Fikret GLGELEYEN Masahiro YAMAMOTO
(Dedicated to the memory of Professor Arif Amirov)
Letn,m∈N andx∈Rn,y∈Rm.We consider the ultrahyperbolic equation
in some bounded domain of(x,y)∈Rn×Rm.We set
and
Ifm=1,then(1.1)is a hyperbolic equation,wherey1is the time variable.Generally,it is considered that one time dimension is fundamentally important in describing many dynamic evolutions of physical quantities in the classical and quantum fields.Multiple times have been considered rarely,because it is widely believed to violate the causality and lead to the instability yielding that the phenomena under consideration are not deterministic in a usual physical sense.However,certain developments in the theoretical physics such as the string theory requireadditional dimensions for the time,and for related literature,we refer to Bars[4],Craig and Weinstein[11],Sparling[29],and Tegmark[31].In particular,the multiple dimensions are considered in the context of the twistor spaces(see[29]).
The quantum kinetic theory is one of the fields in which ultrahyperbolic type equations are arising.For example,let us consider the quantum kinetic equation:
in a domain{(x,p,t);x=whereu(x,p,t)is the quantum distribution function,his Planck’s constant,i is the imaginary unit, Φ(x,t)is the potential andf(x,p,t)is the function characterizing the sources.Applying the Fourier transform with respect topand the change of variables of the form
one can obtain the following ultrahyperbolic type equation:
wherew(ξ,η,t)=denote the Fourier transform ofuandfrespectively(see[2]).The ultrahyperbolic operator appears also as the stationary part of a generalized Schrdinger equation:
and for related nonlinear generalized Schrdinger equations,see[18–19,30].
The solutions of some direct problems to ultrahyperbolic equations were investigated by Kostomarov[24–25]in the case ofn=3,m=2 andn=3,m=3.As for the uniqueness and some mean value property of solutions to general ultrahyperbolic equations,see[10,12,14,27],but there are very few results on the existence of the solution.In[11],the unique existence of solutions was proved forwith suitably given initial data and also some non-uniqueness results were proved by some choice of hyperplanes,where the initial data are given.The proof in[11]assumed that all the coefficients in the ultrahyperbolic equation are constant in the whole domain because the key is the Fourier transform.There seems to be no result on the existence of the solution to a Cauchy problem of the ultrahyperbolic equation with non-analytic coefficients.In the case of analytic coefficients,by the Cauchy-Kovalevskaja theorem,we can establish the well-posedness of the initial value problem of determining the solutionuto(1.1)satisfyingwhereaandbare analytic.
In this article,we discuss inverse problems of determining a coefficient or a source term in an ultrahyperbolic equation.First we formulate an inverse source problem.
LetD⊂Rnbe a bounded domain with smooth boundary∂Dand let
We arbitrarily fix
Henceforth(·,·)means the scalar product in Rnand Rm.ForT,T1>0,we set
In particular,we write
Throughout this article,we identifyLetp(x,y′)be given,ν(x)=(ν1(x),···,νn(x))denote the unit outward normal vector to∂D,and∂νu=(∇xu,ν).Moreover,letT,T1>0 and Γ⊂∂Dbe given.We consider the following system:
We consider an inverse problem of determiningf(x,y′)in(1.2)by extra data of the solution to(1.2)–(1.4).
Inverse Source ProblemLetp,Rbe given suitably.Then determinef(x,y′),x∈D,Here we do not assume the uniqueness ofu,but its existence.
Next we discuss an inverse problem of determining a coefficient by overdetermining lateral boundary data.More precisely,we consider
Letv=v(p)satisfy(1.5)–(1.7).We discuss the following problem.
Coefficient Inverse ProblemDetermine the coefficientin(1.5)by extra data
Our main purpose is to establish the uniqueness and the stability for these inverse problems,assuming the existence ofv(p)andv(q)within adequate classes.
The coefficient inverse problem is reduced to the inverse source problem as follows.Letv(p)andv(q)be two solutions of(1.5)–(1.7)with the coefficientspandqrespectively.Here we do not assume the uniqueness ofv(p)andv(q)but their existence.
The differenceu=v(p)−v(q)satisfies(1.2)–(1.4),whereandR=v(q)(x,y).Therefore the determination ofp,qis reduced to the inverse source problem.
Thus we first discuss the inverse source problem for(1.2)–(1.4).For the statements of the main results,we introduce the following notations.Forδ>0,x0and 0<β<1,we define the domains by
We use the same notationsforG=if there is no fear of confusion.LetM>0 be arbitrarily fixed.
We are ready to state the following theorem.
Theorem 1.1We consider(1.2)–(1.3)in D×G.Let
We further assume that
and that there exists a constant r0>0such that
Finally we assume
and thatΓ⊂∂D satisfies
Then for any δ1>δ,there exist constants C>0and θ∈(0,1),depending on M,r0such that
Theorem 1.1 gives a local estimate.More precisely,given Γ⊂∂DandT>0,we can find a subdomainwhere theL2-norm offis estimated.For example,we chooseδ>0 with> δand 0<t0<Tarbitrarily.We takeβsufficiently small such thatFor thisβ,we chooseT>0 sufficiently large such that(1.8)holds.Then Theorem 1.1 asserts
In fact,we chooseδ1>0 sufficiently close toδsuch thatSincefor|x−x0|<t0,we see thatTherefore(1.10)yields(1.11).
If we want to estimateffor largert0,thenβhas to be small and so we have to chooseT>0 very large,that is,we need to observe longer iny-direction as the right-hand side of(1.11)shows.In particular,for sufficiently largeδ1we haveand so the left-hand side of(1.11)estimatesfoverDprovided thatt0is small andT>0 is very large.The above observation means that if we want to estimatefin a larger subdomain ofD,then the sizeTof the “time” region has to be large.This fact corresponds to the finiteness of the propagation speed,which is a typical character for the case ofm=1.
In Theorem 1.1,it is not clear how largeTand Γ are necessary for identifyingfin a given subdomain orD×G′.Next we derive the estimation offin an arbitrarily given subdomain ofD×G′.For the statement,we recall
withT>0.Forwe set
We note that∂D+is a proper subset of∂Din general.
Theorem 1.2Let u satisfy(1.2)–(1.3)in D×G(T,2T)and u=0on∂D×G(T,2T)and
We further assume that β>0is sufficiently small and
and that
and
Then for any small>0,there exist constants C>0and θ∈(0,1)depending on,M,x0,such that
Next we show stability results for the coefficient inverse problem.We state two results which correspond to Theorems 1.1–1.2,respectively.
Theorem 1.3We consider(1.5)–(1.7).Let
with some r0>0.We assume that0<β<1,(1.8)and(1.9)hold.Then for any δ1>δ,there exist constants C>0and θ ∈(0,1),depending on M,r0,such that
Theorem 1.4Let v(p),v(q)satisfy(1.5)–(1.6)with p,q respectively and v(p)=v(q)on∂D×G(T,2T).We assume
with some r0>0.We further assume
Then for any small>0,there exist constants C>0and θ∈(0,1)depending on,M,x0,such that
As is seen by the proof in Section 4,in Theorem 1.2,we can obtain the same stability in the case whereG(T,2T)is replaced by a smallerG:=if we can take also the norm of data on the other subboundary ofG:
whereνis the unit outward normal vector to∂GandA similar remark holds for Theorem 1.4.Moreover,if we have an a priori Lipschitz estimate for the direct problem for(1.2)–(1.3)withu=0 on(∂D×G)∪(D×then the same method as Imanuvilov and Yamamoto[16]can yield the Lipschitz stability,but we do not know such Lipschitz stability for the direct problem form≥2.In the case ofm=1,that is,the inverse hyperbolic problem,we can replace(1.15)by the Lipschitz stability(see[15–16])and we note that we need not fix>0.Moreover,for the uniqueness offinD×we need a boundary datum∂νuover∂D+×<2T},that is,we need a twice longery′-region for the observation than the domain iny′wherefis determined.
In Theorems 1.2 and 1.4,we can not take=0.However,since>0 is arbitrary,we can prove the uniqueness:For example,in Theorem 1.2,ifu(x,y)=0 forx∈ ∂D,|y1|<Tand<2Tand∂νu(x,y)=0 forx<2T,thenf(x,y′)=0 forx∈Dand
The proofs of the theorems are based on the method by Bukhgeim and Klibanov[9].In[9],the authors first applied a Carleman estimate which is anL2-estimate with large parameters,and then established the uniqueness in determining a spatially varying coefficient by overdetermining lateral boundary data.After[9],there have been many works relying on that method with modified arguments.We refer to Amirov[1–2],Amirov and Yamamoto[3],Baudouin and Puel[5],Bellassoued[6],Bellassoued and Yamamoto[7–8],Imanuvilov and Yamamoto[15–16],Isakov[17],Kha˘ıdarov[20],Klibanov[21–22],Klibanov and Timonov[23],and Yamamoto[32].Here we do not intend to give a complete list of the works and refer to the references therein.There are satisfactory amounts of works on classical equations in mathematical physics,but there are very few works for inverse problems of ultrahyperbolic equations.A key Carleman estimate was proved by Amirov[1–2]and Lavrent’ev,Romanov and Shishat·ski˘ı[26],where they applied the Carleman estimates to the unique continuation and proved stability.See also Romanov[28]for a Carleman estimate for an ultrahyperbolic equation in a Riemannian manifold and an application to some unique continuation problems.In Chapter 4 of Amirov[2],the uniqueness for an inverse source problem of a different type was proved by using the Carleman estimate.To the best knowledge of the authors,there are no results on the conditional stability like Theorems 1.1–1.4.
This paper is composed of four sections and one appendix.In Section 2,we present two Carleman estimates.Sections 3–4 are devoted to the proofs of Theorems 1.1–1.2 respectively.The proof of the key Carleman estimate is given in Appendix.
In this section,we show two Carleman estimates for an ultrahyperbolic equation.The former Carleman estimate is used for the proof of Theorem 1.1 and the latter for the proof of Theorem 1.2.As for the general theory of Carleman estimates for functions with compact supports,we refer to,for example,Hrmander[13]and Isakov[17],but we here give a direct proof because we need a Carleman estimate for functions not having compact supports and the proof of that Carleman estimate does not follow directly from[13,17].Another direct proof of a Carleman estimate for an ultrahyperbolic equation is found in[2,26].
Here and henceforth let=D× ∂G(T,T1),and letand···dSybe the boundary integrals on Γxand Γy,respectively.
We recall that forwe set
whereγis a positive parameter.We consider the following equation:
Here we recall that
and
Letμ(x,y)be the outward unit normal vector to∂(D×G(T,T1))at(x,y)and letHenceforth we recall that∂D+⊂∂Dis defined by(1.13).
Theorem 2.1In(2.1),let us assume thatfor0≤i≤n and1≤j≤m.Moreover,let0<β <1be small and γ>0be sufficiently large,and let
with some δ0>0.Then there exist constants C>0and s0>0such that
for all u∈H2(D×G(T,T1))and s≥s0.
Theorem 2.20≤i≤n,1≤j≤m and(2.2)hold for(x,y)∈D×G(T,T1).Then there exist constants C>0and s0>0such that
for all s≥s0and all u∈H2(D×G(T,T1))satisfying
Theorem 2.1 gives a Carleman estimate which holds only in a level set Ω(δ),while the Carleman estimate in Theorem 2.2 is global over the total domainG×(T,T1).The proofs of Theorems 2.1–2.2 rely on an idea similar to Bellassoued and Yamamoto[8]and the proof is obtained only by integration by parts and is lengthy,so we give the proof in Appendix.
The proofs of Theorems 1.3–1.4 are reduced to the proofs of Theorems 1.1–1.2,respectively,which this follows from settingu=v(p)−v(q),f=p−qandR=v(q).Therefore it is sufficient to prove only Theorems 1.1–1.2.In this section,we will prove Theorem 1.1.
We set
First by(1.8),we see that
In fact,letx∈DandThen(1.8)yields
Therefore,0,that is,|y|<T.Thus(3.1)is verified.
Next,we characterize∂Ω(δ).We can easily have∂Ω(δ)
Then,similar to(3.1),we can prove that Γ2=Ø.In fact,(1.8)implies
which is impossible.
Moreover,noting thatwe see that
Hence
Now we apply the Carleman estimate in Theorem 2.1,but no data are given on
and so we need a cut-offfunction.
Henceforth,C>0 denotes a generic constant which is independent ofs.We define a cut-offfunctionsuch that 0≤χ(x,y)≤1 and
Settingz=for 1≤i≤n,we have
that is,
Similarly,
From(1.2),we obtain
In particular,settingw=ands=0 in(3.4)we have
By(3.2)–(3.3),we see that
By(1.4)we have=0 andon Γ×G.Moreover,by 0<β<1 we note that
Thus the assumptions in Theorem 2.1 are satisfied in Ω(δ).We apply the Carleman estimate given by Theorem 2.1,and we obtain
Here we also used
Sincez=we have
and
We set
On the other hand,by(3.3),the supports of the functionsare the subsets ofso that
In terms of(3.7)–(3.9),we rewrite(3.6)as
We set
We multiply(3.4)byzand integrate it overto have
We denote the left-hand side of(3.11)by I1and the right-hand side by I2.By(3.2),we note that
Moreover,by(1.3)–(1.4)and(3.3),we have
and
Then,we have
Therefore,using the integration by parts,we obtain
Consequently,we have
Hereis the-component of the unit outward normal vectorνtoWe see that=0 on Γ×G.Moreover,=0 onTherefore,(3.12)yields
From(1.2),we have
Thus by(3.3)and the condition>0,we see that
Next we estimate I2.Using the Cauchy-Schwarz inequality,we have
Therefore we absorb the terms includingdxdyintosdxdy,and we obtain
Now by noting that⊂Ω(δ),(3.3)and(3.10),we have
By(3.3)and the a priori boundedness onu,we have
and so
Now we will consider the first term on the right-hand side of(3.15).SinceandR(x,0,>0 onwe can define a function(−T,T)by
Then we can write
On the other hand,we have
In fact,let∈Ω(δ+2).Then
Hence(1.8)impliesand so
that is,|y1|<T.Since
we see that(x,0,+2).
Consequently we obtain
where
Moreover,(−T,T)and the Lebesgue theorem imply
Henceforth,we set
Then(3.15)yields
From(3.14)and(3.16),we obtain
Finally
for all larges≥whereis some constant.Reducing the integral on the left-hand side to Ω′(δ+3),we have
that is,
for alls≥whereμ=−ReplacingCbywe see that(3.18)holds for alls≥0.First,letM≥d.Choosings≥0 such that
we obtain
Second,letM<d.Then settings=0 in(3.18),we have
Therefore
By the a priori boundedness≤Mand the trace theorem,we haved≤CMand so we can haveSince>0 is arbitrarily small,the proof of Theorem 1.1 is completed.
The proof relies on Theorem 2.2 and is similar to that in[16].
Sinceuitself does not satisfy(2.3),we have to introduce a cut-offfunction.Moreover,we have to apply a Carleman estimate by shifting the domain along they′-direction.Thus we need to introduce several notations.We set
Bywe see thatr>0.We chooseρ>1 sufficiently large so that
By(4.1)and the assumption onT,we have
Furthermore,if necessary,we choose smallerβsuch that
We arbitrarily choose∈Rm−1satisfying
We set
and we recall
Moreover let
Then(4.2)yields
and
Therefore,for small>0 there existsδ>0 such that
ifT−2δ≤|y1|≤TorT−2δ≤≤Tand
In order to apply Theorem 2.2,we introduce a cut-offfunctionχ(y)and definesuch that 0≤χ0≤1 and
Setting=we see thatχ0≤χ≤1 and
By choosingδ>0 smaller if necessary,we assume
We set
Then
and
From(4.4),we note that
By(4.12)–(4.13),we can apply the Carleman estimate(see Theorem 2.2)tow1,w2:
Here and henceforth,C>0 denotes a generic constant which is independent ofs>0.From the assumption onR,we have
By(4.10),we see that|y1|≤T−2δorT−δ≤|y1|≤Timpliesχ=χ=0,and|y′−≤T−2δorT−δ≤|y′−≤Timpliesχ=χ=0 for 2≤k≤m.Therefore,if|y1|∈[0,T−2δ]∪[T− δ,T]and|y′−∈[0,T−2δ]∪[T−δ,T],then|∇yχ|=Δyχ=0.Hence
By(4.8),we haveψ(x,y)<−in the regions of the above integrals.Hence
Here and henceforth we set
Finally,we obtain
Here we used(4.14).
Consequently(4.15)yields
Next,sinceχ(−T,by(4.10),the Cauchy-Schwarz inequality yields
For the last inequality,we used(4.16)and
Hence
Applying(4.18),we have
Here we used≤1 andforx∈Dandy∈
On the other hand,substitutingy1=0 in(1.2)and applyingu(x,0,y′)=0 andR(x,0,y′)≠0forx∈and|y′|≤2T,we have
Noting by(4.4)that if<T,then|y′|<2T,we apply(4.20)in(4.19),so that
for all larges>0.Absorbing the first term on the right-hand side into the left-hand side by choosings>0 large,we obtain
for all larges>0.
Replacing the integration domain on the left-hand side byD×⊂D×and using(4.9)–(4.11),we see that=1 there and
for alls≥s0,wheres0is some constant.By the definition,we haveκ2>κ1and setκ=κ2−κ1>0.Then the last inequality implies
for alls≥s0.By the same argument as in the proof of Theorem 1.1 after(3.18),we can chooseθ∈(0,1)such that
for allsatisfying≤M,the trace theorem yieldsd≤CM,which impliesd≤Varyingand noting
we obtain
Thus the proof of Theorem 1.2 is completed.
Thanks to the large parameters,it is sufficient to prove Theorems 2.1–2.2 in the case ofai=bj=0 in(2.1).Let us set
We prove only Theorem 2.2 and the proof of Theorem 2.1 is obtained by replacing the domainD×G(T,T1)by Ω(δ).Henceforth,we writeand useνto denote the unit outward normal vector to a hypersurface under consideration and we set∂νz=(∇xz,ν)or∂νz=(∇yz,ν).Moreover,we set
and
By(5.3),we calculate
where
The first term on the right-hand side of the Carleman estimate isand it suffices to make a lower estimation ofSince
we will estimateas follows.Using(5.5)–(5.6),we obtain
where
Now,we will estimate the terms Ik,1≤k≤6,using the integration by parts and the boundary condition ofz.Then we have
and
Therefore,we can rewrite
where
and
Next we calculate Jk,1≤k≤5 by substituting the concrete form ofϕ.Setting
we have
Therefore,we obtain
and
We can directly verify
In fact,
Consequently,we see that
Since
we have
We can directly verify
and
Therefore,we conclude that
Finally,we obtain the boundary term as follows:
Then from(5.7),we have
where
We haveϕ≥1 onand sok=1,2,3 onMoreover the second,third and fifth terms on the right-hand side of(5.9)are summed up into
Hence
By the assumption(2.2),we have
Therefore,we can write
In(5.10),the signs of the terms ofandare different.Thus we need to perform another estimation for
Multiplying the equationPz=byϕzand applying the integration by parts,we have
Now we estimate the terms Kj,1≤j≤5 as follows:
Therefore we see that
Here
becausez=0 onby(2.3).Now we calculate B0given by(5.8),while(2.3)implies∇yz=0 andon Γxand all the integrations on Γyvanish.Hence
So multiplying(5.11)by−sγ(4β+μ),where we chooseμ>0 later,we have
We add(5.10)and(5.13)to have
On the other hand,since
by the Cauchy-Schwarz inequality,we see
By 0<β<1,we can chooseμ>0 sufficiently small,so that
Absorbing the term ofwe complete the proof of Theorem 2.2.
AcknowledgmentThe authors thank the anonymous referees for valuable comments.
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Chinese Annals of Mathematics,Series B2014年4期