Conservation Laws? the Modern Converse Noether Theorem Vs Pragmatism
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José M. Vega-Guzmán
Jos´eM. Vega-Guzm´an Curriculum Vitae Contact Department of Mathematics Tel: (409) 880-8792 Information College of Arts and Sciences Fax: (409) 880-8794 Lamar University email: [email protected] 200-C Lucas Building URL: https://sites.google.com/site/profjmvg/ Beaumont, TX 77710 Education PhD (Applied Mathematics) 2008{2013 • Arizona State University, Tempe, AZ • Co-Advisors: Sergei K. Suslov and Carlos Castillo-Chavez • Dissertation Title: Solution Methods for Certain Evolution Equations Master in Natural Sciences (Mathematics) 2006{2008 • Arizona State University, Tempe, AZ B.S. (MathEd) 2000{2005 • Universidad de Puerto Rico, Cayey, PR • Advisor: Maria A. Avi~n´o Research Interests Nonlinear Wave Propagation. Quantum Mechanics. Integrability of Nonlinear Evolution Equations. Applications of ODE's and PDE's in the Natural Sciences. Mathematical Modeling. Publications 2017 Vega{Guzm´an,J.M.; Alqahtani, R.; Zhou, Q.; Mahmood, M.F.; Moshokoa, S.P.; Ullah, M.Z.; Biswas, A.; Belic, M. Optical solitons for Lakshmanan-Porsezian-Daniel model with spatio-temporal dispersion using the method of undetermined coefficients. Optik - International Journal for Light and Electron Optics. 144, 115{123. 2017 Wang, G.; Kara, A.H.; Vega{Guzm´an,J.M.; Biswas, A. Group analysis, nonlinear self-adjointness, conser- vation laws and soliton solutions for the mKdV systems. Nonlinear Analysis: Modeling and Control. 22(3), 334{346. 2017 Vega{Guzm´an,J.M.; Ullah, M.Z.; Asma, M.; Zhou, Q.; Biswas, A. Dispersive solitons in magneto-optic waveguides. Superlattices and Microstructures. 103, 161{170. 2017 Vega{Guzm´an,J.M.; Mahmood, M.F.; Zhou, Q.; Triki, H.; Arnous, A.H.; Biswas, A.; Moshokoa, S.P.; Belic, M. -
Introduction to the Modern Calculus of Variations
MA4G6 Lecture Notes Introduction to the Modern Calculus of Variations Filip Rindler Spring Term 2015 Filip Rindler Mathematics Institute University of Warwick Coventry CV4 7AL United Kingdom [email protected] http://www.warwick.ac.uk/filiprindler Copyright ©2015 Filip Rindler. Version 1.1. Preface These lecture notes, written for the MA4G6 Calculus of Variations course at the University of Warwick, intend to give a modern introduction to the Calculus of Variations. I have tried to cover different aspects of the field and to explain how they fit into the “big picture”. This is not an encyclopedic work; many important results are omitted and sometimes I only present a special case of a more general theorem. I have, however, tried to strike a balance between a pure introduction and a text that can be used for later revision of forgotten material. The presentation is based around a few principles: • The presentation is quite “modern” in that I use several techniques which are perhaps not usually found in an introductory text or that have only recently been developed. • For most results, I try to use “reasonable” assumptions, not necessarily minimal ones. • When presented with a choice of how to prove a result, I have usually preferred the (in my opinion) most conceptually clear approach over more “elementary” ones. For example, I use Young measures in many instances, even though this comes at the expense of a higher initial burden of abstract theory. • Wherever possible, I first present an abstract result for general functionals defined on Banach spaces to illustrate the general structure of a certain result. -
On the Ekeland Variational Principle with Applications and Detours
Lectures on The Ekeland Variational Principle with Applications and Detours By D. G. De Figueiredo Tata Institute of Fundamental Research, Bombay 1989 Author D. G. De Figueiredo Departmento de Mathematica Universidade de Brasilia 70.910 – Brasilia-DF BRAZIL c Tata Institute of Fundamental Research, 1989 ISBN 3-540- 51179-2-Springer-Verlag, Berlin, Heidelberg. New York. Tokyo ISBN 0-387- 51179-2-Springer-Verlag, New York. Heidelberg. Berlin. Tokyo No part of this book may be reproduced in any form by print, microfilm or any other means with- out written permission from the Tata Institute of Fundamental Research, Colaba, Bombay 400 005 Printed by INSDOC Regional Centre, Indian Institute of Science Campus, Bangalore 560012 and published by H. Goetze, Springer-Verlag, Heidelberg, West Germany PRINTED IN INDIA Preface Since its appearance in 1972 the variational principle of Ekeland has found many applications in different fields in Analysis. The best refer- ences for those are by Ekeland himself: his survey article [23] and his book with J.-P. Aubin [2]. Not all material presented here appears in those places. Some are scattered around and there lies my motivation in writing these notes. Since they are intended to students I included a lot of related material. Those are the detours. A chapter on Nemyt- skii mappings may sound strange. However I believe it is useful, since their properties so often used are seldom proved. We always say to the students: go and look in Krasnoselskii or Vainberg! I think some of the proofs presented here are more straightforward. There are two chapters on applications to PDE. -
The Original Euler's Calculus-Of-Variations Method: Key
Submitted to EJP 1 Jozef Hanc, [email protected] The original Euler’s calculus-of-variations method: Key to Lagrangian mechanics for beginners Jozef Hanca) Technical University, Vysokoskolska 4, 042 00 Kosice, Slovakia Leonhard Euler's original version of the calculus of variations (1744) used elementary mathematics and was intuitive, geometric, and easily visualized. In 1755 Euler (1707-1783) abandoned his version and adopted instead the more rigorous and formal algebraic method of Lagrange. Lagrange’s elegant technique of variations not only bypassed the need for Euler’s intuitive use of a limit-taking process leading to the Euler-Lagrange equation but also eliminated Euler’s geometrical insight. More recently Euler's method has been resurrected, shown to be rigorous, and applied as one of the direct variational methods important in analysis and in computer solutions of physical processes. In our classrooms, however, the study of advanced mechanics is still dominated by Lagrange's analytic method, which students often apply uncritically using "variational recipes" because they have difficulty understanding it intuitively. The present paper describes an adaptation of Euler's method that restores intuition and geometric visualization. This adaptation can be used as an introductory variational treatment in almost all of undergraduate physics and is especially powerful in modern physics. Finally, we present Euler's method as a natural introduction to computer-executed numerical analysis of boundary value problems and the finite element method. I. INTRODUCTION In his pioneering 1744 work The method of finding plane curves that show some property of maximum and minimum,1 Leonhard Euler introduced a general mathematical procedure or method for the systematic investigation of variational problems. -
Subdifferential Test for Optimality
Subdifferential Test for Optimality Florence JULES and Marc LASSONDE Universit´edes Antilles et de la Guyane 97159 Pointe `aPitre, France E-mail: fl[email protected], [email protected] Abstract. We provide a first-order necessary and sufficient condition for optimality of lower semicontinuous functions on Banach spaces using the concept of subdifferential. From the sufficient condition we derive that any subdifferential operator is monotone absorbing, hence maximal monotone when the function is convex. Keywords: lower semicontinuity, subdifferential, directional derivative, first-order condition, optimality criterion, maximal monotonicity. 2010 Mathematics Subject Classification: 49J52, 49K27, 26D10, 26B25. 1 Introduction First-order sufficient conditions for optimality in terms of derivatives or directional derivatives are well known. Typical such conditions are variants of Minty variational inequalities. Let us quote for example the following simple result (see [3]): Let f be a real-valued function which is continuous on a neighbourhood D centred at a in Rn and differentiable on D \ {a}. Then, f has a local minimum value at a if (x − a) ·∇f(x) > 0 for all x ∈ D \ {a}. For first-order conditions in terms of directional derivatives, we refer to [5]. The main objective of this note is to establish a necessary and sufficient condition for optimality of nonsmooth lower semicontinuous functions on Banach spaces using subdiffer- entials. To this end, we first provide a link between the directional derivative of a function and its dual companion represented by the subdifferential (Theorem 2.1). Then, we prove a sharp version of the mean value inequality for lower semicontinuous function using directional derivative (Lemma 3.1). -
Yesterday, Today, and Forever Hebrews 13:8 a Sermon Preached in Duke University Chapel on August 29, 2010 by the Revd Dr Sam Wells
Yesterday, Today, and Forever Hebrews 13:8 A Sermon preached in Duke University Chapel on August 29, 2010 by the Revd Dr Sam Wells Who are you? This is a question we only get to ask one another in the movies. The convention is for the question to be addressed by a woman to a handsome man just as she’s beginning to realize he isn’t the uncomplicated body-and-soulmate he first seemed to be. Here’s one typical scenario: the war is starting to go badly; the chief of the special unit takes a key officer aside, and sends him on a dangerous mission to infiltrate the enemy forces. This being Hollywood, the officer falls in love with a beautiful woman while in enemy territory. In a moment of passion and mystery, it dawns on her that he’s not like the local men. So her bewitched but mistrusting eyes stare into his, and she says, “Who are you?” Then there’s the science fiction version. In this case the man develops an annoying habit of suddenly, without warning, traveling in time, or turning into a caped superhero. Meanwhile the woman, though drawn to his awesome good looks and sympathetic to his commendable desire to save the universe, yet finds herself taking his unexpected and unusual absences rather personally. So on one of the few occasions she gets to look into his eyes when they’re not undergoing some kind of chemical transformation, she says, with the now-familiar, bewitched-but-mistrusting expression, “Who are you?” “Who are you?” We never ask one another this question for fear of sounding melodramatic, like we’re in a movie. -
The New Adaption Gallery
Introduction In 1991, a group of Heritage Center staff began meeting informally after work to discuss a Heritage Center expansion. This “committee” was formalized in 1992 by Jim Sperry, Superintendent of the State Historical Society of North Dakota, and became known as the Space Planning About Center Expansion (SPACE) committee. The committee consisted of several Historical Society staff and John Hoganson representing the North Dakota Geological Survey. Ultimately, some of the SPACE committee ideas were rejected primarily because of anticipated high cost such as a planetarium, arboretum, and day care center but many of the ideas have become reality in the new Heritage Center expansion. In 2009, the state legislature appropriated $40 million for a $52 million Heritage Center expansion. The State Historical Society of North Dakota Foundation was given the task to raise the difference. On November 23, 2010 groundbreaking for the expansion took place. Planning for three new galleries began in earnest: the Governor’s Gallery (for large, temporary, travelling exhibits), Innovation Gallery: Early Peoples, and Adaptation Gallery: Geologic Time. The Figure 1. Partial Stratigraphic column of North Dakota showing Figure 2. Plate tectonic video. North Dakota's position is indicated by the the age of the Geologic Time Gallery displays. red symbol. JULY 2014 1 Orientation Featured in the Orientation area is an interactive touch table that provides a timeline of geological and evolutionary events in North Dakota from 600 million years ago to the present. Visitors activate the timeline by scrolling to learn how the geology, environment, climate, and life have changed in North Dakota through time. -
The Geology of Cuba: a Brief Cuba: a of the Geology It’S Time—Renew Your GSA Membership and Save 15% and Save Membership GSA Time—Renew Your It’S
It’s Time—Renew Your GSA Membership and Save 15% OCTOBER | VOL. 26, 2016 10 NO. A PUBLICATION OF THE GEOLOGICAL SOCIETY OF AMERICA® The geology of Cuba: A brief overview and synthesis OCTOBER 2016 | VOLUME 26, NUMBER 10 Featured Article GSA TODAY (ISSN 1052-5173 USPS 0456-530) prints news and information for more than 26,000 GSA member readers and subscribing libraries, with 11 monthly issues (March/ April is a combined issue). GSA TODAY is published by The SCIENCE Geological Society of America® Inc. (GSA) with offices at 3300 Penrose Place, Boulder, Colorado, USA, and a mail- 4 The geology of Cuba: A brief overview ing address of P.O. Box 9140, Boulder, CO 80301-9140, USA. and synthesis GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, M.A. Iturralde-Vinent, A. García-Casco, regardless of race, citizenship, gender, sexual orientation, Y. Rojas-Agramonte, J.A. Proenza, J.B. Murphy, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. and R.J. Stern © 2016 The Geological Society of America Inc. All rights Cover: Valle de Viñales, Pinar del Río Province, western reserved. Copyright not claimed on content prepared Cuba. Karstic relief on passive margin Upper Jurassic and wholly by U.S. government employees within the scope of Cretaceous limestones. The world-famous Cuban tobacco is their employment. Individual scientists are hereby granted permission, without fees or request to GSA, to use a single grown in this valley. Photo by Antonio García Casco, 31 July figure, table, and/or brief paragraph of text in subsequent 2014. -
About Symmetries in Physics
LYCEN 9754 December 1997 ABOUT SYMMETRIES IN PHYSICS Dedicated to H. Reeh and R. Stora1 Fran¸cois Gieres Institut de Physique Nucl´eaire de Lyon, IN2P3/CNRS, Universit´eClaude Bernard 43, boulevard du 11 novembre 1918, F - 69622 - Villeurbanne CEDEX Abstract. The goal of this introduction to symmetries is to present some general ideas, to outline the fundamental concepts and results of the subject and to situate a bit the following arXiv:hep-th/9712154v1 16 Dec 1997 lectures of this school. [These notes represent the write-up of a lecture presented at the fifth S´eminaire Rhodanien de Physique “Sur les Sym´etries en Physique” held at Dolomieu (France), 17-21 March 1997. Up to the appendix and the graphics, it is to be published in Symmetries in Physics, F. Gieres, M. Kibler, C. Lucchesi and O. Piguet, eds. (Editions Fronti`eres, 1998).] 1I wish to dedicate these notes to my diploma and Ph.D. supervisors H. Reeh and R. Stora who devoted a major part of their scientific work to the understanding, description and explo- ration of symmetries in physics. Contents 1 Introduction ................................................... .......1 2 Symmetries of geometric objects ...................................2 3 Symmetries of the laws of nature ..................................5 1 Geometric (space-time) symmetries .............................6 2 Internal symmetries .............................................10 3 From global to local symmetries ...............................11 4 Combining geometric and internal symmetries ...............14 -
SMS Unit of Study
SMS Unit of Study Course: Science Teacher(s): Cindy Combs and Sadie Hamm Unit Title: Geologic History of the Earth Unit Length: 8 Days Unit Overview Focus Question: How can rock strata tell the story of Earth’s history? Learning Objective: The student is expected to construct a scientific explanation based on evidence from rock strata for how the geologic time scale is used to organize Earth’s 4.6-billion-year-old history. Standards Set—What standards will I explicitly teach and Summative Assessment—How will I assess my students after explicitly intentionally assess? (Include standard number and complete teaching the standards set? (Describe type of assessment). standard). MS-ESS1.C.1 The History of Planet Earth: The geologic time Ø Presentation of New Species scale interpreted from rock strata provides a way to organize Earth’s history. Analyses of rock strata and the fossil record Ø Presentation of Infomercial or Advertisement provide only relative dates, not an absolute scale. Ø Unit Exam- Multiple Choice, Short Answer, Extended Response MS-ESS1-4 Construct a scientific explanation based on evidence from rock strata for how the geologic time scale is used to organize Earth’s 4.6-billion-year-old history. Time, Space, and Energy Time, space, and energy phenomena can be observed at various scales using models to study systems that are too large or too small. Construct a Scientific Explanation Construct a scientific explanation based on valid and reliable evidence obtained from source (including students' own experiments) and the assumption that theories and laws that describe the natural world operate today as they did in the past and will continue to do so in the future. -
Hebrews 13:8 Jesus Christ the Eternal Unchanging Son Of
Hebrews 13:8 The Unchanging Christ is the Same Forever Jesus Christ the Messiah is eternally trustworthy. The writer of Hebrews simply said, "Jesus Christ is the same yesterday, today and forever" (Hebrews 13:8). In a turbulent and fast-changing world that goes from one crisis to the next nothing seems permanent. However, this statement of faith has been a source of strength and encouragement for Christians in every generation for centuries. In a world that is flying apart politically, economically, personally and spiritually Jesus Christ is our only secure anchor. Through all the changes in society, the church around us, and in our spiritual life within us, Jesus Christ changes not. He is ever the same. As our personal faith seizes hold of Him we will participate in His unchangeableness. Like Christ it will know no change, and will always be the same. He is just as faithful now as He has ever been. Jesus Christ is the same for all eternity. He is changeless, immutable! He has not changed, and He will never change. The same one who was the source and object of triumphant faith yesterday is also the one who is all-sufficient and all-powerful today to save, sustain and guide us into the eternal future. He will continue to be our Savior forever. He steadily says to us, "I will never fail you nor forsake you." In His awesome prayer the night before His death by crucifixion, Jesus prayed, "Now, Father, glorify Me together with Yourself, with the glory which I had with You before the world was" (John 17:5). -
Yesterday and Today
Yesterday and Today IN PARTNERSHIP WITH Yesterday_and_Today_FC.indd 1 3/2/17 2:01 PM 2 Schools Past At school, you learn to read and write and do math, just like children long ago. These things are the same. Then This is what a school looked like in the past. The past means long ago, the time before now. Back then, schools had only one room. Children of all ages learned together. Abacus Hornbook There were no buses Children used Children learned to or cars. Everyone chalk to write read from a hornbook. walked to school. on small boards They used an abacus called slates. for math. yesterday and today_2-3.indd 6 3/2/17 2:04 PM 3 and Present Some things about school How are schools have changed. To change today different from is to become different. schools long ago? Now This photograph shows a school in the present. The present means now. Today, most schools have many rooms. Most children in a class are about the same age. Children may take a bus to school, or get a ride in a car. Special-needs school Home school Children have notebooks, books, There are different and computers. These are tools kinds of schools. for learning. A tool is something people use to do work. yesterday and today_2-3.indd 7 3/2/17 2:05 PM 4 Communities Past A community is a place where people live. In some ways, communities haven’t changed. They have places to live, places to work, and places to buy things.