Module 3 Constitutive Equations
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10-1 CHAPTER 10 DEFORMATION 10.1 Stress-Strain Diagrams And
EN380 Naval Materials Science and Engineering Course Notes, U.S. Naval Academy CHAPTER 10 DEFORMATION 10.1 Stress-Strain Diagrams and Material Behavior 10.2 Material Characteristics 10.3 Elastic-Plastic Response of Metals 10.4 True stress and strain measures 10.5 Yielding of a Ductile Metal under a General Stress State - Mises Yield Condition. 10.6 Maximum shear stress condition 10.7 Creep Consider the bar in figure 1 subjected to a simple tension loading F. Figure 1: Bar in Tension Engineering Stress () is the quotient of load (F) and area (A). The units of stress are normally pounds per square inch (psi). = F A where: is the stress (psi) F is the force that is loading the object (lb) A is the cross sectional area of the object (in2) When stress is applied to a material, the material will deform. Elongation is defined as the difference between loaded and unloaded length ∆푙 = L - Lo where: ∆푙 is the elongation (ft) L is the loaded length of the cable (ft) Lo is the unloaded (original) length of the cable (ft) 10-1 EN380 Naval Materials Science and Engineering Course Notes, U.S. Naval Academy Strain is the concept used to compare the elongation of a material to its original, undeformed length. Strain () is the quotient of elongation (e) and original length (L0). Engineering Strain has no units but is often given the units of in/in or ft/ft. ∆푙 휀 = 퐿 where: is the strain in the cable (ft/ft) ∆푙 is the elongation (ft) Lo is the unloaded (original) length of the cable (ft) Example Find the strain in a 75 foot cable experiencing an elongation of one inch. -
Static Analysis of Isotropic, Orthotropic and Functionally Graded Material Beams
Journal of Multidisciplinary Engineering Science and Technology (JMEST) ISSN: 2458-9403 Vol. 3 Issue 5, May - 2016 Static analysis of isotropic, orthotropic and functionally graded material beams Waleed M. Soliman M. Adnan Elshafei M. A. Kamel Dep. of Aeronautical Engineering Dep. of Aeronautical Engineering Dep. of Aeronautical Engineering Military Technical College Military Technical College Military Technical College Cairo, Egypt Cairo, Egypt Cairo, Egypt [email protected] [email protected] [email protected] Abstract—This paper presents static analysis of degrees of freedom for each lamina, and it can be isotropic, orthotropic and Functionally Graded used for long and short beams, this laminated finite Materials (FGMs) beams using a Finite Element element model gives good results for both stresses and deflections when compared with other solutions. Method (FEM). Ansys Workbench15 has been used to build up several models to simulate In 1993 Lidstrom [2] have used the total potential different types of beams with different boundary energy formulation to analyze equilibrium for a conditions, all beams have been subjected to both moderate deflection 3-D beam element, the condensed two-node element reduced the size of the of uniformly distributed and transversal point problem, compared with the three-node element, but loads within the experience of Timoshenko Beam increased the computing time. The condensed two- Theory and First order Shear Deformation Theory. node system was less numerically stable than the The material properties are assumed to be three-node system. Because of this fact, it was not temperature-independent, and are graded in the possible to evaluate the third and fourth-order thickness direction according to a simple power differentials of the strain energy function, and thus not law distribution of the volume fractions of the possible to determine the types of criticality constituents. -
Arxiv:1910.01953V1 [Cond-Mat.Soft] 4 Oct 2019 Tion of the Load
Geometric charges and nonlinear elasticity of soft metamaterials Yohai Bar-Sinai,1 Gabriele Librandi,1 Katia Bertoldi,1 and Michael Moshe2, ∗ 1School of Engineering and Applied Sciences, Harvard University, Cambridge MA 02138 2Racah Institute of Physics, The Hebrew University of Jerusalem, Jerusalem, Israel 91904 Problems of flexible mechanical metamaterials, and highly deformable porous solids in general, are rich and complex due to nonlinear mechanics and nontrivial geometrical effects. While numeric approaches are successful, analytic tools and conceptual frameworks are largely lacking. Using an analogy with electrostatics, and building on recent developments in a nonlinear geometric formu- lation of elasticity, we develop a formalism that maps the elastic problem into that of nonlinear interaction of elastic charges. This approach offers an intuitive conceptual framework, qualitatively explaining the linear response, the onset of mechanical instability and aspects of the post-instability state. Apart from intuition, the formalism also quantitatively reproduces full numeric simulations of several prototypical structures. Possible applications of the tools developed in this work for the study of ordered and disordered porous mechanical metamaterials are discussed. I. INTRODUCTION tic metamaterials out of an underlying nonlinear theory of elasticity. The hallmark of condensed matter physics, as de- A theoretical analysis of the elastic problem requires scribed by P.W. Anderson in his paper \More is Dif- solving the nonlinear equations of elasticity while satis- ferent" [1], is the emergence of collective phenomena out fying the multiple free boundary conditions on the holes of well understood simple interactions between material edges - a seemingly hopeless task from an analytic per- elements. Within the ever increasing list of such systems, spective. -
Constitutive Relations: Transverse Isotropy and Isotropy
Objectives_template Module 3: 3D Constitutive Equations Lecture 11: Constitutive Relations: Transverse Isotropy and Isotropy The Lecture Contains: Transverse Isotropy Isotropic Bodies Homework References file:///D|/Web%20Course%20(Ganesh%20Rana)/Dr.%20Mohite/CompositeMaterials/lecture11/11_1.htm[8/18/2014 12:10:09 PM] Objectives_template Module 3: 3D Constitutive Equations Lecture 11: Constitutive relations: Transverse isotropy and isotropy Transverse Isotropy: Introduction: In this lecture, we are going to see some more simplifications of constitutive equation and develop the relation for isotropic materials. First we will see the development of transverse isotropy and then we will reduce from it to isotropy. First Approach: Invariance Approach This is obtained from an orthotropic material. Here, we develop the constitutive relation for a material with transverse isotropy in x2-x3 plane (this is used in lamina/laminae/laminate modeling). This is obtained with the following form of the change of axes. (3.30) Now, we have Figure 3.6: State of stress (a) in x1, x2, x3 system (b) with x1-x2 and x1-x3 planes of symmetry From this, the strains in transformed coordinate system are given as: file:///D|/Web%20Course%20(Ganesh%20Rana)/Dr.%20Mohite/CompositeMaterials/lecture11/11_2.htm[8/18/2014 12:10:09 PM] Objectives_template (3.31) Here, it is to be noted that the shear strains are the tensorial shear strain terms. For any angle α, (3.32) and therefore, W must reduce to the form (3.33) Then, for W to be invariant we must have Now, let us write the left hand side of the above equation using the matrix as given in Equation (3.26) and engineering shear strains. -
An Approximate Nodal Is Developed to Calculate the Change of •Laatio Constants Induced by Point Defect* in Hep Metals
1 - INTBOPUCTIOB the elastic conatants.aa well aa othernmechanieal pro partita of* IC/79/lW irradiated materiale (are vary sensitive to tne oonoantration of i- INTERNAL REPORT (Limited distribution) rradiation produced point defeota.One of the firat eatimatee of thla effect waa done by Dienea [l"J who aiaply averaged over the whole la- International Atomic Energy Agency ttice the locally changed interatoalo bonds due to the pxesense of" and the defect.With tola nodal ha predioted an inoreaee of the alaatle United Nations Educational Scientific and Cultural Organization constant* of about 10* par atonic f of interatitlala in Ou and a da. oreaee of l]t par at. % of vacanolea. INTERNATIONAL CENTRE FOE THEORETICAL PHYSICS Later on,experlaental etudiea by Konlg at al.[2]and wanal lilgar* very large decrease a of about 5O}( per at.)t of Vrenlcal dafaota.fha theory waa than iaproved in order to relate the change of a la* tic con a tan t a to the defect lnduoed change of force oonatanta and tno equivalent aethoda were devalopedi the energy-»athod of ludwig [4] CHANGE OF ELASTIC CONSTANTS and the t-aatrix method of Slllot et al.C ?]. INDUCED BY FOIMT DEFECTS IN hep CRYSTALS * Iheoretioal eetlnates for oublo oryetala have been oarrie* out by Ludwig[4] for the caae of vacancleafby Piatorlueld for intarati- Carlos Tome •• tiala and by Sederloaa et al.t?] for duabell interotitiala. International Centre for Theoretical Physics, Trieste, Italy. Re thaoretloal work baa been done ao far for hexagonal cryatmlaj and the experimental neaeurentanta (available only for Kg) ax* eona- ABSTRACT what crude t8,9i,ayan though in the last few. -
Gravitation in the Surface Tension Model of Spacetime
IARD 2018 IOP Publishing IOP Conf. Series: Journal of Physics: Conf. Series 1239 (2019) 012010 doi:10.1088/1742-6596/1239/1/012010 Gravitation in the surface tension model of spacetime H A Perko1 1Office 14, 140 E. 4th Street, Loveland, CO, USA 80537 E-mail: [email protected] Abstract. A mechanical model of spacetime was introduced at a prior conference for describing perturbations of stress, strain, and displacement within a spacetime exhibiting surface tension. In the prior work, equations governing spacetime dynamics described by the model show some similarities to fundamental equations of quantum mechanics. Similarities were identified between the model and equations of Klein-Gordon, Schrödinger, Heisenberg, and Weyl. The introduction did not explain how gravitation arises within the model. In this talk, the model will be summarized, corrected, and extended for comparison with general relativity. An anisotropic elastic tensor is proposed as a constitutive relation between stress energy and curvature instead of the traditional Einstein constant. Such a relation permits spatial geometric terms in the mechanical model to resemble quantum mechanics while temporal terms and the overall structure of tensor equations remain consistent with general relativity. This work is in its infancy; next steps are to show how the anisotropic tensor affects cosmological predictions and to further explore if geometry and quantum mechanics can be related in more than just appearance. 1. Introduction The focus of this research is to find a mechanism by which spacetime might curl, warp, or re-configure at small scales to provide a geometrical explanation for quantum mechanics while remaining consistent with gravity and general relativity. -
Orthotropic Material Homogenization of Composite Materials Including Damping
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Lirias Orthotropic material homogenization of composite materials including damping A. Nateghia,e, A. Rezaeia,e,, E. Deckersa,d, S. Jonckheerea,b,d, C. Claeysa,d, B. Pluymersa,d, W. Van Paepegemc, W. Desmeta,d a KU Leuven, Department of Mechanical Engineering, Celestijnenlaan 300B box 2420, 3001 Heverlee, Belgium. E-mail: [email protected]. b Siemens Industry Software NV, Digital Factory, Product Lifecycle Management – Simulation and Test Solutions, Interleuvenlaan 68, B-3001 Leuven, Belgium. c Ghent University, Department of Materials Science & Engineering, Technologiepark-Zwijnaarde 903, 9052 Zwijnaarde, Belgium. d Member of Flanders Make. e SIM vzw, Technologiepark Zwijnaarde 935, B-9052 Ghent, Belgium. Introduction In the multiscale analysis of composite materials obtaining the effective equivalent material properties of the composite from the properties of its constituents is an important bridge between different scales. Although, a variety of homogenization methods are already in use, there is still a need for further development of novel approaches which can deal with complexities such as frequency dependency of material properties; which is specially of importance when dealing with damped structures. Time-domain methods Frequency-domain method Material homogenization is performed in two separate steps: Wave dispersion based homogenization is performed to a static step and a dynamic one. provide homogenized damping and material -
Lecture 13: Earth Materials
Earth Materials Lecture 13 Earth Materials GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Hooke’s law of elasticity Force Extension = E × Area Length Hooke’s law σn = E εn where E is material constant, the Young’s Modulus Units are force/area – N/m2 or Pa Robert Hooke (1635-1703) was a virtuoso scientist contributing to geology, σ = C ε palaeontology, biology as well as mechanics ij ijkl kl ß Constitutive equations These are relationships between forces and deformation in a continuum, which define the material behaviour. GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Shear modulus and bulk modulus Young’s or stiffness modulus: σ n = Eε n Shear or rigidity modulus: σ S = Gε S = µε s Bulk modulus (1/compressibility): Mt Shasta andesite − P = Kεv Can write the bulk modulus in terms of the Lamé parameters λ, µ: K = λ + 2µ/3 and write Hooke’s law as: σ = (λ +2µ) ε GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Young’s Modulus or stiffness modulus Young’s Modulus or stiffness modulus: σ n = Eε n Interatomic force Interatomic distance GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Shear Modulus or rigidity modulus Shear modulus or stiffness modulus: σ s = Gε s Interatomic force Interatomic distance GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Hooke’s Law σij and εkl are second-rank tensors so Cijkl is a fourth-rank tensor. For a general, anisotropic material there are 21 independent elastic moduli. In the isotropic case this tensor reduces to just two independent elastic constants, λ and µ. -
Analysis of Deformation
Chapter 7: Constitutive Equations Definition: In the previous chapters we’ve learned about the definition and meaning of the concepts of stress and strain. One is an objective measure of load and the other is an objective measure of deformation. In fluids, one talks about the rate-of-deformation as opposed to simply strain (i.e. deformation alone or by itself). We all know though that deformation is caused by loads (i.e. there must be a relationship between stress and strain). A relationship between stress and strain (or rate-of-deformation tensor) is simply called a “constitutive equation”. Below we will describe how such equations are formulated. Constitutive equations between stress and strain are normally written based on phenomenological (i.e. experimental) observations and some assumption(s) on the physical behavior or response of a material to loading. Such equations can and should always be tested against experimental observations. Although there is almost an infinite amount of different materials, leading one to conclude that there is an equivalently infinite amount of constitutive equations or relations that describe such materials behavior, it turns out that there are really three major equations that cover the behavior of a wide range of materials of applied interest. One equation describes stress and small strain in solids and called “Hooke’s law”. The other two equations describe the behavior of fluidic materials. Hookean Elastic Solid: We will start explaining these equations by considering Hooke’s law first. Hooke’s law simply states that the stress tensor is assumed to be linearly related to the strain tensor. -
Efficient Hydraulic Fluids Compressibility Is Still One of the Most Critically Important Factors
WORLDWIDE R. David Whitby Efficient hydraulic fluids Compressibility is still one of the most critically important factors. ydraulic fluids transmit power as a hydraulic system con- while phosphate and vegetable-oil esters have compressibilities H verts mechanical energy into fluid energy and subsequently similar to that of water. Polyalphaolefins are more compressible to mechanical work. To achieve this conversion efficiently, hydrau- than mineral oils. Water-glycol fluids are intermediate between lic fluids need to be relatively incompressible. Hydraulic fluids mineral oils and water. must also minimize wear, reduce friction, provide cooling and pre- Mineral oils are relatively incompressible, but volume reduc- vent rust and corrosion, be compatible with system components tions can be approximately 0.5% for pressures ranging from 6,900 and help keep the system free of deposits. kPa (1,000 psi) up to 27,600 kPa (4,000 psi). Compressibility in- Compressibility measures the rela- creases with pressure and temperature tive change in volume of a fluid or solid and has significant effects on high-pres- as a response to a change in pressure and sure fluid systems. Hydraulic oils typi- is the reciprocal of the volume-elastic cally contain 6% to 10% of dissolved air, modulus or bulk modulus of elasticity. which has no measurable effect on bulk Bulk modulus defines the pressure in- modulus provided it stays in solution. crease needed to cause a given relative Bulk modulus is an inherent property decrease in volume. of the hydraulic fluid and, therefore, is The bulk modulus of a fluid is nonlin- an inherent inefficiency of the hydraulic ear. -
Velocity, Density, Modulus of Hydrocarbon Fluids
Velocity, Density and Modulus of Hydrocarbon Fluids --Data Measurement De-hua Han*, HARC; M. Batzle, CSM Summary measured with pressure up to 55.2 Mpa (8000 Psi) and temperature up to 100 °C. Density and ultrasonic velocity of numerous hydrocarbon fluids (oil, oil based mud filtrate, hydrocarbon gases and Velocity of Dead Oil miscible CO2-oil) were measured at in situ conditions of pressure up to 50 Mpa and temperatures up to100 °C. Initial measurements were on the gas-free or ‘dead’ oils at Dynamic moduli are derived from velocities and densities. pressure and temperature (see Fig. 1). We used the Newly measured data refine correlations of velocity and following model to fit data: density to API gravity, Gas Oil ratio (GOR), Gas gravity and in situ pressure and temperature. Gas in solution is Vp (m/s) = A – B * T + C * P + D * T * P (1) largely responsible for reducing the bulk modulus of the live oil. Phase changes, such as exsolving gas during Here A is a pseudo velocity at 0 °C and room pressure (0 production, can dramatically lower velocities and modulus, Mpa, gauge), B is temperature gradient, C is pressure but is dependent on pressure conditions. Distinguish gas gradient and D is coefficient of coupled temperature and from liquid phase may not be possible at a high pressure. pressure effects. Fluids are often supercritical. With increasing pressure, a gas-like fluid can begin to behave like a liquid Dead & live oil of #1 B.P. = 1900 psi at 60 C Introduction 1800 1600 Hydrocarbon fluids are the primary targets of the seismic exploration. -
Crack Tip Elements and the J Integral
EN234: Computational methods in Structural and Solid Mechanics Homework 3: Crack tip elements and the J-integral Due Wed Oct 7, 2015 School of Engineering Brown University The purpose of this homework is to help understand how to handle element interpolation functions and integration schemes in more detail, as well as to explore some applications of FEA to fracture mechanics. In this homework you will solve a simple linear elastic fracture mechanics problem. You might find it helpful to review some of the basic ideas and terminology associated with linear elastic fracture mechanics here (in particular, recall the definitions of stress intensity factor and the nature of crack-tip fields in elastic solids). Also check the relations between energy release rate and stress intensities, and the background on the J integral here. 1. One of the challenges in using finite elements to solve a problem with cracks is that the stress field at a crack tip is singular. Standard finite element interpolation functions are designed so that stresses remain finite a everywhere in the element. Various types of special b c ‘crack tip’ elements have been designed that 3L/4 incorporate the singularity. One way to produce a L/4 singularity (the method used in ABAQUS) is to mesh L the region just near the crack tip with 8 noded elements, with a special arrangement of nodal points: (i) Three of the nodes (nodes 1,4 and 8 in the figure) are connected together, and (ii) the mid-side nodes 2 and 7 are moved to the quarter-point location on the element side.