Articles | Volume 14, issue 12
https://doi.org/10.5194/gmd-14-7749-2021
https://doi.org/10.5194/gmd-14-7749-2021
Model description paper
 | 
22 Dec 2021
Model description paper |  | 22 Dec 2021

An explicit GPU-based material point method solver for elastoplastic problems (ep2-3De v1.0)

Emmanuel Wyser, Yury Alkhimenkov, Michel Jaboyedoff, and Yury Y. Podladchikov
Abstract

We propose an explicit GPU-based solver within the material point method (MPM) framework using graphics processing units (GPUs) to resolve elastoplastic problems under two- and three-dimensional configurations (i.e. granular collapses and slumping mechanics). Modern GPU architectures, including Ampere, Turing and Volta, provide a computational framework that is well suited to the locality of the material point method in view of high-performance computing. For intense and non-local computational aspects (i.e. the back-and-forth mapping between the nodes of the background mesh and the material points), we use straightforward atomic operations (the scattering paradigm). We select the generalized interpolation material point method (GIMPM) to resolve the cell-crossing error, which typically arises in the original MPM, because of the C0 continuity of the linear basis function. We validate our GPU-based in-house solver by comparing numerical results for granular collapses with the available experimental data sets. Good agreement is found between the numerical results and experimental results for the free surface and failure surface. We further evaluate the performance of our GPU-based implementation for the three-dimensional elastoplastic slumping mechanics problem. We report (i) a maximum 200-fold performance gain between a CPU- and a single-GPU-based implementation, provided that (ii) the hardware limit (i.e. the peak memory bandwidth) of the device is reached. Furthermore, our multi-GPU implementation can resolve models with nearly a billion material points. We finally showcase an application to slumping mechanics and demonstrate the importance of a three-dimensional configuration coupled with heterogeneous properties to resolve complex material behaviour.

1 Introduction

Graphics processing units, or GPUs, have revolutionized the entire field of high-performance computing (HPC) in the last decade. GPUs are many-core processors that were originally developed by the gaming industry in the mid-1990s to accelerate graphics and video rendering. Currently, GPUs are widely employed hardware accelerators used in various applications, including artificial intelligence (AI) and machine learning. GPUs are also increasingly used for high-performance scientific computing (see Dong et al.2015b; Omlin et al.2018; Räss et al.2018; Zhang et al.2021; Alkhimenkov et al.2021). The majority of the scientific algorithms on many-core (e.g. GPU) hardware accelerators are memory-bounded, meaning that data transferring (reading and writing) limits the performance of a solver. This is in contrast to the recent compute-bounded algorithms, where arithmetic floating point calculations are the main limiting factor in solver performance. This GPU supercomputing breakthrough requires re-engineering existing scientific codes or developing new algorithmic structures to efficiently take advantage of the intrinsic low-level parallelism of GPUs.

The material point method (MPM) was first proposed by Sulsky et al. (1994) and was further advanced by the generalized interpolation material point method (GIMPM) by Bardenhagen and Kober (2004). It can be thought of as a finite-element method (FEM) in which (a) integration points (i.e. material points) move and (b) convey state variables, e.g. stress and strain components. The continuum is discretized by material points. The nodal momentum equations are solved on a background mesh, and nodal basis functions provide a mapping framework between the mesh and the material points to transfer either the updated nodal solution or material point properties. The background mesh is reset and actually never deforms. It has been widely used for large deformation geomechanical problems such as retrogressive failure, coupled hydromechanical landslides or granular collapses (Tran and Sołowski2019; Bandara and Soga2015; Dunatunga and Kamrin2015).

From a computational point a view, it is critical for MPM to be able to simulate large-scale problems in both two- and three-dimensional configurations. From this perspective, a few researchers have exploited parallel computing using a single or multiple GPU strategy (Dong et al.2015a; Dong and Grabe2018) to efficiently implement an explicit GIMPM for two-dimensional configurations. More recently, some researchers in the graphics community presented a similar implementation (Gao et al.2018; Hu et al.2019; Wang et al.2020) for three-dimensional configurations. One of the most computationally expensive operations in MPM is mapping between material points and their associated nodes, which is supported by basis functions. When implementing a GPU, the two most common approaches are gathering and scattering. The former gathers the material point's state variables (i.e. mass, velocity component or stresses) to the nodes, whereas the latter scatters (i.e. distributes) the material point's state variables to their associated nodes. This leads to write conflicts, as several threads are writing into the same memory location at the same time. Gao et al. (2018) demonstrated the superiority of scattering over gathering, provided that the write conflicts are handled without atomic operations. Gao et al. (2018) proposed parallel scattering that results in a performance of an order of magnitude higher than that of a naive atomic implementation. Recently, Wang et al. (2020) proposed an Array of Structures of Arrays (AoSoA) as an efficient layout. It is largely responsible for CPU or GPU performances, as it dictates the memory access pattern by ensuring coalesced memory accesses (Wang et al.2020).

We propose an explicit GIMPM implementation in a three-dimensional configuration on a single GPU and multiple GPUs (ep2-3De v1.0), taking advantage of the efficient vectorized algorithmic structure of the MPM solver proposed by Wyser et al. (2020a). Our GPU-based solver relies on built-in functions of atomic operations for the mapping between material points and their associated nodes (i.e. scattering). For large-scale simulations, the main hardware limit is the GPU on-chip memory, which was well documented by Dong and Grabe (2018). To resolve the GPU on-chip memory limitation, we rely on a distributed memory parallelization using the message passing interface (MPI) standard. The multi-GPU implementation can resolve models with nearly a billion material points. The GPU solver ep2-3De v1.01 combines MATLAB for pre- and postprocessing activities with the massive power of the most recent GPU architectures available (Ampere, Turing and Tesla architectures). This approach allows the user to easily set the problem's geometry and initialize the material points as well as their state variables. Everything needed is then passed to the GPU, which further performs the computations. We propose a formal framework to evaluate the performance of our GPU-based implementation based on the metric for memory-bounded codes, i.e. the effective memory throughput (Omlin2017). Since the memory wall has been reached, the memory bandwidth becomes the limiting factor for performance. In addition, it is an easily comparable metric. Similarly, we also report the average number of iterations per second for the same reason: it indicates a relative performance, and it does not depend on material properties (e.g. bulk or shear moduli). We also implement the solver ep2-3De v1.0 under a single-CPU architecture to provide a reference baseline for the performance evaluation of the GPU-based implementation. For the validation of our solver, we simulate the granular collapse problem in a three-dimensional configuration and compare the result against the well-known experimental results of Bui et al. (2008).

2 Numerical implementation

In this section, we briefly describe the governing equations implemented in the MPM solver. We use a linear elastoplastic rheology. Large deformations are carried out via a rate-dependent formulation with the Jaumann stress rate.

2.1 Governing equations

The conservation of linear momentum is given by (using the Einstein summation convention)

(1) ρ v k t = σ k l x l + ρ g k ,

where σkl is the Cauchy stress tensor, vk=uk/t is the velocity, uk is the displacement, gk is the body force, and k,l=13. The conservation of angular momentum is given by σkl=σlk. Dirichlet and Neumann boundary conditions are

(2)uk=ukonΩu,(3)σklnl=τkonΩτ,

where uk and τk are prescribed displacements, and nk is a unit normal vector pointing outward from the boundary ∂Ω of the domain Ω. Following the standard FEM procedure, we use the updated Lagrangian framework; thus, the weak form of Eq. (1) is written in the current spatial configuration. The weak form of Eq. (1) can be obtained by multiplying it with a test function ϕ and then applying integration by parts and divergence theorem, leading to

(4) Ω ϕ ρ a k d Ω = Ω ϕ ρ g k d Ω - Ω ϕ x l σ k l d Ω + Ω τ ϕ τ k d S ,

where vk/t=ak is the acceleration, ϕ is any test function that vanishes on ∂Ωu, and τk is the external traction applied on the boundary ∂Ω, k=13. However, in our MPM implementation, tractions on the boundary are not used. Equation (4) can be solved using a finite-element approach leading to the following compact form:

(5) [ M i j a j ] k = f i ext - f i int k ,

where Mij=p=1npmpϕi(xp)ϕj(xp) is the consistent mass matrix with ϕi(xp) being the basis function between node i and material point p. This work adopts a lumped mass matrix, i.e. miMii=p=1npmpϕi(xp), to avoid an expensive matrix inversion (Sulsky et al.1994; Bardenhagen and Kober2004; González Acosta et al.2020). The external fk,next and internal fk,nint forces at node n are then defined by

(6)fk,next=p=1npmpϕn(xp)gk,(7)fk,nint=p=1npvpϕnxl(xp)σkl,p,

where mp is the material point's mass, vp is the material point's volume and σkl,p is the material point's Cauchy stress tensor. Solving Eq. (5) for the acceleration ak,n, the updated velocity is obtained via a forward-Euler scheme,

(8) v k , n t + Δ t = v k , n t + Δ t a k , n ,

where the velocity is given by vk,nt=mn-1p=1npϕn(xp)mpvk,p and vk,p is the material point's velocity. Boundary conditions are enforced on the boundary nodes. The material point velocity vk,p and coordinates xk,p are defined by mapping (i.e. an interpolation) between the updated solution on the mesh and the material points, i.e.

(9)vk,pt+Δt=vk,pt+Δtn=1nnϕn(xp)ak,n,(10)xk,pt+Δt=xk,pt+Δtn=1nnϕn(xp)vk,nt+Δt,

where nn is the number of associated nodes n to a material point p. The remaining tasks are (i) to update the material point volume and (ii) to solve for the constitutive stress–strain relationship.

2.2 Rate formulation

The large deformation framework necessitates a suitable stress–strain formulation. Some studies prefer the finite deformation framework and employ a linear relationship between Kirchhoff stresses and logarithmic strains (Charlton et al.2017; Gaume et al.2018; Coombs et al.2020). In the present work, we adopt a rate-dependent framework by applying the Jaumann rate (e.g. Huang et al.2015; Wang et al.2016c, b; Bandara et al.2016), which yields an objective stress rate measure.

The Jaumann rate of the Cauchy stress is given by

(11) D σ i j D t = C i j k l 1 2 v l x k + v k x l ,

where Cijkl is the fourth-rank tangent stiffness tensor. Thus, the Jaumann stress derivative may be written as

(12) D σ i j D t = D σ i j D t - σ i k ω ˙ j k - σ j k ω ˙ i k ,

where ωij=(ivj-jvi)/2 is the vorticity tensor, and Dσij/Dt corresponds to the material derivative

(13) D σ i j D t = σ i j t + v k σ i j x k .

By rearranging the Jaumann stress derivative in Eq. (12), we obtain

(14) σ i j t = D σ i j D t + σ i k ω ˙ j k + σ j k ω ˙ i k σ i j R ,

where σijR represents the rotation of the Cauchy stress tensor, which satisfies the stress objectivity for the rate-dependent formulation.

Let us expand σijR in Eq. (14) using identities σij=σji, ω˙ij=-ω˙ji and ω˙kk=0. The Cauchy stress tensor is written using the so-called Voigt notation (as a vector σ={σxx,σyy,σzz,σxy,σyz,σxz}). After expanding, collecting and rearranging terms, the objective stress terms σijR for a three-dimensional configuration are

(15)σxxR=2σxyω˙xy+σxzω˙xz,(16)σyyR=-2σxyω˙xy-σyzω˙yz,(17)σzzR=-2σxzω˙xz+σyzω˙yz,(18)σxyR=ω˙xy(σyy-σxx)+σyzω˙xz+σxzω˙yz,(19)σyzR=ω˙yz(σzz-σyy)-σxyω˙xz-σxzω˙xy,(20)σxzR=ω˙xz(σzz-σxx)+σyzω˙xy-σxyω˙yz,

and, for a two-dimensional configuration assuming plane strain conditions, Eqs. (15), (16) and (18) reduce to

(21)σxxR=2σxyω˙xy,(22)σyyR=-2σxyω˙xy,(23)σxyR=ω˙xy(σyy-σxx).

2.3 Elastoplastic deformation

A non-associated Drucker–Prager (D-P) model with a tension cutoff is used in this study, similar to Huang et al. (2015), Liu et al. (2020), Nguyen et al. (2020) and Zuo et al. (2020), because of its straightforward implementation within explicit numerical solvers. The D-P model has been established as an approximation of the Mohr–Couloumb (M-C) model (Krabbenhoft et al.2012; Alejano and Bobet2012), i.e. a conical yield surface that approximates the M-C yield surface in the principal stress space. The former can be adjusted by parameters, so it passes either through the outer or inner edges of the M-C yield surface (Jiang and Xie2011; De Borst et al.2012).

The D-P yield function f (see Fig. 1) is typically defined in terms of invariants: the first invariant of the Cauchy stress tensor I1=σkk and the second invariant J2=12τijτji of its deviatoric part τij, where the deviatoric part of the Cauchy stress is τij=σij+δijp with the pressure p=-13σkk. The D-P yield surface is made of two surfaces (i.e. representing shear and tensile yield criteria), delimited by

(24)fs(σm,τ)=τ+qϕσm-kϕ,(25)ft(σm)=σm-σt,

where τ=J2 is the effective shear stress, σm=-p is the mean stress, qϕ and kϕ are the material parameters defined by ϕ as the internal friction angle, σt is the tensile strength, and c is the cohesion. Cohesion varies with the accumulated plastic strain ϵp when considering a strain-softening material, i.e. c=f(ϵp). These two surfaces define two plastic regions (see Fig. 1) corresponding to either the shear or tensile failure mode. We use a non-associated plastic flow law for shear and tensile failures; thus, the plastic potential function g is written as

(26)gs(σm,τ)=τ+qψσm,(27)gt(σm)=σm,

where qψ is a material parameter estimated with the dilation angle ψ.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f01

Figure 1Drucker–Prager yield surface in the (σmτ) space. The yield surface is made of a shear line segment (in red) and a tensile line segment (in blue).

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The line segment h(σm,τ)=0 represents the diagonal line between fs(σm,τ)=0 and ft(σm,τ)=0 in the (σm,τ) plane; i.e. h is the boundary between shear and tensile failure modes. The function h(σm,τ) is given by

(28) h ( σ m , τ ) = τ - τ P - α P σ m - σ t ,

with the constants τP=kϕ-qϕσt and αP=(1-qϕ2)1/2-qϕ2. We consider an inner adjustment of the D-P yield surface with respect to the M-C yield surface (de Souza Neto et al.2011), and the model parameter used in Eqs. (24) and (26) are given by

(29)qϕ=6sinϕ3(3+sinϕ),(30)qψ=6sinψ3(3+sinψ),(31)kϕ=6ccosϕ3(3+sinϕ).

In the following, we briefly detail the return mapping strategy used to return the trial Cauchy stress σijtr (i.e. assuming pure elastic deformation only) onto the yield surfaces considering ψ=0. A complete description of such return mapping can be found in Huang et al. (2015). Shear failure is declared when (i) fs(σmtr,τtr)>0 and σmtr<σt or if (ii) h(σtr,τtr)>0 and σmtrσt. The corrected Cauchy stress tensor now reads

(32) σ i j t + Δ t = τ i j tr k ϕ - q ϕ σ tr τ tr + σ tr δ i j ,

with δ the Kronecker tensor. Tensile failure is declared when h(σtr,τtr)0 and σmtrσt. The corrected Cauchy stress tensor reads as

(33) σ i j t + Δ t = σ i j tr + σ t - σ m tr δ i j .
3 GIMPM implementation under a GPU architecture

We propose an explicit generalized interpolation material point method (GIMPM) implementation (Dong and Grabe2018; Wang et al.2020) in a three-dimensional configuration on a GPU, taking advantage of the efficient vectorized algorithmic structure (Wyser et al.2020a, b). We select an explicit GIMPM implementation, which is valid for a variety of problems compared to other recent variants (Wang et al.2019; Coombs et al.2020), i.e. CPDI or CPDI2q. Additionally, we use a double-mapping approach (MUSL; see Nairn2003; Buzzi et al.2008), which consists of updating the stress at the end of the time step. We implement the following domain-update methods: (a) no update of the material point domain, further labelled uGIMPM, and (b) a domain update controlled by the determinant of the deformation gradient, i.e. det(Fij), further labelled cpGIMPM. These domain-update methods are commonly used in the literature (Baumgarten and Kamrin2019; Tran and Sołowski2019). The limitation of the two methods is that they are not ideally suited for specific tests: simple stretching and compression modes (Coombs et al.2020).

3.1 Implementation on a graphical processing unit (GPU)

Graphical processing units (GPUs) are many-core processors originally designed to refresh screen pixels (e.g. for computer games) independently. A schematic representation of the main architecture differences between a CPU and a GPU is depicted in Fig. 2. On the GPU chip, most of the physical space is dedicated to arithmetic logical units, whereas on a CPU, most of the physical space is dedicated to chip host scheduling and control microsystems. GPUs feature many more cores, a lower thread-scheduling cost and a higher memory bandwidth than CPUs. The programming model is based on a parallel principle called single instruction and multiple data (or SIMD); i.e. every single instruction is executed on different data. GPUs feature a hierarchical structure. The lowest computational unit is the thread. Threads are organized into blocks of threads, the whole constituting a hierarchical grid of blocks of threads. A GPU typically launches thousands of threads, which execute the same instruction in parallel, thus achieving massive parallelism. Additionally, the most recent GPUs offer a high throughput (close to a TB per second peak memory throughput).

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f02

Figure 2Schematic chip representation for both the central processing unit (CPU) and the graphical processing unit (GPU) architecture (Nvidia2007). The latter is made of thousands of arithmetic logical units (ALUs). The CPU architecture is primarily dedicated to controlling units and cache memory, and the physical space allowed for ALUs is considerably reduced compared to a GPU architecture.

Currently, most of the algorithms are memory-bounded, meaning that memory transfers limit the performance, in contrast to computer-bounded algorithms, where floating point (arithmetic) operations limit the performance. Thus, for an efficient implementation of an algorithm, one must consider (a) limiting the memory transfers to the bare minimum and (b) avoiding complex data structures (Räss et al.2019a) to benefit from the high throughput capabilities of GPUs. The ability of a GPU is particularly well suited to efficiently execute a large number of local operations in parallel, i.e. SIMD programming. In the case of a GIMPM implementation, this includes the calculation of shape functions and the update of various quantities at the material point level (i.e. stresses, domain lengths, material point volumes, etc.). Below, we present key aspects of our GPU-based implementation using the Compute Unified Device Architecture (CUDA C) language of the Nvidia Corporation, which is a syntax extension of the C programming language.

3.2 The multi-GPU code implementation

One of the major limitations of a single-GPU implementation is the on-chip memory. It is then essential to overcome this limit in order to resolve larger computational domains with a greater amount of material points. We address this concern by implementing a distributed memory parallelization using the message passing interface (MPI) standard. However, we limit our implementation efforts by considering (1) a one-dimensional GPU topology, (2) no computation–communication overlaps, and (3) only mesh-related quantities are shared amongst GPUs; i.e. the material points are not transferred between GPUs during a simulation. We also selected a non-adaptive time step to avoid the collection of the material point's velocities located in different GPUs at the beginning of each calculation cycle.

3.2.1 Algorithm workflow

In our implementation, MATLAB acts as an architect (see Fig. 3). It (1) defines the problem geometry (i.e. the background mesh, material point locations and related quantities, etc.), which can be tedious to initialize in a CUDA C environment. It also calls an external MATLAB script, which compiles the necessary source codes, i.e. gpu.cu or cpu.cu. It further (2) calls either a CUDA C or plain C executable, i.e. gpu.exe or cpu.exe, within a Windows operating system (OS) to solve for the numerical problem and finally (3) imports the results of calculations for further postprocessing tasks.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f03

Figure 3Multifunctional workflow: (1) usage of MATLAB for data initialization, compilation and postprocessing activities and (2) system calls to a performance compiled language such as C (CPU-based) and CUDA C (GPU-based) for heavy calculations. Here, I/O stands for input/output, and the colouring (red or green) specifies which one is active.

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This is a powerful combination between a high-level language such as MATLAB and a performant low-level language such as CUDA C or plain C. It is also easy to invoke system commands directly via MATLAB, i.e. to compile source codes and/or run executables using the built-in command system('…'). We focus on OS-free scripting in MATLAB using a built-in command (i.e. isunix or ispc) to ensure that it performs well under all OS architectures. In addition, such a workflow can be easily extended to other high-level languages such as Python.

3.2.2 Kernels and launch configuration

We briefly describe our GPU-based implementation (gpu_main.cu) while focusing mainly on the computational aspects of the implementation. Implementation of an explicit GIMPM solver into the CUDA C language requires dispatching computational activities into several kernels, i.e. similar to classic functions for a serial implementation in the C language. Each kernel is operated by the GPU only, and kernel launch configuration parameters must be defined for its proper execution. Among them, one must define the number of active threads per block (i.e. the block size) and the number of blocks (i.e. the grid size). A typical kernel is executed N times in parallel by N distinct threads organized into blocks of threads, i.e. a grid of blocks of threads. The principal hardware limitation is the total number of threads within a block: it cannot exceed 1024 threads per block. One must ensure that the maximal size of a block is lower than or equal to this limit.

The computational activities are handled by multiple GPU kernels; 11 kernels are successively launched over a computational cycle. An overall description is given in Fig. 4. A while loop is used to perform the computational cycles, and an MPM step is solved at every cycle. nIO (i.e. the number of accesses to the GPU global memory) is reported in Fig. 4 for each kernel and is estimated by a careful examination of relevant operations within the kernels. Note that all calculations are performed on the GPU, except the calculation of the adaptive time step, which is serially executed by the CPU.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f04

Figure 4Specific workflow for the source code running of the GPU; tend is a user-defined time that controls the total time of the simulation, and the operator * stands for the pointer object, as in the C language. It should be noted that a vast majority of operations within kernels are performed on pointers.

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In our GPU-based implementation, we define two distinct types of kernel launch parameters: (1) those used for mapping between material points and background nodes (i.e. accumulations and projections between material points with their associated nodes and back and forth) and (2) those used for local calculation at the material point or node level (i.e. update of material point stresses or the solution to the momentum balance equations on the Eulerian background mesh). We use regular background mesh because it is straightforward to find the material point's location. However, computing a material point's location using an irregular background mesh is more complicated.

3.2.3 Adaptive time step

An adaptive time step is implemented. For three-dimensional configurations, the maximum elastic wave speed of the material (Anderson1987; Zhang et al.2017) reads as

(34) ( c x , c y , c z ) = c el + max p ( | v x , p | ) , max p ( | v y , p | ) , max p ( | v z , p | ) ,

where cel=((K+4G/3)/ρ)12 is the elastic wave speed of the material; K and G are the bulk and shear moduli, respectively; ρ is the material density; and vx,p, vy,p and vz,p are the material point velocity components. The time step Δt is then restricted by the CFL condition,

(35) Δ t = α min Δ x c x , Δ y c y , Δ z c z ,

where α[0;1] is the time step multiplier, and Δx,Δy, and Δz are the background mesh resolutions.

This requires evaluation of the maximum velocity of all material points at the beginning of each calculation cycle. We choose to sequentially find the maximum velocity using the CPU instead of a parallel implementation on the GPU. This results in systematic memory transfers between the GPU global memory and the random access memory (RAM) of the CPU. However, we report a low performance loss due to these transfers, i.e. a maximal loss of 2 %–5 % in performance, which is acceptable.

3.2.4 Back-and-forth mapping between material points and their associated nodes

The GPU-based algorithm relies heavily on the use of arrays p2e and e2n (Wyser et al.2020a). Elements are numbered with an increasing index. Associated nodes are also numbered in a similar manner. The array e2n of dimension nel×nn, where nel is the total number of nodes and nn is the number of nodes associated with an element e, describes the topological relation between the elements and the nodes of the mesh. Similarly, the array p2e describes the topological relation between the material points and the element in which they are located. These two arrays provide an intuitive definition of the relations between (i) the material points and the nodes they are associated with (i.e. p2n) and (ii) the element and their nodes (i.e. e2n). Then, it is a computationally straightforward process to identify which nodes n are associated with a material point p, which is occupying an element e.

The GPU-based implementation relies on the built-in function atomicAdd() in CUDA C. It performs atomic operations, which avoid the data race of multiple threads, from the same or different blocks to update the same memory location. Atomic operations are extensively used to calculate internal and external force contributions (Eqs. 6 and 7), as well as the lumped mass matrix, and to update the material point's properties such as velocities and coordinates (Eqs. 9 and 10). Dong et al. (2015a) and Wang et al. (2020) reported (for older GPU architectures such as Pascal or Kepler) that atomic scattering can be significantly slower compared to an optimized parallel implementation. However, atomic operations are (a) intuitive to both understand and implement, and (b) they avoid a complex data layout, such as recently proposed in Wang et al. (2020). The use of built-in atomic operations considerably reduces programming efforts.

3.2.5 Treatment of volumetric locking for low-order elements

When low-order elements are used in a GIMP formulation, volumetric locking arises and results in spurious oscillations of the stress field (Jassim et al.2013; Coombs et al.2018; González Acosta et al.2019, 2021). We implement a simple procedure to mitigate volumetric locking when considering near-incompressible behaviour for isochoric plastic flows. Cuomo et al. (2019) and Lei et al. (2020) introduced an element-based averaging method, following Mast et al. (2012). Selected material point properties are reconstructed based on an average value calculated at the element's centre at the end of a time step. However, we propose averaging only the volumetric part of the stress tensor, i.e. the pressure p=-13σkk, while its deviatoric part τij=σij-pδij remains unchanged. We believe our approach is conceptually similar to the B-bar technique (Hughes1980; Bisht et al.2021). This results in the following:

(36) p e = p e v p p p p e v p ,

where vp is the material point's volume. This gives a constant distribution of the pressure field over an element because of its zero-order reconstruction (Lei et al.2020). The Cauchy stress tensor σij,p of a material point p occupying an element e is corrected as

(37) σ i j , p = τ i j , p + δ i j ( p e ) p ,

where δij is the Kronecker delta and (pe)p is the averaged pressure within an element e and assigned to a material point p.

3.3 Available computational resources

The CPU- and GPU-based simulations are performed on a modern workstation running on a Windows 10 operating system with the latest CUDA version v11.2. The CPU is an Intel Core i9-10900K with 10 physical cores of base clock speed (or frequency) of 3.70 GHz, which can rise up to a maximum clock speed of 5.30 GHz, supported with 64 GB DDR4 RAM. It hosts a consumer electronics Nvidia RTX 3090 GPU (the latest Ampere architecture) with 82 streaming multiprocessors (SM units) with a base frequency of 1.40 GHz. This results in 10490 CUDA cores that are supported with an on-chip memory of 24 GB GDDR6 (i.e. the GPU global memory). Other GPUs installed on older desktops are also used to compare their respective GPU performances, i.e. an RTX 2080 Ti (workstation) and a GTX 1650 (laptop), both running on a Windows 10 operating system. Additional simulations were also run on a workstation equipped with the latest Nvidia A100 GPU at the Lomonosov Moscow State University.

Table 1List of the graphical processing units (GPUs) used throughout this study. We also report the peak memory throughput, i.e. MTPpeak, measured thanks to the routine bandwidthTest.cu provided by Nvidia alongside with the CUDA toolkit. When compared with the effective memory throughput MTPeff, one can estimate the possible gain of an additional optimization of the algorithm. This is particularly useful when estimating the level of optimization of a GPU-based implementation.

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Furthermore, GPU-based simulations are also performed on the Octopus GPU supercomputer at the Swiss Geocomputing Centre, University of Lausanne, Switzerland. In particular, the GPU-based simulations are run on the Volta node, hosting a 16 GB Nvidia Tesla V100 (Volta architecture), supported by an Intel(R) Xeon(R) E5-2620 v2 (Haswell) with 2.1 GHz CPU. The latest CUDA version installed is v11.0, and the supercomputer Octopus is operated under a CentOS 6.9. environment. To summarize the computational resources in use, Table 1 presents the main characteristics of the GPUs used in this study.

The multi-GPU simulations are run on the two different systems. The first one is an Nvidia DGX-1 – like node hosting eight Nvidia Tesla V100 Nvlink (32 GB) GPUs and two Intel Xeon Silver 4112 (2.6 GHz) CPUs. The second one is composed of 32 nodes, each featuring four Nvidia GeForce GTX Titan X Maxwell (12 GB) GPUs and two Intel XEON E5-2620V3 4112 (2.4 GHz) CPUs. To summarize the computational resources in use, Table 2 presents the main characteristics of the GPUs used in this study.

Table 2List of the graphical processing units (GPUs) used for multi-GPU simulations.

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3.4 Measuring computational performance on a GPU

Omlin (2017), Räss et al. (2019a, b) and Alkhimenkov et al. (2021) demonstrated that a pertinent metric to quantify the performance of memory-bounded algorithms is the effective memory throughput, i.e. MTPeff in GB s−1. It quantifies the efficiency of data transfers between the global memory (i.e. the on-chip memory of the GPU) and the arithmetic logical units (ALUs) of the GPU. To determine the effective memory throughput, one must estimate (or quantify) the overall set of memory operations (read-and-write or read-only), i.e. nIO, which are needed to resolve a given problem. Consequently, we carefully estimate the minimum number of memory operations while considering a GIMPM-based implementation. This results in the following effective memory throughput:

(38) MTP eff = n iter n IO n p 1024 3 t GPU ( GB s - 1 ) ,

where np is the arithmetic precision (i.e. single-precision floating-point format FP32 or double-precision floating-point format FP64) and tGPU is the wall-clock time in seconds to complete the niter iterations to solve for the numerical problem. For three-dimensional problems, we estimate the minimal number of memory operations for an explicit GIMP implementation as

(39) n IO = 2 n mp ( 43 + 22 n n ) + 26 n no + 2 n el ,

where nmp is the number of material points, nn is the number of associated nodes for an element (i.e. nn=16 in 2D and nn=64 in 3D), nno is the number of nodes, and nel is the number of elements. Additionally, we also report the count of calculation cycles per second of the GPU, i.e. iterations s−1 as well as the wall-clock time. These two metrics give an intuitive sense of the time-to-solution, which is convenient for potential application purposes.

4 Results

In this section, we present two numerical models using the solver ep2-3De v1.0, namely,

  1. Model 1, the granular collapse, which serves as

    • a.

      a validation benchmark against the results of the widely accepted experiment of Bui et al. (2008) under a three-dimensional configuration and

    • b.

      a demonstration of the influence of the mesh resolution on plastic strain localization under a plane strain configuration;

  2. Model 2, the three-dimensional earth slump (Varnes1958, 1978), which serves as

    • a.

      an evaluation of the relative performances of a single- and multiple-GPU-based and CPU-based implementations of the solver ep2-3De v1.0 considering a variety of recent GPU architectures and

    • b.

      a showcase of a potential application of the solver ep2-3De v1.0 for an elastoplastic problem considering different isotropic peak cohesion fields (homogeneous and heterogeneous).

4.1 Model 1

4.1.1 Settings for Models 1a and 1b

We investigate the granular collapse of an aluminium-bar assemblage (Bui et al.2008) under three-dimensional or plane strain configurations. The geometry of the problem is shown in Fig. 5, and its variables are summarized in Table 3 for both three-dimensional and plane strain configurations. Note that for Model 1a, we use the same number of elements in the x direction nel,x=80 as in Huang et al. (2015). As a direct comparison for Model 1b under a plane strain configuration, Huang et al. (2015) used nel=15 360, Δx=Δz=2.5 mm and nmp=25 600.

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Figure 5Initial configuration for the granular collapse numerical model. The blue surrounding frame depicts the computational domain (i.e. the background Eulerian mesh), and the red volume is the granular material, which is discretized by 8 material points. The total number of background elements nel depends on the number of elements in the x direction nel,x used to discretize the granular material.

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Table 3Parameters used in Models 1a and 1b for the granular collapse. nel,i is the number of elements to discretize the granular material in the ith direction, nel and nno are the total number of elements and nodes of the background mesh, npe is the number of material points per element, and nmp is the total number of material points. Note that the mesh resolution is Δx=Δy=Δz= 2.5 mm.

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We consider a non-cohesive granular material of density ρ= 2650 kg m−3, with a bulk modulus K= 0.7 MPa and a Poisson's ratio ν=0.3, as in Huang et al. (2015). The cohesion is c= 0 Pa, and the internal friction angle is ϕ= 19.8 with a dilatancy angle ψ=0 according to Bui et al. (2008). However, the density and stiffness properties have negligible effects on the granular flow dynamics, as reported by Nguyen et al. (2020). We introduce local damping D (see Wang et al.2016b) to resolve numerical results that are compatible with the experimental results of Bui et al. (2008). We find that D=0.025 results in the most compatible dynamics. The reasons for the introduction of local damping can be found in Appendix C. Fully fixed boundary conditions (i.e. no slip) are enforced at the bottom and rollers on the sidewalls. The total simulation time is 1.0 s, considering a the time step multiplier α=0.5.

4.1.2 Model 1a: the three-dimensional granular collapse

To validate the numerical implementation under a GPU architecture, we first compare it against the well-known granular collapse experiments initially performed by Bui et al. (2008). Here, we present and compare numerical results without focusing on the performance of the GPU-based implementation. All the simulations are performed on a consumer electronics RTX 3090 GPU with double-arithmetic precision (i.e. np= 8 bytes).

The results from the numerical simulation under a three-dimensional configuration are shown in Fig. 6. A direct and visual comparison demonstrates excellent agreement between the numerical solver and the experiments of Bui et al. (2008). We observe a slightly lower run-out distance, but the overall geometry of both the failure surface and the free surface is very close to the experimental data. We also report an angle of repose of  13. This value is also consistent with the value reported by Bui et al. (2008), i.e. 14. The good agreement between the numerical results and the experimental work of Bui et al. (2008) demonstrates that the solver ep2-3De v1.0 is suitable to simulate large deformation elastoplastic problems such as granular collapses.

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Figure 6Final geometry of the granular collapse for three-dimensional configuration of our GPU-based explicit GIMPM implementation ep3De v1.0. The green region (i.e. the intact region) is defined by the L2 norm of the material point displacement up=||up||2 0.5 mm, whereas the red region (i.e. the deformed region) is defined by up=||up||2> 0.5 mm. The experiment of Bui et al. (2008) is indicated by the blue dashed line (i.e. the free surface) and the blue dotted line (i.e. the failure surface).

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The equivalent accumulated plastic strain ϵeqvp is shown in Fig. 7. We observe a coherent deformation of the granular material with a large shear zone that propagates backward from the base of the material to the top of the granular material. The mobilized granular material flows along a principal failure surface. However, the overall deformation pattern is rather coarse, i.e. fine structures or local shear bands are not yet observed, even though slight deformation heterogeneities can be observed. This coarse behaviour of shear banding is also consistent with previous studies (see Huang et al.2015; Chalk et al.2020; Zhang et al.2021). This is mainly due to the background mesh resolution used in the numerical simulation. We further investigate shear banding using a higher background mesh resolution under a plane strain configuration in Model 1b.

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Figure 7Equivalent plastic strain ϵeqvp for the final configuration of the granular collapse. The principal feature of a granular collapse can be observed, i.e. a backward propagation of plastic deformation along a principal failure surface.

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4.1.3 Model 1b: the plane strain granular collapse

We investigate granular collapse under a plane strain configuration, as this allows an increase in the number of elements, resulting in an even finer background mesh (see Table 3). For Model 1a, the numerical solution is in agreement with the experimental work of Bui et al. (2008) regarding either the free surface or the failure surface (see Fig. 8). This demonstrates that both the three-dimensional and plane strain configurations are in agreement with each other. However, we observe a lower run-out for the granular collapse under a plane strain configuration.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f08

Figure 8Final geometry of the granular collapse for the plane-strain configuration for our GPU-based explicit GIMPM implementation ep2De v1.0. The numerical solution and the experimental results are in good agreement. Some differences are more pronounced when compared with the numerical results obtained under a three-dimensional configuration.

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An interesting feature of granular collapse is the equivalent accumulated plastic strain (see Figs. 9 and 10a and b). The GPU-based implementation allows both the background mesh resolution and the total number of material points to be increased. This results in finer plastic strain localizations, as demonstrated in Fig. 10a by the various shear bands and their complex interactions during collapse. Such detailed shear bands are almost impossible to obtain at lower resolutions, which demonstrates the importance of a GPU-based implementation to overcome the hardware limitation of a CPU-based implementation, i.e. mainly longer wall-clock times.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f09

Figure 9Equivalent plastic strain ϵeqvp for the final configuration of the granular collapse. The dashed red rectangle denotes the location of the zoomed-in region in Fig. 10a. One can observe more complex plastic strain localizations compared to the numerical results obtained in Fig. 7 for a three-dimensional configuration with a coarser background mesh resolution.

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Figure 10(a) ϵeqvp for the zoomed-in area in Fig. 9. A shallow granular flow clearly appears, as suggested by the higher values of ϵeqvp. This supports evidence of shallower granular avalanches during collapses. Deeper structures, which result in lower accumulated plastic strains, probably highlight slower deformation modes along well-defined and persistent shear bands. (b) ϵeqvp for a coarser background mesh resolution, which demonstrates the influence of the mesh resolution over shear bands.

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Furthermore, Fig. 10a and b demonstrate the influence of the mesh resolution over shear banding: the finer the background mesh, the thinner the shear bands. This is significant since it shows that the dynamics of shallower granular avalanches appears to be more complex for higher resolutions.

4.2 Model 2

4.2.1 Settings for Models 2a and 2b

Here, we select a cohesive elastoplastic isotropic material (i.e. a homogeneous or heterogeneous peak cohesion field) with no dilatancy behaviour. It is modelled with a pressure-sensitive Drucker–Prager model with linear strain-softening behaviour. It is well known that the numerical solutions (as in FEM) are mesh-dependent when considering the strain-softening behaviour of the material. We did not implement techniques to address this issue, but the use of non-local plasticity (Galavi and Schweiger2010; Burghardt et al.2012) or viscoplastic formulations (Duretz et al.2019) are possible ways to address this specific task.

We have chosen an arbitrary geometry (see Fig. 11 and Table 5), which represents an idealized three-dimensional setting, to observe elastoplastic slumps (i.e. earth slumps according to the original classification proposed by Varnes1958, 1978), which are now classified as rotational slides in the recent update of the Varnes classification proposed by Hungr et al. (2014). The geometrical setting differs from the one typically used in the literature, as in Zhang et al. (2021). However, it promotes the compression of the toe, which is an expected feature we want to reproduce. The size of the physical domain lz×lx×ly is, at most, 12 m× 64 m× 1024 m for Model 2a, whereas it is 12 m× 64 m× 16 m for Model 2b.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f11

Figure 11Geometry for the earth slump. The number of elements in the y direction nel,y and the width of the problem ly are variable. This allows us to increase (or decrease) the number of both elements and material points without decreasing the mesh resolution. The parameter n controls the dimension of the domain and the number of elements in the y direction. The wall-clock time depends only on the total number of elements, nodes and material points and is not influenced by the mesh resolution.

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We assume this setting features the principal first-order characteristics of a typical rotational earth slump (Varnes1958, 1978), i.e. a complex zone of scarps (minor and major) delimiting a crown-like structure, followed by a transition (or depletion) zone in which the material flows homogeneously along internal shear zones due to severe plastic strain localizations and, finally, a compression (or accumulation) zone resulting in complex thrusting at the toe of the slump. Because of the nature of the boundary condition at the bottom of the material (i.e. free-slip), an additional horizontal sliding component is introduced within the rotational part of the displacement. This results in stronger deformations, which we want to highlight. However, the bottom boundary condition influences the shear band propagation and the overall behaviour by introducing a stronger horizontal component in the motion.

We select material properties (i.e. bulk and shear moduli K and G, friction angle ϕ, and peak and residual cohesion cpeak and cres) that result in severe deformation processes and strain localizations. The material properties are presented in Table 4. They are close to the values commonly used in the literature (Wang et al.2016b, a; Bandara et al.2016; Zhang et al.2021). To increase deformations even more, we also introduce a weak layer of thickness 0.3 ×lzm at the base of the material with a lower friction angle ϕweak. A time step multiplier α=0.5 is selected; i.e. Δtmin= 1.56 × 10−2s is obtained over the whole simulation according to the CFL condition for both Models 2a and b. As in Zhang et al. (2021), elastic loading dynamic relaxation is applied for a period of t= 8 s (i.e. Models 2a and b), and the elastoplastic behaviour is activated for an additional 7 s, resulting in a total simulation time t= 15 s (i.e. Model 2b only).

Table 4Material properties shared by both Models 2a and 2b.

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Table 5Geometrical and material properties for Models 2a and b. The correlation length vector is λ=(λx,λy,λz)=(2.5,2.5,2.5)m for both Gaussian and exponential isotropic covariance functions. The grid spacing is always constant in Models 2a and b, i.e. Δz=Δy=Δx=0.8m.

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Gaussian random fields (see Appendix B) are used to initialize the peak cohesion field cpeak, which is parametrized by an average cohesion cpeak and its standard deviation σ (see Table 5) along with the residual cohesion cres=cpeak/4. This allows us to account for heterogeneities within the material, which lead to complex and heterogeneous displacement fields. We first perform preliminary simulations with a constant cohesion field and notice a homogenous solution of the displacement field in the y direction. Using Gaussian fields allows us to mitigate this homogeneity.

Free-slip boundary conditions are applied on the sides and the bottom of the computational domain; only the normal component to the boundary is constrained, while the two others are free. Finally, and as suggested in Wang et al. (2016b) for landslide applications, we introduce local damping, i.e. D=0.1.

4.2.2 Model 2a: single GPU performances

Here, we investigate the computational performances of the solver ep2-3De v1.0 under a three-dimensional configuration on a variety of GPUs with recent architectures: Ampere, Turing and Volta. Furthermore, we restrict our performance analysis only for the elastic loading phase (i.e. 8 s of simulation) because it is more complex to determine the exact number of material points that are yielding during each computational cycle (see Fig. 4) and to infer the exact effective memory throughput.

All the numerical simulations are performed on the computational resources and GPU hardware presented in Table 1 under double-arithmetic precision (i.e. np= 8 bytes in Eq. 38). As a reference baseline, we use the performance obtained for a CPU-based single-threaded implementation of ep2-3De v1.0 on an i9-10900K CPU (e.g. latest Intel CPU chip). However, this is not representative of a highly optimized multithreaded implementation under a CPU architecture.

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Figure 12(a) Effective memory throughput MTPeff of the solver ep2-3De v1.0 for double-arithmetic precision. One can see the on-chip memory limit, as neither the RTX 2080 Ti nor V100 can resolve the same number of material points as the RTX 3090. (b) GPU on-chip memory load increases with the number of material points nmp, which demonstrates, as expected, one of the GPU's hardware limits.

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We report the effective memory throughput MTPeff of the solver ep2-3De v1.0 on various GPUs and CPUs (see Fig. 12). An increase in the effective memory throughput is observed as the number of material points increases. All GPUs reach a maximum effective throughput, but the Tesla V100 scores a maximum effective throughput of  650 GB s−1. This corresponds to 88 % of its peak throughput (for the GPU's hardware limit, see Table 1). We report a similar observation for the RTX 2080 Ti, MTPeff 320 GB s−1 corresponding to 62 % of its hardware limit. RTX 3090 and GTX 1650 reach MTPeff 405 GB s−1 and MTPeff 75 GB s−1, respectively, which correspond to 52 % and 44 % of their respective hardware limits. Finally, we report a memory throughput of at least MTPeff 5 GB s−1 for the i9-10900K CPU (10 % of its hardware limit).

The overall results suggest, as in Räss et al. (2019b), that most recent GPUs, such as the data-centre Tesla V100 (Volta), offer significant performances compared to entry-level consumer electronics GPUs, such as the GTX 1650. In terms of absolute performance, the more recent the GPU is, the higher its performance. A demonstration is given by the absolute effective throughput between the RTX 2080 Ti and the RTX 3090: the latter achieves an additional 20 % throughput compared to the former. We highly suspect the hardware itself to be the main reason for this. We further investigate the performances of the most recent data-centre GPU, i.e. the A100 (Ampere architecture), with its predecessor the V100 (Tesla architecture). The A100 reaches  1100 GB s−1, which yields a 1.6-fold performance gain with respect to the Tesla V100. When compared to the maximum effective memory throughput in Table 1, this corresponds to 97 % of the hardware limit.

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Figure 13(a) Wall-clock time reported for various computing architectures (GPUs and CPU). The differences in the maximal number of material points nmp are due to the on-chip memory limit. A significant difference in terms of wall-clock time is observed between the CPU and GPUs, even for the low-entry consumer electronic GTX 1650, i.e. a performance gain of  10×. (b) Performance gains of GPUs relative to the CPU, i.e. with 1× as a baseline. We add the CPU and the GTX 1650 wall-clock time for an easier comparison.

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Finally, we report the wall-clock time for various computing architectures (see Fig. 13a). As expected by the maximum effective memory throughput, A100 delivers the fastest solution, regardless of the number of material points nmp. The A100 GPU resolves a geometry of nmp 3.2 × 106 in less than a minute (29 s), whereas the i9-10900K CPU resolves the same problem in more than an hour (5949 s). This corresponds to a 200-fold performance gain (123-fold performance gain for the V100; see Fig. 13b compared to the CPU-based implementation of ep2-3De v1.0. The RTX 2080 Ti and the RTX 3090 reach a 60-fold and 77-fold performance gain, respectively. However, the entry-level GTX 1650 is only 10 times faster than i9-10900 K. As already shown in Fig. 12a, these performance gains are only expected when the different GPUs reach their maximum effective memory throughput. In terms of runtime, the performance gain (Fig. 13b) is in agreement with the memory throughputs reported in Fig. 12a.

4.2.3 Model 2a: multi-GPU performances

To avoid transfers of frequent material points transfers amongst the GPUs, we consider an overlap of eight elements between neighbouring meshes, i.e. nine nodes. This results in a one-dimensional GPU topology, for which both material points and meshes are distributed in the y direction of the global computational domain (see Figs. 11 and 14). Arranging GPUs in this direction allows the need to transfer material points amongst GPUs to be overcome, provided that the material point's displacement is not greater than the buffer zone, i.e. the element overlap. The evaluation of the multi-GPU implementation is based on the Model 2a, with slight modifications; i.e. the number of elements in the y direction is largely increased. The size of the physical domain lz×lx×ly is, at most, 12 m× 64 m× (64 × 2048) m.

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Figure 14Domain partition of the material points amongst eight GPUs. Combined with an overlap of eight elements in the y direction, material points can moderately move while still residing within the same GPU during the whole simulation.

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We consider two distributed computing systems for parallel GPU computation, using up to 8 Tesla V100 (Volta architecture) or 128 Geforce GTX Titan X (Maxwell architecture) GPUs. All numerical simulations are performed using a single-arithmetic precision (i.e. np= 4 bytes). This allows the maximum number of material points and mesh dimensions to be increased. In addition, our GPU implementation relies on the usage of the built-in function atomicAdd(). It does not support the double-precision floating-point format FP64 for GPUs with compute capabilities lower than 6.0, i.e. the Maxwell architecture amongst others. Note that, unlike the Tesla V100, the Geforce GTX Titan X only delivers an effective memory throughput of MTPeff 100 GB s−1. This corresponds to 38 % of its hardware limit. This was already reported by Räss et al. (2019a) and Alkhimenkov et al. (2021), and it could be attributed to its older Maxwell architecture (Gao et al.2018). This performance drop is even more severe, mainly due to the use of built-in functions like atomicAdd().

We first performed parallel simulations with a moderate number of GPUs, up to 8 Tesla V100 NVlink (32 GB). The respective wall-clock times are reported in Fig. 15. We report a wall-clock time of  110 s for nmp 108. If nmp is increased by a factor 2, 4 or 8, the wall-clock time is roughly similar to the baseline, i.e. nGPU=1. The effective memory throughput MTPeff is shown in Fig. 16 (the total sum of MTPeff across all the GPUs). Based on the memory throughput of one GPU, an estimation of a perfect weak scaling is possible. For eight GPUs, an ideal weak scaling corresponds to MTPeff= 4824 GB s−1, whereas we report MTPeff= 4538 GB s−1. This gives a parallel efficiency of  94 % and, an effective 7.5-fold speed-up. Similar observations are made for nGPU=2 and nGPU=4.

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Figure 15Wall-clock time for one, two, four and eight Tesla V100 GPUs.

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Figure 16Sum across the GPUs involved of the MTPeff. We roughly report a weak scaling between the number of GPUs and the overall effective memory throughput.

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We investigate a parallel GPU computation using up to 128 Geforce GTX Titan X GPUs. This allows even larger geometries to be addressed, as shown in Fig. 17 where the geometry of nearly nmp 9.75 × 108 is resolved in less than 8 min. For parallel computations of up to 64 GPUs, the wall-clock time evolution is smooth. For 128 GPUs, the wall-clock time is chaotic for fewer material points, whereas it stabilizes as the number of material points increases. We suspect the absence of computation–communication overlaps to be the main reason for this erratic behaviour. The communication between many GPUs requires careful synchronization between GPUs which can be hidden under computation–communication overlap (Räss et al.2019a; Alkhimenkov et al.2021). The total size of the overlap is constant, regardless of the y dimension. As the number of material points increases, the time spent on computation becomes larger compared to the time spent on exchanges between GPUs and the wall-clock time stabilizes. The effective memory throughput MTPeff is shown in Fig. 18. An ideal weak scaling corresponds to the effective memory throughput MTPeff= 12 800 GB s−1 for 128 GPUs, whereas we report only MTPeff= 11 326 GB s−1. This gives a parallel efficiency of  90 % and an effective  113-fold speed-up.

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Figure 17Wall-clock time reported for up to 128 Geforce GTX Titan X GPUs and up to nmp 9.75 × 108.

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Figure 18MTPeff sum across the GPUs involved.

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4.3 Model 2b: homogeneous and heterogeneous slumps

As a final experiment, we show the results of the ep2-3De v1.0 solver for a slump with homogeneous or heterogeneous cohesion fields. In this numerical model, we only show the displacement field at the end of the numerical simulation at t= 15 s. The interested reader is referred to Appendix D for an overview of the temporal evolution of the equivalent plastic strain ϵeqv for the slump under the three settings of the peak cohesion field. All the numerical simulations are run on a laptop equipped with GTX 1650; tGPU 30 s with the settings presented in Table 5. In the following, we present the main results for the three peak cohesion fields, and we discuss the main characteristics obtained for typical slumping mechanics.

4.3.1 Homogeneous peak cohesion field

The homogeneous solution gives preliminarily interesting results (see Fig. 19). The first-order characteristics of a slump can be observed, even though their magnitude is relatively fair compared to the real slump. The most striking feature is the development of one major shear zone, along which the material flows (i.e. depletion) towards the toe of the slump, resulting in a compression zone (i.e. thrusting and folding deformations). The crown-like structure develops linearly in the y direction and is highly localized at the surface of the slump (at x 20 m in Fig. 19). However, the material flows homogeneously in the x direction (see the vertical profile in Fig. 19), as shown by the displacement field. The lateral variation of the displacement field (along the y direction) is almost non-existent, which is mainly due to the spatial homogeneity of the peak cohesion field.

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Figure 19Displacement field obtained after t= 15 s for a homogeneous peak cohesion field. One can see an overall homogenous displacement field with some of the first-order characteristics of a slump, i.e. a rotational displacement with a compression zone at the toe, a transition zone delimited by one principal shear zone and a major scarp at the top of the material.

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4.3.2 Isotropic Gaussian covariance

Considering heterogeneities with a Gaussian covariance function for the cohesion field, the displacement field starts to resolve a differential behaviour (see Fig. 20). Higher and/or weaker values of the peak cohesion field yield lower and/or greater displacements. This is obvious, especially in the transition zone where this differential is observable. In addition, the compression zone also starts to resolve spatial variations due to weaker and stronger cohesion values.

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Figure 20Displacement field obtained after t= 15 s for a heterogeneous peak cohesion field with a Gaussian covariance function.

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A striking difference is the shear zone itself (see Fig. D2): the shear zone exhibits a more complex spatial pattern, whereas only one major shear zone is observed in Fig. D2. Retrogressive shear banding appears during the time evolution of the slump, which suggests the development of a secondary shear zone within the slump. Moreover, the crown-like structure is now curved and not linear in the y direction. Its spatial extent is more important and is not as localized as in the homogeneous case. Nevertheless, a more complex arrangement of major and minor scarps within the crown-like structure has not yet been observed. Such a structure is more evident if one observes the accumulated equivalent plastic strain ϵeqvp in Fig. D2 in Appendix D.

The high magnitude of the displacement field in the areas x[20;40] and y 8 m is due to a weaker zone in the peak cohesion field (see Fig. D2). This shows a strong influence of the heterogeneous peak cohesion field on the final displacement field. A lower shear strength of the material yields faster strain-softening behaviour, promoting a faster response of shear banding.

4.3.3 Isotropic exponential covariance

Shear banding activities become even more complex when an exponential covariance function is used, relative to Fig. 19 and even to Fig. 20 to some extent. The spatial distribution of the peak cohesion (see Fig. D3) resolves finer heterogeneities with a smaller length scale compared to when Gaussian covariance is used. Principal differences are observed at the top and toe of the slump, where the crown-like structure turns into a complex zone made of minor and major scarps (see Fig. 21). The displacement field becomes highly heterogeneous, particularly at the toe and the top of the slump. However, it is also more homogeneous when compared with Fig. 20, particularly in x[25;35]. The difference is evident between Figs. 22 and 20 at this particular location.

https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f21

Figure 21Heterogeneous cohesion field with an exponential covariance function: time evolution of the equivalent plastic strain ϵeqvp. Similar to Fig. D2, heterogeneous behaviour is observed. However, the exponential covariance function results in an even more complex pattern of strain localization, i.e. minor and major scarps develop at the top. The crown-like structure of the slump becomes even more heterogeneous.

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Figure 22Displacement field obtained after t= 15 s for a heterogeneous peak cohesion field with an exponential covariance function.

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The difference between the Gaussian and exponential covariance of the peak cohesion suggests the following. Heterogeneous displacement fields could be influenced by larger and/or coarser fluctuations of the shear strength within the material. By extrapolation, this could imply that the magnitude of the heterogeneity might be related to the fluctuation scales of the peak cohesion field. Locally rather homogeneous fluctuations of the peak cohesion (i.e. Gaussian covariance) seem to promote an increasingly heterogeneous displacement field at the surface. The characteristic length scale of spatial fluctuations could have important implications for highly heterogeneous displacements within landslides. The same assumption could hold for understanding the more complex crown-like structure of slumps (see Fig. D3)

5 Discussion

5.1 GIMPM suitability

We investigated granular collapses in both three-dimensional and plane strain configurations. Our numerical results demonstrated the suitability of GIMPM to correctly reproduce experimental granular collapses. They also demonstrated that the results did not significantly differ between these two spatial configurations and that both approaches give similar numerical solutions.

5.2 Collapse limitation

For Model 1a, the principal hardware limit is the on-chip memory of the GPU. Even though RTX3090 is supported by 24 GB DDR4, it is physically impossible to achieve the resolution used for plane strain granular collapse. This would require more than 24 GB of on-chip memory. Model 1b demonstrated the importance of the background mesh resolution over strain localization. Using a higher numerical resolution (i.e. finer background mesh) allows full-resolution plastic strain localization. Similarly, future additional development efforts towards MPI implementation could resolve highly detailed three-dimensional granular collapse simulations in the future. This will definitely benefit future studies on complex strain localization.

The wall-clock time for Model 1b is tGPU= 1470.5 s (25 min), and the number of iterations per second is 85.5 iterations s−1 for nmp= 819 200. As a preliminary example, the same numerical model was performed by Wyser et al. (2020a), who reported 19.98 iterations s−1 for nmp= 12 800. Proportionally, this corresponds to a performance gain factor of 275 for the GPU-based implementation (ep2-3De v1.0) over the MATLAB-based implementation (fMPMM-solver v1.1) (Wyser et al.2020a).

5.3 Performance

The performance analysis we carried out in Model 2a demonstrated that even though the algorithm heavily relies on atomic operations to accumulate material point quantities on the nodes, the effective memory throughput reaches 88 % at most (for Tesla V100). We expected a much lower throughput due to the use of these atomic operations, since they are likely known to undermine the computational performances of an implementation under previous GPU architectures (e.g. Kepler) (Dong et al.2015a; Dong and Grabe2018; Gao et al.2018). Our actual understanding (at least for a GPU-based implementation of GIMPM) is that the latest GPU architecture (Ampere and Turing) is now efficient when dealing with atomic operations and that the need to use a complex data layout for scattering is not as important as before. Furthermore, we identify the memory throughput as the main bottleneck: an additional 12 % performance improvement on the V100 before reaching the hardware limit of the memory bandwidth. The A100 shows that the solver reaches the hardware limit with an effective memory throughput which is very close (i.e. 97 %) to the actual maximum memory throughput. Similarly, the true limiting factor of the single GPU implementation is the hardware limit of the GPU on-chip memory.

The multi-GPU implementation resolves the on-chip memory limitation problem. Our multi-GPU implementation is particularly well-suited to resolve highly detailed three-dimensional shear-banding. We also reported decent wall-clock times (less than 8 min) for simulations with nearly a billion material points. However, investigating high-resolution three-dimensional granular collapses is not possible under the assumptions made, because of small displacement required in the y direction. This is incompatible with three-dimensional granular collapses. Hence, this motivates future deeper investigations toward a more versatile multi-GPU implementation. In addition, we report a slight drop of the parallel efficiency, as the number of GPUs increases. Future works should be directed toward a parallel strategy that hides communication latency, as proposed in Räss et al. (2019a), Räss et al. (2020) and Alkhimenkov et al. (2021). This will allow us to achieve an optimal parallel efficiency of 95 %–98 % of the weak scaling tests involving up to 128 GPUs.

5.4 Slumping mechanics

We show the application of the GIMPM solver ep2-3De v1.0 for slumping mechanics. We have presented various slump results and demonstrated the significant influence of heterogeneities within the peak cohesion field over the displacement field or the equivalent plastic strain. However, we have arbitrarily selected values that resulted in severe deformations of the material, which we wanted to highlight to demonstrate the potential of the solver. Further efforts should now be oriented towards numerical models that are closer to real and well-documented cases, such as in Tran and Sołowski (2019) and Ying et al. (2021). Despite the simplifications we made, we have reported three-dimensional simulations that resolve all the first-order characteristics of slumps, including complex major and minor scarps, different shear zones of various activities, and a complex arrangement within the compression zone. The use of a three-dimensional GIMPM implementation under a GPU architecture will highly benefit future studies in the field, allowing faster and more detailed numerical simulations of heterogeneous and complex strain localization problems.

5.5 Local damping coefficient

Due to our explicit formulation, a damping relaxation term should be introduced to mitigate dynamic wave propagations (Wang et al.2016c). In this work, we selected damping values that were either commonly accepted (e.g. D=0.1 for slumps) or that were better at resolving experimental results (e.g. D=0.025 for granular collapses). Future investigations should specifically address the influence of damping terms on the material's behaviour.

5.6 Code portability

Our numerical models showed the efficient computing capabilities of modern GPUs under the latest Nvidia GPU architectures. An important concern is the code portability. CUDA C is only applicable for Nvidia's GPUs and is not yet compatible with other corporations' GPUs, such as AMD (ATI Technologies). As such, an extension of the ep2-3De v1.0 solver towards an OpenCL-based implementation would ensure better code portability in the future.

6 Conclusions

We developed ep2-3De v1.0, an explicit GPU-based implementation of the generalized interpolation material point method that exploits the capabilities of the most recent GPU architectures (Ampere, Turing and Volta). We achieved fast execution times on a single GPU with a scattering approach that relies on extensive usage of atomic operations. We report, at most, an effective memory bandwidth of 88 % relative to the maximal hardware capabilities of the GPUs. We achieve, at most, a 200-fold performance gain on a single GPU compared to a single-threaded CPU-based implementation of the solver. On entry-level customer electronics GPUs, we report a  10-fold performance gain. Our multi-GPU implementation permits geometries with almost a billion material points to be resolved and demonstrates fast execution times. We achieve a parallel efficiency of  94 % on weak scaling tests for 8 GPUs and  90 % for 128 GPUs. We also report that the memory bandwidth is the main limiting performance factor. We validated our solver against the well-known experimental results of the granular collapse problem in a three-dimensional configuration. We show applications of the solver to model slumping mechanics in three-dimensional configurations considering different material heterogeneities.

Appendix A: GIMPM basis functions and derivatives

One of the most important problems of any sMPM formulation is the cell-crossing instability (or error; see Steffen et al.2008; Wilson et al.2021). As material points move through the mesh, they cross element boundaries. The discontinuous gradient due to the C0 continuity of the basis functions results in spurious oscillations of the stress field and internal forces (González Acosta et al.2020, 2019; Bardenhagen and Kober2004) when material points cross element boundaries.

To solve for this instability, Bardenhagen and Kober (2004) introduced the generalized interpolation material point method (GIMPM). Whereas the material point is treated as a point in sMPM, Bardenhagen and Kober (2004) assigned a spatial extent or a domain to the material point. Alternative basis functions are constructed, i.e. to consider the material point domain, as follows:

(A1) ϕ n p ϕ n ( x p ) = 1 v p Ω p Ω χ p ( x ) N n ( x ) d Ω ,

where vp is the material point volume, Ωp denotes the material point domain, χp(x) is the particle characteristic function, Nn(x) is the basis function (or shape function) for the mapping between the material point p and its associated nodes n, and x=xp-xn are the local coordinates between node n and material point p.

The particle characteristic function must satisfy the partition of unity property, i.e. pχp(x)=1 (Bardenhagen and Kober2004). The simplest particle characteristic function is given by the hat function, i.e.

(A2) χ p ( x ) = 1 , if x Ω p , 0 otherwise .

The GIMPM basis functions and derivatives are constructed analytically (Coombs et al.2020; Charlton et al.2017) in one dimension from a convolution of the standard finite-element basis functions and the material point characteristic function (Steffen et al.2008), i.e.

(A3) ϕ n ( x p ) = 1 - 4 x 2 + l p 2 / ( 4 h l p )  if  | x | < l p / 2 1 - | x | / h  if  l p / 2 | x | < h - l p / 2 h + l p / 2 - | x | 2 / ( 2 h l p )  if  h - l p / 2 | x | < h + l p / 2 0  otherwise  ,

where lp is the length of the material point domain, h is the mesh resolution, and x=xp-xn, where xp is the coordinate of a material point and xn is the coordinate of its associated node n. The two-dimensional basis function of a node n with its material point p is constructed as

(A4) ϕ n p ϕ n ( x p ) = ϕ n ( x p ) ϕ n ( y p ) ,

for which the gradient is defined as

(A5) ϕ n p ϕ n ( x p ) = ( x ϕ n ( x p ) ϕ n ( y p ) , ϕ n ( x p ) y ϕ n ( y p ) ) .
Appendix B: Gaussian random cohesion fields

In earth sciences, random fields (Christakos1992) are numerically generated predictions of a geophysical property (i.e. rock- or soil-related properties) with probabilistic spatial variability. These predictions are based on (i) an assumed probability density function, i.e. characterized by a mean value μ with a standard deviation σ, and (ii) an assumed spatial correlation function, characterized by fluctuation scales in a vector format, i.e. λ=(λx,λy,λz). In regard to numerical modelling, the principal requirement is that both small and large scales are simultaneously resolved over the computational mesh to ensure physically meaningful solutions.

Recently, Räss et al. (2019b) presented an efficient implementation based on a spectral representation of Gaussian random fields for geophysical applications using either Gaussian or exponential covariance functions. The numerical codes, named GRFS, were made available by Räss et al. (2019b) in both native MATLAB and CUDA C languages2. However, a sufficiently large number of harmonics should be used to obtain convergent Gaussian random fields, as stated in Räss et al. (2019b).

Similar to the random material point method (RMPM; see Wang et al.2016a; Liu et al.2019; Remmerswaal et al.2021) initially proposed by Fenton and Vanmarcke (1990) to generate RFs for a finite-element mesh (RFEM), we combined this approach with the codes proposed by Räss et al. (2019b) to generate an isotropic peak cohesion field to demonstrate its influence on the mechanical behaviour.

Appendix C: Volumetric locking and damping corrections

In Huang et al. (2015), no volumetric locking mitigation strategy was introduced, even though low-order elements were used. This should promote volumetric locking and an overall stiffer response of the granular material. In addition, Huang et al. (2015) used the standard (or original) material point method (instead of the generalized interpolation material point method), which is well known to introduce spurious oscillations of internal forces (González Acosta et al.2020).

When implementing the proposed volumetric locking mitigation strategy, we observed (a) larger deformations of the granular material with a stronger vertical compaction (i.e. stronger vertical displacement) and (b) slightly longer run-out distances when compared to the experimental data. The softer mechanical response of the granular material had to be compensated for somehow, which can be achieved by the introduction of a small local damping parameter.

We reproduced the numerical setting used in Huang et al. (2015) with the same mesh resolution, i.e. Δxy= 2.5 mm, and a similar number of material points nmp= 28 800 with an initial number of material points per initially filled element npe=9. The material parameters used for this preliminary investigation are presented in Sect. 4.1.1.

Figure C1a and b show the major differences between either a locking-free or a locking-prone solution and the experimental results. As mentioned before, a slightly longer run-out distance is obtained for the locking-free solution. As a result, the numerical prediction given by the locking-free solution of the free surface is underestimated. However, the most noticeable difference is the failure surface. Whereas the failure surface predicted by the locking-prone solution fits with the experiment of Bui et al. (2008), it diverges for a locking-free solution. In particular, the onset of the failure surface at the top of the material is underestimated by the locking-free solution compared to the experimental results. This is due to the softer response of the granular material when volumetric locking is mitigated, which promotes greater vertical compaction and a stronger run-out distance at the same time.

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Figure C1(a) Numerical solution without any volumetric locking strategy and (b) numerical solution with the proposed volumetric locking strategy. For both cases, no damping is introduced.

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Even though the introduction of local damping better resolves the experimental results, one can argue that the locking-free solution without the introduction of local damping still agrees with the experiment of Bui et al. (2008). The overall response of the numerical granular collapse is still very close to the actual physical experiment, and the differences between the numerical and experimental results can still be considered acceptable.

We further present additional three-dimensional results for Model 2b for a homogeneous cohesion field (see Figs. C2 and C3). Three-dimensional simulations of cohesive material better illustrate the influence of volumetric locking. Figure C3 demonstrates that a significantly smoother pressure field is resolved with the proposed method.

In addition, the pressure field is certainly smoothed, but it does not significantly differ from the original pressure field (in locations where locking is minimum). Volumetric locking is particularly highlighted within shear bands due to isochoric plastic flows, resulting in significant stress oscillations.

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Figure C2Non-smooth pressure field due to volumetric locking. The typical check-board pattern of volumetric locking can be observed where the material has yielded, i.e. the shear band.

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Figure C3Smoother pressure field when volumetric locking is mitigated with the proposed solution.

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Appendix D: Heterogeneities for the peak cohesion field
https://gmd.copernicus.org/articles/14/7749/2021/gmd-14-7749-2021-f26

Figure D1Homogeneous cohesion field: time evolution of the equivalent plastic strain ϵeqvp. Its evolution is rather homogeneous, and the overall plastic behaviour is free of any heterogeneities. Some of the first-order characteristics are observed, i.e. a principal shear zone and a compression zone at the toe of the slump.

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Figure D2Heterogeneous cohesion field with a Gaussian covariance function: time evolution of the equivalent plastic strain ϵeqvp. Unlike Fig. D1, heterogeneous behaviour is observed, i.e. the appearance of a second shear zone highlights a more complex deformation pattern. Moreover, a crown-like structure starts to develop at the top of the material, where an initial weak zone is located.

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Figure D3Heterogeneous cohesion field with an exponential covariance function: time evolution of the equivalent plastic strain ϵeqvp. Similar to Fig. D2, heterogeneous behaviour is observed. However, the exponential covariance function results in an even more complex pattern of strain localization; i.e. minor and major scarps develop at the top. The crown-like structure of the slump becomes even more heterogeneous.

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Code availability

The solver ep2-3De v1.0 developed in this study is licensed under the GPLv3 free software licence. The solver ep2-3De v1.0 archive (v1.0) is available from a permanent DOI repository (Zenodo) at https://doi.org/10.5281/zenodo.5600373 (Wyser et al.2021) (the latest version of the code is available for download from GitHub at https://github.com/ewyser/ep2-3De, last access: 26 October 2021).

Data availability

The data used can be found in Bui et al. (2008).

Author contributions

EW and YA wrote the original manuscript and developed the first version the ep2-3De v1.0 solver. MJ and YYP supervised the early stages of the study and provided guidance. All authors have reviewed and approved the final version of the paper.

Competing interests

The contact author has declared that neither they nor their co-authors have any competing interests.

Disclaimer

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Acknowledgements

Yury Alkhimenkov gratefully acknowledges support from the Swiss National Science Foundation (grant no. 172691). Yury Alkhimenkov and Yury Y. Podladchikov gratefully acknowledge support from the Russian Ministry of Science and Higher Education (project no. 075-15-2019-1890). We gratefully acknowledge Thomas Poulet, Quoc Anh Tran and José León González Acosta for constructive suggestions that helped us to improve the quality of the paper.

Financial support

This research has been supported by the Swiss National Science Foundation (grant no. 172691) and the Russian Ministry of Science and Higher Education (project no. 075-15-2019-1890).

Review statement

This paper was edited by Thomas Poulet and reviewed by José León González Acosta and Quoc Anh Tran.

References

Alejano, L. R. and Bobet, A.: Drucker–Prager Criterion, Rock Mech. Rock Eng., 45, 995–999, https://doi.org/10.1007/s00603-012-0278-22012. a

Alkhimenkov, Y., Räss, L., Khakimova, L., Quintal, B., and Podladchikov, Y.: Resolving wave propagation in anisotropic poroelastic media using graphical processing units (GPUs), J. Geophys. Res.-Sol. Ea., 126, e2020JB021175, https://doi.org/10.1029/2020JB021175, 2021. a, b, c, d, e

Anderson, C. E.: An overview of the theory of hydrocodes, Int. J. Impact Eng., 5, 33–59, https://doi.org/10.1016/0734-743X(87)90029-7, 1987. a

Bandara, S. and Soga, K.: Coupling of soil deformation and pore fluid flow using material point method, Comput. Geotech., 63, 199–214, https://doi.org/10.1016/j.compgeo.2014.09.009, 2015. a

Bandara, S., Ferrari, A., and Laloui, L.: Modelling landslides in unsaturated slopes subjected to rainfall infiltration using material point method, Int. J. Numer. Anal. Met., 40, 1358–1380, https://doi.org/10.1002/nag.2499, 2016. a, b

Bardenhagen, S. G. and Kober, E. M.: The Generalized Interpolation Material Point Method, CMES-Comp. Model. Eng., 5, 477–496, https://doi.org/10.3970/cmes.2004.005.477, 2004. a, b, c, d, e, f

Baumgarten, A. S. and Kamrin, K.: A general fluid–sediment mixture model and constitutive theory validated in many flow regimes, J. Fluid Mech., 861, 721–764, https://doi.org/10.1017/jfm.2018.914, 2019. a

Bisht, V., Salgado, R., and Prezzi, M.: Simulating penetration problems in incompressible materials using the material point method, Comput. Geotech., 133, 103593, https://doi.org/10.1016/j.compgeo.2020.103593, 2021. a

Bui, H. H., Fukagawa, R., Sako, K., and Ohno, S.: Lagrangian meshfree particles method (SPH) for large deformation and failure flows of geomaterial using elastic–plastic soil constitutive model, Int. J. Numer. Anal. Met., 32, 1537–1570, https://doi.org/10.1002/nag.688, 2008. a, b, c, d, e, f, g, h, i, j, k, l, m, n

Burghardt, J., Brannon, R., and Guilkey, J.: A nonlocal plasticity formulation for the material point method, Comput. Method. Appl. M., 225-228, 55–64, https://doi.org/10.1016/j.cma.2012.03.007, 2012. a

Buzzi, O., Pedroso, D. M., and Giacomini, A.: Caveats on the Implementation of the Generalized Material Point Method, CMES-Comp. Model. Eng., 31, 85–106, https://doi.org/10.3970/cmes.2008.031.085, 2008. a

Chalk, C. M., Pastor, M., Peakall, J., Borman, D. J., Sleigh, P. A., Murphy, W., and Fuentes, R.: Stress-Particle Smoothed Particle Hydrodynamics: An application to the failure and post-failure behaviour of slopes, Comput. Method. Appl. M., 366, 113034, https://doi.org/10.1016/j.cma.2020.113034, 2020. a

Charlton, T. J., Coombs, W. M., and Augarde, C. E.: iGIMP: An implicit generalised interpolation material point method for large deformations, Comput. Struct., 190, 108–125, https://doi.org/10.1016/j.compstruc.2017.05.004, 2017. a, b

Christakos, G.: 2 – The Spatial Random Field Model, in: Random Field Models in Earth Sciences, edited by: Christakos, G., Academic Press, Boston, https://doi.org/10.1016/B978-0-12-174230-0.50007-X, pp. 21–106, 1992. a

Coombs, W. M., Charlton, T. J., Cortis, M., and Augarde, C. E.: Overcoming volumetric locking in material point methods, Comput. Method. Appl. M., 333, 1–21, https://doi.org/10.1016/j.cma.2018.01.010, 2018. a

Coombs, W. M., Augarde, C. E., Brennan, A. J., Brown, M. J., Charlton, T. J., Knappett, J. A., Motlagh, Y. G., and Wang, L.: On Lagrangian mechanics and the implicit material point method for large deformation elasto-plasticity, Comput. Method. Appl. M., 358, 112622, https://doi.org/10.1016/j.cma.2019.112622, 2020. a, b, c, d

Cuomo, S., Ghasemi, P., Martinelli, M., and Calvello, M.: Simulation of Liquefaction and Retrogressive Slope Failure in Loose Coarse-Grained Material, Int. J. Geomech., 19, 04019116, https://doi.org/10.1061/(ASCE)GM.1943-5622.0001500, 2019. a

De Borst, R., Crisfield, M. A., Remmers, J. J. C., and Verhoosel, C. V.: Nonlinear finite element analysis of solids and structures, John Wiley & Sons, Chichester, UK, 2012. a

de Souza Neto, E. A., Peric, D., and Owen, D. R. J.: Computational methods for plasticity: theory and applications, John Wiley & Sons, Chichester, UK, 2011. a

Dong, Y. and Grabe, J.: Large scale parallelisation of the material point method with multiple GPUs, Comput. Geotech., 101, 149–158, https://doi.org/10.1016/j.compgeo.2018.04.001, 2018. a, b, c, d

Dong, Y., Wang, D., and Randolph, M. F.: A GPU parallel computing strategy for the material point method, Comput. Geotech., 66, 31–38, https://doi.org/10.1016/j.compgeo.2015.01.009, 2015a. a, b, c

Dong, Y., Wang, D., and Randolph, M. F.: A GPU parallel computing strategy for the material point method, Comput. Geotech., 66, 31–38, https://doi.org/10.1016/j.compgeo.2015.01.009, 2015b. a

Dunatunga, S. and Kamrin, K.: Continuum modelling and simulation of granular flows through their many phases, J. Fluid Mech., 779, 483–513, https://doi.org/10.1017/jfm.2015.383, 2015. a

Duretz, T., de Borst, R., and Le Pourhiet, L.: Finite Thickness of Shear Bands in Frictional Viscoplasticity and Implications for Lithosphere Dynamics, Geochem. Geophy. Geosy., 20, 5598–5616, https://doi.org/10.1029/2019GC008531, 2019. a

Fenton, G. A. and Vanmarcke, E. H.: Simulation of Random Fields via Local Average Subdivision, J. Eng. Mech., 116, 1733–1749, https://doi.org/10.1061/(ASCE)0733-9399(1990)116:8(1733), 1990. a

Galavi, V. and Schweiger, H. F.: Nonlocal Multilaminate Model for Strain Softening Analysis, Int. J. Geomech., 10, 30–44, https://doi.org/10.1061/(ASCE)1532-3641(2010)10:1(30), 2010. a

Gao, M., Wang, X., Wu, K., Pradhana, A., Sifakis, E., Yuksel, C., and Jiang, C.: GPU Optimization of Material Point Methods, ACM T. Graphic., 37, 254, https://doi.org/10.1145/3272127.3275044, 2018. a, b, c, d, e

Gaume, J., Gast, T., Teran, J., van Herwijnen, A., and Jiang, C.: Dynamic anticrack propagation in snow, Nat. Commun., 9, 3047, https://doi.org/10.1038/s41467-018-05181-w, 2018. a

González Acosta, J. L., Zheng, X., Vardon, P. J., Hicks, M. A., and Pisano, F.: On stress oscillation in MPM simulations involving one or two phases, in: Proceedings of the Second International Conference on the Material Point Method for Modelling Soil-Water-Structure Interaction, 8–10 January 2019, Cambridge, UK, 135–139, 2019. a, b

González Acosta, J. L., Vardon, P. J., Remmerswaal, G., and Hicks, M. A.: An investigation of stress inaccuracies and proposed solution in the material point method, Comput. Mech., 65, 555–581, https://doi.org/10.1007/s00466-019-01783-3, 2020. a, b, c

González Acosta, J. L., Vardon, P. J., and Hicks, M. A.: Development of an implicit contact technique for the material point method, Comput. Geotech., 130, 103859, https://doi.org/10.1016/j.compgeo.2020.103859, 2021. a

Hu, Y., Li, T.-M., Anderson, L., Ragan-Kelley, J., and Durand, F.: Taichi: A Language for High-Performance Computation on Spatially Sparse Data Structures, ACM T. Graphic., 38, 201, https://doi.org/10.1145/3355089.3356506, 2019. a

Huang, P., Li, S.-L., Guo, H., and Hao, Z.-M.: Large deformation failure analysis of the soil slope based on the material point method, Computat. Geosci., 19, 951–963, https://doi.org/10.1007/s10596-015-9512-9, 2015. a, b, c, d, e, f, g, h, i, j

Hughes, T. J. R.: Generalization of selective integration procedures to anisotropic and nonlinear media, Int. J. Numer. Meth. Eng., 15, 1413–1418, https://doi.org/10.1002/nme.1620150914, 1980. a

Hungr, O., Leroueil, S., and Picarelli, L.: The Varnes classification of landslide types, an update, Landslides, 11, 167–194, https://doi.org/10.1007/s10346-013-0436-y, 2014. a

Jassim, I., Stolle, D., and Vermeer, P.: Two-phase dynamic analysis by material point method, Int. J. Numer. Anal. Met., 37, 2502–2522, https://doi.org/10.1002/nag.2146, 2013. a

Jiang, H. and Xie, Y.: A note on the Mohr–Coulomb and Drucker–Prager strength criteria, Mech. Res. Commun., 38, 309–314, https://doi.org/10.1016/j.mechrescom.2011.04.001, 2011. a

Krabbenhoft, K., Karim, M. R., Lyamin, A. V., and Sloan, S. W.: Associated computational plasticity schemes for nonassociated frictional materials, Int. J. Numer. Meth. Eng., 90, 1089–1117, https://doi.org/10.1002/nme.3358, 2012. a

Lei, X., He, S., and Wu, L.: Stabilized generalized interpolation material point method for coupled hydro-mechanical problems, Computational Particle Mechanics, 8, 701–720, https://doi.org/10.1007/s40571-020-00365-y, 2020. a, b

Liu, X., Wang, Y., and Li, D.-Q.: Investigation of slope failure mode evolution during large deformation in spatially variable soils by random limit equilibrium and material point methods, Comput. Geotech., 111, 301–312, https://doi.org/10.1016/j.compgeo.2019.03.022, 2019. a

Liu, X., Wang, Y., and Li, D.-Q.: Numerical simulation of the 1995 rainfall-induced Fei Tsui Road landslide in Hong Kong: new insights from hydro-mechanically coupled material point method, Landslides, 17, 2755–2775, https://doi.org/10.1007/s10346-020-01442-2, 2020. a

Mast, C. M., Mackenzie-Helnwein, P., Arduino, P., Miller, G. R., and Shin, W.: Mitigating kinematic locking in the material point method, J. Comput. Phys., 231, 5351–5373, https://doi.org/10.1016/j.jcp.2012.04.032, 2012. a

Nairn, J. A.: Material Point Method Calculations with Explicit Cracks, CMES-Comp. Model. Eng., 4, 649–664, https://doi.org/10.3970/cmes.2003.004.649, 2003. a

Nguyen, N. H. T., Bui, H. H., and Nguyen, G. D.: Effects of material properties on the mobility of granular flow, Granul. Matter, 22, 59, https://doi.org/10.1007/s10035-020-01024-y, 2020. a, b

Nvidia: CUDA Programming Guide Version 1.0, available at: http://developer.download.nvidia.com/compute/cuda/1.0/NVIDIA_CUDA_Programming_Guide_1.0.pdf (last access: 25 May 2021), 2007. a

Omlin, S.: Development of massively parallel near peak performance solvers for three-dimensional geodynamic modelling, PhD thesis, University of Lausanne, Lausanne, Switzerland, 2017. a, b

Omlin, S., Räss, L., and Podladchikov, Y. Y.: Simulation of three-dimensional viscoelastic deformation coupled to porous fluid flow, Tectonophysics, 746, 695–701, https://doi.org/10.1016/j.tecto.2017.08.012, 2018. a

Räss, L., Simon, N. S. C., and Podladchikov, Y. Y.: Spontaneous formation of fluid escape pipes from subsurface reservoirs, Sci. Rep., 8, 11116, https://doi.org/10.1038/s41598-018-29485-5, 2018. a

Räss, L., Duretz, T., and Podladchikov, Y. Y.: Resolving hydromechanical coupling in two and three dimensions: spontaneous channelling of porous fluids owing to decompaction weakening, Geophys. J. Int., 218, 1591–1616, https://doi.org/10.1093/gji/ggz239, 2019a. a, b, c, d, e

Räss, L., Kolyukhin, D., and Minakov, A.: Efficient parallel random field generator for large 3-D geophysical problems, Comput. Geosci., 131, 158–169, https://doi.org/10.1016/j.cageo.2019.06.007, 2019b. a, b, c, d, e, f

Räss, L., Licul, A., Herman, F., Podladchikov, Y. Y., and Suckale, J.: Modelling thermomechanical ice deformation using an implicit pseudo-transient method (FastICE v1.0) based on graphical processing units (GPUs), Geosci. Model Dev., 13, 955–976, https://doi.org/10.5194/gmd-13-955-2020, 2020. a

Remmerswaal, G., Vardon, P. J., and Hicks, M. A.: Evaluating residual dyke resistance using the Random Material Point Method, Comput. Geotech., 133, 104034, https://doi.org/10.1016/j.compgeo.2021.104034, 2021. a

Steffen, M., Kirby, R. M., and Berzins, M.: Analysis and reduction of quadrature errors in the material point method (MPM), Int. J. Numer. Meth. Eng., 76, 922–948, https://doi.org/10.1002/nme.2360, 2008. a, b

Sulsky, D., Chen, Z., and Schreyer, H. L.: A particle method for history-dependent materials, Comput. Method. Appl. M., 118, 179–196, https://doi.org/10.1016/0045-7825(94)90112-0, 1994. a, b

Tran, Q.-A. and Sołowski, W.: Generalized Interpolation Material Point Method modelling of large deformation problems including strain-rate effects – Application to penetration and progressive failure problems, Comput. Geotech., 106, 249–265, https://doi.org/10.1016/j.compgeo.2018.10.020, 2019. a, b, c

Varnes, D. J.: Landslide types and processes, Landslides and Engineering Practice, 24, 20–47, 1958. a, b, c

Varnes, D. J.: Slope movement types and processes, in: Special Report 176: Landslides: Analysis and Control, edited by: Schuster, R. L. and Krizek, R. J., Transportation and Road Research Board, National Academy of Science, Washington, DC, pp. 11–33, 1978. a, b, c

Wang, B., Hicks, M. A., and Vardon, P. J.: Slope failure analysis using the random material point method, Geotech. Lett., 6, 113–118, https://doi.org/10.1680/jgele.16.00019, 2016a. a, b

Wang, B., Vardon, P. J., and Hicks, M. A.: Investigation of retrogressive and progressive slope failure mechanisms using the material point method, Comput. Geotech., 78, 88–98, https://doi.org/10.1016/j.compgeo.2016.04.016, 2016b. a, b, c, d

Wang, B., Vardon, P. J., Hicks, M. A., and Chen, Z.: Development of an implicit material point method for geotechnical applications, Comput. Geotech., 71, 159–167, https://doi.org/10.1016/j.compgeo.2015.08.008, 2016c. a, b

Wang, L., Coombs, W. M., Augarde, C. E., Cortis, M., Charlton, T. J., Brown, M. J., Knappett, J., Brennan, A., Davidson, C., Richards, D., and Blake, A.: On the use of domain-based material point methods for problems involving large distortion, Comput. Method. Appl. M., 355, 1003–1025, https://doi.org/10.1016/j.cma.2019.07.011, 2019. a

Wang, X., Qiu, Y., Slattery, S. R., Fang, Y., Li, M., Zhu, S.-C., Zhu, Y., Tang, M., Manocha, D., and Jiang, C.: A Massively Parallel and Scalable Multi-GPU Material Point Method, ACM T. Graphic., 39, 30, https://doi.org/10.1145/3386569.3392442, 2020. a, b, c, d, e, f

Wilson, P., Wüchner, R., and Fernando, D.: Distillation of the material point method cell crossing error leading to a novel quadrature-based C0 remedy, Int. J. Numer. Meth. Eng., 122, 1513–1537, https://doi.org/10.1002/nme.6588, 2021. a

Wyser, E., Alkhimenkov, Y., Jaboyedoff, M., and Podladchikov, Y. Y.: A fast and efficient MATLAB-based MPM solver: fMPMM-solver v1.1, Geosci. Model Dev., 13, 6265–6284, https://doi.org/10.5194/gmd-13-6265-2020, 2020a. a, b, c, d, e

Wyser, E., Alkhimenkov, Y., Jaboyedoff, M., and Podladchikov, Y. Y.: fMPMM-solver, Zenodo [code], https://doi.org/10.5281/zenodo.4068585, 2020b.  a

Wyser, E., Alkhimenkov, Y., Jaboyedoff, M., and Podladchikov, Y. Y.: ep2-3De v1.0, Zenodo [code], https://doi.org/10.5281/zenodo.5600373, 2021. a, b

Ying, C., Zhang, K., Wang, Z.-N., Siddiqua, S., Makeen, G. M. H., and Wang, L.: Analysis of the run-out processes of the Xinlu Village landslide using the generalized interpolation material point method, Landslides, 18, 1519–1529, https://doi.org/10.1007/s10346-020-01581-6, 2021. a

Zhang, F., Zhang, X., Sze, K. Y., Lian, Y., and Liu, Y.: Incompressible material point method for free surface flow, J. Comput. Phys., 330, 92–110, https://doi.org/10.1016/j.jcp.2016.10.064, 2017. a

Zhang, W., hao Zhong, Z., Peng, C., hai Yuan, W., and Wu, W.: GPU-accelerated smoothed particle finite element method for large deformation analysis in geomechanics, Comput. Geotech., 129, 103856, https://doi.org/10.1016/j.compgeo.2020.103856, 2021. a, b, c, d, e

Zuo, Z., Gong, S., and Xie, G.: Numerical simulation of granular mixing in a rotary drum using a generalized interpolation material point method, Asia-Pac. J. Chem. Eng., 15, e2426, https://doi.org/10.1002/apj.2426, 2020. a

1

The routines of the ep2-3De v1.0 solver are available for download from GitHub at https://github.com/ewyser/ep2-3De (last access: 26 October 2021). The routines archive (v1.0) (Wyser et al.2021) is available from a permanent DOI repository (Zenodo) at https://doi.org/10.5281/zenodo.5600373.

2

The GRFS routines are available at https://bitbucket.org/lraess/grfs/src/master/ (last access: 25 February 2021).

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Short summary
We propose an implementation of the material point method using graphical processing units (GPUs) to solve elastoplastic problems in three-dimensional configurations, such as the granular collapse or the slumping mechanics, i.e., landslide. The computational power of GPUs promotes fast code executions, compared to a traditional implementation using central processing units (CPUs). This allows us to study complex three-dimensional problems tackling high spatial resolution.