Momentum Balance Principles
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Multidisciplinary Design Project Engineering Dictionary Version 0.0.2
Multidisciplinary Design Project Engineering Dictionary Version 0.0.2 February 15, 2006 . DRAFT Cambridge-MIT Institute Multidisciplinary Design Project This Dictionary/Glossary of Engineering terms has been compiled to compliment the work developed as part of the Multi-disciplinary Design Project (MDP), which is a programme to develop teaching material and kits to aid the running of mechtronics projects in Universities and Schools. The project is being carried out with support from the Cambridge-MIT Institute undergraduate teaching programe. For more information about the project please visit the MDP website at http://www-mdp.eng.cam.ac.uk or contact Dr. Peter Long Prof. Alex Slocum Cambridge University Engineering Department Massachusetts Institute of Technology Trumpington Street, 77 Massachusetts Ave. Cambridge. Cambridge MA 02139-4307 CB2 1PZ. USA e-mail: [email protected] e-mail: [email protected] tel: +44 (0) 1223 332779 tel: +1 617 253 0012 For information about the CMI initiative please see Cambridge-MIT Institute website :- http://www.cambridge-mit.org CMI CMI, University of Cambridge Massachusetts Institute of Technology 10 Miller’s Yard, 77 Massachusetts Ave. Mill Lane, Cambridge MA 02139-4307 Cambridge. CB2 1RQ. USA tel: +44 (0) 1223 327207 tel. +1 617 253 7732 fax: +44 (0) 1223 765891 fax. +1 617 258 8539 . DRAFT 2 CMI-MDP Programme 1 Introduction This dictionary/glossary has not been developed as a definative work but as a useful reference book for engi- neering students to search when looking for the meaning of a word/phrase. It has been compiled from a number of existing glossaries together with a number of local additions. -
On the Geometric Character of Stress in Continuum Mechanics
Z. angew. Math. Phys. 58 (2007) 1–14 0044-2275/07/050001-14 DOI 10.1007/s00033-007-6141-8 Zeitschrift f¨ur angewandte c 2007 Birkh¨auser Verlag, Basel Mathematik und Physik ZAMP On the geometric character of stress in continuum mechanics Eva Kanso, Marino Arroyo, Yiying Tong, Arash Yavari, Jerrold E. Marsden1 and Mathieu Desbrun Abstract. This paper shows that the stress field in the classical theory of continuum mechanics may be taken to be a covector-valued differential two-form. The balance laws and other funda- mental laws of continuum mechanics may be neatly rewritten in terms of this geometric stress. A geometrically attractive and covariant derivation of the balance laws from the principle of energy balance in terms of this stress is presented. Mathematics Subject Classification (2000). Keywords. Continuum mechanics, elasticity, stress tensor, differential forms. 1. Motivation This paper proposes a reformulation of classical continuum mechanics in terms of bundle-valued exterior forms. Our motivation is to provide a geometric description of force in continuum mechanics, which leads to an elegant geometric theory and, at the same time, may enable the development of space-time integration algorithms that respect the underlying geometric structure at the discrete level. In classical mechanics the traditional approach is to define all the kinematic and kinetic quantities using vector and tensor fields. For example, velocity and traction are both viewed as vector fields and power is defined as their inner product, which is induced from an appropriately defined Riemannian metric. On the other hand, it has long been appreciated in geometric mechanics that force should not be viewed as a vector, but rather a one-form. -
Leonhard Euler - Wikipedia, the Free Encyclopedia Page 1 of 14
Leonhard Euler - Wikipedia, the free encyclopedia Page 1 of 14 Leonhard Euler From Wikipedia, the free encyclopedia Leonhard Euler ( German pronunciation: [l]; English Leonhard Euler approximation, "Oiler" [1] 15 April 1707 – 18 September 1783) was a pioneering Swiss mathematician and physicist. He made important discoveries in fields as diverse as infinitesimal calculus and graph theory. He also introduced much of the modern mathematical terminology and notation, particularly for mathematical analysis, such as the notion of a mathematical function.[2] He is also renowned for his work in mechanics, fluid dynamics, optics, and astronomy. Euler spent most of his adult life in St. Petersburg, Russia, and in Berlin, Prussia. He is considered to be the preeminent mathematician of the 18th century, and one of the greatest of all time. He is also one of the most prolific mathematicians ever; his collected works fill 60–80 quarto volumes. [3] A statement attributed to Pierre-Simon Laplace expresses Euler's influence on mathematics: "Read Euler, read Euler, he is our teacher in all things," which has also been translated as "Read Portrait by Emanuel Handmann 1756(?) Euler, read Euler, he is the master of us all." [4] Born 15 April 1707 Euler was featured on the sixth series of the Swiss 10- Basel, Switzerland franc banknote and on numerous Swiss, German, and Died Russian postage stamps. The asteroid 2002 Euler was 18 September 1783 (aged 76) named in his honor. He is also commemorated by the [OS: 7 September 1783] Lutheran Church on their Calendar of Saints on 24 St. Petersburg, Russia May – he was a devout Christian (and believer in Residence Prussia, Russia biblical inerrancy) who wrote apologetics and argued Switzerland [5] forcefully against the prominent atheists of his time. -
Fundamental Governing Equations of Motion in Consistent Continuum Mechanics
Fundamental governing equations of motion in consistent continuum mechanics Ali R. Hadjesfandiari, Gary F. Dargush Department of Mechanical and Aerospace Engineering University at Buffalo, The State University of New York, Buffalo, NY 14260 USA [email protected], [email protected] October 1, 2018 Abstract We investigate the consistency of the fundamental governing equations of motion in continuum mechanics. In the first step, we examine the governing equations for a system of particles, which can be considered as the discrete analog of the continuum. Based on Newton’s third law of action and reaction, there are two vectorial governing equations of motion for a system of particles, the force and moment equations. As is well known, these equations provide the governing equations of motion for infinitesimal elements of matter at each point, consisting of three force equations for translation, and three moment equations for rotation. We also examine the character of other first and second moment equations, which result in non-physical governing equations violating Newton’s third law of action and reaction. Finally, we derive the consistent governing equations of motion in continuum mechanics within the framework of couple stress theory. For completeness, the original couple stress theory and its evolution toward consistent couple stress theory are presented in true tensorial forms. Keywords: Governing equations of motion, Higher moment equations, Couple stress theory, Third order tensors, Newton’s third law of action and reaction 1 1. Introduction The governing equations of motion in continuum mechanics are based on the governing equations for systems of particles, in which the effect of internal forces are cancelled based on Newton’s third law of action and reaction. -
Application of Newton's Second
Chapter 8 Applications of Newton’s Second Law 8.1 Force Laws ............................................................................................................... 1 8.1.1 Hooke’s Law ..................................................................................................... 1 8.2.2 Principle of Equivalence: ................................................................................ 5 8.2.3 Gravitational Force near the Surface of the Earth ....................................... 5 8.2.4 Electric Charge and Coulomb’s Law ............................................................. 6 Example 8.1 Coulomb’s Law and the Universal Law of Gravitation .................. 7 8.3 Contact Forces ......................................................................................................... 7 8.3.1 Free-body Force Diagram ................................................................................... 9 Example 8.2 Tug-of-War .......................................................................................... 9 8.3.3 Normal Component of the Contact Force and Weight ............................... 11 8.3.4 Static and Kinetic Friction ............................................................................ 14 8.3.5 Modeling ......................................................................................................... 16 8.4 Tension in a Rope .................................................................................................. 16 8.4.1 Static Tension in a Rope ............................................................................... -
CONTINUUM MECHANICS (Lecture Notes)
CONTINUUM MECHANICS (Lecture Notes) Zdenekˇ Martinec Department of Geophysics Faculty of Mathematics and Physics Charles University in Prague V Holeˇsoviˇck´ach 2, 180 00 Prague 8 Czech Republic e-mail: [email protected]ff.cuni.cz Original: May 9, 2003 Updated: January 11, 2011 Preface This text is suitable for a two-semester course on Continuum Mechanics. It is based on notes from undergraduate courses that I have taught over the last decade. The material is intended for use by undergraduate students of physics with a year or more of college calculus behind them. I would like to thank Erik Grafarend, Ctirad Matyska, Detlef Wolf and Jiˇr´ıZahradn´ık,whose interest encouraged me to write this text. I would also like to thank my oldest son Zdenˇekwho plotted most of figures embedded in the text. I am grateful to many students for helping me to reveal typing misprints. I would like to acknowledge my indebtedness to Kevin Fleming, whose through proofreading of the entire text is very much appreciated. Readers of this text are encouraged to contact me with their comments, suggestions, and questions. I would be very happy to hear what you think I did well and I could do better. My e-mail address is [email protected]ff.cuni.cz and a full mailing address is found on the title page. ZdenˇekMartinec ii Contents (page numbering not completed yet) Preface Notation 1. GEOMETRY OF DEFORMATION 1.1 Body, configurations, and motion 1.2 Description of motion 1.3 Lagrangian and Eulerian coordinates 1.4 Lagrangian and Eulerian variables 1.5 Deformation gradient 1.6 Polar decomposition of the deformation gradient 1.7 Measures of deformation 1.8 Length and angle changes 1.9 Surface and volume changes 1.10 Strain invariants, principal strains 1.11 Displacement vector 1.12 Geometrical linearization 1.12.1 Linearized analysis of deformation 1.12.2 Length and angle changes 1.12.3 Surface and volume changes 2. -
Stress, Cauchy's Equation and the Navier-Stokes Equations
Chapter 3 Stress, Cauchy’s equation and the Navier-Stokes equations 3.1 The concept of traction/stress • Consider the volume of fluid shown in the left half of Fig. 3.1. The volume of fluid is subjected to distributed external forces (e.g. shear stresses, pressures etc.). Let ∆F be the resultant force acting on a small surface element ∆S with outer unit normal n, then the traction vector t is defined as: ∆F t = lim (3.1) ∆S→0 ∆S ∆F n ∆F ∆ S ∆ S n Figure 3.1: Sketch illustrating traction and stress. • The right half of Fig. 3.1 illustrates the concept of an (internal) stress t which represents the traction exerted by one half of the fluid volume onto the other half across a ficticious cut (along a plane with outer unit normal n) through the volume. 3.2 The stress tensor • The stress vector t depends on the spatial position in the body and on the orientation of the plane (characterised by its outer unit normal n) along which the volume of fluid is cut: ti = τij nj , (3.2) where τij = τji is the symmetric stress tensor. • On an infinitesimal block of fluid whose faces are parallel to the axes, the component τij of the stress tensor represents the traction component in the positive i-direction on the face xj = const. whose outer normal points in the positive j-direction (see Fig. 3.2). 6 MATH35001 Viscous Fluid Flow: Stress, Cauchy’s equation and the Navier-Stokes equations 7 x3 x3 τ33 τ22 τ τ11 12 τ21 τ τ 13 23 τ τ 32τ 31 τ 31 32 τ τ τ 23 13 τ21 τ τ τ 11 12 22 33 x1 x2 x1 x2 Figure 3.2: Sketch illustrating the components of the stress tensor. -
Model Comparison of DBD-PA-Induced Body Force in Quiescent Air and Separated Flow Over NACA0015
Model comparison of DBD-PA-induced body force in quiescent air and separated flow over NACA0015 Di Chen, Kengo Asada, Satoshi Sekimoto, Kozo Fujii Tokyo University of Science, Katsushika, Tokyo 125-8585, Japan Hiroyuki Nishida Tokyo University of Agriculture and Technology, Koganei, Tokyo 184-8588, Japan Numerical simulations of plasma flows induced by dielectric barrier discharge plasma actuators (DBD-PA) are conducted with two different body-force models: Suzen-Huang (S- H) model and drift-diffusion (D-D) model. The induced flow generated in quiescent air over a flat plate in continuous actuation and the PA-based flow control effect with burst actuation in separated flow over NACA0015 are studied. In the comparative study, the body-force field and the induced velocity field are firstly investigated in the quiescent field to see the spatial difference and the temporal difference in a single discharge cycle. The D-D body force is computed with flush-mounted and bulge configuration of the exposed electrode, which is operated at the peak-to-peak AC voltage of 7kV and 10kV. The D-D models generate momentarily higher body force in the positive-going phase of the AC power, but activate smaller flow region than the S-H model with Dc = 0.0117, which is given by the experiment beforehand at 7kV.[21] The local induced velocity of the D-D bulge case at 7kV measured in the downstream flow has the best agreement with the experimental result.[36] The maximum wall-parallel induced velocity in the S-H case with Dc = 0.0117 is consistent with that in the experiment, however, the local induced velocity is relatively high with different flow structure. -
Dynamic Meteorology - Introduction
Dynamic Meteorology - Introduction Atmospheric dynamics – the study of atmospheric motions that are associated with weather and climate We will consider the atmosphere to be a continuous fluid medium, or continuum. Each “point” in the atmosphere will be made up of a large number of molecules, with certain properties. These properties are assumed to be continuous functions of position and time. The basic laws of thermodynamics and fluid mechanics can be expressed in terms of partial differential equations, with space and time as independent variables and the atmospheric properties as dependent variables. Physical Dimensions and Units Dimensional homogeneity – all terms in the equations that describe the atmosphere must have the same physical dimensions (units) The four base units we will use are: From these we will also use the following derived units: Fundamental Forces Newton’s Second Law: F=ma In atmospheric science it is typical to consider the force per unit mass acting on the atmosphere: Force = a mass In order to understand atmospheric motion (accelerations) we need to know what forces act on the atmosphere. € What are the fundamental forces of interest in atmospheric science? Body (or volume) force – a force that acts on the center of mass of a fluid parcel Surface force – a force that acts across the boundary separating a fluid parcel from its surroundings. The magnitude of surface forces are independent of the mass of the parcel. What are examples of body and surface forces? Pressure Gradient Force Example: Real-time weather map The force exerted on the left face of this air parcel due to pressure is: pA = pδyδz The force exerted on the right face of this air parcel due to pressure is: € % ∂p ( −(p + δp)δyδz = −' p + δx*δ yδz & ∂x ) The net force exerted by pressure on this air parcel is the sum of these forces and is equal to: € ∂p − δxδyδz ∂x By dividing by the mass of the air parcel (ρδxδyδz) we get the force per unit mass due to changes in pressure (i.e. -
Introduction to Atmospheric Dynamics Chapter 1
Introduction to Atmospheric Dynamics Chapter 1 Paul A. Ullrich [email protected] How to Read These Slides Defnition: A defnition is an explanation or outline for relevant jargon or terms. Concept: An idea that draws a connection between subjects or provides an answer for a question. Question: What is something that motivates delving into this topic? Paul Ullrich The Equations of Atmospheric Dynamics March 2014 Part 1: Forces in the Atmosphere Radius of the Earth 6371.22 km Atmosphere Depth 100 km Troposphere Depth 10 km Mountain Height 8.8 km Paul Ullrich The Equations of Atmospheric Dynamics March 2014 Question: How do we understand the dynamics of the atmosphere? Answer: The principles of atmospheric dynamics are drawn from basic physical principles. Paul Ullrich The Equations of Atmospheric Dynamics March 2014 Question: What are the basic physical principles that govern the atmosphere? Newton’s Second Law: The change in momentum of an object is equal to the sum of forces acting on that object. d(mv) = F dt i allXi Conservation of Momentum: With no external forces momentum must be conserved. Paul Ullrich The Equations of Atmospheric Dynamics March 2014 Basic Principles of Physics dx Defnition: Velocity is the change of u = position with respect to time dt du Defnition: Acceleration is the change a = of velocity with respect to time dt Hence, for an object of constant mass: d(mu) du 1 = m = ma Newton’s a = F dt dt Second Law m i allXi Paul Ullrich The Equations of Atmospheric Dynamics March 2014 Basic Principles of Physics l How do these forces induce acceleration? l We assume the existence of an idealized “parcel” of fuid. -
Lecture 18: Planar Kinetics of a Rigid Body
ME 230 Kinematics and Dynamics Wei-Chih Wang Department of Mechanical Engineering University of Washington Planar kinetics of a rigid body: Force and acceleration Chapter 17 Chapter objectives • Introduce the methods used to determine the mass moment of inertia of a body • To develop the planar kinetic equations of motion for a symmetric rigid body • To discuss applications of these equations to bodies undergoing translation, rotation about fixed axis, and general plane motion W. Wang 2 Lecture 18 • Planar kinetics of a rigid body: Force and acceleration Equations of Motion: Rotation about a Fixed Axis Equations of Motion: General Plane Motion - 17.4-17.5 W. Wang 3 Material covered • Planar kinetics of a rigid body : Force and acceleration Equations of motion 1) Rotation about a fixed axis 2) General plane motion …Next lecture…Start Chapter 18 W. Wang 4 Today’s Objectives Students should be able to: 1. Analyze the planar kinetics of a rigid body undergoing rotational motion 2. Analyze the planar kinetics of a rigid body undergoing general plane motion W. Wang 5 Applications (17.4) The crank on the oil-pump rig undergoes rotation about a fixed axis, caused by the driving torque M from a motor. As the crank turns, a dynamic reaction is produced at the pin. This reaction is a function of angular velocity, angular acceleration, and the orientation of the crank. If the motor exerts a constant torque M on Pin at the center of rotation. the crank, does the crank turn at a constant angular velocity? Is this desirable for such a machine? W. -
Ch.9. Constitutive Equations in Fluids
CH.9. CONSTITUTIVE EQUATIONS IN FLUIDS Multimedia Course on Continuum Mechanics Overview Introduction Fluid Mechanics Lecture 1 What is a Fluid? Pressure and Pascal´s Law Lecture 3 Constitutive Equations in Fluids Lecture 2 Fluid Models Newtonian Fluids Constitutive Equations of Newtonian Fluids Lecture 4 Relationship between Thermodynamic and Mean Pressures Components of the Constitutive Equation Lecture 5 Stress, Dissipative and Recoverable Power Dissipative and Recoverable Powers Lecture 6 Thermodynamic Considerations Limitations in the Viscosity Values 2 9.1 Introduction Ch.9. Constitutive Equations in Fluids 3 What is a fluid? Fluids can be classified into: Ideal (inviscid) fluids: Also named perfect fluid. Only resists normal, compressive stresses (pressure). No resistance is encountered as the fluid moves. Real (viscous) fluids: Viscous in nature and can be subjected to low levels of shear stress. Certain amount of resistance is always offered by these fluids as they move. 5 9.2 Pressure and Pascal’s Law Ch.9. Constitutive Equations in Fluids 6 Pascal´s Law Pascal’s Law: In a confined fluid at rest, pressure acts equally in all directions at a given point. 7 Consequences of Pascal´s Law In fluid at rest: there are no shear stresses only normal forces due to pressure are present. The stress in a fluid at rest is isotropic and must be of the form: σ = − p01 σδij =−∈p0 ij ij,{} 1, 2, 3 Where p 0 is the hydrostatic pressure. 8 Pressure Concepts Hydrostatic pressure, p 0 : normal compressive stress exerted on a fluid in equilibrium. Mean pressure, p : minus the mean stress.