Representation Theory and the Quantum Inverse Scattering ...
Inverse scattering on graphenshu/Lecture-Slides/Isozaki...INVERSE SCATTERING ON GRAPHEN-VERTEX MODEL...
Transcript of Inverse scattering on graphenshu/Lecture-Slides/Isozaki...INVERSE SCATTERING ON GRAPHEN-VERTEX MODEL...
INVERSESCATTERING ON
GRAPHEN- VERTEX MODEL
AND EDGE MODEL
Hiroshi Isozaki
University of Tsukuba, Professor Emeritus
Tosio Kato CentennialConference
September 8, 2017, TokyoUniversity
Joint work with
Kazunori Ando Ehime University
Hisashi Morioka Doshisha University
Evgeny Korotyaev St. Petersburg
State University
Based on the works
• Spectral properties of Schroedinger operators on perturbed lattices,
K. Ando, H. Isozaki and H. Morioka,
Ann. Henri Poincare, 17 (2016), 2103-2171
• Inverse scattering for Schroedinger operators on perturbed lattices,
K. Ando, H. Isozaki and H. Morioka, in preparation
• The work in progress,
K. Ando, H. Isozaki, E. Korotyaev and H. Morioka,
Graphen as a material
The plan of the talk
Vertex Laplacian and
edge Laplacian
Helmholtz equations
Inverse scattering
KAGOME LATTICE
GRAPHITE
DIAMOND LATTICE
A possible extension
• Asymptotically cylindrical domain = carbon nanotube
Multiple Lattice Structure
• Basic lattice
• Vertex set
Wave functions and Laplacians on the vertex model• The wave function has two components
each of which corresponds to respective lattices.
• The Laplacian takes the mean
over nearest neighbors
Scattering in the continuous model
• For the case of continuous model, the free Schroedinger equation is
• Passing to the Fourier transform, it becomes
• We consider the solution living on the sphere
• Which has the asymptotic expansion
Incoming and outgoing states
• It also holds for the perturbed equation :
• The operator is the S-matrix.
• Remember that the sphere is the characteristic surface of the Laplacian.
Fermi surface (Characteristic surface)• The free Schroedinger equation on the hexagonal lattice is
• Passing to the Fourier series, it becomes
• So, the solution lives on the submanifold in the 2-dim. torus
Scattering on the lattice
• The physical solution is written as
• This holds also asymptotically (in the sense of singularities) for the perturbed lattice.
• The operator is the S-matrix.
Radiation on the lattice
• The outgoing radiation and incoming radiation are distinguished by their spatial behavior at infinity.
• For the lattice, this does not work well, since the Fermi surface is complicated and we have difficulties in applying the stationary phase method to the integral on it.
• We pass to the Fourier series and observe the singularities of wave functions on the torus.
What is the perturbed lattice?
Given a hexagonal lattice, perturb its finite part by
adding a scalar potential, or (and)
replacing a finite part by a general graph.
Edge model (metric graph)
• Hexagonal lattice with vertex set and edge set . Each edge
is oriented and identified with
• The Laplacian is defined to be
assuming the Kirchhoff condition
Kirchhoff condition
• For each , denote its end points by
• is continuous on
• For each , , and at each vertex
Assumptions on the edge Laplacian
• is real-valued, and
• except for a finite number of edges
• On each edge
Relation between vertex Laplacian and edge Laplacian
Trick• On each edge, the solution of the Schroedinger equation
is written as
• The coefficients are determined by the Kirchhoff condition
Kirchhoff condition = Vertex equation• The Kirchhoff condition is rewritten as
Which is the Schroedinger equation on the vertex set.
The symmetric assumption of the potential is used here.
Rellich type theorem ーContinuous case• Define the Besov type space by
Fourier Analysis on the lattice
• Define the Besov type space by
• Passing to the torus by the Fourier series, we have
Sometimes, it is more convenient to pass to the Fourier transform• Multiply a cut off function (a partition of unity), and pass to the Fourier
transform
Rellich type theorem on the lattice
• Suppose satisfies the Helmholtz equation near infinity of the lattice
• Extending to be zero in the finite part, and passing to the Fourier series
where is a trigonometric polynomial
Rellich type theorem
• The HilbertNullStellenSatz from Algebraic Geometry (in its simplest form) is used in the proof.
• This theorem implies the non-existence of embedded eigenvalues.
• It also plays an important role in the inverse problem.
• The same theorem also holds for the edge model.
The tools we are using
• Sometimes, the discrete model is harder than the continuous model. Because, we do not have so many tools available in the former.
We are using
• Real Fourier analysis (Ps. D. OP.’s)
• Complex analysis (Simplest cases in the theory of several complex variables and algebraic geometry)
Forward problem ---- stationary scattering theory
Resolvent estimates --- Limiting
absorption principle
Spectral representation S-matrix Helmholtz equation
Forward problem
• Limiting absorption principle
• Spectral representation
• S-matrix
Expansion in the sense of singularities
• Instead of observing the spatial behavior of the resolvent at infinity, we observe its singularities by passing it on the torus by using the Fourier series.
• Then, the most singular part of the resolvent has the form
which gives us the spectral representation and the S-matrix.
Helmholtz equation and S-matrix
• has eigenvalues , and eigenprojections
The same theorem holds for the edge model
It is hard to tell the details of the formulas
• Sorry. I can only give the flavor
Interior boundary value problem
• Neumann derivative
• DN map
The whole space problem and the interior problem
• Divide the lattice into two parts : exterior domain and interior domain
• Then, the Schroedinger equation on the whole space is divided into
the exterior problem + the interior problem + the integral equation on the boundary
S-matrix at a fixed energy determines the D-N map
The same is true for the edge model
• The S-matrix for the whole space problem determines the D-N map for the interior boundary value problem and vice versa.
• Moreover, the S-matrix for the edge model is computed from that of the vertex model.
The inverse scattering problem is reduced to the inverse boundary value problem• In the case of the planar graph, the inverse problem from the D-N map has is
solved by
Colin de Verdiere (1994, 1996)
Curtis-Morrow (1994)
Similarity between the inverse problemsfor the continuous case and discrete case
• In 2-dim, the metric is determined by the D-N map up to a diffeomorphism leaving the boundary invariant
• The same is considered to be true (and is proved for the analytic case) for higher dimensions.
• The planar graph is determined from the diffeomorphism up to elementary transformations.
ELEMENTARY TRANSFORMATIONS
So, in general, local perturbations in a periodic graph is determined, as a planar graph up to elementary transformations, from the S-matrix of all energies.
• This is true for a wider class of periodic graph.
• It determines the “toplogy” and the “conductivity” of the planar graph.
• However, it does not determine the location of defects.
Conitnuous case-exponentially growingsolutions to the SchroEdinger equation
• So, it is exponentially growing in a half-space and exponentially decaying in the opposite half-space
• Faddeev (1966), Calderon (1980), Sylvester-Uhlmann (1987)
Discrete analogue of the exponentially growing solution
• It is non-zero above , and zero below
Potential is computed from the S-matrix.
• Adopting this solution as a boundary data, one can compute the potential by using the solution of the interior Dirichlet problem.
• Recall that the S-matrix and the D-N map are mutually related:
Reconstruction of the potential
This idea can be also used to detect the defects of the lattice
• Consider the solution for the free equation which vanishes below the line .
• If is very high, it satisfies the Schroedinger equation on the lattice with defects.
• Let the line move downward. Then the solution touches the defect, and has a different behavior.
• It will be observed by the D-N map.
Proving for the defects of the lattice
The same idea works well for the edge model
Reduction to 1-dimensional inverse spectral problem• By observing the waves on the lattice, one can determine the coefficients of the
vertex Laplacian.
• They are the values at the end point of solutions to the equation
• They give the Dirichlet eigenvalues.
Borg’s classical result (1946)
• The symmetric potential is determined by the Dirichlet eigenvalues.
Problems onthe tree
The inverse problem on the tree is hard to solve when it contains a loop.
The edge model has loops, however, our method works well.
I t is because we are using the special structure of the periodic lattice, in particular, the analogue of exponentially growing solution for the continuous model.
NON-ZERO BACK GROUND POTENTIALS
Thank you for your attention!