Heisenberg uncertainty principle for a fractional power of the Dunkl transform on the real line

Abstract

The aim of this paper is to prove Heisenberg-Pauli-Weyl inequality for a fractional power of the Dunkl transform on the real line for which there is an index law and a Plancherel theorem.

FRACTIONAL INTEGRATION OPERATOR ON SOME RADIAL RAYS AND INTERTWINING FOR THE DUNKL OPERATOR

Abstract

In this paper we consider the differential-difference reflection operator associated with a finite cyclic group, 

Y(v)f(x) = df(x)/dx + Sigma(m-1)(i-1)mv(i) + m - i/x Sigma(m-1)(j-1)epsilon(-ij) f(epsilon(j)x). 

SDS 423

CLINICAL REMOVABLE PROSTHODONTICS

ملحقات المادة الدراسية

Experimental and theoretical study of the electronic structure and optical spectral features of PbIn6Te10

We present measurements of the optical properties of crystalline PbIn6Te10. The samples are grown in the form of parallelepipeds of size [similar]5 [times] 3 [times] 0.3 mm3. The absorption coefficient [small alpha](h[small nu]) shows an exponential behavior with energy in the energy range 0.82-0.99 eV followed by an abrupt increase in the absorption from 1.07-1.13 eV. According to the analysis of the data{,} the indirect gap is 0.88 eV while the direct gap is 1.05 eV.

Gravity analysis of the Precambrian basement topography associated with the northern boundary of Ghadames Basin (Southern Tunisia)

Gravity datawere analyzed to determine the structural development of the northern boundary of the Ghadames
Basin in southern Tunisia. The Ghadames Basin which also occurs in eastern Algeria and northwestern Libya is
one of the most prolific hydrocarbon producers in North Africa with several of the largest oil fields occurring
along its northern boundary. The Ghadames Basin was formed during a series of tectonic events ranging from
the Early Paleozoic to the Early Cenozoic. These tectonic events produced a basin in southern Tunisia that has a

Hypsometric integral for the identification of neotectonic and lithology differences in low tectonically active area (Utica-Mateur region, northeastern Tunisia)

The present work tests the use of hypsometric integral (HI) in identifying
neotectonic and lithology signals in the Utica-Mateur basin (north-eastern
Tunisia), a region recognised by low deformation rates. We computed HI
values using three digital elevation models (DEMs) of 10, 30 and 90 m pixel
resolution. We extracted maximum, minimum and mean elevations from
each DEM. The obtained results reveal that the HI spatial distributions did
not demonstrate clear spatial patterns and did not correlate with geological

Phys 499 - Graduation project

This course aim is to guide the student to perform scientific project in selected areas of theoretical or experimental Physics and to train him/her to write a scientific report using the necessary references.

ملحقات المادة الدراسية

الصفحات

اشترك ب KSU Faculty آر.إس.إس