10626 FACTA UNIVERSITATIS Series: Mechanical Engineering https://doi.org/10.22190/FUME220327020F © 2020 by University of Niš, Serbia | Creative Commons License: CC BY-NC-ND Original scientific paper NUMERICAL SIMULATION OF DYNAMICS OF BLOCK MEDIA BY MOVABLE LATTICE AND MOVABLE AUTOMATA METHODS Alexander E. Filippov1,2, Valentin L. Popov2 1Donetsk Institute for Physics and Engineering, Donetsk, Ukraine 2Technische Universität Berlin, Berlin, Germany Abstract. Two versions of modified Burridge-Knopoff model including state dependent friction, elastic force and thermal conductivity are derived. The friction model describes a velocity weakening of friction and elasticity between moving blocks and an increase of both static friction and rigidity during stick periods as well their weakening during motion. It provides a simplified but qualitatively correct behavior including the transition from smooth sliding to stick-slip behavior, which is often observed in various tribological and tectonic systems. Attractor properties of the model dynamics is studied also. The alternative versions of the model are proposed which apply a simulation of the motion of interacting elastically connected mesh elements and motion of relatively large solid blocks, utilizing technique of the movable cellular automata. First version of the model was already basically studied before. Its advanced version here involves all components of the real system: state-depending friction and changeable rigidity, as well as heat production and thermal conductivity. Model based on the movable automata also involves the components included into traditional lattice model. It has its own ad-vantages and disadvantages which are also discussed in the paper. Key words: Burridge-Knopoff model, Friction, Tectonics, Voronoi diagram, Delaunay triangulation 1. INTRODUCTION One of the most important applications in the study of the behavioral patterns of mechanical systems of block structures are the geological faults and block environments. Of particular interest, of course, is the study of the possible variations of their deformation, potential prediction or even prevention of the strong seismic shocks. The Received: March 27, 2022 / Accepted April 23, 2022 Corresponding author: Alexander E. Filippov Donetsk Institute for Physics and Engineering, R. Luxemburg Str. 72, 83114 Donetsk, Ukraine E-mail: filippov_ae@yahoo.com 2 A.E. FILIPPOV, V.L. POPOV fact that the statistics of earthquake force and their time correlations meet the laws of Gutenberg-Richter [1,2] and Omori [1,3], typical for self-organized critical systems [4,5], is often the basis for the conclusion that earthquakes are a process formed on all spatial scales ranging from microscopic to continental plate scale. During last decades [6,10] on the basis of modeling by movable cellular automatons and full-scale experiments it was shown some possibility of initiation of the fault wing displacement and, consequently, the release of a part of the accumulated elastic energy as a result of local effects on the fault area, including vibration load and watering [11-16]. One of the often applied to study the problems under interest is the well-known Burridge-Knopoff (BK) model [17,18] initially proposed many years ago to investigate statistical properties of earthquakes. Numerical studies by Carlson et al. [19,20] have demonstrated that BK model can reproduce characteristic empirical features of tectonic processes such as the Gutenberg-Richter law for the magnitude distribution of earthquakes, or the Omori law for statistics of aftershocks [19-22], both properties stemming from the so called “self-organized criticality” of this system. It has been intensively used to simulate different aspects of the problem [21-40] and to discuss general properties of earthquakes statistics as well as predictability of earthquakes. Numerical simulations give evidences that the self-organized criticality and the corresponding fractal attractor of the system is closely related to dynamic structures with “traveling waves” [23], their ordering and specific “phase transitions” [24] controlled by a number of parameters (external driving velocity, springs stiffness, number of blocks, their mutual interaction and so on). It is in particular the dependence of the dynamic properties of the BK model on spring stiffness which makes it necessary to introduce the generalization of the friction law proposed in the works [41,17]. The physical reason for the stick-slip instability in the Burridge-Knopoff model is the assumed decrease of the friction force with the sliding velocity [19,20]. Motion of a single block with this friction law is always unstable which does not correspond to properties of real tribological systems. The real law of rock friction is more complicated [29,34]. In this article we base on the realistic friction laws described in the handbooks [34,35]. The main qualitative pictures of a realistic law are: (a) approximately logarithmic increase of the static friction force as a function of contact time – the property, found already by Coulomb, and (b) a logarithmic dependence of the sliding friction on the sliding velocity. Both properties can be described in the frame of “state dependent” friction laws by introducing additional internal variables describing the state of the contact [17,41-43] as well as shear band propagation effect on the deformation and fracture [44,45], generation and propagation of slow deformation in geomedia [46-48]. Modified version of the BK model with a state dependent friction force, reproduces in the simplest way both the velocity weakening friction and the increase of static friction with time when the block is not moving. 2. METHOD Let us briefly remind the original BK model. The blocks of mass m are attached to a moving surface by springs with stiffness k1 and are coupled to each other by springs with stiffness k2. The moving surface has velocity v, and the blocks are in contact with a rough Block-media Motion Lattice and Movable Automata Numerical Models 3 substrate. The friction force F between the blocks and the rough surface is assumed to depend only on velocity. The equations of the BK model can be written in the following form:     2 2 1 1 12 2 ( ) j j j j j j u m k u u u k vt u F v t           , (1) where v=const is the external driving velocity and vj≡∂uj/∂t is an array of individual block velocities (j=1, … N). The sliding friction force is supposed to decrease monotonously from a constant initial value F0. It is further supposed that the static friction F(vj→0) can possess any necessary negative value to prevent back sliding 0 0 , 1 ; / 0 1 2 / (1 )( ) ( , 0] / 0 j jj j F F u t vF v u t                  . (2) The parameter α defines a rate of friction decrease when block starts to slide, and σ is the acceleration of a block at instant when slipping begins [19,20]. The friction equation (2) is an oversimplification of real properties of static and kinetic friction which is now explained in detail in the books [34,35]. Dieterich has proposed friction equations with internal variables [29,30], where the friction force is dependent upon an additional variable that describes the state of the contact zone. This variable is in a sense a “melting parameter.” Friction force at non-zero velocity drops down from its initial value due to a “shear melting” effect which may have different physical nature [17-20]. When the motion stops, the surfaces start to form new bonds and the static friction increases with time. The dynamics of systems with state dependent friction has been investigated in a number of papers [29-37]. Majority of these studies were devoted to the simple one- particle version of the model, but it was also done for many-body BK model with a state dependent friction [17], where the friction force is defined by the additional kinetic equation:  1 0 2 [ ( )] j j j j F v t F F v t        . (3) with β2<0, at vj>0, and F(vj)=-∞ in opposite case vj≤0. The parameters β1 and β2 have following meaning. When a block starts to slide with vj>0 its friction force monotonously decreases from an initial value F0. General time scale of this process is determined by the first parameter β1 and an effectiveness of the melting is given by a relation between absolute value of negative parameter β2<0 and β1. It should be noted that the kinetic equations for state dependent friction at sliding are not unique. Different forms of this equation have been proposed [17,18] leading to qualitatively similar behavior of the dynamic friction at vj>0. The above form is just simplest and even linear one. The equations of motion in Eqs. (1-3) are nonlinear wave equations. Last few decades different variants of such equations have been widely studied, starting from the very early implementation of the numerical simulations [38]. In particular, it has been shown that N interacting segments of the nonlinear chain form a collective attractor with energy transfer 4 A.E. FILIPPOV, V.L. POPOV performed by nonlinear excitations [39,40]. Depending on the relations between total energy and strength of the interaction between the blocks k2, the chain can form nearly uniform or strongly non-uniform structures and phase patterns. Analogous behavior should be expected in the modified Burridge-Knopoff model as well. Instantaneously moving blocks must be involved with stationary ones in the overall motion. This causes a “detachment” wave, propagating along the chain. Such waves were found and studied in the original BK model [18], and the analogous process exists in the modified one. There are two possible types of traveling waves: (a) after a transition time all the blocks are provoked to move simultaneously, (b) in steady state some of the blocks can be found instantaneously motionless while others move. One would expect the reaction of the chain to depend on the strength of the interaction between the blocks. This question has been studied for the original BK model in [20], and a specific “phase transition” between correlated and uncorrelated behavior has been found. Real contact of two surfaces is two-dimensional. Let us generalize the MBK to the case. The generalized model is very similar to the one-dimensional model but incorporates a 2D array of blocks connected by elastic springs in both directions. All other components of the MBK remain unchanged. The system of equations of motion takes the form:     2 , , 2 1, 1, , 1 , 1 , 1 , ,2 4 ( ); j n j n j n j n j n j n j n j n j n u u m k u u u u u k vt u F v t t                   (4)   , , 1 0 , 2 , , , , ( ( )) , 0, 0 ( ) 0 j n j n j n j n j n j n j n F v t F F v v t F v v              . (5) where j=1, …, Nx and n=1, …, Ny. Nx and Ny are the numbers of elements in the x- and y- directions. For general applicability to tribological problems Eq.(4) contains also a viscous term η∂uj/∂t. Our calculations show that attractor properties are weakly influenced by the viscous term at sufficiently high velocities vj. For generality, we keep small nonzero value η=0.05. Other parameters are: β1=1, β2=125, F0=1, k1=1. k2=36, v=0.2. Large scale structure of the wave state in the two-dimensional model with number of dimensionless grid cells (Nx = 700, Ny = 300) shown by the velocities v=v(x,y;t)≡∂u/∂t is reproduced in Fig. 1 by the colored surface (MatLab color-map ‘jet’). Dark blue corresponds to zero. Mutual scattering manifests itself in high sharp peaks of the “events” reproduced here by the intensive red of the corresponding densities. Instant structure of the wave state and history of the events are combined in Fig. 2. The subplots (a) and (c) here represent snapshots of the instantaneous densities of the local displacements u=u(x,y;t) and velocities v=v(x,y;t)≡∂u/∂t, respectively. Time-space representation of this process is shown in the subplot (b), and time dependency of total area of events (d). The information about attractor behavior is accumulated in Fig. 3 and briefly described in the caption to this figure. Block-media Motion Lattice and Movable Automata Numerical Models 5 Fig. 1 Large scale structure of the wave state in the two-dimensional model shown by the velocities v=v(x,y;t)≡∂u/∂t reproduced by the colored surface (MatLab color-map ‘jet’). Dark blue corresponds to zero. Mutual scattering manifests itself in high sharp peaks of the “events” reproduced here by the intensive red of the corresponding densities. Fig. 2 Instant structure of the wave state and history of the events in the model. Subplots (a) and (c) represent snapshots of the instantaneous densities of the local displacements u=u(x,y;t) and velocities v=v(x,y;t)≡∂u/∂t, respectively. The colormaps are equidistant and normalized to the intervals between maximum (red) and minimum (blue) values for the displacements [-1,1] and velocities [0 1.5]. Time-space representation of this process is shown in the (b) and (d) by the spatial-temporal map and time dependency of total area of events. 6 A.E. FILIPPOV, V.L. POPOV Fig. 3 The attractor of the variable effective friction in projection to the plane {v, Ffriction}, where = is shown by color-map ‘jet’ in the subplot (a). The attractor behavior of the system causes quasi-periodic behavior of the mean area of the events. Correlation function in the subplot (b) here is calculated for the area of events shown in Fig. 2a. The same attractor is projected onto the plane {v,u} in subplot (c). To characterize the difference of the correlated and uncorrelated behavior, an order parameter has been introduced in ref. [25]. If we define a value hj in block number j by the condition: 1 u / 0 (the block is moving); 0 u / 0 j j j t h t         , (6) then the local density of the order parameter H*j can be written as H * j=hj(hj+1+hj-1). This function takes on unit value H*j=hj(hj+1+hj-1)=1 if block j is moving and exactly one of its nearest neighbors is also moving. Further, H*j=hj(hj+1+hj-1)=2 when both nearest neighbors of the moving block are in motion. All other cases yield H*j=0. Our observations with the modified model show that even for blocks at vanishing inter-block interaction k2→0 (when the motion of neighboring blocks is almost uncorrelated), the fraction of configurations where sets of neighboring blocks are moving is still relatively high. All that to say, the combination H*j=hj(hj+1+hj-1) does not vanish in such an uncorrelated system. It is therefore convenient to construct another simple combination: 1 1 1 all 3 blocks , 1, 1 in contact are moving 0 otherwise j j j j j j j H h h h         . (7) This makes Hj=hjhj+1hj-1 zero in all cases except when both neighboring blocks of a central sliding block are also in motion. This combination can be used as an “order parameter”. To extract integral quantitative information about the steady ordered and disordered states we calculate also the time evolution of the ensemble-averaged order parameter: H(t>≡ =1/t ∫Hj(t)dt. As an illustration the dependence of the integrated order parameter on the stiffness k2, showing a transition from correlated to uncorrelated block motion was calculated for one- dimensional system. It is shown in Fig.4. Two well defined limiting cases can be seen easily: the order parameter tends to a constant non-zero asymptote →const≠0 at strong interaction k2>>1 and vanishes →0 below the transition point k2≈0. Block-media Motion Lattice and Movable Automata Numerical Models 7 Fig. 4 Phase transition from correlated to uncorrelated motion of blocks in a one- dimensional system. The order parameter tends to a constant asymptote at high mutual interaction k2>>1 and vanishes below transition point k2= k2,critical≈1. Two intermediate fluctuation regions A and B correspond to the states with short-range and long-range correlated nonlinear excitations, respectively. Let us return now to general problem. If the interaction is already varied due to the motion with nonzero velocity, it sounds natural to modify the elasticity (potential channel of the interaction) of the system into the state dependent one, which varies at nonzero velocity and gradually returns to the initial one in static limit:     2; , 2 2; 1, 2; 1, 2; , 1 2; , 1 2; , 1 20 2 , 4 j nj n j n j n j n j n k j n k k k k k k k k v t                  . (8) The same note can be done about the thermalization of the system by a heating produced by the mechanical work performed by the external force. Local power consumed by the system in every node of the lattice can be calculated as a work per unit of time: Q(rj,n)=fj,nvj,n. It can be treated as local source of energy acting in every node and temperature expansion inside the system should be described by the thermal conductivity equation:  , 1, 1, , 1 , 1 , ,4 ( ) j n j n j n j n j n j n j n T T T T T T Q r t              . (9) It is possible to repeat all the simulations of the previous section, reproduce all the results presented in Figs.1-3 and demonstrate that these properties are common for all the modifications of the model. So, let us concentrate below on some additions coming from generalized version of the model. Large scale structure of the velocity fluctuations analogous to that plotted in Fig. 1 accompanied by the variations of the elasticity self-consistently calculated according to Eq. (8) is shown by the colored surfaces (mainly red picks and blue smooth relief, respectively) in Fig. 5. One can see directly that strong fluctuations of the velocity cause deep valleys in the surface of elasticity and in turn “prefer” to appear in the same places again. 8 A.E. FILIPPOV, V.L. POPOV Fig. 5 Large scale structure of the velocity fluctuations accompanied self-consistently by the variations of the elasticity are shown by the colored surfaces (mainly red picks and blue smooth relief, respectively). Fig. 6 The temperature deviations (bright spots in Matlab color-map ‘hot’ normalized in the interval [0 2]) caused by the same instant configuration of the system as in Fig. 5. Green contour lines show median value of the elasticity profile and mark mutual correlation between its deep valleys and hot regions. The same correlation exists between the spatially dependent elasticity and the temperature deviations. In Fig. 6 the temperature deviations (bright spots in Matlab color- map ‘hot’) caused by the same instant configuration of the system as in Fig. 5 are shown. Green contour lines show median value of the elasticity profile and mark mutual correlation between its deep valleys and hot regions. To extract physically meaningful quantitative information about the earthquakes in the system different time moments one can calculate a density of power consumed by the Block-media Motion Lattice and Movable Automata Numerical Models 9 system at each time moment and overlap it other densities of the system like: distributed rigidity, friction constant and temperature. The local power in the frames of the model can be calculated as a work produced by the forces acting on each lattice node of the system pij=fijvij during a unit of time. Calculating spatially distributed power pi=fivi enables one to evaluate the degree of localization of excitations and hence the fraction of the regions in which the fragments of the lattice move practically as a whole. As at a particular site the energy is absorbed and released at different points in time, it is useful to characterize these sites by the absolute value of the power, |pi|=|fivi|. However, if formally accumulate the statistics of such “events” using all the nodes as independent realizations, strongly overestimated value of the small “events” will be obtained. Physically only the quakes with a magnitude higher than a critical one would be treated as the observable ones. Moreover, if the amplitude of the power exceeds the critical value for a number of mutually connected nodes, all of them will be treated by the potential observers as one common event with an average amplitude in this connected area. So, we organized the procedure in this manner: all the nodes were found with the amplitudes higher than the critical one; defined all the connected domains of them and calculated mean amplitudes for every such a region. To control visually the above procedure, we plotted these domains by the (bright) ‘jet’ colors over the (blue) map of the rigidity for every time moment. Typical instant realization of such a picture is presented in Fig. 7. The histogram calculated for these events, as it is shown in Fig. 8 in double-logarithmic scale. Fig. 7 Instant connected regions of the “earthquakes” (bright spots) and valleys of the small rigidity (deep blue) plotted together to illustrate their mutual correlations. The artificial colors for the magnitude and rigidity are shifted to red and blue parts of the spectrum to clearly overlap both densities in one picture. As we already noted above the variations of the friction, elasticity and local velocities are mutually correlated. In other words, new events are preferably generated in the same regions (as it is in the reality). As a result, the system partially memorizes such a common relief for extremely long times. One can calculate, for example, time-averaged relief of effective rigidity, and we did this. It is quite expected that the variations are found to be much smaller than local instant variations of the same value, but they exist. 10 A.E. FILIPPOV, V.L. POPOV Fig. 8 Scaling of the probability to find an earthquake with a particular value of magnitude calculated for the connected event regions. Physically it corresponds to a selection of the rare but intensive “events”, which is compatible with the ideology of the empirical Gutenberg-Richter law. There are also some correlations between such a memorized structure and preferable channels of the wave propagation. Again, the correlation is much weaker than it is observed between instant variations of different densities, but it still exists. These results are illustrated in Fig. 9, where instant and almost stationary time averaged elastic coefficient integrated over long time periods ((a) and (b) sub-plots, respectively) shown by the ‘jet’ color-map. Black contour line depicts mean value of the long-time living rigidity surface. It marks only partial correlations between the averaged and instant rigidities, Analogous (only partial) correlation is found between travelling regions of maximal power production (deep red spots in subplot (b)) and time-averaged relief of the rigidity. Fig. 9 Instant and almost stationary time averaged elastic coefficient integrated over long time periods ((a) and (b) subplots, respectively) shown by the ‘jet’ color-map. Contour line marks only partial correlations between the averaged and instant rigidities, Analogous (only partial) correlation is found between travelling regions of maximal power production (deep red spots in subplot (b)) and time-averaged relief of the rigidity. Block-media Motion Lattice and Movable Automata Numerical Models 11 3. MOVABLE AUTOMATA MODEL Generally, the variant of the model which uses movable system is based on a description of a system of interacting N “particles”. In contrast to described above lattice model which treats system as deformable elastic medium with varied friction and rigidity, here each “particle” simulates a complete block (“solid plate”) in some instant position represented radius-vector ri of its center and the mechanical momentum pi. In simplest approximation, the plates interact with a potential U(ri-rj) depending on the distance |ri-rj| between their centers. It formally leads to the following many-body Hamiltonian: 2 1 , 1 ( , ) / 2 (| |) / 2 N N i i i i i j i i j H m U      r p p r r . (10) In a static configuration the plates are supposed to occupy some equilibrium positions defined by a competition of the repulsion and attraction forces acting between them. In the context of this study, it is convenient to represent the interaction potential by a pair of the Gauss potentials: 2 2(| |) exp{ [( ) / ] } exp{ [( ) / ] } i j ij i j ij ij i j ij U C c D d      r r r r r r , (11) where Cij and Dij define the magnitude, while cij and dij the radii of attraction and repulsion, respectively. The minimization of the energy corresponding to a desired equilibrium with some characteristic distance between the centers corresponds to the inequalities between the parameters: Cij>>Dij, cij>Cij and c<=V0 . Fig. 13 Two projections of the phase portrait on different planes (subplots (a) and (b)). The colors and sizes of the circles depict velocities and interaction coefficients of the individual plates, respectively. Green line with the arrows shows typical individual trajectory, which every point passes in phase space with the time. 18 A.E. FILIPPOV, V.L. POPOV Fig. 14 Instant configuration of the density (surface in subplot (a)) and time-space diagram of the history of events (colormap in subplot (b)). Bold black contours mark intensive “earthquake” events near the propagating right boundary. Different speed of the front and some “epochs” of intensive events can be seen from different inclination of the front and horizontal lines in the recorded history. In particular, it causes quasi-periodic oscillations of the velocity of boundary which are typical for the “stick-slip” nature of the processes. It is actually the same phenomenon, which takes place in ordinary BK model, shown above in Figs. 2-3. In the discrete model one can additionally observe the waves of the velocities, densities and power of the events, which are accompanied by quasi-periodic “epochs” of intensive “earthquakes”. Instant configuration of the density and history of the density integrated along y-axis corresponding to the magenta curve in Fig. 12a are shown in Fig. 14. The instant surface is plotted in subplot (a) and corresponding time-space diagram of the history of events is presented in the subplot (b). Bold black contours mark intensive “earthquake” events near the propagating right boundary. Different speed of the front and some “epochs” of intensive events can be seen from different inclination of the front and deeply colored almost horizontal lines in the recorded history. Exactly the same history of the events (recorded during the same calculation run) as in Fig. 14, is depicted by the intensity of power production (shown by the ‘hot’ color map). The epochs of the intensive earthquakes are much stronger pronounced here than in the previous figure. Block-media Motion Lattice and Movable Automata Numerical Models 19 Fig. 15 Exactly the same history of the events, as in Fig.14, depicted by the intensity of power production (shown by the ‘hot’ colormap). The epochs of the intensive earthquakes are much stronger pronounced here than in the previous figure. 4. CONCLUSION It is shown that original Burridge-Knopoff model allows a number of the modifications which can increase its ability to be adapted to description of the different practically important features of the tectonic phenomena. Basic modifications of the model were already made previously. They incorporate naturally introduced state dependent friction where the friction force is defined by the additional kinetic equation as well as extension of the model to more realistic two-dimensional case. In the present paper we continued previous modifications and mainly concentrated on the following extensions of the model. First of all, elastic force and thermal conductivity were added into consideration. Besides to the velocity weakening of friction between moving blocks, we combined an increase of both static friction and rigidity during stick periods as well their simultaneous weakening during motion. It is expected to give better and qualitatively correct description of plural transitions from smooth sliding to stick-slip behavior, which are normally observed in various tribological and tectonic systems. To 20 A.E. FILIPPOV, V.L. POPOV get easier comparison with the previous versions of the model we initially did this using in standard approach based on interacting elastically connected mesh elements. An alternative version of the model is finally proposed. It applies a simulation of the motion of relatively large solid blocks, utilizing technique of the movable cellular automata. In this advanced version we also involve all the components of the real system: state depending friction, changeable rigidity, as well as heat production and thermal conductivity due to dynamics of the interacting plates, which were already included into the previous versions based on traditional lattice model. Proposed modification has its own advantages and disadvantages, which were discussed in the paper step by step. However, a combination of the different approaches gives additional degrees of freedom, which allows select more convenient or adequate approach depending on the particular problem under consideration. 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