1. Introduction
Microlocal analysis originated in the 1950s, and by now it is a substantial mathematical theory with many different facets and applications. One might view microlocal analysis as
      
- a kind of “variable coefficient Fourier analysis” for solving variable coefficient PDEs; or 
- as a theory of pseudodifferential operators (DOs) and Fourier integral operators (FIOs); or 
- as a phase space (or time-frequency) approach to studying functions, operators and their singularities (wave front sets). 
DOs were introduced by Kohn and Nirenberg [
1], and FIOs and wave front sets were studied systematically by Hörmander [
2]. Much of the theory up to the early 1980s is summarized in the four volume treatise of Hörmander [
3]. There are remarkable applications of microlocal analysis and related ideas in many fields of mathematics. Classical examples include spectral theory and the Atiyah-Singer index theorem, and more recent examples include scattering theory [
4], behavior of chaotic systems [
5], general relativity [
6], and inverse problems.
In this note we will describe certain classical applications of microlocal analysis in inverse problems, together with a very rough non-technical overview of relevant parts of microlocal analysis (intended for readers who may not be previously familiar with microlocal analysis). In a nutshell, here are a few typical applications:
- 1.
- Computed tomography/X-ray transform—the X-ray transform is an FIO, and under certain conditions its normal operator is an elliptic DO. Microlocal analysis can be used to predict which sharp features (singularities) of the image can be reconstructed in a stable way from limited data measurements. Microlocal analysis is also a powerful tool in the study of geodesic X-ray transforms related to seismic imaging applications. 
- 2.
- Calderón problem/Electrical Impedance Tomography—the boundary measurement map (Dirichlet-to-Neumann map) is a DO, and the boundary values of the conductivity as well as its derivatives can be computed from the symbol of this DO. 
- 3.
- Gel’fand problem/seismic imaging—the boundary measurement operator (hyperbolic Dirichlet-to-Neumann map) is an FIO, and the scattering relation of the sound speed as well as certain X-ray transforms of the coefficients can be computed from the canonical relation and the symbol of this FIO. 
This note is organized as follows—in 
Section 2, we will motivate the theory of 
DOs and discuss some of its properties without giving proofs. 
Section 3 will continue with a brief introduction to wave front sets and FIOs (again with no proofs). The rest of the note is concerned with applications to inverse problems. 
Section 4 considers the Radon transform in 
 and its normal operator, and describes what kind of information about the singularities of 
f can be stably recovered from the Radon transform. 
Section 5 and 
Section 6 discuss the Gel’fand and Calderón problems, and prove results related to recovering X-ray transforms or boundary determination. The treatment is motivated by 
DO and FIO theory, but we give direct and (in principle) elementary proofs based on quasimode constructions.
The results discussed in this note are classical. For more recent results and for further references, we refer to the surveys [
7,
8] on X-ray type transforms, survey [
9] on inverse problems for hyperbolic equations, and survey [
10] on inverse problems for elliptic equations. We also mention the article [
11] that studies inverse problems in rather general settings by using constructions like the ones in 
Section 5 and 
Section 6.
  Notation
We will use multi-index notation. Let 
 be the set natural numbers. Then 
 consists of all 
n-tuples 
 where the 
 are nonnegative integers. Such an 
n-tuple 
 is called a 
multi-index. We write 
 and 
 for 
. For partial derivatives, we will write
        
If  is a bounded domain with  boundary, we denote by  the set of infinitely differentiable functions in  whose all derivatives extend continuously to . The space  consists of  functions having compact support in . The standard  based Sobolev spaces are denoted by  with norm , with  denoting the Fourier transform. We also write . The notation  means that  for some uniform (with respect to the relevant parameters) constant C. In general, all coefficients, boundaries and so forth are assumed to be  for ease of presentation.
  2. Pseudodifferential Operators
In this note we will give a very brief idea of the different points of view to microlocal analysis mentioned in the introduction (and repeated below), as
      
- (1)
- a kind of “variable coefficient Fourier analysis” for solving variable coefficient PDEs; or 
- (2)
- a theory of DOs and FIOs; or 
- (3)
- a phase space (or time-frequency) approach to studying functions, operators and their singularities (wave front sets). 
In this section we will discuss (1) and (2) in the context of 
DOs. We will continue with (2) and (3) in the context of FIOs in 
Section 3. The treatment is mostly formal and we will give no proofs whatsoever. A complete reference for the results in this section is ([
3], Section 18.1).
  2.1. Constant Coefficient PDEs
We recall the following facts about the Fourier transform (valid for sufficiently nice functions):
- If  u-  is a function in  - , its  Fourier transform-  is the function
             
- The Fourier transform converts derivatives to polynomials (this is why it is useful for solving PDEs):
             
- A function  u-  can be recovered from  -  by the Fourier inversion formula  - , where
             - 
            is the  inverse Fourier transform- . 
As a motivating example, let us solve formally (i.e., without worrying about how to precisely justify each step) the equation
        
This is a constant coefficient PDE, and such equations can be studied with the help of the Fourier transform. We formally compute
        
The same formal argument applies to a general constant coefficient PDE
        
        where 
. Then 
 where 
 is the 
symbol of 
. Moreover, one has
        
The argument leading to (
1) gives a formal solution of 
:
Thus, formally 
 can be solved by dividing by the symbol 
 on the Fourier side. Of course, to make this precise one would need to show that the division by 
 (which may have zeros) is somehow justified. This can indeed be done, and the basic result in this direction is the Malgrange-Ehrenpreis theorem ([
3], Theorem 7.3.10).
  2.2. Variable Coefficient PDEs
We now try to use a similar idea to solve the variable coefficient PDE
        
        where 
 and 
 for all multi-indices 
. Since the coefficients 
 depend on 
x, Fourier transforming the equation 
 is not immediately helpful. However, we can compute an analogue of (
2):    
        where
        
        is the (full) 
symbol of 
.
Now, we could try to obtain a solution to 
 in 
 by dividing by the symbol 
 as in (
3):
Again, this is only formal since the division by  needs to be justified. However, this can be done in a certain sense if A is elliptic:
Definition 1. The principal symbol (i.e., the part containing the highest order derivatives) of the differential operator  is We say that A is elliptic if its principal symbol is nonvanishing for .
 A basic result of microlocal analysis states that the function
        
        with
        
        where 
 is a cutoff with 
 in a sufficiently large neighborhood of 
 (so that 
 does not vanish outside this neighborhood), is an 
approximate solution of 
 in the sense that
        
        where 
 is one derivative smoother than 
f. Applying this construction iteratively to the error term—thus to 
 in the first step above—it is possible to construct an approximate solution 
 so that
        
  2.3. Pseudodifferential Operators
In analogy with the Formula (
4), a 
pseudodifferential operator (
DO) is an operator 
A of the form
        
        where 
 is a 
symbol with certain properties. The most standard symbol class 
 is defined as follows:
Definition 2. The symbol class  consists of functions  such that for any  there is  with If , the corresponding Ψ
DO  is defined by (7). We denote by  the set of Ψ
DOs corresponding to .  Note that symbols in 
 behave roughly like polynomials of order 
m in the 
-variable. In particular, the symbols 
 in (
5) belong to 
 and the corresponding differential operators 
 belong to 
. Moreover, if 
 is elliptic, then the symbol 
 as in (
6) belongs to 
. Thus the class of 
DOs is large enough to include differential operators as well as approximate inverses of elliptic operators. Also normal operators of the X-ray transform or Radon transform in 
 are 
DOs (see 
Section 4 and ([
12], Appendix A)).
Remark 1 (Homogeneous symbols)
. We saw in Section 2.1 that the elliptic operator  has the inverseThe symbol  is not in , since it is not smooth near 0. However, G is still considered to be a Ψ
DO. In fact, one can writewhere  satisfies  near 0. Now  is a Ψ
DO in , since , and  is smoothing in the sense that it maps any  function into a  function (at least if ). In general, in Ψ
DO theory smoothing operators are considered to be negligible (since at least they do not introduce new singularities), and many computations in Ψ
DO calculus are made only modulo smoothing error terms. In this sense one often views G as a Ψ
DO by identifying it with . The same kind of identification is done for operators whose symbol  is homogeneous of some order m in ξ, i.e.,  for . More generally one can consider(step one) polyhomogeneous
symbols  having the formwhere each  is homogeneous of order  in ξ for , and ∼ denotes asymptotic summation meaning that  for any . Corresponding Ψ
DOs are called classical 
DOs.
  It is very important that one can compute with DOs in much the same way as with differential operators. One often says that DOs have a calculus, and in fact the DOs defined above form an algebra with respect to composition. The following theorem lists typical rules of computation (it is instructive to think first why such rules are valid for differential operators):
Theorem 1 (DO calculus). 
-  (a)
- (Principal symbol) There is a one-to-one correspondence between operators in  and (full) symbols in , and each operator  has a well defined principal symbol . The principal symbol may be computed by testing A against highly oscillatory functions (this is valid if A is a classical-  Ψ DO):
 
-  (b)
- (Composition) If  and , then  and ; 
-  (c)
- (Sobolev mapping properties) Each  is a bounded operator  for any ; 
-  (d)
- (Elliptic operators have approximate inverses) If  is elliptic, there is  so that  and  where , i.e.,  are smoothing (they map any  function to  for any t, hence also to  by Sobolev embedding). 
 The above properties are valid in the standard DO calculus in . However, motivated by different applications, DOs have been considered in various other settings. Each of these settings comes with an associated calculus whose rules of computation are similar but adapted to the situation at hand (for instance, one may need extra conditions for compositions to be well defined). Examples of different settings for DOs include
        
- open sets in  -  (local setting) ([ 3- ], Section 18.1); 
- compact manifolds without boundary, possibly acting on sections of vector bundles ([ 3- ], Section 18.1); 
- compact manifolds with boundary (transmission condition/Boutet de Monvel calculus) [ 13- ]; 
- non-compact manifolds (e.g., Melrose scattering calculus) [ 14- ]; 
- operators with a small or large parameter (semiclassical calculus) [ 15- ]; and 
- operators with real-analytic coefficients (analytic microlocal analysis) [ 16- , 17- ]. 
  3. Wave Front Sets and Fourier Integral Operators
For a reference to wave front sets, see Reference ([
3], Chapter 8). Sobolev wave front sets are considered in Reference ([
3], Section 18.1). FIOs are discussed in Reference ([
3], Chapter 25). We mention that FIO type methods were independently developed by Maslov [
18].
  3.1. The Role of Singularities
We first discuss the singular support of u, which consists of those points  such that u is not a smooth function in any neighborhood of . We also consider the Sobolev singular support, which also measures the “strength” of the singularity (in the  Sobolev scale).
Definition 3 (Singular support)
. We say that a function or distribution u is (resp. 
) near 
if there is  with  near  such that  is in  (resp. in ). We define Example 1. Let  be bounded domains with  boundary in  so that  for , and definewhere  are constants, and  is the characteristic function of . Thensince  for , butsince u is not  near any boundary point. Thus in this case the singularities of u are exactly at the points where u has a jump discontinuity, and their strength is precisely . Knowing the singularities of u can already be useful in applications. For instance, if u represents some internal medium properties in medical imaging, the singularities of u could determine the location of interfaces between different tissues. On the other hand, if u represents an image, then the singularities in some sense determine the “sharp features” of the image.  Next we discuss the 
wave front set which is a more refined notion of a singularity. For example, if 
 is the characteristic function of a bounded strictly convex 
 domain 
D and if 
, one could think that 
f is in some sense smooth in tangential directions at 
 (since 
f restricted to a tangent hyperplane is identically zero, except possibly at 
), but that 
f is not smooth in normal directions at 
 since in these directions there is a jump. The wave front set is a subset of 
, the cotangent space with the zero section removed:
Definition 4 (Wave front set)
. Let u be a distribution in . We say that u is (microlocally)  (resp. 
) near 
 if there exist  with  near  and  so that  near  and ψ is homogeneous of degree 0, such that(resp. ). The wave front set  (resp.  wave front set ) consists of those points  where u is not microlocally  (resp. ). Example 2. The wave front set of the function u in Example 1 iswhere  is the conormal bundle of ,  The wave front set describes singularities more precisely than the singular support, since one always has
        
        where 
 is the projection to 
x-space.
It is an important fact that applying a DO to a function or distribution never creates new singularities:
Theorem 2 (Pseudolocal/microlocal property of 
DOs)
. Any  has the pseudolocal propertyand the microlocal property Elliptic operators are those that completely preserve singularities:
Theorem 3 (Elliptic regularity)
. Let  be elliptic. Then, for any u,Thus any solution u of  is singular precisely at those points where f is singular. There are corresponding statements for Sobolev singularities.
 Proof.  First note that by Theorem 2,
          
Conversely, since 
 is elliptic, by Theorem 1(d) there is 
 so that
          
Since 
L is smoothing, 
, which implies that 
 modulo 
. Thus it follows that
          
Thus 
. The claim for singular supports follows by (
9). □
   3.2. Fourier Integral Operators
We have seen in 
Section 2.3 that the class of pseudodifferential operators includes approximate inverses of elliptic operators. In order to handle approximate inverses for hyperbolic and transport equations, it is required to work with a larger class of operators.
Motivation 1. Consider the initial value problem for the wave equation, This is again a constant coefficient PDE, and we will solve this formally by taking the Fourier transform in space, After taking Fourier transforms in space, the above equation becomes For each fixed  this is an ODE in t, and the solution is Taking inverse Fourier transforms in space, we obtain Generalizing (
10), we can consider operators of the form
        
        where 
 is a symbol (for instance in 
), and 
 is a real valued phase function. Such operators are examples of 
Fourier integral operators (more precisely, FIOs whose canonical relation is locally the graph of a canonical transformation, see ([
3], Section 25.3)). For 
DOs the phase function is always 
, but for FIOs the phase function can be quite general, though it is usually required to be homogeneous of degree 1 in 
, and to satisfy the non-degeneracy condition 
.
 We will not go into precise definitions, but only remark that the class of FIOs includes pseudodifferential operators as well as approximate inverses of hyperbolic and transport operators (or more generally real principal type operators). There is a calculus for FIOs, analogous to the pseudodifferential calculus, under certain conditions in various settings. An important property of FIOs is that they, unlike pseudodifferential operators, can move singularities. This aspect will be discussed next.
  3.3. Propagation of Singularities
Example 3. Let  be fixed, and consider the operators from (10), Using FIO theory, since the phase functions are , it follows thatwhere  is the canonical transformation 
(i.e., diffeomorphism of  that preserves the symplectic structure) given by This means that the FIO  takes a singularity  of the initial data f and moves it along the line through x in direction  to . In fact one has equality in (12) since  has inverse  and  has inverse . Thus singularities of solutions of the wave equation  propagate along straight lines with constant speed one.  Remark 2. In general, any FIO has an associated canonical relation 
that describes what the FIO does to singularities. The canonical relation of the FIO A defined in (11) is (see ([3], Section 25.3))and A moves singularities according to the rulewhere Using these formulas, it is easy to check that the canonical relation  of  in Example 3 is the graph of  in the sense thatand one indeed has .  There is a far reaching extension of Example 3, which shows that the singularities of a solution of  propagate along certain curves in phase space (so called null bicharacteristic curves) as long as P has real valued principal symbol.
Theorem 4 (Propagation of singularities, ([
3], Theorem 26.1.1))
. Let  have real principal symbol  that is homogeneous of degree m in ξ. Ifthen  is contained in the characteristic set . Moreover, if , then the whole null bicharacteristic curve  through  is in  as long as it remains in . Here  is the solution of the Hamilton equations Example 4. We compute the null bicharacteristic curves for the wave operator . The principal symbol of P is The characteristic set iswhich consists of light-like 
cotangent vectors on . The equations for the null bicharacteristic curves are Thus, if , then the null bicharacteristic curve through  is The result of Example 3 may thus be interpreted so that singularities of solutions of the wave equation propagate along null bicharacteristic curves for the wave operator.
   4. The Radon Transform in the Plane
In this section we outline some applications of microlocal analysis to the study of the Radon transform in the plane. Similar ideas apply to X-ray and Radon transforms in higher dimensions and Riemannian manifolds as well. The microlocal approach to Radon transforms was introduced by Guillemin [
19]. We refer to [
8,
12] and references therein for a more detailed treatment of the material in this section.
  4.1. Basic Properties of the Radon Transform
The X-ray transform  of a function f in  encodes the integrals of f over all straight lines, whereas the Radon transform  encodes the integrals of f over -dimensional planes. We will focus on the case , where the two transforms coincide. There are many ways to parametrize the set of lines in . We will parametrize lines by their direction vector  and distance s from the origin.
Definition 5. If , the Radon transform
of f is the function Here  is the vector in  obtained by rotating ω counterclockwise by .
 There is a well-known relation between  and the Fourier transform . We denote by  the Fourier transform of  with respect to s.
Proof.  Parametrizing 
 by 
, we have
          
 This result gives the first proof of injectivity of the Radon transform:
Corollary 1. If  is such that , then .
 Proof.  If , then  by Theorem 5 and consequently . □
 To obtain a different inversion method, and for later purposes, we will consider the adjoint of 
R. The formal adjoint of 
R is the 
backprojection operator . The formula for 
 is obtained as follows: if 
, 
 one has
        
The following result shows that the normal operator  is a classical DO of order  in , and also gives an inversion formula.
Theorem 6 (Normal operator)
. One hasand f can be recovered from  by the formula Remark 3. Above we have written, for , The notation  is also used.
 Proof.  The proof is based on computing 
 using the Parseval identity, Fourier slice theorem, symmetry and polar coordinates:
          
 The same argument, based on computing 
 instead of 
, leads to the famous 
filtered backprojection (FBP) inversion formula:
        where 
. This formula is efficient to implement and gives good reconstructions when one has complete X-ray data and relatively small noise, and hence FBP (together with its variants) has been commonly used in X-ray CT scanners.
However, if one is mainly interested in the singularities (i.e., jumps or sharp features) of the image, it is possible to use the even simpler 
backprojection method: just apply the backprojection operator 
 to the data 
. Since 
 is an elliptic 
DO, Theorem 3 guarantees that the singularities are recovered:
Moreover, since 
 is a 
DO of order 
, hence smoothing of order 1, one expects that 
 gives a slightly blurred version of 
f where the main singularities should still be visible. The ellipticity of the normal operator is also important in the analysis of statistical methods for recovering 
f from 
 [
20].
  4.2. Visible Singularities
There are various imaging situations where complete X-ray data (i.e., the function  for all s and ) is not available. This is the case for limited angle tomography (e.g., in luggage scanners at airports, or dental applications), region of interest tomography, or exterior data tomography. In such cases explicit inversion formulas such as FBP are usually not available, but microlocal analysis (for related normal operators or FIOs) still provides a powerful paradigm for predicting which singularities can be recovered stably from the measurements.
We will try to explain this paradigm a little bit more, starting with an example:
Example 5. Let f be the characteristic function of the unit disc , i.e.,  if  and  for . Then f is singular precisely on the unit circle (in normal directions). We have Thus  is singular precisely at those points  with , which correspond to those lines that are tangent to the unit circle.
 There is a similar relation between the singularities of f and  in general, and this is explained by microlocal analysis:
Theorem 7. The operator R is an elliptic FIO of order . There is a precise relationship between the singularities of f and singularities of .
 We will not spell out the precise relationship here, but only give some consequences. It will be useful to think of the Radon transform as defined on the set of (non-oriented) lines in . If  is an open subset of lines in , we consider the Radon transform  restricted to lines in . Recovering f (or some properties of f) from  is a limited data tomography problem. Examples:
- If , then  is called exterior data. 
- If  and , then  is called limited angle data. 
It is known that any 
 is uniquely determined by exterior data (Helgason support theorem ([
21], Theorem 2.6)), and any 
 is uniquely determined by limited angle data (Fourier slice and Paley-Wiener theorems). However, both inverse problems are very unstable (inversion is not Lipschitz continuous in any Sobolev norms, but one has conditional logarithmic stability).
Definition 6. A singularity at  is called visible from if the line through  in direction  is in .
 One has the following dichotomy:
- If  is visible from , then from the singularities of  one can determine for any  whether or not . If  uniquely determines f, one expects the reconstruction of visible singularities to be stable. 
- If  is not visible from , then this singularity is smoothed out in the measurement . Even if  would determine f uniquely, the inversion is not Lipschitz stable in any Sobolev norms. 
  5. Gel’fand Problem
Seismic imaging gives rise to various inverse problems related to determining interior properties, for example, oil deposits or deep structure, of the Earth. Often this is done by using acoustic or elastic waves. We will consider the following problem, also known as the 
inverse boundary spectral problem (see the monograph [
22]):
      
Gel’fand problem: Is it possible to determine the interior structure of Earth by controlling acoustic waves and measuring vibrations at the surface?
In seismic imaging one often tries to recover an unknown sound speed. However, in this presentation we consider the simpler case where the sound speed is constant (equal to one) and one attempts to recover an unknown potential  at each point , where  is a ball in .
Consider the free wave operator
      
We assume that the medium is at rest at time 
 and that we take measurements until time 
. If we prescribe the amplitude of the wave to be 
 on 
, this leads to a solution 
u of the wave equation
      
Given any 
, there is a unique solution 
 (see ([
23], Theorem 7 in §7.2.3)). We assume that we can measure the normal derivative 
, where 
 and 
 is the outer unit normal to 
. Doing such measurements for many different functions 
f, the ideal boundary measurements are encoded by the hyperbolic Dirichlet-to-Neumann map (DN map for short)
      
The Gel’fand problem for this model amounts to recovering 
 from the knowledge of the map 
. We will prove the following result due to [
24].
Theorem 8 (Recovering the X-ray transform)
. Let  and assume that . Ifthen  and  satisfywhenever γ is a maximal line segment in  with length . It is natural that the region where one can recover information depends on 
T. By finite propagation speed the map 
 is unaffected if one changes 
q outside the set
      
Indeed, if 
u and 
 solve (
13) for potentials 
q and 
 with the same Dirichlet data 
f, and if 
 in 
, then 
 solves 
 where 
 vanishes in 
 and in 
. Moreover, 
 on 
 and 
. By finite speed of propagation 
. This proves that 
.
For T large enough, one can recover everything:
Corollary 2. If , then  implies .
 Proof.  If 
, then by Theorem 8 one has
        
        for any maximal line segment 
 in 
. Thus 
 and 
 have the same X-ray transform in 
. This transform is injective by Corollary 1 when 
. Tiling 
 by two-planes gives injectivity when 
. Thus 
. □
 Theorem 8 could be proved based on the following facts, see e.g., [
25]:
- The map  is an FIO of order 1 on . 
- The X-ray transform of q can be read off from the symbol of  (more precisely, from the principal symbol of ). 
We will give an elementary proof that is based on testing 
 against highly oscillatory boundary data (compare with (
8)).
The first step is an integral identity.
Lemma 1 (Integral identity)
. Assume that . For any , one haswhere  solves (13) with  and , and  solves an analogous problem with vanishing Cauchy data on : Proof.  We first compute the adjoint of the DN map: one has
        
        where 
 with 
v solving 
 so that 
 and 
 on 
. To prove this, we let 
u be the solution of (
13) and integrate by parts:
        
Now, if 
 and 
 are as stated, the computation above gives
        
        and
		  
The result follows by subtracting these two identities. □
 The second step is to construct special solutions to the wave equation that concentrate near curves 
 where 
 is a line segment. These curves are projections to the 
 variables of null bicharacteristic curves for □ (see Example 4). These solutions are closely related to Theorem 4 concerning propagation of singularities. In fact, similar methods can be used to prove that Theorem 4 is sharp in the sense that there are approximate solutions whose wave front set is precisely on a given null bicharacteristic curve ([
3], Theorem 26.1.5). One can also go in the other direction and use suitable concentrating solutions to prove Theorem 4, see Reference [
26].
The proof is based on a standard geometrical optics/WKB quasimode construction.
Proposition 1 (Concentrating solutions)
. Assume that , and let  be a maximal line segment in  with . For any  there is a solution  of  in  with  on , such that for any  one hasMoreover, if , there is a solution  of  in  with  on , such that for any  one has  At this point it is easy to prove the main result:
Proof (Proof of Theorem 8). (Proof of Theorem 8)
. Using the assumption 
 and Lemma 1, we have
        
        for any solutions 
 of 
 in 
 so that 
 on 
, and 
 on 
.
Let 
 be a maximal unit speed line segment in 
 with 
, and let 
 be the solution constructed in Proposition 1 for the potential 
 with 
 on 
. Moreover, let 
 be the solution constructed in the end of Proposition 1 for the potential 
 with 
 on 
. Taking the limit as 
 in (17) and using (16) with 
, we obtain that
        
Thus the integrals of  and  over maximal line segments of length  in  are the same. □
 Proof of Proposition 1. Let  be a maximal unit speed line segment in  with , and let  be the unit speed line so that  for . Write  and , so that  and . After a translation and rotation, we may assume that  and .
We first construct an approximate solution 
 for the operator 
, having the form
        
        where 
 is a real phase function, and 
a is an amplitude supported near the curve 
. Note that
        
Using a similar expression for 
, we compute
        
We would like to have 
. To this end, we first choose 
 so that the 
 term in (
18) vanishes. This will be true if 
 solves the 
eikonal equationThere are many possible solutions, but we make the simple choice
        
With this choice, (
18) becomes
        
        where 
L is the constant vector field
        
It is convenient to consider new coordinates 
 in 
, where
        
Then 
L corresponds to 
 in the sense that
        
        where 
 corresponds to 
F in the new coordinates:
        
We next look for the amplitude 
a in the form
        
Inserting this to (
18) and equating like powers of 
, we get
        
We would like the last expression to be 
. This will hold if 
 and 
 satisfy the 
transport equationsLet 
 be supported near 0, and choose
        
We will later choose 
 to depend on 
. Next we choose
        
These functions satisfy (22), and they vanish unless 
w is small (i.e., 
 is close to 
t). Then (21) becomes
        
        where
        
Using the Cauchy-Schwarz inequality, one can check that
        
        uniformly over 
. This concludes the construction of the approximate solution 
.
We next find an exact solution 
 of (
13) having the form
        
        where 
r is a correction term. Note that for 
t close to 0, 
 is supported near 
 and hence 
 on 
. Note also that 
. Thus 
u will solve (
13) for 
 if 
r solves
        
By the wellposedness of this problem ([
23], Theorem 5 in §7.2.3), there is a unique solution 
r with
        
We now fix the choice of 
 so that (15) will hold. Let 
 satisfy 
 near 0 and 
, and choose
        
        where
        
Since 
, the integral in (
15) has the form
        
Using that 
 is compactly supported in 
, we have
        
        by changing variables as in (20). Finally, changing 
 to 
 and 
w to 
 and letting 
 (so 
) yields
        
        by the normalization 
 and the fact that 
. This proves (15).
It remains to prove (16). Since , we have  on , and we may alternatively arrange that r solves (23) with  on  instead of . We can do such a construction for the potential  instead of q. Since  and  are independent of q, the same argument as above proves (16). □
   6. Calderón Problem: Boundary Determination
Electrical Impedance Tomography (EIT) is an imaging method with potential applications in medical imaging and nondestructive testing. The method is based on the following important inverse problem.
      
Calderón problem: Is it possible to determine the electrical conductivity of a medium by making voltage and current measurements on its boundary?
The treatment in this section follows [
27].
Let us begin by recalling the mathematical model of EIT. The purpose is to determine the electrical conductivity  at each point , where  represents the body which is imaged (in practice ). We assume that  is a bounded open set with  boundary, and that  is positive.
Under the assumption of no sources or sinks of current in 
, a voltage potential 
f at the boundary 
 induces a voltage potential 
u in 
, which solves the Dirichlet problem for the conductivity equation,
      
Since 
 is positive, the equation is uniformly elliptic, and there is a unique solution 
 for any boundary value 
. One can define the Dirichlet-to-Neumann map (DN map) as
      
Here  is the outer unit normal to  and  is the normal derivative of u. Physically,  is the current flowing through the boundary.
The Calderón problem (also called the inverse conductivity problem) is to determine the conductivity function  from the knowledge of the map . That is, if the measured current  is known for all boundary voltages , one would like to determine the conductivity .
We will prove the following theorem.
Theorem 9 (Boundary determination)
. Let  be positive. Ifthen the Taylor series of  and  coincide at any point of . This result was proved in Reference [
28], and it in particular implies that any real-analytic conductivity is uniquely determined by the DN map. The argument extends to piecewise real-analytic conductivities. A different proof was given in [
29], based on two facts:
Remark 4. The above argument is based on studying the singularities of the integral kernel of the DN map, and it only determines the Taylor series of the conductivity at the boundary. The values of the conductivity in the interior are encoded in the  part of the kernel, and different methods (based on complex geometrical optics solutions) are required for interior determination.
 Let us start with a simple example:
Example 6 (DN map in half space is a 
DO)
. Let , so . We wish to compute the DN map for the Laplace equation (i.e., ) in Ω. 
ConsiderWriting  and taking Fourier transforms in  gives Solving this ODE for fixed  and choosing the solution that decays for  gives We may now compute the DN map: Thus the DN map on the boundary  is just  corresponding to the Fourier multiplier . This shows that at least in this simple case, the DN map is an elliptic ΨDO of order 1.
 We will now prove Theorem 9 by an argument that avoids showing that the DN map is a DO, but is rather based on directly testing the DN map against oscillatory boundary data. The first step is a basic integral identity (sometimes called Alessandrini identity) for the DN map.
Lemma 2 (Integral identity)
. Let . If , thenwhere  solves  in Ω with . Proof.  We first observe that the DN map is symmetric: if 
 is positive and if 
 solves 
 in 
 with 
, then an integration by parts shows that
        
The result follows by subtracting the above two identities. □
 Next we show that if 
 is a boundary point, there is an approximate solution of the conductivity equation that concentrates near 
, has highly oscillatory boundary data, and decays exponentially in the interior. As a simple example, the solution of
      
      that decays for 
 is given by 
, which concentrates near 
 and decays exponentially when 
 if 
 is large. Roughly, this means that the solution of a Laplace type equation with highly oscillatory boundary data concentrates near the boundary. Note also that in a region like 
, the function 
u is harmonic and concentrates near the origin.
Proposition 2. (Concentrating approximate solutions) Let  be positive, let , let  be a unit tangent vector to  at , and let  be supported near . Let also . For any  there exists  having the formsuch thatand as  Moreover, if  is positive and  is the corresponding approximate solution constructed for , then for any  and  one hasfor some .  We can now give the proof of the boundary determination result.
Proof of Theorem 9. Using the assumption that 
 together with the integral identity in Lemma 2, we have that
        
        whenever 
 solves 
 in 
.
Let 
, let 
 be a unit tangent vector to 
 at 
, and let 
 satisfy 
 near 
. We use Proposition 2 to construct functions
        
        so that
        
We obtain exact solutions 
 of 
 by setting
        
        where the correction terms 
 are the unique solutions of
        
By standard energy estimates ([
23], Section 6.2) and by (27), the solutions 
 satisfy
        
We now insert the solutions 
 into (26). Using (28) and (27), it follows that
        
        as 
. Letting 
, the formula (25) yields
        
In particular, .
We will prove by induction that
        
The case 
 was proved above (here we may vary 
 slightly). We make the induction hypothesis that (30) holds for 
. Let 
 be boundary normal coordinates so that 
 corresponds to 0, and 
 near 
 corresponds to 
. The induction hypothesis states that
        
Considering the Taylor expansion of 
 with respect to 
 gives that
        
        for some smooth function 
f with 
. Inserting this formula in (29), we obtain that
        
Now 
 in boundary normal coordinates. Assuming that 
N was chosen larger than 
k, we may take the limit as 
 and use (25) to obtain that
        
This shows that  for  near 0, which concludes the induction. □
 It remains to prove Proposition 2, which constructs approximate solutions (also called quasimodes) concentrating near a boundary point. This is a typical geometrical optics/WKB type construction for quasimodes with complex phase. The proof is elementary, although a bit long. The argument is simplified slightly by using the Borel summation lemma, which is used frequently in microlocal analysis in various different forms.
Lemma 3 (Borel summation, ([
3] Theorem 1.2.6))
. Let  for . There exists  such that Proof of Proposition 2. We will first carry out the proof in the case where  and  is flat near 0, i.e.,  for some  (the general case will be considered in the end of the proof). We also assume  where .
We look for 
v in the form
        
Write 
. The principal symbol of 
P is
        
Since 
, we compute
        
We want to choose 
 and 
b so that 
. Looking at the 
 term in (32), we first choose 
 so that
        
We additionally want that 
 and 
 (this will imply that 
). In fact, using (31) we can just choose
        
        and then 
 in 
.
We next look for 
b in the form
        
Since 
, (32) implies that
        
We will choose the functions 
 so that
        
We will additionally arrange that
        
        and that each 
 is compactly supported so that
        
        for some fixed 
.
To find 
, we prescribe 
, 
… successively and use the Borel summation lemma to construct 
 with this Taylor series at 
. We first set 
. Writing 
, we observe that
        
Thus, in order to have 
 we must have
        
We prescribe 
 to have the above value (which depends on the already prescribed quantity 
). Next we compute
        
        where 
Q depends on the already prescribed quantities 
 and 
. We thus set
        
        which ensures that 
. Continuing in this way and using Borel summation, we obtain a function 
 so that 
 to infinite order at 
. The other equations in (35) are solved in a similar way, which gives the required functions 
. In the construction, we may arrange so that (36) and (37) are valid.
If 
 and 
 are chosen in the above way, then (34) implies that
        
        where each 
 vanishes to infinite order at 
 and is compactly supported in 
. Thus, for any 
 there is 
 so that 
 in 
, and consequently
        
Since 
 in 
 we have
        
Choosing 
 and computing the integrals over 
, we get that
        
It is also easy to compute that
        
Thus, choosing , we have proved all the claims except (25).
To show (25), we observe that
        
Using a similar formula for 
 (where 
 is independent of the conductivity), we have
        
Now 
 and 
 where 
, and similarly for 
. Hence
        
We can change variables 
 and use dominated convergence to take the limit as 
. The limit is
        
        where 
.
The proof is complete in the case when 
 and 
 is flat near 0. In the general case, we choose boundary normal coordinates 
 so that 
 corresponds to 0 and 
 near 
 locally corresponds to 
. The equation 
 in the new coordinates becomes an equation
        
        where 
A is a smooth positive matrix only depending on the geometry of 
 near 
. The construction of 
v now proceeds in a similar way as above, except that the equation (33) for the phase function 
 can only be solved to infinite order on 
 instead of solving it globally in 
. □