On finding a buried obstacle in a layered medium via the time domain enclosure method
Masaru Ikehata, Mishio Kawashita

TL;DR
This paper develops a method to detect and analyze a penetrable obstacle in a layered medium using wave observations in the time domain, providing insights into the obstacle's geometry and properties.
Contribution
It introduces an indicator function based on the time domain enclosure method for inverse obstacle problems in layered media, revealing geometric and qualitative obstacle information.
Findings
The indicator function can determine the obstacle's shape and location.
Asymptotic analysis yields qualitative properties of the obstacle.
Method applicable to penetrable obstacles in layered environments.
Abstract
An inverse obstacle problem for the wave equation in a two layered medium is considered. It is assumed that the unknown obstacle is penetrable and embedded in the lower half-space. The wave as a solution of the wave equation is generated by an initial data whose support is in the upper half-space and observed at the same place as the support over a finite time interval. From the observed wave an indicator function in the time domain enclosure method is constructed. It is shown that, one can find some information about the geometry of the obstacle together with the qualitative property in the asymptotic behavior of the indicator function.
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On finding a buried obstacle in a layered medium
via the time domain enclosure method
Masaru IKEHATA
Laboratory of Mathematics, Graduate School of Engineering, Hiroshima University, Higashihiroshima 739-8527, JAPAN; [email protected]
Mishio KAWASHITA Department of Mathematics, Graduate School of Sciences, Hiroshima University, Higashihiroshima 739-8526, JAPAN; [email protected]
Abstract
An inverse obstacle problem for the wave equation in a two layered medium is considered. It is assumed that the unknown obstacle is penetrable and embedded in the lower half-space. The wave as a solution of the wave equation is generated by an initial data whose support is in the upper half-space and observed at the same place as the support over a finite time interval. From the observed wave an indicator function in the time domain enclosure method is constructed. It is shown that, one can find some information about the geometry of the obstacle together with the qualitative property in the asymptotic behavior of the indicator function.
**2010 Mathematics Subject Classification: ** 35L05, 35P25, 35B40, 35R30.
Keywords enclosure method, inverse obstacle scattering problem, buried obstacle, wave equation, subsurface radar, ground probing radar
1 Introduction
The problem of finding an obstacle embedded or hidden in a complicated environment by using the electromagnetic wave appears in, for example, ground penetrating or subsurface radar [4] and the through-wall imaging [2].
In this paper, we consider such type of the problems in a simplest, however, important mathematical model which employs a wave governed by a scalar wave equation in a two homogeneous layered medium over a finite time interval.
Let . Consider given by
[TABLE]
where are positive constants.
Let be a bounded open subset of with a -boundary and satisfy . Consider given by
[TABLE]
where , is a real symmetric -matrix valued function and satisfies that: all the components of are essentially bounded on ; there exists a positive constant such that for all and a.e. .
Let . Given let be the weak solution of the initial value problem:
[TABLE]
Note that the solution class is taken from [5]. See also [10] for its detailed description.
We consider the following problem:
Problem. Assume that . Fix a large (to be determined later). Assume that is known and that both and are unknown. Let be an open ball whose closure is contained in . Fix a with and satisfying that there exists a positive constant such that a.e. or a.e. . Generate of the solution of (1.1) by the . Extract information about the location and shape of from the measured data on over the time interval .
It should be emphasized that the problem asks us to extract information about unknown obstacle from a single wave observed over a finite time interval at the same place where the wave is generated. There are some studies which consider the time harmonic reduced case in a two layered medium. See [17] for uniqueness issue of impenetrable obstacles using infinitely many incident fields; [18] a reconstruction scheme of an impenetrable obstacle using a far-field pattern corresponding to a single incident plane wave; [6] study of a direct problem with an application to mine detection and propose a numerical reconstruction scheme using near field measurements corresponding to finitely many incident sources. Clearly our problem formulation is different from their one and to our best knowledge there is no result for the problem.
In [10] Ikehata has considered the case when and the wave is observed on a closed surface over a finite time interval which encloses the obstacle. He assumed that satisfies one of the following two conditions:
(A1) there exists a positive constant such that for all and a.e. ;
(A2) there exists a positive constant such that for all and a.e. .
In Theorem 1.2 of [10] he showed that if is outside surface , then one can extract the distance from the observed wave and also can distinguish whether (A1) or (A2) is satisfied by using the signature of an indicator function computed from the observed wave. This is the beginning of the multi-dimensional version of the time domain enclosure method [9] for inverse obstacle scattering in the time domain. In [11] this idea has been extended to the case when the wave is observed on the same place as the support of an initial data. This is a version of the near field inverse back-scattering problem. One can easily transplant the results in [10] to this case as pointed out in Subsection 1.3 of [11]. However, the case when is not trivial. Clearly this is a quite interesting case from practical and mathematical point of view. The unknown obstacle is embedded in the lower half-space which has a different refractive index from the upper half-space. Thus the wave generated by an initial data produces reflected and refracted waves at the interface. The produced refracted wave hits the surface of the obstacle and generates reflected and refracted waves. How can one extract information about the geometry of the obstacle from the observed wave? The aim of this paper is to extend the previous result to the case when using the enclosure method in the time domain.
Now let us describe our main result. Let . Let be the solution of (1.1). Define
[TABLE]
Let be the weak solution of
[TABLE]
Define
[TABLE]
We call the function the indicator function. Note that this symbol follows from that of [12].
Define
[TABLE]
where
[TABLE]
and
[TABLE]
The quantity corresponds to the optical distance or optical path length between and in optics and it is easy to see that we have
[TABLE]
where and denote the center and radius of , respectively and
[TABLE]
Thus the unknown obstacle is contained in the set
[TABLE]
The following theorem is the main result of this paper.
Theorem 1.1
Assume that . Then, we have:
[TABLE]
Moreover, if satisfies (A1) or (A2), then for all
[TABLE]
From Theorem 1.1 we see that the in the problem should be an arbitrary number satisfying . We think that this is optimal. From the indicator function one gets the value and thus the set which encloses . Moreover, one can distinguish whether unknown obstacle satisfies (A1) or (A2) which is a qualitative property of relative to the surrounding background medium, by checking the asymptotic behavior of the indicator function.
Remark 1.2
Intuitively, any signal emanating from reaches . For these signals to go back to the upper side, we need to catch the refracted waves of the reflected waves by . Hence we need to take measurement in at least till time for which the fastest signals may come back. To check whether signals are exactly coming back, we need to take account of total reflection waves. Assumption means that the propagation speed of waves in the upper side is slower than that of the lower side. Hence, there is no total reflected wave for the incident waves from the lower side. This is the case that we do not need to take care of it. Mathematically, this is appeared as a difficulty for obtaining asymptotics of the refracted wave. As is in (1.14) and (1.15) below, it is relatively simple since it does not contain waves for total reflection.
The proof of Theorem 1.1 employs two important facts. The first one is the following lemma.
Lemma 1.3
We have, as
[TABLE]
and
[TABLE]
For the proof see Appendix. Combining (1.6) and (1.7) under the assumption (A1) or (A2), we can easily see that Theorem 1.1 can be proved if one has the following fact concerning with the asymptotic behavior of on as .
Theorem 1.4
Assume that is and that . Then, there exist positive numbers and such that, for all we have
[TABLE]
This is the second important fact. We found that the proof of Theorem 1.4 is not a simple matter and thus the remaining part of this paper is devoted to the proof. In this sense, the main contribution of this paper to the enclosure method in the time domain is the establishment of the estimate (1.8). Note that in [16, 3] one can find some formal asymptotic computation of the solution of (1.3), however, we do not know whether or not their formal theory enables us to derive estimate (1.8).
In [12], Ikehata considered a mathematical model of the through-wall imaging by using the enclosure method in the time domain. Originally the governing equation should be the Maxwell system, however, as a first step, it is assumed that the governing equation is given by the single wave equation in with the initial data and in . The assumption on the function is that: has a positive lower bound in and takes the form
[TABLE]
where the function is essentially bounded in with a positive lower bound; is an arbitrary bounded open set of the whole space with a Lipschitz boundary; the function or has a positive essential infimum on .
Remarkably enough, in [12] a higher regularity more than the essential boundedness of is not assumed. Thus the model covers various background media such as multilayered media with complicated interfaces or unions of various domains with different refractive indexes. He showed that an indicator function computed from the wave observed on the same place as the support of an initial data yields lower and upper estimates of the distance together with a criterion whether or provided is known. The result is based on a system of inequalities similar to (1.6) and (1.7) in Lemma 1.3 and explicit upper and lower estimates of the solution of the equation
[TABLE]
In contrast to this result, Theorem 1.1 tells us that one can extract the exact value of the optical distance from the asymptotic behavior of the indicator function under the assumption that the background medium consists of two isotropic homogeneous layered media. It would be possible to apply the idea of the derivation of the estimate in Theorem 1.4 to the case when takes two different constants, in and in provided which corresponds to . However, a typical case to be considered for the Maxwell system is: the upper layer consists of air and the lower of material, like soil, wall, etc., see [4] and [2]. In our problem setting this corresponds to the case when . Developing an analysis that covers this case together with application to the Maxwell system belongs to our next project. See also [13] for a survey on recent results for inverse obstacle scattering via the time domain enclosure method and [15] for applications to the inverse boundary value problems for the heat equation in three-dimensional space.
The outline of this paper is as follows. Let be the fundamental solution of (1.3), which satisfies
[TABLE]
Since the solution of (1.3) is written by the convolution of and as
[TABLE]
we obtain
[TABLE]
Thus, we need to know an asymptotic behavior of as for with , and .
The first step for obtaining the asymptotic behavior of (1.9) is to show that the fundamental solution for is given by
[TABLE]
which is given in Section 2. In (1.10), is a function given by
[TABLE]
where is the point on the transmission boundary and is a function of standing for the transmission coefficient given by
[TABLE]
Note that can be interpreted as the refracted part of the fundamental solution.
We put
[TABLE]
which is a fundamental solution for the equation corresponding to the case that there is no transmission boundary, i.e. , and given by
[TABLE]
Thus, (1.10) stands for the refraction phenomena by the transmission boundary .
As in Proposition 3.1, for any , the refracted wave is of the form:
[TABLE]
where each is a function in , and is a continuous for and , and satisfies
[TABLE]
For the gradient , as is in Proposition 3.1 and Remark 3.2, we have
[TABLE]
where each is a function in , and is continuous for and , and satisfies
[TABLE]
The main task of Section 3 is to show (1.14) and (1.15).
From (1.14), (1.15) and (1.10), the original problem can be reduced to finding asymptotics of the Laplace integral of the form:
[TABLE]
where , i.e., the function belongs to the space of all functions in of whose all derivatives are bounded functions in . For , we put .
By usual Laplace’s method, the main part of the asymptotics for (1.16) is given by points attaining the minimum of . We can check the point uniquely exists, which corresponds to Snell’s law in geometrical optics. Further, we can show that is a function for and is positive definite, where (cf. Lemma 4.1). We put and
[TABLE]
Take with and near the set , and divide (1.16) into two parts,
[TABLE]
Note that usual Laplace’s method (cf. Theorem 7.7.5 of Hörmander [7], which is for oscillatory integrals, however, the proof also works for this case) can be applied for the first integral of (1.17). For the second integral of (1.17), integration by parts implies that this term is negligible. Hence we obtain
[TABLE]
where is a differential operator of order less than or equal to given by
[TABLE]
and for any , there exists a constant depending also on such that
[TABLE]
From (1.18), we can obtain the asymptotic expansion of of the form:
Proposition 1.5
Assume . Then have the following asymptotics:
[TABLE]
where are in , for any , are continuous in with a constant satisfying
[TABLE]
Moreover, are given by
[TABLE]
Note that in (1.19), is the function appeared in (1.14). The form of is given by (3.26) in Section 3.
Proposition 1.5 is crucial to obtain Theorem 1.4. A proof of Proposition 1.5 is given in Section 4. In Section 5, we show Theorem 1.4 by using Proposition 1.5. This is the outline of this paper.
2 The refracted part of the fundamental solution
In what follows, we only treat the case , , for large . Note that the fundamental solution is given by
[TABLE]
where is the solution of
[TABLE]
and satisfy
[TABLE]
In what follows, we also write , .
For , Fourier transform implies
[TABLE]
We put
[TABLE]
Since
[TABLE]
we obtain
[TABLE]
which is the representation by the partial Fourier transform
[TABLE]
of for the tangential direction .
To obtain , we take the partial Fourier transform
[TABLE]
which satisfy the partial Fourier transform of (2.3), that is,
[TABLE]
Since are bounded, from (2.5), the solutions of (2.8) are given by
[TABLE]
where
[TABLE]
We concentrate on for . From (2.9), (2.4) and (2.5), it follows that
[TABLE]
which yields
[TABLE]
Since for , and , we obtain
[TABLE]
for . Since (1.12) implies , noting (1.13), (1.11) and the above formula of for , we obtain (1.10).
We can also obtain the formula of for , which is for the reflected phenomena. In this case, , which yields
[TABLE]
for similarly. In this paper, we do not use this formula.
3 Asymptotics of the refracted waves
In this section, we show the asymptotics (1.14) and (1.15) for the refracted wave defined by (1.11). We put and . From (1.11), it follows that
[TABLE]
where
[TABLE]
Note that from (2.4), it follows that
[TABLE]
which yields
[TABLE]
by rotating the coordinate. Thus, we obtain
[TABLE]
We change the variable , and have
[TABLE]
which yields
[TABLE]
For , , we put
[TABLE]
where
[TABLE]
To obtain the asymptotics of and , we need to study the asymptotics of (3.3). We use the steepest decent method, which is similar to getting the distribution kernel for the usual wave equations in the two dimensional half-space by Hankel functions (cf. [1], p. 286 for example).
We take satisfying
[TABLE]
and put and
[TABLE]
Then, (3.3) is written by
[TABLE]
From (3.8), it follows that . Hence, putting for , we have , which yields
[TABLE]
We denote by the curve defined by (3.10). This is the steepest decent curve of integral (3.9). The contour of (3.9) should be changed for .
We take any with . Then, for with and ,
[TABLE]
since for . Hence, we have
[TABLE]
since for . Similarly, we also obtain
[TABLE]
since in this case, it follows that
[TABLE]
From these asymptotics, it follows that defined by (3.8) satisfies
[TABLE]
Noting , and (3.11) and (3.12), we also have
[TABLE]
for .
From (1.12), it follows that
[TABLE]
where
[TABLE]
Since , we have
[TABLE]
where
[TABLE]
In what follows, we assume , being the case that there is no total reflected wave for incident waves coming from the lower side (cf. Remark 1.2). In this case, . Hence, and are holomorphic for . From this, (3.13) and (3.14), we can change the contour of (3.9) for , which yields
[TABLE]
We can express this integral by using the parametrization of given by (3.10). In this parametrization, , and (3.10) and (3.15) implies
[TABLE]
and we obtain
[TABLE]
Note that are function of since imples . For simplicity, we write , and , and put
[TABLE]
Notice that (3.6), (3.10) and (3.15) imply that
[TABLE]
From (3.1), (3.2) and (3.18), it follows that
[TABLE]
From (3.22)-(3.25), the problem is reduced to finding the asymptotics of
[TABLE]
as . For treating these integrals, we need to assume , which implies that the amplitude functions in (3.23)-(3.25) are smooth. This allows to use the Laplace methods to give the asymptotic expansions for and its gradient.
Proposition 3.1
Assume . Then, it follows that
[TABLE]
where , ( and are functions for and . Here, the remainder terms and are estimated by
[TABLE]
for some constant depending only on . In particular, we have
[TABLE]
where is given by (3.16), and
[TABLE]
Proof: Note that in the integrals of (3.23)-(3.25) has only one critical point , and , where is the Hessian of at and is the unit matrix. Since for , we have
[TABLE]
Further, there exists a constant such that
[TABLE]
Take with , for , and . From (3.27) and (3.28), it follows that
[TABLE]
and usual Laplace’s method as is stated in Introduction implies
[TABLE]
where and
[TABLE]
In (3.30), is given by
[TABLE]
where .
Since , for
[TABLE]
we have for , which yields that holds for with . Thus, the summation of (3.31) is not taken from all pairs in (3.31). It consists only from pairs with and , which implies
[TABLE]
From (3.7) and (3.22), it follows that
[TABLE]
Since (3.32) and (3.10) imply that for ,
[TABLE]
From (3.6) and (3.17), it follows that which yields
[TABLE]
where the relations between and is given by (3.7).
Combining (3.23)-(3.25) with (3.29) and (3.30), we obtain the asymptotics stated in Proposition 3.1 except the properties of the coefficients functions and . Notice that and are given by
[TABLE]
and
[TABLE]
From (3.36), (3.37) and (3.7), we also have the forms of , , and . The remaining parts are to prove smoothness of the coefficients.
For , we denote by the set consisting of functions of of the form:
[TABLE]
where are for with some positive . Note that any is regarded as a function in by relations (3.7).
First, we show smoothness of . Since is an even function with respect to each of and , (i.e. and ), and is a function for and , for , is of the form:
[TABLE]
where for is a function for , with a sufficiently small , and is an even function with respect to each of and , (i.e. ), and is a and an odd function in a neighborhood of . From (3.32) and (3.38), it suffices to show for any ,
[TABLE]
Since is an even function with respect to and , it follows that
[TABLE]
where is defined by
[TABLE]
for and . Since is odd, \partial_{\rho}^{2l}\big{[}\rho^{2\gamma_{1}}(\varphi(\rho))^{\gamma_{2}}\big{]}\big{|}_{\rho=0}=0 for any odd , Taylor’s theorem implies since can be written as
[TABLE]
Combining shown in the above, (3.42) with (3.44), we obtain (3.43), which yields smoothness of in and for (3.32).
Next, we show smoothness of . From (3.35) and (3.41), are given by
[TABLE]
Since is also a function for and , is the same form as (3.42), which yields that is for and . Thus, it suffices to show that is for and .
From (3.19), by using a function with the same property as for in (3.42), we can write as
[TABLE]
Since there is in (3.45) for , we have
[TABLE]
Moreover, Taylor’s theorem implies
[TABLE]
since \partial_{\rho}^{2l-1}\big{[}(\rho^{2\gamma_{1}}(\varphi(\rho))^{\gamma_{2}}\big{]}\big{|}_{\rho=0}=0 for even . From these equalities, we obtain
[TABLE]
with some . From this property and (3.32), is of the form:
[TABLE]
with some function for and . Hence, we have
[TABLE]
which complete the proof of Proposition 3.1.
Remark 3.2
We put . From the proof of Proposition 3.1, the vector valued functions are of the form
[TABLE]
Using these and putting , we obtain (1.15). Further,
[TABLE]
4 Snell’s law and the asymptotics of and
In this section, the Laplace integral (1.16) is treated. First, we check the properties of function (1.5), which describes Snell’s law.
Lemma 4.1
The function in defined by (1.5) satisfies the following properties:
(1) Fix with and . For the function defined by (1.4), there exists the unique point satisfying . This point is denoted by . This point is on the line segment .
(2) There exists a constant such that
[TABLE]
(3) The point is for with and .
Proof: In the beginning, we show
[TABLE]
To obtain (4.1), it suffices to show for satisfying , and for . Suppose , then it follows that
[TABLE]
Since , we have
[TABLE]
For , is shown similarly, which yields (4.1).
From (4.1) and , there exists a point attaining the minimum of . Since this point satisfies ,
[TABLE]
where is taken by
[TABLE]
From (4.2), it follows that is on the segment , and satisfies Snell’s law,
[TABLE]
We show that this point is unique. If , then , which yields . Thus, is uniquely determined. If , this point is expressed by for some . We define by . Note that satisfies . Since , and for , there exists only one with , which yields uniqueness of . Thus, we obtain (1) of Lemma 4.1.
For (2), differentiate and obtain
[TABLE]
We put . Then, (4.2) and (4.3) implies since is in the line segment , which yields
[TABLE]
Hence, we have
[TABLE]
Since is bounded, there exist constants and such that
[TABLE]
Note that is monotone increasing for , for , it follows that
[TABLE]
Combining the above estimate with (4.5), we obtain
[TABLE]
which yields (2).
Last, we show (3). We put , which is for , and . Further, from (2), we obtain {\rm det}\Big{(}\frac{\partial{F}}{\partial{z^{\prime}}}(z^{\prime}(x,y))\Big{)}\neq 0. Hence implicit function theorem yields smoothness of .
Note that (4.4) implies
[TABLE]
for and . Hence, the eigenvalues and eigenvectors of the Hessian are given by
[TABLE]
where is a unit vector with . Thus, we also obtain
[TABLE]
Now we are in the position to show Proposition 1.5. Here, we need to assume .
Proof of Proposition 1.5. From (1.10) and (1.14), we have
[TABLE]
where
[TABLE]
From Proposition 3.1, are for and , which yields . Hence, we can apply (1.18) for each Laplace integral with , and obtain the asymptotics. For the remainder term of (4.6),
[TABLE]
Thus, we obtain the asymptotics for in Proposition 1.5 uniformly in , where is given by . Hence, we also have , which yields (1.19).
For , differentiating (1.10), and using (1.15), we obtain
[TABLE]
where
[TABLE]
From Proposition 3.1, are for and , which yields . Hence, as for , we obtain the asymptotics for described in Proposition 1.5. In this case, is given by . From this and Remark 3.2, we obtain
[TABLE]
which yields (1.20). This completes the proof of Proposition 1.5.
5 Proof of Theorem 1.4
We put ,
[TABLE]
[TABLE]
and . From Proposition 1.5 for , it follows that
[TABLE]
where . From (3.26), there exist constants such that
[TABLE]
Lemma 5.1
Put and .
(1) . Further, if , satisfy , then .
(2) If , satisfy , then and . Further,
[TABLE]
where and are the unit outer normal of and at and , respectively.
(3) If , satisfy , then and .
Proof: For any and , . Since is continuous on the compact set , we can take points and satisfying , which implies . Thus, we obtain (1).
To show (2), assume that , satisfy . If , there exists such that , where for and , we put . We put , , and . Then, for , and . These imply
[TABLE]
which is contradiction. Thus, we obtain . Similarly, we have .
Next, we show is a unit outer normal of at . Take any class curve with . Since
[TABLE]
and , the function take a minimum at . This implies
[TABLE]
which yields is a unit normal of .
To obtain is outward, it suffices to show for small enough. For any , it follows that
[TABLE]
which yields . For , we can show similarly, which obtain (2).
Last, we show (3). Take and with . From , , it follows that
[TABLE]
which yields . We can obtain similarly. To finish the proof, it suffices to show .
We put , , and , where and are determined by (1) of Lemma 4.1, respectively. From (2) of Lemma 5.1, . Taking the inner product of this vector and , we obtain , where . Since , it follows that , which yields . From this and , also follows.
Now, we remember Snell’s law,
[TABLE]
which are derived from (4.2) and (4.3). These relations imply . Since , it follows that , which yields since both are positive. Thus, we obtain , which completes the proof of Lemma 5.1.
Now, we are in a position to show Theorem 1.4. Combining (5.1)-(5.4) and (1.9) with (1) of Lemma 5.1, we obtain the estimate of the right side in (1.8). The problem is to show the left side of (1.8).
Since for , , and is continuous for , , which is from Lemma 4.1, there exists a constant such that
[TABLE]
We can take in (5.5) sufficiently small to be .
Put and . (1) and (3) of Lemma 5.1 imply and , and . Since is a compact set, there exist finite points such that , where is given in (5.5). Then, holds.
We put . Since for , from (5.5), it follows that
[TABLE]
Since , on the compact set . Thus, there exists such that
[TABLE]
From (5.6), (5.3) and (5.4), for any , it follow that
[TABLE]
which yields that there exists a constant such that . From (5.3) and (5.4), for any , it follows that
[TABLE]
which imples .
From the above estimates of , and (5.1), (5.7), (5.2), (5.4), (1.9) and the assumption for , it follows that
[TABLE]
where . Thus, to obtain the left hand of (1.8), it suffices to show the following estimate:
Lemma 5.2
There exist and such that
[TABLE]
Proof: In what follows, we write and as and , respectively. Since (2) of Lemma 5.1 implies and , and and are surfaces, there exist , and such that , , and . Then, , and
[TABLE]
We put and . Since
[TABLE]
it follows that
[TABLE]
As in (2) of Lemma 5.1, , which yields . Then, from Proposition 3.2 of [14], it follows that there exist constants and such that
[TABLE]
Similarly, taking the constants and larger if necessary, we also obtain
[TABLE]
Hence, we have
[TABLE]
since
[TABLE]
which completes the proof of Lemma 5.2.
Acknowledgements
MI was partially supported by JSPS KAKENHI Grant Number JP17K05331. MK was partially supported by JSPS KAKENHI Grant Number JP16K05232.
Appendix A Appendix. Proof of Lemma 1.3
The function defined by (1.2) satisfies
[TABLE]
where
[TABLE]
Define
[TABLE]
It is easy to derive the following decomposition formula of the indicator function which formally corresponds to the case when on (3.2) of Proposition 3.1 in [10].
Proposition A.1
We have
[TABLE]
It follows from (A.1) that satisfies
[TABLE]
where
[TABLE]
And also satisfies
[TABLE]
where
[TABLE]
Thus, changing the role of and in (A.3), we obtain
[TABLE]
This is noting but the following formula.
Proposition A.2
We have
[TABLE]
Now we are ready to prove (1.6) and (1.7). It follows from (1.3) that
[TABLE]
that is
[TABLE]
This yields, as
[TABLE]
Hence we obtain, as
[TABLE]
and
[TABLE]
Rewrite (A.3) as
[TABLE]
Here from (A.2) we have
[TABLE]
This together with (A.5) and (A.6) yields that the right-hand side on (A.7) has a bound . Thus we obtain
[TABLE]
and, in particular,
[TABLE]
Now applying (A.5) , (A.8) and (A.9) to the fourth-term in the right-hand side on (A.3) we obtain
[TABLE]
This immediately yields (1.6).
For the proof of (1.7) we recall the following inequality (see [8])
[TABLE]
where and are real vectors. Applying this to the first and second term in the right-hand side on (A.4), we obtain
[TABLE]
Now applying (A.5), (A.8) and (A.9) to the second term in this right-hand side we obtain (1.7).
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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