2008
DOI: 10.1063/1.3003062
|View full text |Cite
|
Sign up to set email alerts
|

On computing the trace of the kernel of the homogeneous Fredholm’s equation

Abstract: A method for computing the trace of the kernel of the homogeneous Fredholm’s equation for resonant states arising from nonlocal potentials is proposed. We show that this integral formulation is convergent.

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
16
0

Year Published

2011
2011
2017
2017

Publication Types

Select...
5
3

Relationship

3
5

Authors

Journals

citations
Cited by 15 publications
(16 citation statements)
references
References 16 publications
0
16
0
Order By: Relevance
“…Before we make of the Fredholm's alternative (FA) the center of our attention we recall that only recently we can talk about the connection between evanescent waves [6][7][8][9][10][11][12] and resonant solutions of the homogeneous Fredholm's equation. [13][14][15][16][17][18] But then we have a physical interpretation of the solutions we want to classify, that is if the integral equation is inhomogeneous we have a positive refraction index-like conditions but if the equation that describes the physical situation is homogeneous we then have negative refraction index-like conditions and the solutions can be called resonances. the two different kinds of physical conditions there are travelling waves that allow communications, their frequencies are basically different because in the positive refraction index-like conditions, the corresponding frequency values to the resonant ones are really hidden or in a practical sense are confined to the so called near zone without the possibility to bring any information because of their exponentially decaying amplitudes.…”
Section: Introductionmentioning
confidence: 99%
“…Before we make of the Fredholm's alternative (FA) the center of our attention we recall that only recently we can talk about the connection between evanescent waves [6][7][8][9][10][11][12] and resonant solutions of the homogeneous Fredholm's equation. [13][14][15][16][17][18] But then we have a physical interpretation of the solutions we want to classify, that is if the integral equation is inhomogeneous we have a positive refraction index-like conditions but if the equation that describes the physical situation is homogeneous we then have negative refraction index-like conditions and the solutions can be called resonances. the two different kinds of physical conditions there are travelling waves that allow communications, their frequencies are basically different because in the positive refraction index-like conditions, the corresponding frequency values to the resonant ones are really hidden or in a practical sense are confined to the so called near zone without the possibility to bring any information because of their exponentially decaying amplitudes.…”
Section: Introductionmentioning
confidence: 99%
“…For normalization conditions (the auxiliary and original equations must have the same solutions) the structure of must be the same of a phase factor, that is: (10) And when the resonant conditions are imposed, h must satisfy that ( ) q q q ih e (11) for the resonant frequency q , where in general That is, the resonant solutions vanish at the point sources.…”
Section: General Behavior Ofmentioning
confidence: 99%
“…978-1-4673-5707-4/13/$31.00 ©2013 IEEE But if we want to take advantage of the resonant solutions of the homogeneous vector Fredholm's equation we can follow the recipe for quantum Gamow (resonant) states [2,4,10,11]. That is we deform the path of integration over the real axis of equation (1) ; ;…”
Section: Introductionmentioning
confidence: 99%
“…To this end, we assume that the theory of homogeneous Fredholm's equations [3,4,5] is applied and written explicitly the kernel ) (…”
Section: The Orthogonality Relation For Resonancesmentioning
confidence: 99%