Chapter 4 Central Forces
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A Physical Constants1
A Physical Constants1 Constants in Mechanics −11 3 −1 −2 Gravitational constant G =6.672 59(85) × 10 m kg s (1996) −11 3 −1 −2 =6.673(10) × 10 m kg s (2002) −2 Gravitational acceleration g =9.806 65 m s 30 Solar mass M =1.988 92(25) × 10 kg 8 Solar equatorial radius R =6.96 × 10 m 24 Earth mass M⊕ =5.973 70(76) × 10 kg 6 Earth equatorial radius R⊕ =6.378 140 × 10 m 22 Moon mass M =7.36 () × 10 kg 6 Moon radius R =1.738 × 10 m 9 Distance of Earth from Sun Rmax =0.152 1 × 10 m 9 Rmin =0.147 1 × 10 m 9 Rmean =0.149 6 × 10 m 8 Distance of Moon from Earth Rmean =0.380 × 10 m 7 Period of Earth w.r.t. Sun T⊕ = 365.25 d = 3.16 × 10 s 6 Period of Moon w.r.t. Earth T =27.3d=2.36 × 10 s 1 From Particle Data Group, American Institute of Physics 2002 http://pdg.lbl.gov/2002/contents http://physics.nist.gov/constants 326 A Physical Constants Constants in Electromagnetism def Velocity of light c =. 299, 792, 458 ms−1 def. −7 −2 Vacuum permeability μ0 =4π × 10 NA =12.566 370 614 ...× 10−7 NA−2 1 × −12 −1 Vacuum dielectric constant ε0 = 2 =8.854 187 817 ... 10 Fm μ0c Elementary charge e =1.602 177 33 (49) × 10−19 C e2 =1.439 × 10−9 eV m = 2.305 × 10−28 Jm 4πε0 Constants in Thermodynamics −23 −1 Boltzmann constant kB =1.380 650 3 (24) × 10 JK =8.617 342 (15) × 105 eV K−1 23 −1 Avogadro number NA =6.022 136 7(36) × 10 mole Derived quantities : Gas constant R = NLkB Particle number N,molenumbernN= NLn Constants in Quantum Mechanics Planck’s constant h =6.626 068 76 (52) × 10−34 Js h = =1.054 571 596 (82) × 10−34 Js 2π =6.582 118 89 (26) × 10−16 eV s 2 4πε0 -
Particle Nature of Matter
Solved Problems on the Particle Nature of Matter Charles Asman, Adam Monahan and Malcolm McMillan Department of Physics and Astronomy University of British Columbia, Vancouver, British Columbia, Canada Fall 1999; revised 2011 by Malcolm McMillan Given here are solutions to 5 problems on the particle nature of matter. The solutions were used as a learning-tool for students in the introductory undergraduate course Physics 200 Relativity and Quanta given by Malcolm McMillan at UBC during the 1998 and 1999 Winter Sessions. The solutions were prepared in collaboration with Charles Asman and Adam Monaham who were graduate students in the Department of Physics at the time. The problems are from Chapter 3 The Particle Nature of Matter of the course text Modern Physics by Raymond A. Serway, Clement J. Moses and Curt A. Moyer, Saunders College Publishing, 2nd ed., (1997). Coulomb's Constant and the Elementary Charge When solving numerical problems on the particle nature of matter it is useful to note that the product of Coulomb's constant k = 8:9876 × 109 m2= C2 (1) and the square of the elementary charge e = 1:6022 × 10−19 C (2) is ke2 = 1:4400 eV nm = 1:4400 keV pm = 1:4400 MeV fm (3) where eV = 1:6022 × 10−19 J (4) Breakdown of the Rutherford Scattering Formula: Radius of a Nucleus Problem 3.9, page 39 It is observed that α particles with kinetic energies of 13.9 MeV or higher, incident on copper foils, do not obey Rutherford's (sin φ/2)−4 scattering formula. • Use this observation to estimate the radius of the nucleus of a copper atom. -
Generalisations of the Laplace-Runge-Lenz Vector
Journal of Nonlinear Mathematical Physics Volume 10, Number 3 (2003), 340–423 Review Article Generalisations of the Laplace–Runge–Lenz Vector 1 2 3 1 4 P G L LEACH † † † and G P FLESSAS † † 1 † GEODYSYC, School of Sciences, University of the Aegean, Karlovassi 83 200, Greece 2 † Department of Mathematics, University of the Aegean, Karlovassi 83 200, Greece 3 † Permanent address: School of Mathematical and Statistical Sciences, University of Natal, Durban 4041, Republic of South Africa 4 † Department of Information and Communication Systems Engineering, University of the Aegean, Karlovassi 83 200, Greece Received October 17, 2002; Revised January 22, 2003; Accepted January 27, 2003 Abstract The characteristic feature of the Kepler Problem is the existence of the so-called Laplace–Runge–Lenz vector which enables a very simple discussion of the properties of the orbit for the problem. It is found that there are many classes of problems, some closely related to the Kepler Problem and others somewhat remote, which share the possession of a conserved vector which plays a significant rˆole in the analysis of these problems. Contents arXiv:math-ph/0403028v1 15 Mar 2004 1 Introduction 341 2 Motions with conservation of the angular momentum vector 346 2.1 The central force problem r¨ + fr =0 .....................346 2.1.1 The conservation of the angular momentum vector, the Kepler problemandKepler’sthreelaws . .346 2.1.2 The model equation r¨ + fr =0.....................350 2.2 Algebraic properties of the first integrals of the Kepler problem . 355 2.3 Extension of the model equation to nonautonomous systems.........356 Copyright c 2003 by P G L Leach and G P Flessas Generalisations of the Laplace–Runge–Lenz Vector 341 3 Conservation of the direction of angular momentum only 360 3.1 Vector conservation laws for the equation of motion r¨ + grˆ + hθˆ = 0 . -
Kepler's Laws of Planetary Motion
Kepler's laws of planetary motion In astronomy, Kepler's laws of planetary motion are three scientific laws describing the motion ofplanets around the Sun. 1. The orbit of a planet is an ellipse with the Sun at one of the twofoci . 2. A line segment joining a planet and the Sun sweeps out equal areas during equal intervals of time.[1] 3. The square of the orbital period of a planet is directly proportional to the cube of the semi-major axis of its orbit. Most planetary orbits are nearly circular, and careful observation and calculation are required in order to establish that they are not perfectly circular. Calculations of the orbit of Mars[2] indicated an elliptical orbit. From this, Johannes Kepler inferred that other bodies in the Solar System, including those farther away from the Sun, also have elliptical orbits. Kepler's work (published between 1609 and 1619) improved the heliocentric theory of Nicolaus Copernicus, explaining how the planets' speeds varied, and using elliptical orbits rather than circular orbits withepicycles .[3] Figure 1: Illustration of Kepler's three laws with two planetary orbits. Isaac Newton showed in 1687 that relationships like Kepler's would apply in the 1. The orbits are ellipses, with focal Solar System to a good approximation, as a consequence of his own laws of motion points F1 and F2 for the first planet and law of universal gravitation. and F1 and F3 for the second planet. The Sun is placed in focal pointF 1. 2. The two shaded sectors A1 and A2 Contents have the same surface area and the time for planet 1 to cover segmentA 1 Comparison to Copernicus is equal to the time to cover segment A . -
A Historical Discussion of Angular Momentum and Its Euler Equation
A Historical Discussion of Angular Momentum and its Euler Equation Amelia Carolina Sparavigna1 1Department of Applied Science and Technology, Politecnico di Torino, Italy Abstract: We propose a discussion of angular momentum and its Euler equation, with the aim of giving a short outline of their history. This outline can be useful for teaching purposes too, to amend some problems that students can have in learning this important physical quantity. Keywords: History of Physics, History of Science, Physics Classroom, Euler’s Laws 1. Introduction of his Principia: “Projectiles persevere in their motions, When we are teaching the laws concerning angular so far as they are retarded by the resistance of the air, momentum to the students of a physics classroom, we or impelled downwards by the force of the gravity. A are usually proposing them as the angular version of top, whose parts, by their cohesion, are perpetually Newton’s Laws, in particular when we are discussing drawn aside from rectilinear motions, does not cease its the rotational motion. To illustrate it we need several rotation otherwise than it is retarded by the air”. He concepts and physics quantities: angular velocity and also linked spinning tops and planets, telling that the acceleration, cross product of vectors, torques and “greater bodies of the planets and comets, meeting with moments of inertia. Therefore, the discussion of less resistance in more free spaces, preserve their angular momentum is rather complex, and requiring a motions both progressive and circular for a much large number of examples in order to have the student longer time” [2]. -
Physics Formulas List
Physics Formulas List Home Physics 95 Physics Formulas 23 Listen Physics Formulas List Learning physics is all about applying concepts to solve problems. This article provides a comprehensive physics formulas list, that will act as a ready reference, when you are solving physics problems. You can even use this list, for a quick revision before an exam. Physics is the most fundamental of all sciences. It is also one of the toughest sciences to master. Learning physics is basically studying the fundamental laws that govern our universe. I would say that there is a lot more to ascertain than just remember and mug up the physics formulas. Try to understand what a formula says and means, and what physical relation it expounds. If you understand the physical concepts underlying those formulas, deriving them or remembering them is easy. This Buzzle article lists some physics formulas that you would need in solving basic physics problems. Physics Formulas Mechanics Friction Moment of Inertia Newtonian Gravity Projectile Motion Simple Pendulum Electricity Thermodynamics Electromagnetism Optics Quantum Physics Derive all these formulas once, before you start using them. Study physics and look at it as an opportunity to appreciate the underlying beauty of nature, expressed through natural laws. Physics help is provided here in the form of ready to use formulas. Physics has a reputation for being difficult and to some extent that's http://www.buzzle.com/articles/physics-formulas-list.html[1/10/2014 10:58:12 AM] Physics Formulas List true, due to the mathematics involved. If you don't wish to think on your own and apply basic physics principles, solving physics problems is always going to be tough. -
Runge-Lenz Method for the Energy Level of Hydrogen Atom Masatsugu Sei Suzuki Department of Physics, SUNY at Binghamton (Date: January 06, 2015)
Runge-Lenz method for the energy level of hydrogen atom Masatsugu Sei Suzuki Department of Physics, SUNY at Binghamton (Date: January 06, 2015) Runge-Lentz (or Laplace-Runge-Lentz) vector In classical mechanics, the Runge–Lenz vector (or simply the RL vector) is a vector used chiefly to describe the shape and orientation of the orbit of one astronomical body around another, such as a planet revolving around a star. For two bodies interacting by Newtonian gravity, the LRL vector is a constant of motion, meaning that it is the same no matter where it is calculated on the orbit; equivalently, the LRL vector is said to be conserved. More generally, the RL vector is conserved in all problems in which two bodies interact by a central force that varies as the inverse square of the distance between them; such problems are called Kepler problems. The hydrogen atom is a Kepler problem, since it comprises two charged particles interacting by Coulomb's law of electrostatics, another inverse square central force. The RL vector was essential in the first quantum mechanical derivation of the spectrum of the hydrogen atom, before the development of the Schrödinger equation. However, this approach is rarely used today. http://en.wikipedia.org/wiki/Laplace%E2%80%93Runge%E2%80%93Lenz_vector Wolfgang Pauli in 1926 used the matrix mechanics of Heisenberg to give the first derivation of the energy levels of hydrogen and their degeneracies. Pauli's derivation is based on the Runge- Lenz vector multiplied by the particle mass. [W. Pauli, Z. Physik 36, 336 (1926).] 1. -
Classical Mechanics (MP350)
MP350 Classical Mechanics Jon-Ivar Skullerud with modifications by Brian Dolan December 11, 2020 1 Contents 1 Introduction 5 1.1 Physics is where the action is . .5 1.2 Overview . .6 2 Lagrangian mechanics 8 2.1 From Newton II to the Lagrangian . .8 2.2 The principle of least action . .8 2.2.1 Hamilton's principle . 11 2.3 The Euler{Lagrange equations . 12 2.4 Generalised coordinates . 15 2.4.1 The shortest path between two points (optional) . 20 2.4.2 Polar and spherical coordinates . 21 2.5 Lagrange multipliers [Optional] ........................ 24 2.5.1 Constraints . 24 2.6 Canonical momenta and conservation laws . 29 2.6.1 Angular momentum . 30 2.7 Energy conservation: the hamiltonian . 32 2.7.1 When is H conserved? . 33 2.7.2 The Energy and H .......................... 34 2.8 Lagrangian mechanics | summary sheet . 37 3 Hamiltonian dynamics 39 3.1 Hamilton's equations of motion . 40 3.2 Cyclic coordinates and effective potential . 42 3.3 Hamilton's equations from a variational principle . 44 3.4 Phase space [Optional] ............................ 45 3.5 Liouville's theorem [Optional] ......................... 48 2 3.6 Poisson brackets . 50 3.6.1 Properties of Poisson brackets . 50 3.6.2 Poisson brackets and conservation laws . 52 3.6.3 The Jacobi identity and Poisson's theorem . 53 3.7 Noethers theorem . 54 3.8 Hamiltonian dynamics | summary sheet . 57 4 Central forces 59 4.1 One-body reduction, reduced mass . 59 4.2 Angular momentum and Kepler's second law . 61 4.3 Effective potential and classification of orbits . -
Kepler's Law; Areal Velocity Is Constant: R
Harvard Physics Department - NASA Physics Lies Newtonian Solution of the Interplanetary Positioning System around the Sun Real time delays ΔΓ = 16πGM/c³ [1 + (v°/v*)] ² and Universal Constant Γ0 =16πGM/C³ = 247.597μs By Professor Joe Nahhas 1977 [email protected] This is me Joe Nahhas October 2009 showing my October 1979 picture stapled next to physics notable on my 1979 thermo book whispering and the time is now. Abstract: In 1970's NASA dropped a repeater on planet mars which is an instrument that sends a signal back to transmitter immediately after it receives the signal. Harvard DR Shapiro was with NASA on this adventure and after analysis of the returned signal Harvard and NASA made a claim that there was 250 μ s Space - time travel delays that Einstein's theory and Harvard professors along with NASA can account for 247 μ s providing the experimental proofs of relativity theory. The answer to this nothing answer is: there is a time delay due to orbital motion v* and spin motion v° that the transmitted signal experience due to Earth - Mars motions and due to Earth - Mars spins and it is equal to 250 μ s; however, this time delay is and can be derived from Newton's - Kepler's equations that gives 250 μ s and has nothing to do with relativity and insignificant self graded # 1 Harvard nothing physics department and silly NASA. A Round trip interplanetary telecommunications time delays around the moving sun have nothing to do with space-time confusion of physics of relativity theory and are derived from three dimensional time-dependent Newton - Kepler's equations solution. -
What Is a Tensor ?
What is a tensor ? Johann Colombano-Rut February 2016 v3.2 01/05/2020 This is the print version of the post www.naturelovesmath.com Cliquer ici pour le pdf en francais The (foolish) purpose of this post is to tackle the concept of tensor, while trying to keep it accessible to the widest audience possible. For the layman (or specialist from another field of study) who just wants to know what this is about without the rigidity and complexity of reading an indecipherable math handbook, for the student who already had a course on tensor calculus but can’t figure out some of the "obvious" stuff the teacher didn’t linger on, and finally for any math teacher or expert looking for a fresh eye on the subject (meaning not the handbook type) maybe to help describe it and teach it to his own audience. It doesn’t mean there won’t be any formalism though, it will just be stripped down to the bare minimum while trying not to take too big of a shortcut when needed. So, you will find a lot of visual representations along this post, that I hope will assist and guide you to understand each step, but keep in mind that visual aids are just that, they should not be the basis for understanding, only afterthoughts and guides. A few sections are a little heavy on technical terms and symbols, that’s because they are very important (so, to the layman : just get over it, tensors are not for the faint of heart.). -
1 Survey of Elementary Principles
1 Survey of elementary principles Some history: 1600: Galileo Galilei 1564 – 1642 cf. section 7.0 ∼ Johannes Kepler 1571 – 1630 cf. section 3.7 1700: IsaacNewton 1643–1727 cf. section 1.1 ∼ 1750–1800: LeonhardEuler 1707–1783 cf. section 1.4 ∼ JeanLeRondd’Alembert 1717–1783 cf. section 1.4 Joseph-LouisLagrange 1736–1813 cf. section 1.4, 2.3 1850: CarlGustavJacobJacobi 1804–1851 cf. section 10.1 ∼ William Rowan Hamilton 1805 – 1865 cf. section 2.1 Joseph Liouville 1809 – 1882 cf. section 9.9 1900: Albert Einstein 1879 – 1955 cf. section 7.1 ∼ Emmy Amalie Noether 1882 – 1935 cf. section 8.2 1950: Vladimir Igorevich Arnold 1937 – 2010 cf. section 11.2 ≥ Alexandre Aleksandrovich Kirillov 1936 – BertramKostant 1928– Jean-MarieSouriau 1922–2012 JerroldEldonMarsden 1942–2010 Alan David Weinstein 1943 – FYGB08 – HT14 1 2014-11-24 1.1 Mechanics of a particle 1.1 Concepts: space, time kinematics, dynamics, statics coordinate system, reference frame, inertial frame, Galilean frame position, velocity, acceleration mass point, point mass inertial mass, gravitational mass, rest mass momentum, angular momentum force, torque, force field work, kinetic energy, conservative force, friction simply connected region, curl-free field potential energy, potential, total energy conservation law, conserved quantity, conserved charge Results: Newton’s second law conservation of momentum conservation of angular momentum conservation of total energy Formulas: (1.3) F~ = ~p˙ (1.12) W (P)= F~ d~s 12 P · (1.16) F~ (~r)= ~R V (~r) −∇ Elementary fact: Physics is independent of the choice of coordinate system. Warnings: j Do not mix up the notions ‘frame’ and ‘coordinate system’. -
Arxiv:1807.10685V1 [Physics.Gen-Ph] 25 Jul 2018 Hamilton (1834), Liouville (1836), Jacobi (1843), and Poincar´E(1889) [1] and Xia (1992) [2]
Kepler's third law of n-body periodic orbits in a Newtonian gravitation field Bohua Sun1 1Cape Peninsula University of Technology, Cape Town, South Africa email:[email protected] This study considers the periodic orbital period of an n-body system from the perspective of dimension analysis. According to characteristics of the n-body system with point masses (m1; m2; :::; mn), the gravitational field parameter, α ∼ Gmimj , the n-body system reduction mass Mn, and the area, An, of the periodic orbit are selected as the basic parameters, while the period, Tn, and the system energy, jEnj, are expressed as the three basic parameters. Using the Bucking- ham π theorem, We obtained an epic result, by working with a reduced gravitation parameter αn, 3=2 p then predicting a dimensionless relation TnjEnj = const × αn µn (µn is reduced mass). The const= pπ is derived by matching with the 2-body Kepler's third law, and then a surprisingly simple 2 relation for Kepler's third law of an n-body system is derived by invoking a symmetry constraint Pn Pn 3 1=2 3=2 π i=1 j=i+1(mimj ) inspired from Newton's gravitational law: TnjEnj = p G Pn . This for- 2 k=1 mk mulae is, of course, consistent with the Kepler's third law of 2-body system, but yields a non-trivial 3 3 3 1=2 3=2 π h (m1m2) +(m1m3) +(m2m3) i prediction of the Kepler's third law of 3-body: T3jE3j = p G .A 2 m1+m2+m3 numerical validation and comparison study was conducted.