
On the order of magnitude of the coefficients of a fourier series
Publication year - 1917
Publication title -
proceedings of the royal society of london. series a, containing papers of a mathematical and physical character
Language(s) - English
Resource type - Journals
eISSN - 2053-9150
pISSN - 0950-1207
DOI - 10.1098/rspa.1917.0002
Subject(s) - lipschitz continuity , mathematics , lebesgue integration , sine , bounded function , zero (linguistics) , fourier series , series (stratigraphy) , mathematical analysis , pure mathematics , order (exchange) , function (biology) , type (biology) , bounded variation , trigonometric functions , absolute convergence , paleontology , philosophy , linguistics , ecology , geometry , finance , evolutionary biology , economics , biology
§ 1. Riemann’s theorem that the coefficients of a Fourier series converge to zero was shown by Lebesgue to still hold when integration is understood to be in the general sense now employed, absolutely convergent, or Lebesgue integration. Little progress has, however, been made in the determination of the order of magnitude of the coefficients. It has, indeed, been proved that, when the function has bounded variation,na n andnb n are bounded functions ofn , and that, when the function is a continuous function of such a type as satisfies a condition of Lipschitz,n q a n andn q b n converge to zero, whereq is a positive number not greater than unity, depending on the particular Lipschitz condition satisfied by the function. As regards the second of these results, involving the satisfying of a condition of Lipschitz, it is to be remarked that, in well-known series of the type Σn -q cosnx and Σn -q sinnx , the functions of which they are the Fourier series do not, in any interval containing the origin, satisfy any condition of Lipschitz, being, indeed, unbounded. In the present communication I obtain a number of theorems corresponding to each of these two results, including them as particular cases, and, at the same time, leading to the known properties of the simple sine and cosine series above referred to.