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Glossary Physics (I-Introduction)
1 Glossary Physics (I-introduction) - Efficiency: The percent of the work put into a machine that is converted into useful work output; = work done / energy used [-]. = eta In machines: The work output of any machine cannot exceed the work input (<=100%); in an ideal machine, where no energy is transformed into heat: work(input) = work(output), =100%. Energy: The property of a system that enables it to do work. Conservation o. E.: Energy cannot be created or destroyed; it may be transformed from one form into another, but the total amount of energy never changes. Equilibrium: The state of an object when not acted upon by a net force or net torque; an object in equilibrium may be at rest or moving at uniform velocity - not accelerating. Mechanical E.: The state of an object or system of objects for which any impressed forces cancels to zero and no acceleration occurs. Dynamic E.: Object is moving without experiencing acceleration. Static E.: Object is at rest.F Force: The influence that can cause an object to be accelerated or retarded; is always in the direction of the net force, hence a vector quantity; the four elementary forces are: Electromagnetic F.: Is an attraction or repulsion G, gravit. const.6.672E-11[Nm2/kg2] between electric charges: d, distance [m] 2 2 2 2 F = 1/(40) (q1q2/d ) [(CC/m )(Nm /C )] = [N] m,M, mass [kg] Gravitational F.: Is a mutual attraction between all masses: q, charge [As] [C] 2 2 2 2 F = GmM/d [Nm /kg kg 1/m ] = [N] 0, dielectric constant Strong F.: (nuclear force) Acts within the nuclei of atoms: 8.854E-12 [C2/Nm2] [F/m] 2 2 2 2 2 F = 1/(40) (e /d ) [(CC/m )(Nm /C )] = [N] , 3.14 [-] Weak F.: Manifests itself in special reactions among elementary e, 1.60210 E-19 [As] [C] particles, such as the reaction that occur in radioactive decay. -
Classical Mechanics
Classical Mechanics Hyoungsoon Choi Spring, 2014 Contents 1 Introduction4 1.1 Kinematics and Kinetics . .5 1.2 Kinematics: Watching Wallace and Gromit ............6 1.3 Inertia and Inertial Frame . .8 2 Newton's Laws of Motion 10 2.1 The First Law: The Law of Inertia . 10 2.2 The Second Law: The Equation of Motion . 11 2.3 The Third Law: The Law of Action and Reaction . 12 3 Laws of Conservation 14 3.1 Conservation of Momentum . 14 3.2 Conservation of Angular Momentum . 15 3.3 Conservation of Energy . 17 3.3.1 Kinetic energy . 17 3.3.2 Potential energy . 18 3.3.3 Mechanical energy conservation . 19 4 Solving Equation of Motions 20 4.1 Force-Free Motion . 21 4.2 Constant Force Motion . 22 4.2.1 Constant force motion in one dimension . 22 4.2.2 Constant force motion in two dimensions . 23 4.3 Varying Force Motion . 25 4.3.1 Drag force . 25 4.3.2 Harmonic oscillator . 29 5 Lagrangian Mechanics 30 5.1 Configuration Space . 30 5.2 Lagrangian Equations of Motion . 32 5.3 Generalized Coordinates . 34 5.4 Lagrangian Mechanics . 36 5.5 D'Alembert's Principle . 37 5.6 Conjugate Variables . 39 1 CONTENTS 2 6 Hamiltonian Mechanics 40 6.1 Legendre Transformation: From Lagrangian to Hamiltonian . 40 6.2 Hamilton's Equations . 41 6.3 Configuration Space and Phase Space . 43 6.4 Hamiltonian and Energy . 45 7 Central Force Motion 47 7.1 Conservation Laws in Central Force Field . 47 7.2 The Path Equation . -
THE EARTH's GRAVITY OUTLINE the Earth's Gravitational Field
GEOPHYSICS (08/430/0012) THE EARTH'S GRAVITY OUTLINE The Earth's gravitational field 2 Newton's law of gravitation: Fgrav = GMm=r ; Gravitational field = gravitational acceleration g; gravitational potential, equipotential surfaces. g for a non–rotating spherically symmetric Earth; Effects of rotation and ellipticity – variation with latitude, the reference ellipsoid and International Gravity Formula; Effects of elevation and topography, intervening rock, density inhomogeneities, tides. The geoid: equipotential mean–sea–level surface on which g = IGF value. Gravity surveys Measurement: gravity units, gravimeters, survey procedures; the geoid; satellite altimetry. Gravity corrections – latitude, elevation, Bouguer, terrain, drift; Interpretation of gravity anomalies: regional–residual separation; regional variations and deep (crust, mantle) structure; local variations and shallow density anomalies; Examples of Bouguer gravity anomalies. Isostasy Mechanism: level of compensation; Pratt and Airy models; mountain roots; Isostasy and free–air gravity, examples of isostatic balance and isostatic anomalies. Background reading: Fowler §5.1–5.6; Lowrie §2.2–2.6; Kearey & Vine §2.11. GEOPHYSICS (08/430/0012) THE EARTH'S GRAVITY FIELD Newton's law of gravitation is: ¯ GMm F = r2 11 2 2 1 3 2 where the Gravitational Constant G = 6:673 10− Nm kg− (kg− m s− ). ¢ The field strength of the Earth's gravitational field is defined as the gravitational force acting on unit mass. From Newton's third¯ law of mechanics, F = ma, it follows that gravitational force per unit mass = gravitational acceleration g. g is approximately 9:8m/s2 at the surface of the Earth. A related concept is gravitational potential: the gravitational potential V at a point P is the work done against gravity in ¯ P bringing unit mass from infinity to P. -
Force and Motion
Force and motion Science teaching unit Disclaimer The Department for Children, Schools and Families wishes to make it clear that the Department and its agents accept no responsibility for the actual content of any materials suggested as information sources in this publication, whether these are in the form of printed publications or on a website. In these materials icons, logos, software products and websites are used for contextual and practical reasons. Their use should not be interpreted as an endorsement of particular companies or their products. The websites referred to in these materials existed at the time of going to print. Please check all website references carefully to see if they have changed and substitute other references where appropriate. Force and motion First published in 2008 Ref: 00094-2008DVD-EN The National Strategies | Secondary 1 Force and motion Contents Force and motion 3 Lift-off activity: Remember forces? 7 Lesson 1: Identifying and representing forces 12 Lesson 2: Representing motion – distance/time/speed 18 Lesson 3: Representing motion – speed and acceleration 27 Lesson 4: Linking force and motion 49 Lesson 5: Investigating motion 66 © Crown copyright 2008 00094-2008DVD-EN The National Strategies | Secondary 3 Force and motion Force and motion Background This teaching sequence bridges from Key Stage 3 to Key Stage 4. It links to the Secondary National Strategy Framework for science yearly learning objectives and provides coverage of parts of the QCA Programme of Study for science. The overall aim of the sequence is for pupils to review and refine their ideas about forces from Key Stage 3, to develop a meaningful understanding of ways of representing motion (graphically and through calculation) and to make the links between different kinds of motion and forces acting. -
Outline of Physical Science
Outline of physical science “Physical Science” redirects here. It is not to be confused • Astronomy – study of celestial objects (such as stars, with Physics. galaxies, planets, moons, asteroids, comets and neb- ulae), the physics, chemistry, and evolution of such Physical science is a branch of natural science that stud- objects, and phenomena that originate outside the atmosphere of Earth, including supernovae explo- ies non-living systems, in contrast to life science. It in turn has many branches, each referred to as a “physical sions, gamma ray bursts, and cosmic microwave background radiation. science”, together called the “physical sciences”. How- ever, the term “physical” creates an unintended, some- • Branches of astronomy what arbitrary distinction, since many branches of physi- cal science also study biological phenomena and branches • Chemistry – studies the composition, structure, of chemistry such as organic chemistry. properties and change of matter.[8][9] In this realm, chemistry deals with such topics as the properties of individual atoms, the manner in which atoms form 1 What is physical science? chemical bonds in the formation of compounds, the interactions of substances through intermolecular forces to give matter its general properties, and the Physical science can be described as all of the following: interactions between substances through chemical reactions to form different substances. • A branch of science (a systematic enterprise that builds and organizes knowledge in the form of • Branches of chemistry testable explanations and predictions about the • universe).[1][2][3] Earth science – all-embracing term referring to the fields of science dealing with planet Earth. Earth • A branch of natural science – natural science science is the study of how the natural environ- is a major branch of science that tries to ex- ment (ecosphere or Earth system) works and how it plain and predict nature’s phenomena, based evolved to its current state. -
Newtonian Mechanics Is Most Straightforward in Its Formulation and Is Based on Newton’S Second Law
CLASSICAL MECHANICS D. A. Garanin September 30, 2015 1 Introduction Mechanics is part of physics studying motion of material bodies or conditions of their equilibrium. The latter is the subject of statics that is important in engineering. General properties of motion of bodies regardless of the source of motion (in particular, the role of constraints) belong to kinematics. Finally, motion caused by forces or interactions is the subject of dynamics, the biggest and most important part of mechanics. Concerning systems studied, mechanics can be divided into mechanics of material points, mechanics of rigid bodies, mechanics of elastic bodies, and mechanics of fluids: hydro- and aerodynamics. At the core of each of these areas of mechanics is the equation of motion, Newton's second law. Mechanics of material points is described by ordinary differential equations (ODE). One can distinguish between mechanics of one or few bodies and mechanics of many-body systems. Mechanics of rigid bodies is also described by ordinary differential equations, including positions and velocities of their centers and the angles defining their orientation. Mechanics of elastic bodies and fluids (that is, mechanics of continuum) is more compli- cated and described by partial differential equation. In many cases mechanics of continuum is coupled to thermodynamics, especially in aerodynamics. The subject of this course are systems described by ODE, including particles and rigid bodies. There are two limitations on classical mechanics. First, speeds of the objects should be much smaller than the speed of light, v c, otherwise it becomes relativistic mechanics. Second, the bodies should have a sufficiently large mass and/or kinetic energy. -
Physical Science Forces and Motion Vocabulary
Physical Science -Forces and Motion Vocabulary 1. scientific method - The way we learn and study the world around us through a process of steps. ( Six Giant Hippos Eat Red & Orange Candy) 2. position – the exact location of an object. 3. direction – the line or course along which something moves. 4. speed – measures how fast an object is moving in a given amount of time. 5. motion – the change in position of an object. 6. constant – remaining steady and unchanged (stays the same.) 7. force – push or pull 8. interaction – the action or influence of people, groups or things on one another. 9. exert – to put forth as strength (exert a force) 10. friction - a force that opposes (goes against) motion. Friction is created when two surfaces rub together. Effects of friction: slowing down or stopping an object, producing heat, or wearing away an object. 11. Newton’s 1 st Law of Motion : an object at rest will stay at rest and an object in motion will stay in motion until a force acts upon it. 12. inertia – the tendency for an object to keep doing what it is doing (resting or moving) 13. mass – the amount of matter (“stuff”) - in an object. 14. weight - the amount of force (pull) that gravity has on an object's mass. Your weight depends on the gravitational pull of your location. 15. gravity – a force that attracts (pulls) all objects to the center of the Earth 16. acceleration – the changes in an object’s motion. This can be speeding up, slowing down or changing direction. -
Thermodynamic Processes: the Limits of Possible
Thermodynamic Processes: The Limits of Possible Thermodynamics put severe restrictions on what processes involving a change of the thermodynamic state of a system (U,V,N,…) are possible. In a quasi-static process system moves from one equilibrium state to another via a series of other equilibrium states . All quasi-static processes fall into two main classes: reversible and irreversible processes . Processes with decreasing total entropy of a thermodynamic system and its environment are prohibited by Postulate II Notes Graphic representation of a single thermodynamic system Phase space of extensive coordinates The fundamental relation S(1) =S(U (1) , X (1) ) of a thermodynamic system defines a hypersurface in the coordinate space S(1) S(1) U(1) U(1) X(1) X(1) S(1) – entropy of system 1 (1) (1) (1) (1) (1) U – energy of system 1 X = V , N 1 , …N m – coordinates of system 1 Notes Graphic representation of a composite thermodynamic system Phase space of extensive coordinates The fundamental relation of a composite thermodynamic system S = S (1) (U (1 ), X (1) ) + S (2) (U-U(1) ,X (2) ) (system 1 and system 2). defines a hyper-surface in the coordinate space of the composite system S(1+2) S(1+2) U (1,2) X = V, N 1, …N m – coordinates U of subsystems (1 and 2) X(1,2) (1,2) S – entropy of a composite system X U – energy of a composite system Notes Irreversible and reversible processes If we change constraints on some of the composite system coordinates, (e.g. -
Designing a Physics Learning Environment: a Holistic Approach
Designing a physics learning environment: A holistic approach David T. Brookes and Yuhfen Lin Department of Physics, Florida International University, 11200 SW 8th St, Miami, 33199 Abstract. Physics students enter our classroom with significant learning experiences and learning goals that are just as important as their prior knowledge. Consequently, they have expectations about how they should be taught. The instructor enters the same classroom and presents the students with materials and assessments that he/she believes reflect his/her learning goals for the students. When students encounter a reformed physics class, there is often a “misalignment” between students’ perceptions, and learning goals the instructor designed for the students. We want to propose that alignment can be achieved in a reformed physics class by taking a holistic view of the classroom. In other words, it is not just about teaching physics, but a problem of social engineering. We will discuss how we applied this social engineering idea on multiple scales (individual students, groups, and the whole class) to achieve alignment between students’ expectations and the instructor’s learning goals. Keywords: Physics education, learning environment, learning goals, attitudes, motivation PACS: 01.40.Fk, 01.40.Ha INTRODUCTION his/her students. 3) We paid careful attention to designing the learning environment to maximize Many Research-Based Instructional Strategies effective communication and interaction between (RBIS) in physics are initially successful when students. implemented by their developers, but other adopters sometimes struggle to achieve the same level of THEORY AND COURSE SETTING success. Firstly, students are resistant to reform [1]. Secondly, when physics instructors try implementing Interacting System Model one or more RBIS, they quickly discover that they do not work as advertised [2]. -
Glossary of Materials Engineering Terminology
Glossary of Materials Engineering Terminology Adapted from: Callister, W. D.; Rethwisch, D. G. Materials Science and Engineering: An Introduction, 8th ed.; John Wiley & Sons, Inc.: Hoboken, NJ, 2010. McCrum, N. G.; Buckley, C. P.; Bucknall, C. B. Principles of Polymer Engineering, 2nd ed.; Oxford University Press: New York, NY, 1997. Brittle fracture: fracture that occurs by rapid crack formation and propagation through the material, without any appreciable deformation prior to failure. Crazing: a common response of plastics to an applied load, typically involving the formation of an opaque banded region within transparent plastic; at the microscale, the craze region is a collection of nanoscale, stress-induced voids and load-bearing fibrils within the material’s structure; craze regions commonly occur at or near a propagating crack in the material. Ductile fracture: a mode of material failure that is accompanied by extensive permanent deformation of the material. Ductility: a measure of a material’s ability to undergo appreciable permanent deformation before fracture; ductile materials (including many metals and plastics) typically display a greater amount of strain or total elongation before fracture compared to non-ductile materials (such as most ceramics). Elastic modulus: a measure of a material’s stiffness; quantified as a ratio of stress to strain prior to the yield point and reported in units of Pascals (Pa); for a material deformed in tension, this is referred to as a Young’s modulus. Engineering strain: the change in gauge length of a specimen in the direction of the applied load divided by its original gauge length; strain is typically unit-less and frequently reported as a percentage. -
Week 11: Chapter 11
The Vector Product There are instances where the product of two Week 11: Chapter 11 vectors is another vector Earlier we saw where the product of two vectors Angular Momentum was a scalar This was called the dot product The vector product of two vectors is also called the cross product The Vector Product and Torque The Vector Product Defined The torque vector lies in a Given two vectors, A and B direction perpendicular to the plane formed by the The vector (cross) product of A and B is position vector and the force vector defined as a third vector, CAB Fr C is read as “A cross B” The torque is the vector (or cross) product of the The magnitude of vector C is AB sin position vector and the is the angle between A and B force vector More About the Vector Product Properties of the Vector Product The quantity AB sin is The vector product is not commutative. The equal to the area of the order in which the vectors are multiplied is parallelogram formed important by A and B To account for order, remember The direction of C is A BBA perpendicular to the plane formed by A and B If A is parallel to B ( = 0o or 180o), then The best way to A B 0 determine this direction is to use the right-hand Therefore A A 0 rule 1 More Properties of the Vector Final Properties of the Vector Product Product If A is perpendicular to B , then ABAB The derivative of the cross product with The vector product obeys the distributive law respect to some variable such as t is ddA dB ABCABAC x ( + ) = x + x AB -
The Influence of Thermodynamic Ideas on Ecological Economics: an Interdisciplinary Critique
Sustainability 2009, 1, 1195-1225; doi:10.3390/su1041195 OPEN ACCESS sustainability ISSN 2071-1050 www.mdpi.com/journal/sustainability Article The Influence of Thermodynamic Ideas on Ecological Economics: An Interdisciplinary Critique Geoffrey P. Hammond 1,2,* and Adrian B. Winnett 1,3 1 Institute for Sustainable Energy & the Environment (I•SEE), University of Bath, Bath, BA2 7AY, UK 2 Department of Mechanical Engineering, University of Bath, Bath, BA2 7AY, UK 3 Department of Economics, University of Bath, Bath, BA2 7AY, UK; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +44-12-2538-6168; Fax: +44-12-2538-6928. Received: 10 October 2009 / Accepted: 24 November 2009 / Published: 1 December 2009 Abstract: The influence of thermodynamics on the emerging transdisciplinary field of ‗ecological economics‘ is critically reviewed from an interdisciplinary perspective. It is viewed through the lens provided by the ‗bioeconomist‘ Nicholas Georgescu-Roegen (1906–1994) and his advocacy of ‗the Entropy Law‘ as a determinant of economic scarcity. It is argued that exergy is a more easily understood thermodynamic property than is entropy to represent irreversibilities in complex systems, and that the behaviour of energy and matter are not equally mirrored by thermodynamic laws. Thermodynamic insights as typically employed in ecological economics are simply analogues or metaphors of reality. They should therefore be empirically tested against the real world. Keywords: thermodynamic analysis; energy; entropy; exergy; ecological economics; environmental economics; exergoeconomics; complexity; natural capital; sustainability Sustainability 2009, 1 1196 ―A theory is the more impressive, the greater the simplicity of its premises is, the more different kinds of things it relates, and the more extended is its area of applicability.