wave-field distribution of the structure.We can study the propagation mechanism of seismic waves and the interpretation of complex strata by simulating the wave propagation of the composite media.erefore, more and more numerical simulation methods are used to study the propagation characteristics of seismic waves in structures.For example, Kim et al. implemented the finite element method to study the elastic wave propagation of a three-dimensional solid concrete model under the influence of cracks [9].Narayan studied the propagation characteristics of Rayleigh waves in layered media by the finite difference method [10].Bakamjian studied the simulation of the three-dimensional seismic wave propagation by the boundary integral equation method [11].Du simulated the wave field of the anisotropic viscoelastic media via pseudospectrum method [12].
In summary, the interpretation method and wave-field characteristics of the existing nondestructive test data cannot directly serve as the basis for detecting the hidden dam's hazard.It is necessary to describe the wave-field characteristics of an earth-rock dam via wave detection technique.

Three-Dimensional Wave-Field Analysis Model for Earth-Rock Dams
Zhao et al. [8] have proposed a numerical simulation method for three-dimensional wave field of earth-rock dams.According to this method, a three-dimensional finite element model is established.e model size is shown in Figures 1 and 2, and the different hazardous materials have been considered in the model.First, the three-dimensional wave-field characteristics of earth-rock dams with/without hazards are compared, then, the effects of hidden hazards are analyzed.e parameters of the hazardous material are shown in Tables 1 and 2.
(1) Geometric division: theoretically, the wave phenomenon can be observed in a finite element model, so the unit grid size should be less than the wavelength.Usually, the unit grid size is selected less than half of a wavelength to increase accuracy [7].e unit grid density can be increased depending on the actual model size to improve the accuracy.e data collection interval is the step length of the finite element analysis.In principle, the time step should set to a value where the wave cannot pass through the unit.
In this paper, tetrahedron unit SOLID92 with 10 nodes is selected.e grid can be divided freely.e grid size of the dam mass is 4 m, and the grid size of the hazardous mass is 2 m. e analysis time T � 0.8 s, and the time step Δt � 1 ms.
(2) Boundary conditions: based on the viscoelastic boundary conditions in ANSYS software, a spring damper is utilized to mitigate the effects of boundary-reflected waves on the wave-field analysis.(3) Centrum: the centrum is excited by a delta impulse function.Its expression is where A is the maximum amplitude of the excitation force.f is the dominant frequency of the wave load function, where the dominant frequency magnitude directly represents the width of the frequency band.t 0 is the main peak time of the wave load, and T is the centrum cycle.In this paper, A → � −20 kN (vertical downward direction), f � 25 Hz, t 0 � 0.02 s, and T � 0.04 s.

Three-Dimensional Wave-Field Characteristics of Earth-Rock Dams with/ without Hazards
Wave propagation can be directly judged on the basis of the displacement field.us, the displacement field is used to analyze the characteristic rules of the wave field.e threedimensional wave-field characteristics obtained from numerical simulation are shown in Figure 3.By analyzing Figure 3, it is clear that a direct wave can produce scattered waves when it interacts with a hazardous mass different from the dam material.e scattered wave spreads from the hazardous site to the surface of the dam mass over time exhibiting significant motion.
e direct wave gradually spreads out to the distance until eventual absorption caused by the action of the viscous-elastic boundary.At this point, the vibration of the dam particle becomes smooth.e time-history curves are collected at various measuring points parallel to the dam axis on the dam crest.Figure 4 shows the time-history profile that reflects the overall wave-field characteristics.
Based on a contrastive analysis of the time-history profile (Figure 4), it is thus clear that the wave-field information of the earth-rock dam spreads out in the periphery in a very regular manner, and there is no other wave information after the direct wave over time when there is no hazardous mass.When a hazardous mass is present, a scattered wave is produced which spreads to the dam crest once the direct wave reaches the hazardous mass.erefore, significant wave motion signals occur again on the time-history profile in the period following the passage of the direct wave, and these signals are the scattered waves arising due to the presence of the hazardous mass.Figure 3 (wave field) and Figure 4 (time-history profile) indicate that the scattered wave spreads to the dam crest along the surface of the dam slope and leads to significant phase changes in wave motion.e figures show that the X direction has more significant characteristics than the other two directions.us, the existence and characteristics of the hazardous mass within the dam mass can be judged depending on the scattered wave signals received by the surface of the dam.  1.    e time-history curve for all measuring points is used to establish a pro le to analyze the full wave-eld characteristics (Figure 5).

Analysis and Discussion for the Effects of Hidden Hazards
e rst phase of the scattering signal received in the X direction is between 0.1 s and 0.18 s and the central position in the vicinity of the 8th-10th scattering phase.e second phase of the scattering signal received in the X direction is between 0.17 s and 0.24 s and the central position in the vicinity of the 8th-10th scattering phase.It can be concluded that the time points at which the scattered wave generated by the hazardous mass in the same position received on the same measuring line of the dam crest are basically the same.However, the closer the proximity of the defects to that of the surrounding media, the less signi cant the scattering result.
ere is limited information available regarding the lineups for Y direction and Z direction.
e time points for all lineups are basically the same.A greater di erence in material parameters presents a clearer lineup.

Characteristic Analysis for Wave Signals. Time domain analysis:
to enrich the analysis results, the time-history data of a single measuring point is subjected to a quantitative contrastive analysis based on the analysis for the full wave eld.e time-history curve for the same measuring point on the measuring line is selected for comparison (Figure 6, No. 14 measuring point is selected).A single wave signal on the dam surface in the case of di erent hazard characteristics has the following regularities: the vibration amplitude of single measuring points at the same distance from the centrum decreases with the decreased di erence in material properties between the defects and the surrounding media.
erefore, the wave amplitude with an initiation point of scattered signals serves as a parameter for judging the material properties of the defects.
Frequency domain analysis: a time-frequency analysis is conducted for the time-history data of No. 8 measuring point in di erent models mentioned above.Accordingly, we can obtain the regularity concerning the e ect of 6 Advances in Civil Engineering characteristics of the hazardous material on the wave-eld characteristics in the frequency domain (Figure 7).
As the dam and hazard materials exhibit decreasing di erences in wave parameters, the dominant frequency amplitude of the wave signal decreases signi cantly, and the regularities in three directions stay consistent.Obviously, the dominant frequency amplitude is highly sensitive in the wave eld.erefore, it can serve as an important parameter in an inversion study in the actual detection of wave motion, and the expected degree of damage can be estimated on the basis of the dominant frequency amplitude of the wave signal of a single measuring point in the site investigation.

Impact Analysis for Poisson's Ratio.
Based on the nature of homogeneous media, Poisson's ratio is another parameter determining the elastic characteristics of a material.erefore, it is necessary to study the e ect of Poisson's ratio on the wave-eld information.e elasticity modulus and density of the hazardous material remain unchanged.e speci c material parameters are shown in Table 2. e model size and design are the same as mentioned above.e time-history curves for all measuring points on the same measuring line are generated by changing Poisson's ratio of the hazardous material.e analysis of the wave eld of the hazardous earth-rock dam shows that the wave eld in the X direction is highly sensitive to changes in hazards.
erefore, the time-history pro les for wave motions in the X direction are shown in Figure 8.
Figure 8 shows that the characteristic of the scattered wave is not signi cant by changing Poisson's ratio alone, and there are no signi cant changes in phase that can be observed in the time-history pro le.A weak scattering result can still be observed when the elasticity modulus and density are changed and the wave velocity of the longitudinal wave reaches approximately 500 m/s.No scattering result can be observed  Advances in Civil Engineering when only Poisson's ratio is changed and the wave velocity of the longitudinal wave is 484.3 m/s.erefore, we conclude that Poisson's ratio of the defects has little e ect on the scattered wave eld of the earth-rock dam.In other words, the scattered wave eld is not too sensitive to the changes in Poisson's ratio of the hazardous material.
e time-history curve for the same measuring point on the measuring line is selected for comparison (Figure 9).With increasing di erence in wave velocity between the defect material and the dam mass material, the wave motion increases slightly.However, there is no signi cantly abnormal wave motion in the later stage.We conclude that Poisson's ratio has little e ect on the wave eld of the threedimensional earth-rock dam.

Conclusion and Suggestions
A nite element model for the analysis of the threedimensional wave eld of the earth-rock dam with defects was established for numerical simulation of a wave eld.e wave-eld characteristics of the earth-rock dam with/without defects were analyzed.We concluded the following: (1) When hazards are present in the earth-rock dam and the size of the defects are not signi cant enough to cause di raction, it will produce a series of scattering phenomena, such as re ection and refraction, when the direct wave meets the defect.e scattered wave spreads out and reaches the surface of the dam mass and then is nally received by the detector.It indicates a signi cant wave-eld disturbance.e time-history curve still uctuates after the direct wave is propagated.e lineups of the scattered wave are present in the time-history pro le re ecting the overall wave eld.
e lineups are an important signal that re ects the characteristics of the scattered wave eld.It can be used for judging the presence or absence of hazards.
(2) e result of the nite element value calculation in the wave-eld analysis shows that the vertical triangular load excitation method will be used in the wave motion model of earth-rock dam.e threedimensional wave eld of a through leakage passage is highly sensitive to abnormal wave motions in the direction vertical to the dam's axis.(3) e result of the numerical calculation of the nite element model of the earth-rock dam with di erent hazardous material characteristics shows that a greater di erence in wave velocity between the defect's material and the dam's material indicates a more intensive scattered wave eld and a clearer scattering axis on the time-history pro le.In terms of a single wave motion signal, the amplitude corresponding to the dominant frequency is exponentially correlated with the longitudinal wave velocity of the hazardous material.erefore, the amplitude corresponding to the dominant frequency in the inverse analysis for wave motion can serve as one of the control parameters for inversion.(4) When the di erences in longitudinal wave velocity are the same between hazardous materials of the hazardous earth-rock dam, the elasticity modulus and density of hazardous material have a signi cant e ect on the wave eld.ey are highly sensitive in the wave motion analysis; Poisson's ratio is less sensitive in the wave motion analysis.Advances in Civil Engineering difficult to distinguish between defects with different Poisson's ratios during the process of actual exploration.

Figure 1 :Figure 2 :
Figure 1: Schematic diagram for size of the nite element model of a hazard-free earth-rock dam.(a) Transverse section.(b) Longitudinal section.

Figure 3 :
Figure 3: ree-dimensional wave eld of the earth-rock dams with/without hidden hazards.(a) Displacement in x direction at 0.3 s in a case with no hazards.(b) Displacement in y direction at 0.3 s in a case with no hazards.(c) Displacement in z direction at 0.3 s in a case with no hazards.(d) Displacement in x direction at 0.3 s in a case with hazards.(e) Displacement in y direction at 0.3 s in a case with hazards.(f ) Displacement in z direction at 0.3 s in a case with hazards.

Figure 4 :Figure 5 :
Figure 4: Time-history pro le of the earth-rock dams with/without hidden hazards at the same measuring line.(a) Displacement in x direction in a case with no hazards.(b) Displacement in y direction in a case with no hazards.(c) Displacement in z direction in a case with no hazards.(d) Displacement in x direction in a case with hazards.(e) Displacement in y direction in a case with hazards.(f ) Displacement in z direction in a case with hazards.

Figure 6 :
Figure 6: Time-history curve for displacement of No. 8 measuring point of earth-rock dam with di erent hazard characteristics.(a) X direction.(b) Y direction.(c) Z direction.

Figure 9 :
Figure 9: Time-history curve for displacement of No. 8 measuring point on the measuring line of defects in the case of di erent Poisson's ratios.(a) X direction.(b) Y direction.(c) Z direction.

Table 1 :
Material parameters for three-dimensional nite element models.

Table 2 :
Material parameters for defects corresponding to di erent Poisson's ratios.
It is very