7,706 research outputs found
A Parseval equation and a generalized finite Hankel transformation
summary:In this paper, we study the finite Hankel transformation on spaces of ge\-ne\-ra\-lized functions by developing a new procedure. We consider two Hankel type integral transformations and connected by the Parseval equation A space of functions and a space of complex sequences are introduced. is an isomorphism from onto when . We propose to define the generalized finite Hankel transform of by \langle (h'_\mu f), ((h_\mu ^{\ast } \varphi )(n))_{n=0}^{\infty }\rangle =\langle f,\varphi \rangle, \quad \text{for } \varphi \in S_\mu . $
Fast multi-dimensional scattered data approximation with Neumann boundary conditions
An important problem in applications is the approximation of a function
from a finite set of randomly scattered data . A common and powerful
approach is to construct a trigonometric least squares approximation based on
the set of exponentials . This leads to fast numerical
algorithms, but suffers from disturbing boundary effects due to the underlying
periodicity assumption on the data, an assumption that is rarely satisfied in
practice. To overcome this drawback we impose Neumann boundary conditions on
the data. This implies the use of cosine polynomials as basis
functions. We show that scattered data approximation using cosine polynomials
leads to a least squares problem involving certain Toeplitz+Hankel matrices. We
derive estimates on the condition number of these matrices. Unlike other
Toeplitz+Hankel matrices, the Toeplitz+Hankel matrices arising in our context
cannot be diagonalized by the discrete cosine transform, but they still allow a
fast matrix-vector multiplication via DCT which gives rise to fast conjugate
gradient type algorithms. We show how the results can be generalized to higher
dimensions. Finally we demonstrate the performance of the proposed method by
applying it to a two-dimensional geophysical scattered data problem
Effects of MHD on the Unsteady Rotating Flow of a Generalized Maxwell Fluid with Oscillating Gradient Between Coaxial Cylinders
The aim of this paper is studied the effect of magnetic field on the unsteady rotating flow of a generalized Maxwell fluid with fractional derivative between two infinite straight circular cylinder .The velocity field and the shear stress are obtained by means of discrete Laplace transform and finite Hankel transform. The exact solution for the velocity field and the shear stress that have been obtained by integral and series form in terms of the generalized G functions and Mitting –leffer function .the graphs are plotted to show the effects of the fractional parameter on the fluid dynamic characteristics with MHD on the velocity and shear stress
Pitt's inequalities and uncertainty principle for generalized Fourier transform
We study the two-parameter family of unitary operators which are called
-generalized Fourier transforms and defined by the -deformed Dunkl
harmonic oscillator , , where
is the Dunkl Laplacian. Particular cases of such operators are the
Fourier and Dunkl transforms. The restriction of to radial
functions is given by the -deformed Hankel transform .
We obtain necessary and sufficient conditions for the weighted
Pitt inequalities to hold for the -deformed Hankel
transform. Moreover, we prove two-sided Boas--Sagher type estimates for the
general monotone functions. We also prove sharp Pitt's inequality for
transform in with the corresponding
weights. Finally, we establish the logarithmic uncertainty principle for
.Comment: 16 page
The asymptotics a Bessel-kernel determinant which arises in Random Matrix Theory
In Random Matrix Theory the local correlations of the Laguerre and Jacobi
Unitary Ensemble in the hard edge scaling limit can be described in terms of
the Bessel kernel (containing a parameter ). In particular, the
so-called hard edge gap probabilities can be expressed as the Fredholm
determinants of the corresponding integral operator restricted to the finite
interval [0, R]. Using operator theoretic methods we are going to compute their
asymptotics as R goes to infinity under certain assumption on the parameter
.Comment: 50 page
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