Fourier Analysis
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Modelling for Aquifer Parameters Determination
Journal of Engineering Science, Vol. 14, 71–99, 2018 Mathematical Implications of Hydrogeological Conditions: Modelling for Aquifer Parameters Determination Sheriffat Taiwo Okusaga1, Mustapha Adewale Usman1* and Niyi Olaonipekun Adebisi2 1Department of Mathematical Sciences, Olabisi Onabanjo University, Ago-Iwoye, Nigeria 2Department of Earth Sciences, Olabisi Onabanjo University, Ago-Iwoye, Nigeria *Corresponding author: [email protected] Published online: 15 April 2018 To cite this article: Sheriffat Taiwo Okusaga, Mustapha Adewale Usman and Niyi Olaonipekun Adebisi. (2018). Mathematical implications of hydrogeological conditions: Modelling for aquifer parameters determination. Journal of Engineering Science, 14: 71–99, https://doi.org/10.21315/jes2018.14.6. To link to this article: https://doi.org/10.21315/jes2018.14.6 Abstract: Formulations of natural hydrogeological phenomena have been derived, from experimentation and observation of Darcy fundamental law. Mathematical methods are also been applied to expand on these formulations, but the management of complexities which relate to subsurface heterogeneity is yet to be developed into better models. This study employs a thorough approach to modelling flow in an aquifer (a porous medium) with phenomenological parameters such as Transmissibility and Storage Coefficient on the basis of mathematical arguments. An overview of the essential components of mathematical background and a basic working knowledge of groundwater flow is presented. Equations obtained through the modelling process -
The Fast Fourier Transform
The Fast Fourier Transform Derek L. Smith SIAM Seminar on Algorithms - Fall 2014 University of California, Santa Barbara October 15, 2014 Table of Contents History of the FFT The Discrete Fourier Transform The Fast Fourier Transform MP3 Compression via the DFT The Fourier Transform in Mathematics Table of Contents History of the FFT The Discrete Fourier Transform The Fast Fourier Transform MP3 Compression via the DFT The Fourier Transform in Mathematics Navigating the Origins of the FFT The Royal Observatory, Greenwich, in London has a stainless steel strip on the ground marking the original location of the prime meridian. There's also a plaque stating that the GPS reference meridian is now 100m to the east. This photo is the culmination of hundreds of years of mathematical tricks which answer the question: How to construct a more accurate clock? Or map? Or star chart? Time, Location and the Stars The answer involves a naturally occurring reference system. Throughout history, humans have measured their location on earth, in order to more accurately describe the position of astronomical bodies, in order to build better time-keeping devices, to more successfully navigate the earth, to more accurately record the stars... and so on... and so on... Time, Location and the Stars Transoceanic exploration previously required a vessel stocked with maps, star charts and a highly accurate clock. Institutions such as the Royal Observatory primarily existed to improve a nations' navigation capabilities. The current state-of-the-art includes atomic clocks, GPS and computerized maps, as well as a whole constellation of government organizations. -
B1. Fourier Analysis of Discrete Time Signals
B1. Fourier Analysis of Discrete Time Signals Objectives • Introduce discrete time periodic signals • Define the Discrete Fourier Series (DFS) expansion of periodic signals • Define the Discrete Fourier Transform (DFT) of signals with finite length • Determine the Discrete Fourier Transform of a complex exponential 1. Introduction In the previous chapter we defined the concept of a signal both in continuous time (analog) and discrete time (digital). Although the time domain is the most natural, since everything (including our own lives) evolves in time, it is not the only possible representation. In this chapter we introduce the concept of expanding a generic signal in terms of elementary signals, such as complex exponentials and sinusoids. This leads to the frequency domain representation of a signal in terms of its Fourier Transform and the concept of frequency spectrum so that we characterize a signal in terms of its frequency components. First we begin with the introduction of periodic signals, which keep repeating in time. For these signals it is fairly easy to determine an expansion in terms of sinusoids and complex exponentials, since these are just particular cases of periodic signals. This is extended to signals of a finite duration which becomes the Discrete Fourier Transform (DFT), one of the most widely used algorithms in Signal Processing. The concepts introduced in this chapter are at the basis of spectral estimation of signals addressed in the next two chapters. 2. Periodic Signals VIDEO: Periodic Signals (19:45) http://faculty.nps.edu/rcristi/eo3404/b-discrete-fourier-transform/videos/chapter1-seg1_media/chapter1-seg1- 0.wmv http://faculty.nps.edu/rcristi/eo3404/b-discrete-fourier-transform/videos/b1_02_periodicSignals.mp4 In this section we define a class of discrete time signals called Periodic Signals. -
7: Inner Products, Fourier Series, Convolution
7: FOURIER SERIES STEVEN HEILMAN Contents 1. Review 1 2. Introduction 1 3. Periodic Functions 2 4. Inner Products on Periodic Functions 3 5. Trigonometric Polynomials 5 6. Periodic Convolutions 7 7. Fourier Inversion and Plancherel Theorems 10 8. Appendix: Notation 13 1. Review Exercise 1.1. Let (X; h·; ·i) be a (real or complex) inner product space. Define k·k : X ! [0; 1) by kxk := phx; xi. Then (X; k·k) is a normed linear space. Consequently, if we define d: X × X ! [0; 1) by d(x; y) := ph(x − y); (x − y)i, then (X; d) is a metric space. Exercise 1.2 (Cauchy-Schwarz Inequality). Let (X; h·; ·i) be a complex inner product space. Let x; y 2 X. Then jhx; yij ≤ hx; xi1=2hy; yi1=2: Exercise 1.3. Let (X; h·; ·i) be a complex inner product space. Let x; y 2 X. As usual, let kxk := phx; xi. Prove Pythagoras's theorem: if hx; yi = 0, then kx + yk2 = kxk2 + kyk2. 1 Theorem 1.4 (Weierstrass M-test). Let (X; d) be a metric space and let (fj)j=1 be a sequence of bounded real-valued continuous functions on X such that the series (of real num- P1 P1 bers) j=1 kfjk1 is absolutely convergent. Then the series j=1 fj converges uniformly to some continuous function f : X ! R. 2. Introduction A general problem in analysis is to approximate a general function by a series that is relatively easy to describe. With the Weierstrass Approximation theorem, we saw that it is possible to achieve this goal by approximating compactly supported continuous functions by polynomials. -
Triangular Numbers /, 3,6, 10, 15, ", Tn,'" »*"
TRIANGULAR NUMBERS V.E. HOGGATT, JR., and IVIARJORIE BICKWELL San Jose State University, San Jose, California 9111112 1. INTRODUCTION To Fibonacci is attributed the arithmetic triangle of odd numbers, in which the nth row has n entries, the cen- ter element is n* for even /?, and the row sum is n3. (See Stanley Bezuszka [11].) FIBONACCI'S TRIANGLE SUMS / 1 =:1 3 3 5 8 = 2s 7 9 11 27 = 33 13 15 17 19 64 = 4$ 21 23 25 27 29 125 = 5s We wish to derive some results here concerning the triangular numbers /, 3,6, 10, 15, ", Tn,'" »*". If one o b - serves how they are defined geometrically, 1 3 6 10 • - one easily sees that (1.1) Tn - 1+2+3 + .- +n = n(n±M and (1.2) • Tn+1 = Tn+(n+1) . By noticing that two adjacent arrays form a square, such as 3 + 6 = 9 '.'.?. we are led to 2 (1.3) n = Tn + Tn„7 , which can be verified using (1.1). This also provides an identity for triangular numbers in terms of subscripts which are also triangular numbers, T =T + T (1-4) n Tn Tn-1 • Since every odd number is the difference of two consecutive squares, it is informative to rewrite Fibonacci's tri- angle of odd numbers: 221 222 TRIANGULAR NUMBERS [OCT. FIBONACCI'S TRIANGLE SUMS f^-O2) Tf-T* (2* -I2) (32-22) Ti-Tf (42-32) (52-42) (62-52) Ti-Tl•2 (72-62) (82-72) (9*-82) (Kp-92) Tl-Tl Upon comparing with the first array, it would appear that the difference of the squares of two consecutive tri- angular numbers is a perfect cube. -
Fourier Series
Academic Press Encyclopedia of Physical Science and Technology Fourier Series James S. Walker Department of Mathematics University of Wisconsin–Eau Claire Eau Claire, WI 54702–4004 Phone: 715–836–3301 Fax: 715–836–2924 e-mail: [email protected] 1 2 Encyclopedia of Physical Science and Technology I. Introduction II. Historical background III. Definition of Fourier series IV. Convergence of Fourier series V. Convergence in norm VI. Summability of Fourier series VII. Generalized Fourier series VIII. Discrete Fourier series IX. Conclusion GLOSSARY ¢¤£¦¥¨§ Bounded variation: A function has bounded variation on a closed interval ¡ ¢ if there exists a positive constant © such that, for all finite sets of points "! "! $#&% (' #*) © ¥ , the inequality is satisfied. Jordan proved that a function has bounded variation if and only if it can be expressed as the difference of two non-decreasing functions. Countably infinite set: A set is countably infinite if it can be put into one-to-one £0/"£ correspondence with the set of natural numbers ( +,£¦-.£ ). Examples: The integers and the rational numbers are countably infinite sets. "! "!;: # # 123547698 Continuous function: If , then the function is continuous at the point : . Such a point is called a continuity point for . A function which is continuous at all points is simply referred to as continuous. Lebesgue measure zero: A set < of real numbers is said to have Lebesgue measure ! $#¨CED B ¢ £¦¥ zero if, for each =?>A@ , there exists a collection of open intervals such ! ! D D J# K% $#L) ¢ £¦¥ ¥ ¢ = that <GFIH and . Examples: All finite sets, and all countably infinite sets, have Lebesgue measure zero. "! "! % # % # Odd and even functions: A function is odd if for all in its "! "! % # # domain. -
An Introduction to Fourier Analysis Fourier Series, Partial Differential Equations and Fourier Transforms
An Introduction to Fourier Analysis Fourier Series, Partial Differential Equations and Fourier Transforms Notes prepared for MA3139 Arthur L. Schoenstadt Department of Applied Mathematics Naval Postgraduate School Code MA/Zh Monterey, California 93943 August 18, 2005 c 1992 - Professor Arthur L. Schoenstadt 1 Contents 1 Infinite Sequences, Infinite Series and Improper Integrals 1 1.1Introduction.................................... 1 1.2FunctionsandSequences............................. 2 1.3Limits....................................... 5 1.4TheOrderNotation................................ 8 1.5 Infinite Series . ................................ 11 1.6ConvergenceTests................................ 13 1.7ErrorEstimates.................................. 15 1.8SequencesofFunctions.............................. 18 2 Fourier Series 25 2.1Introduction.................................... 25 2.2DerivationoftheFourierSeriesCoefficients.................. 26 2.3OddandEvenFunctions............................. 35 2.4ConvergencePropertiesofFourierSeries.................... 40 2.5InterpretationoftheFourierCoefficients.................... 48 2.6TheComplexFormoftheFourierSeries.................... 53 2.7FourierSeriesandOrdinaryDifferentialEquations............... 56 2.8FourierSeriesandDigitalDataTransmission.................. 60 3 The One-Dimensional Wave Equation 70 3.1Introduction.................................... 70 3.2TheOne-DimensionalWaveEquation...................... 70 3.3 Boundary Conditions ............................... 76 3.4InitialConditions................................ -
The Cauchy-Kovalevskaya Theorem
CHAPTER 2 The Cauchy-Kovalevskaya Theorem This chapter deals with the only “general theorem” which can be extended from the theory of ODEs, the Cauchy-Kovalevskaya Theorem. This also will allow us to introduce the notion of non-characteristic data, principal symbol and the basic clas- sification of PDEs. It will also allow us to explore why analyticity is not the proper regularity for studying PDEs most of the time. Acknowledgements. Some parts of this chapter – in particular the four proofs of the Cauchy-Kovalevskaya theorem for ODEs – are strongly inspired from the nice lecture notes of Bruce Diver available on his webpage, and some other parts – in particular the organisation of the proof in the PDE case and the discussion of the counter-examples – are strongly inspired from the nice lectures notes of Tsogtgerel Gantumur available on his webpage. 1. Recalls on analyticity Let us first do some recalls on the notion of real analyticity. Definition 1.1. A function f defined on some open subset U of the real line is said to be real analytic at a point x if it is an infinitely di↵erentiable function 0 2U such that the Taylor series at the point x0 1 f (n)(x ) (1.1) T (x)= 0 (x x )n n! − 0 n=0 X converges to f(x) for x in a neighborhood of x0. A function f is real analytic on an open set of the real line if it is real analytic U at any point x0 . The set of all real analytic functions on a given open set is often denoted by2C!U( ). -
Physics 403, Spring 2011 Problem Set 2 Due Thursday, February 17
Physics 403, Spring 2011 Problem Set 2 due Thursday, February 17 1. A Differential Equation for the Legendre Polynomials (15 pts): In this prob- lem, we will derive a second order linear differential equation satisfied by the Legendre polynomials (−1)n dn P (x) = [(1 − x2)n] : n 2nn! dxn (a) Show that Z 1 2 0 0 Pm(x)[(1 − x )Pn(x)] dx = 0 for m 6= n : (1) −1 Conclude that 2 0 0 [(1 − x )Pn(x)] = λnPn(x) 0 for λn a constant. [ Prime here and in the following questions denotes d=dx.] (b) Perform the integral (1) for m = n to find a relation for λn in terms of the leading n coefficient of the Legendre polynomial Pn(x) = knx + :::. What is kn? 2. A Generating Function for the Legendre Polynomials (20 pts): In this problem, we will derive a generating function for the Legendre polynomials. (a) Verify that the Legendre polynomials satisfy the recurrence relation 0 0 0 Pn − 2xPn−1 + Pn−2 − Pn−1 = 0 : (b) Consider the generating function 1 X n g(x; t) = t Pn(x) : n=0 Use the recurrence relation above to show that the generating function satisfies the first order differential equation d (1 − 2xt + t2) g(x; t) = tg(x; t) : dx Determine the constant of integration by using the fact that Pn(1) = 1. (c) Use the generating function to express the potential for a point particle q jr − r0j in terms of Legendre polynomials. 1 3. The Dirac delta function (15 pts): Dirac delta functions are useful mathematical tools in quantum mechanics. -
Polynomial Sequences Generated by Linear Recurrences
Innocent Ndikubwayo Polynomial Sequences Generated by Linear Recurrences: Location and Reality of Zeros Polynomial Sequences Generated by Linear Recurrences: Location and Reality of Zeros Linear Recurrences: Location by Sequences Generated Polynomial Innocent Ndikubwayo ISBN 978-91-7911-462-6 Department of Mathematics Doctoral Thesis in Mathematics at Stockholm University, Sweden 2021 Polynomial Sequences Generated by Linear Recurrences: Location and Reality of Zeros Innocent Ndikubwayo Academic dissertation for the Degree of Doctor of Philosophy in Mathematics at Stockholm University to be publicly defended on Friday 14 May 2021 at 15.00 in sal 14 (Gradängsalen), hus 5, Kräftriket, Roslagsvägen 101 and online via Zoom, public link is available at the department website. Abstract In this thesis, we study the problem of location of the zeros of individual polynomials in sequences of polynomials generated by linear recurrence relations. In paper I, we establish the necessary and sufficient conditions that guarantee hyperbolicity of all the polynomials generated by a three-term recurrence of length 2, whose coefficients are arbitrary real polynomials. These zeros are dense on the real intervals of an explicitly defined real semialgebraic curve. Paper II extends Paper I to three-term recurrences of length greater than 2. We prove that there always exist non- hyperbolic polynomial(s) in the generated sequence. We further show that with at most finitely many known exceptions, all the zeros of all the polynomials generated by the recurrence lie and are dense on an explicitly defined real semialgebraic curve which consists of real intervals and non-real segments. The boundary points of this curve form a subset of zero locus of the discriminant of the characteristic polynomial of the recurrence. -
Contentscontents 2323 Fourier Series
ContentsContents 2323 Fourier Series 23.1 Periodic Functions 2 23.2 Representing Periodic Functions by Fourier Series 9 23.3 Even and Odd Functions 30 23.4 Convergence 40 23.5 Half-range Series 46 23.6 The Complex Form 53 23.7 An Application of Fourier Series 68 Learning outcomes In this Workbook you will learn how to express a periodic signal f(t) in a series of sines and cosines. You will learn how to simplify the calculations if the signal happens to be an even or an odd function. You will learn some brief facts relating to the convergence of the Fourier series. You will learn how to approximate a non-periodic signal by a Fourier series. You will learn how to re-express a standard Fourier series in complex form which paves the way for a later examination of Fourier transforms. Finally you will learn about some simple applications of Fourier series. Periodic Functions 23.1 Introduction You should already know how to take a function of a single variable f(x) and represent it by a power series in x about any point x0 of interest. Such a series is known as a Taylor series or Taylor expansion or, if x0 = 0, as a Maclaurin series. This topic was firs met in 16. Such an expansion is only possible if the function is sufficiently smooth (that is, if it can be differentiated as often as required). Geometrically this means that there are no jumps or spikes in the curve y = f(x) near the point of expansion. -
Fourier Analysis
Chapter 1 Fourier analysis In this chapter we review some basic results from signal analysis and processing. We shall not go into detail and assume the reader has some basic background in signal analysis and processing. As basis for signal analysis, we use the Fourier transform. We start with the continuous Fourier transformation. But in applications on the computer we deal with a discrete Fourier transformation, which introduces the special effect known as aliasing. We use the Fourier transformation for processes such as convolution, correlation and filtering. Some special attention is given to deconvolution, the inverse process of convolution, since it is needed in later chapters of these lecture notes. 1.1 Continuous Fourier Transform. The Fourier transformation is a special case of an integral transformation: the transforma- tion decomposes the signal in weigthed basis functions. In our case these basis functions are the cosine and sine (remember exp(iφ) = cos(φ) + i sin(φ)). The result will be the weight functions of each basis function. When we have a function which is a function of the independent variable t, then we can transform this independent variable to the independent variable frequency f via: +1 A(f) = a(t) exp( 2πift)dt (1.1) −∞ − Z In order to go back to the independent variable t, we define the inverse transform as: +1 a(t) = A(f) exp(2πift)df (1.2) Z−∞ Notice that for the function in the time domain, we use lower-case letters, while for the frequency-domain expression the corresponding uppercase letters are used. A(f) is called the spectrum of a(t).