Strojniski vestnik - Journal of Mechanical Engineering 56(2010)4, 275-283 UDC 620.19:666.11 Paper received: 23.02.2010 Paper accepted: 30.04.2010 Impact of Solid Particulate on Brittle Materials Donato Aquaro University of Pisa, Department of Mechanical, Nuclear and Production Engineering, Italy This paper deals with the erosion of brittle materials due to the impact of solid particulate. Erosion tests are characterized by a great uncertainty in the results and high costs. These difficulties led the author to develop alternative methods based on numerical simulations for calculating the erosion rate of brittle and ductile materials. Erosion criteria, based on fracture energy, were developed and implemented as Fortran routines in a commercial FEM code. In this paper the proposed method was applied to calculate the erosion rate of glass and glass ceramics. Fracture energy was obtained using four points bending tests. The numerical results were compared with a developed theoretical model and with the experimental results, available in the literature. In spite of several simplifying assumptions, there was a good agreement between the numerical and experimental results. This method could be a powerful tool for assessing the erosion resistance of components in real operating conditions. © 2010 Journal of Mechanical Engineering. All rights reserved. Keywords: erosion model, impact wear, finite element, glass, glass ceramic erosion 0 INTRODUCTION The erosion mechanism of brittle materials occurs through cracking and chipping and very much depends on the toughness of the material. The maximum erosion rate is obtained with impacts normal to the target (impact angle a=90°) [1]. Several theoretical methods have been developed for determining the volume of eroded material as a function of the characteristics of the impacting particles (velocity, radius, density) and of the mechanical properties of the target (hardness, toughness, Young module) [2] and [3]. The functional dependence of the brittle material erosion rate (eroded volume, V, per erodent particle) on the fundamental variables is expressed using the following formula: v=Cwp Rpe pp Kjf4 H Ee,j (1) where the exponents ei depend on the different theories. For the method, developed by the author, (see Appendix I), the exponents are the following: e1 = 21/10, e2 = 11/3, e3 = 21/10, e4 = -4/3, e5 = -1/4, e6 = -8/15. The quantitative value of the eroded volume is calculated knowing the proportionality constant C1, which would be material independent and determined by erosion tests. These tests are intrinsically very uncertain. In fact constants for several theoretical approaches, calculated in [2] considering experimental values found in the literature, vary greatly, even though homogeneous classes of material (ceramics) were used. The greatest difficulty derives from the stochastic characteristics of erosion. Some of the possible causes which influence the variability of the results include the following: the fluid dynamic interaction between the erodent flow and the target, which determines the true value of the velocity vector (direction and magnitude), the actual value of particle energy transmitted to the target, the shielding effects produced by the rebounding of the particles, the actual friction coefficient between particle and target. Numerical simulations, performed with Finite Element Method (FEM) codes, can describe the erosion mechanisms and can predict the life of components subjected to this phenomenon. The author developed numerical predictive methods [2] and [3] to determine the erosion resistance of brittle and ductile materials. The erosion rate was obtained using numerical simulations of impacts of particulate on the material under examination. Failure criteria, based on the fracture energy, were implemented in a commercial computer code dedicated to the impulsive mechanics [4]. The main hypotheses of the method, applied to brittle materials are : - erosion is due to a tensile stress state in the elastic regime; - element damage is assumed to be cumulative and a damage indicator, calculated at each time step and for each element in a tensile stress state represents the eroded fraction of the element at each time step; *Corr. Author's Address: Dip. Di Ingegneria Meccanica Nucleare e della Produzione, via Diotisalvi n. 2, 56100 Pisa, Italy, aquaro@ing.unipi.it - an element is considered eroded and eliminated from the mesh when the cumulative deformation energy reaches the value of the fracture energy. After a brief description of the method reported in detail in [2], the following sections illustrate the determination of the erosion rate of glass and glass ceramics using numerical simulations. 1 THEORETICAL MODEL OF EROSION OF GLASS AND GLASS CERAMICS Glass and glass ceramic materials are brittle. Glass is an amorphous material characterized by very low values of toughness and ultimate tensile stress. Partial crystallization produces glass ceramics with improved mechanical characteristics. In several applications, these materials are subjected to erosion due to the impact of particles which also degrade their mechanical characteristics. Our fracture model predicts a cumulative damage in the zones subject to a tensile stress state, while the compressed zones are strengthened due to densification or viscous deformation phenomena and can yield. In the impact, each element is subjected to several cycles of traction and compression due to the transmission and reflection of stress waves on the boundaries. In order to consider this different behavior in tensile and compressive states, the damage variable is calculated as half of the difference between the maximum tensile energy and the maximum compressive energy accumulated in each element during the transient phase. The criterion is equivalent to that used in fatigue resistance calculations. In fact fatigue resistance depends on half of the difference between the maximum and minimum stresses. In the numerical model, each element is associated with two variables, the first stores the maximum tensile energy and the other the absolute value of the maximum compressive energy. The damage energy is equal to half of the difference between the previous variables. The fractured element fraction (called "damage"), Deli, is calculated as the ratio between the damage energy and the energy needed to form fracture surfaces. If DeU becomes equal to 1, the element is removed by the mesh. The total eroded mass is determined by multiplying the damage DeU by the element mass and adding it to the mass of all the fractured elements. The model considers the elements in a tensile stress state defined by a positive value of the first invariant stress tensor (I1=ax+ay+az > 0) and calculates the element damage function DeU as: D = 0.5 Yd V the erosion rate is calculated as: / e (2) (3) where o, _ as = C^PfieuKli )/"pM p { a¡jSijdKl, is the deformation energy, accumulated in the element, due to both a tensile and compressive stress state, respectively; Efr is the fracture energy of the material per unit of volume, Veli is the volume of the element and np is the number of erodent particles. If DeU = 1, the element is considered eroded and is removed by the mesh. If Deli < 1, the element is considered partially eroded. In this case it is assumed that the material strength of the element is reduced. This reduction is taken into account by decreasing the bulk modulus, BMt., and the shear modulus, Gt, of the material of the partially eroded element using the following expression: BM ite,= (1-Dell / DeHmJBMt G'tel=(1-Deli /Delimax)Gt Deiimax= 0.7 in order to avoid numerical instabilities. Differently from [2] and [3], in this application of the fracture model, the degradation Table 1. Properties of the materials used in the numerical simulations Material Bulk modulus [MPa] Shear modulus [MPa] Hardness [MPa] Ultimate tensile stress [MPa] Fracture energy [J/m3] Density [kg/m3] Fracture toughness [MPa m05] Glass 62330 38958 6390 60.9 32224 2200 0.71 Glass Ceramic 71733 43040 8410 197.3 397129 2200 1.72 si el of mechanical characteristics were not been taken into account during the transient, in order to reduce the complexity of the calculations. The damage function Deli enables us to implement an erosion model independent of mesh size. In fact the element is eliminated only when the deformation energy of the element is equal to the energy needed to crack the element (Deii = 1). 1.1 Characteristics of Glass and Glass Ceramics The glass and glass ceramics were simulated using a linear equation of state and an elastic plastic constitutive equation in compression. The particle erodent has a spherical geometry (r = 12.5 |) and is assumed to be rigid. The mechanical characteristics of the examined materials are reported in Table 1. The material data were obtained from [5]. The glass is made of SiO2 (80%)-Al203-Li20 using ZrO2 and Ti02 as nucleant agents. The glass ceramics was obtained performing partial crystallization of the above mentioned glass. The specific fracture energy was obtained from four-points bending tests on polished samples of glass (L = 40 mm; b = 3.97 mm; w = 9.25 mm) and glass ceramics (L = 40mm; b = 4.57mm; w = 9.36 mm) respectively [5]. Fig. 1. shows the load-displacement curves until rupture, which enabled us to calculate the specific fracture energy. Fig. 2 shows the geometry (x = 50 y = 100 z = 37.5 |) of the implemented model. Considering the symmetry of the problem only half of the geometry was meshed with 576600 elements. The target was subdivided into two parts: a central zone (control volume, meshed by 375000 cubic elements 0.5 | of side, analyzed for the erosion) and a lateral zone on which the boundary conditions were applied. Three impact velocities (50, 100 and 150 m/s) were considered. For each case the loading and unloading phase were examined. 3.5 z 2 / / o 1.5 / 1 / 0.5 0 - 0 0.1 0.2 0.3 0.4 0.5 displacement (mm) Fig. 1. Load versus displacement of glass and giass ceramic in four points bending tests Fig. 3 Distribution of the damage produced by the impact of the particle at 50 m/s against a glass sample and elements eroded around the impacted zone t=0.060^s Fig. 4. Distribution of the damage produced by the impact of the particle at 100 m/s against a glass sample and elements eroded around the impacted zone t=0.034^s Fig. 5. Distribution of the damage produced by the impact of the particle at 150 m/s against a glass sample and elements eroded around the impacted zone Fig. 6. Distribution of the damage produced by the impact of the particle at 150 m/s against a glass ceramic sample and elements eroded around the impacted zone 2 NUMERICAL RESULTS Figs. 3 to 6 illustrate the distribution of the damage, Deii on the glass and glass ceramic models, respectively. In addition the spatial distributions of the eroded elements are also shown. The damage morphology is characterized by a compressed central zone, corresponding to the cavity caused by the sphere that penetrates the target and can crush the material underneath. Around the cavity, a high tensile stress produces a fractured collar, which expands in the internal layer to form a fractured conical surface. The extension of the collar and the conical surface depends on the velocity of the impact. Fig. 7. Velocity of erodentparticle versus time At 50 m/s, only few elements of glass are fractured. These fractured elements are located on the upper surface around the cavity and start in radial direction from it. The conical surface appears at a velocity greater than 50 m/s (Figs. 4 and 5). For impacts on glass with a>p= 50 m/s, the compression stresses are in elastic regimen and only 0.7% of the energy of the particle erodent is absorbed by the target. This figure becomes approximately 60 and 70% for impact velocities of 100 and 150 m/s, respectively. Glass ceramics have a specific fracture energy than 10 times higher of that of glass and therefore there are eroded elements only for cop > 150 m/s (Fig. 6). The pattern of the fractured elements of glass ceramic for cop = 150 m/s looks like that of glass for cop = 50 m/s. Fig. 8. Load applied by the particle on the target versus time For lower values of impact velocity, the damage, Deh is lower than 1 in all the elements. Figs. 7 to 10 illustrate the time histories of the main variables of the erodent particle during the transient. The rebound velocity of the particle is reduced when large erosion occurs (a>p > 100 m/s on glass). In the other case only a small percentage of the particle kinetic energy is absorbed by the target. Fig. 9. Penetration depth of the particle into the target versus time For elastic impacts (impact on glass-ceramic or on glass with

100 m/s on glass), the dependence on particle velocity is reduced to < p0.88. As the particle is rigid, vertical displacement can be considered as the penetration depth of the particle in the target and enables us to calculate the impact area. Fig. 10. Pressure on the target versus time Fig. 9. shows that the maximum value of the particle penetration, in the case of an elastic impact, is proportional to < p0.83 which is similar to 100 m/s, the fracture occurs with a yielding in the compressed zones. Fig. 11. Erosion rate versus velocity determined by Eq. (1) Fig. 11 shows the erosion rate curves versus velocity for glass and glass ceramic compared with the numerical values. The curves were obtained by applying the Eq. (1) separately to the two materials and determining the following constants; glass: C1 = 0.418±0.15; glass ceramic: C1 = 0.103±0.034. The theory is based on elastic fracture and establishes that the constant has to be material independent. The disagreement is due to the high compression stresses which cause the material to yield. It is known [6] that there is a distinction between low-energy and high-energy impact. The damage in the first case is controlled by preexistent surface flaws (i.e. it depends on the fracture energy corresponding to Kc,t) while in the latter, it is controlled by the cracks produced by the impacting particle (in this case the fracture energy corresponds to the ultimate tensile stress). The previous considerations demonstrate that the ultimate tensile stress is an important variable in the case of high-energy impact. Therefore Eq. (1) was modified introducing the ultimate tensile stress, cu: V = C.m^Re ppe Kc/4 Hp Ee6\ -f (4) where jef is a reference ultimate tensile stress. u Fig. 12 shows the erosion rate versus velocity, obtained by applying the Eq. (4) to the glass and glass ceramic, assuming that the reference ultimate tensile stress is that of the glass ceramics. Fig. 12 also reports the numerical results of the erosion rate, normalized to the ratio (a /> Mp. Substituting Eqs. (5) in (6) and multiplying both sides by: da a = — dt we obtain: (7) - M paa = c2 a3/2a Eq. (7) can be written: Then integrating it with the following initial conditions: at t = 0 a = 0 and a = &p we have: 4c2 a5/2 2) --2-= (a-®J 5M p p The maximum approach am is obtained when: a = 0 and it is equal to am = ( 5Mpwl ^ 4c, Therefore substituting am in Eq. (5) we obtain the maximum contact force: Fm. (5MpW2p } 4c0 2000n Rppyp 243D2 In Eq. (8) we substituted the expressions of c2 and Mp= 4/3nRp3pp. In the impact of a spherical particle on a brittle material, radial and conical cracks (starting at the boundary of the contact area) develop during the loading phase, while during the unloading phase (the particle rebound) lateral cracks form, starting at the conical cracks and reaching the free surface. Therefore we can assume that the eroded volume V, is proportional to a cylinder volume with a radius equal to cr (the maximum length of the radial crack) and height equal hf (the maximum depth of the lateral cracks): V = c3ncrhf (9) where c3 is a proportionality constant. Evans has elaborated relations that give : - the maximum contact force versus cr and the material toughness KIc [10]: Fmax = C4 KIctCr 3/2 (10) - hf versus the kinetic energy of the particle and the material hardness Ht [10]: hf = C5 R4 pr< v" H, (11) where c4 and c5 are constants. Substituting the Eqs. (8) in (10) and rearranging for cr, we obtain: ( 2000n3 Ryyp ^2/15 243D2 K - (12) Substituting the expression of cr and hf in Eq. (9) we obtain the expression of the eroded volume: V=C®;ll%ulPp2moKIc;mH-l/4E -8/15 (13) where: -4/3 c3c4 c5 2000n 243 c- = + 2