1D linear elasticity Taking the limit as the number of springs and masses goes to infinity (and the forces and masses go to zero): If density and Young’s.

Slides:



Advertisements
Similar presentations
Common Variable Types in Elasticity
Advertisements

Navier-Stokes.
Continuity Equation. Continuity Equation Continuity Equation Net outflow in x direction.
Normal Strain and Stress
1cs533d-term Notes  No lecture Thursday (apologies)
1 LECTURE 2: DIVERGENCE THEOREM, PRESSURE, ARCHIMEDES PRINCIPLE Outward normal vector: consider an arbitrarily shaped simply- connected volume. I have.
Equilibrium and Elasticity Equilibrium Center of gravity Static Equilibrium Indeterminate Structures Elasticity Tension, Compression and Shearing pps by.
Some Ideas Behind Finite Element Analysis
Constitutive Relations in Solids Elasticity
APPLIED MECHANICS Lecture 10 Slovak University of Technology
Notes Assignment questions… cs533d-winter-2005.
1cs533d-term Notes  Assignment 2 is up. 2cs533d-term Modern FEM  Galerkin framework (the most common)  Find vector space of functions that.
1cs533d-term Notes  Braino in this lecture’s notes about last lectures bending energy…
1 MECH 221 FLUID MECHANICS (Fall 06/07) Tutorial 7.
1cs533d-winter-2005 Notes  Read “Physically Based Modelling” SIGGRAPH course notes by Witkin and Baraff (at least, rigid body sections) An alternative.
1cs533d-winter-2005 Notes  Final Project Please contact me this week with ideas, so we can work out a good topic.
1cs533d-term Notes  Required reading: Baraff & Witkin, “Large steps in cloth animation”, SIGGRAPH’98 Grinspun et al., “Discrete shells”, SCA’03.
1cs533d-term Notes  I am back, but still catching up  Assignment 2 is due today (or next time I’m in the dept following today)  Final project.
1Notes  Demetri Terzopoulos talk: Thursday, 4pm Dempster 310.
Overview Class #6 (Tues, Feb 4) Begin deformable models!! Background on elasticity Elastostatics: generalized 3D springs Boundary integral formulation.
1cs533d-winter-2005 Notes  More optional reading on web for collision detection.
Physics 430: Lecture 10 Energy of Interaction Dale E. Gary NJIT Physics Department.
Bars and Beams FEM Linear Static Analysis
1cs533d-winter-2005 Notes  Assignment 2 going okay? Make sure you understand what needs to be done before the weekend  Read Guendelman et al, “Nonconvex.
1cs533d-winter-2005 Notes. 2 Simplifications of Elasticity.
Finite Element Method in Geotechnical Engineering
Theory of Elasticity Theory of elasticity governs response – Symmetric stress & strain components Governing equations – Equilibrium equations (3) – Strain-displacement.
1cs533d-winter-2005 Notes  More reading on web site Baraff & Witkin’s classic cloth paper Grinspun et al. on bending Optional: Teran et al. on FVM in.
1cs533d-term Notes  list Even if you’re just auditing!
1cs533d-winter-2005 Notes  Some example values for common materials: (VERY approximate) Aluminum: E=70 GPa =0.34 Concrete:E=23 GPa =0.2 Diamond:E=950.
MECH 221 FLUID MECHANICS (Fall 06/07) Chapter 4: FLUID KINETMATICS
1cs533d-term Notes. 2 Poisson Ratio  Real materials are essentially incompressible (for large deformation - neglecting foams and other weird composites…)
Fluids. Eulerian View  In a Lagrangian view each body is described at each point in space. Difficult for a fluid with many particles.  In an Eulerian.
Numerical Hydraulics Wolfgang Kinzelbach with Marc Wolf and Cornel Beffa Lecture 1: The equations.
Stress, Strain, and Viscosity San Andreas Fault Palmdale.
Forces. Normal Stress A stress measures the surface force per unit area.  Elastic for small changes A normal stress acts normal to a surface.  Compression.
Computer graphics & visualization Rigid Body Simulation.
Physics 430: Lecture 22 Rotational Motion of Rigid Bodies
Conservation Laws for Continua
Review (2 nd order tensors): Tensor – Linear mapping of a vector onto another vector Tensor components in a Cartesian basis (3x3 matrix): Basis change.
Eigenvectors and Eigenvalues
Chapter 9 Static Equilibrium; Elasticity and Fracture
ME 520 Fundamentals of Finite Element Analysis
Rheology I. Rheology Part of mechanics that deals with the flow of rocks, or matter in general Deals with the relationship of the following: (in terms.
CEE 262A H YDRODYNAMICS Lecture 5 Conservation Laws Part I 1.
Defining sign of stress tensor Kittel’s Fig. 15 may be confusing about sign of T xx (which he calls X x ) Stress tensor component T xx is defined as the.
Wednesday, Nov. 12, 2003PHYS , Fall 2003 Dr. Jaehoon Yu 1 PHYS 1443 – Section 003 Lecture #19 Wednesday, Nov. 12, 2003 Dr. Jaehoon Yu 1.Conditions.
KINEMATICS Kinematics describes fluid flow without analyzing the forces responsibly for flow generation. Thereby it doesn’t matter what kind of liquid.
1 MAE 5130: VISCOUS FLOWS Momentum Equation: The Navier-Stokes Equations, Part 2 September 9, 2010 Mechanical and Aerospace Engineering Department Florida.
Chapter 12 Static Equilibrium and Elasticity. Introduction Equilibrium- a condition where an object is at rest OR its center of mass moves with a constant.
Dr. Wang Xingbo Fall , 2005 Mathematical & Mechanical Method in Mechanical Engineering.
FLUID PROPERTIES Independent variables SCALARS VECTORS TENSORS.
GG313 Lecture 14 Coordinate Transformations Strain.
Analysis of a cracked plate
Static Equilibrium and Elasticity
P1 Chapter 12 & 15 CIE Centre A-level Pure Maths © Adam Gibson.
Elasticity I Ali K. Abdel-Fattah. Elasticity In physics, elasticity is a physical property of materials which return to their original shape after they.
The Generalized Interpolation Material Point Method.
Monday, Nov. 18, 2002PHYS , Fall 2002 Dr. Jaehoon Yu 1 PHYS 1443 – Section 003 Lecture #18 Monday, Nov. 18, 2002 Dr. Jaehoon Yu 1.Elastic Properties.
Equilibrium and Elasticity Ch 12 (all). Equilibrium An object is in equilibrium when: - The vector sum of all the external forces that act the body must.
Spring 2002 Lecture #17 Dr. Jaehoon Yu 1.Conditions for Equilibrium 2.Center of Gravity 3.Elastic Properties of Solids Young’s Modulus Shear Modulus.
Wednesday, Nov. 17, 2004PHYS , Fall 2004 Dr. Jaehoon Yu 1 1.Conditions for Equilibrium 2.Mechanical Equilibrium 3.How to solve equilibrium problems?
Basic Geometric Nonlinearities Chapter Five - APPENDIX.
Introduction to strain and borehole strainmeter data
Physics 141Mechanics Lecture 17 Equilibrium and Elasticity Yongli Gao A rigid body has six degrees of freedom: three for linear motion and three for rotational.
Continuum Mechanics (MTH487)
CHAPTER 2 - EXPLICIT TRANSIENT DYNAMIC ANALYSYS
Chapter 9: Differential Analysis of Fluid Flow
Lecture Rigid Body Dynamics.
Continuum Mechanics for Hillslopes: Part III
Presentation transcript:

1D linear elasticity Taking the limit as the number of springs and masses goes to infinity (and the forces and masses go to zero): If density and Young’s modulus constant, cs533d-winter-2005

Sound waves Try solution x(p,t)=x0(p-ct) And x(p,t)=x0(p+ct) So speed of “sound” in rod is Courant-Friedrichs-Levy (CFL) condition: Numerical methods only will work if information transmitted numerically at least as fast as in reality (here: the speed of sound) Usually the same as stability limit for good explicit methods [what are the eigenvalues here] Implicit methods transmit information infinitely fast cs533d-winter-2005

Why? Are sound waves important? Visually? Usually not However, since speed of sound is a material property, it can help us get to higher dimensions Speed of sound in terms of one spring is So in higher dimensions, just pick k so that c is constant m is mass around spring [triangles, tets] Optional reading: van Gelder cs533d-winter-2005

Damping Figuring out how to scale damping is more tricky Go to differential equation (no mesh) So spring damping should be cs533d-winter-2005

Extra effects with springs (Brittle) fracture Whenever a spring is stretched too far, break it Issue with loose ends… Plasticity Whenever a spring is stretched too far, change the rest length part of the way More on this later cs533d-winter-2005

Mass-spring problems [anisotropy] [stretching, Poisson’s ratio] So we will instead look for a generalization of “percent deformation” to multiple dimensions: elasticity theory cs533d-winter-2005

Studying Deformation Let’s look at a deformable object World space: points x in the object as we see it Object space (or rest pose): points p in some reference configuration of the object (Technically we might not have a rest pose, but usually we do, and it is the simplest parameterization) So we identify each point x of the continuum with the label p, where x=X(p) The function X(p) encodes the deformation cs533d-winter-2005

Going back to 1D Worked out that dX/dp-1 was the key quantity for measuring stretching and compression Nice thing about differentiating: constants (translating whole object) don’t matter Call A= X/p the deformation gradient cs533d-winter-2005

Strain A isn’t so handy, though it somehow encodes exactly how stretched/compressed we are Also encodes how rotated we are: who cares? We want to process A somehow to remove the rotation part [difference in lengths] ATA-I is exactly zero when A is a rigid body rotation Define Green strain cs533d-winter-2005

Why the half?? [Look at 1D, small deformation] A=1+ ATA-I = A2-1 = 2+2 ≈ 2 Therefore G ≈ , which is what we expect Note that for large deformation, Green strain grows quadratically - maybe not what you expect! Whole cottage industry: defining strain differently cs533d-winter-2005

Cauchy strain tensor Get back to linear, not quadratic Look at “small displacement” Not only is the shape only slightly deformed, but it only slightly rotates (e.g. if one end is fixed in place) Then displacement x-p has gradient D=A-I Then And for small displacement, first term negligible Cauchy strain Symmetric part of deformation gradient Rotation is skew-symmetric part cs533d-winter-2005

Analyzing Strain Strain is a 3x3 “tensor” (fancy name for a matrix) Always symmetric What does it mean? Diagonalize: rotate into a basis of eigenvectors Entries (eigenvalues) tells us the scaling on the different axes Sum of eigenvalues (always equal to the trace=sum of diagonal, even if not diagonal): approximate volume change Or directly analyze: off-diagonals show skew (also known as shear) cs533d-winter-2005

Force In 1D, we got the force of a spring by simply multiplying the strain by some material constant (Young’s modulus) In multiple dimensions, strain is a tensor, but force is a vector… And in the continuum limit, force goes to zero anyhow---so we have to be a little more careful cs533d-winter-2005

Conservation of Momentum In other words F=ma Decompose body into “control volumes” Split F into fbody (e.g. gravity, magnetic forces, …) force per unit volume and traction t (on boundary between two chunks of continuum: contact force) dimensions are force per unit area (like pressure) cs533d-winter-2005

Cauchy’s Fundamental Postulate Traction t is a function of position x and normal n Ignores rest of boundary (e.g. information like curvature, etc.) Theorem If t is smooth (be careful at boundaries of object, e.g. cracks) then t is linear in n: t=(x)n  is the Cauchy stress tensor (a matrix) It also is force per unit area Diagonal: normal stress components Off-diagonal: shear stress components cs533d-winter-2005

Cauchy Stress From conservation of angular momentum can derive that Cauchy stress tensor  is symmetric:  = T Thus there are only 6 degrees of freedom (in 3D) In 2D, only 3 degrees of freedom What is ? That’s the job of constitutive modeling Depends on the material (e.g. water vs. steel vs. silly putty) cs533d-winter-2005

Divergence Theorem Try to get rid of integrals First make them all volume integrals with divergence theorem: Next let control volume shrink to zero: Note that integrals and normals were in world space, so is the divergence (it’s w.r.t. x not p) cs533d-winter-2005

Constitutive Modeling This can get very complicated for complicated materials Let’s start with simple elastic materials We’ll even leave damping out Then stress  only depends on strain, however we measure it (say G or ) cs533d-winter-2005

Linear elasticity Very nice thing about Cauchy strain: it’s linear in deformation No quadratic dependence Easy and fast to deal with Natural thing is to make a linear relationship with Cauchy stress  Then the full equation is linear! cs533d-winter-2005

Young’s modulus Obvious first thing to do: if you pull on material, resists like a spring: =E E is the Young’s modulus Let’s check that in 1D (where we know what should happen with springs) cs533d-winter-2005

Poisson Ratio Real materials are essentially incompressible (for large deformation - neglecting foams and other weird composites…) For small deformation, materials are usually somewhat incompressible Imagine stretching block in one direction Measure the contraction in the perpendicular directions Ratio is , Poisson’s ratio [draw experiment; ] cs533d-winter-2005

What is Poisson’s ratio? Has to be between -1 and 0.5 0.5 is exactly incompressible [derive] Negative is weird, but possible [origami] Rubber: close to 0.5 Steel: more like 0.33 Metals: usually 0.25-0.35 [cute: cork is almost 0] cs533d-winter-2005