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The Pauli problem and wave function lifting: reconstruction of quantum states from physical observables

  • In this paper we consider the problem to determine a unique quantum state from given distribution of position (density) and momentum density of particles, namely the so called Pauli problem in quantum physics. In the first part, we will review the method of wave function lifting developed in [4,5] to construct a complex wave function ψHs(Rd), s=1,2, associated to given density and momentum density. The second part is focused on the dynamical version of the wave function lifting, namely we study the relation between solutions to quantum fluid models and wave functions solving the nonlinear Schrödinger equation. The uniqueness of the lifted wave function is essentially related to the structure of vacuum regions of the position density.

    Citation: Hao Zheng. The Pauli problem and wave function lifting: reconstruction of quantum states from physical observables[J]. Mathematics in Engineering, 2024, 6(4): 648-675. doi: 10.3934/mine.2024025

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  • In this paper we consider the problem to determine a unique quantum state from given distribution of position (density) and momentum density of particles, namely the so called Pauli problem in quantum physics. In the first part, we will review the method of wave function lifting developed in [4,5] to construct a complex wave function ψHs(Rd), s=1,2, associated to given density and momentum density. The second part is focused on the dynamical version of the wave function lifting, namely we study the relation between solutions to quantum fluid models and wave functions solving the nonlinear Schrödinger equation. The uniqueness of the lifted wave function is essentially related to the structure of vacuum regions of the position density.



    In quantum physics, the state of a particle is characterised by a complex wave function ψ (quantum state) in a suitable Hilbert space H. However, it is impossible to directly observe a complex quantity in experiments, instead physical observable quantities of a particle are given by the expectation values of operators with respect to the quantum state, such as the probability distribution of position and momentum of particles. It is natural to ask whether it is possible to uniquely determine a quantum state from an appropriate set of physical observables, namely the so called Pauli problem, originally from a footnote in Pauli's article in Handbuch der Physik [21], see also for related researches [9,25]. In this paper, we will partly answer the Pauli problem, by collecting the method of wave function lifting to reconstruct a complex wave function ψ from given distribution of position (density) ρ and momentum J, which is formally equivalent to knowing the expectations of all powers of the position and momentum operators.

    The relationship between quantum states ψ and physical observable quantities (ρ,J) was early interpreted by Madelung [17] to obtain a hydrodynamic formulation of quantum mechanics. For a given complex wave function ψH1x(Rd), it can be formally decomposed in terms of its amplitude and phase,

    ψ=ρeiS, (1.1)

    where ρ=|ψ|2, and by defining the phase velocity v=S and momentum J=ρv, we obtain (ρ,J) as the distribution of the position and momentum densities associated to the quantum state ψ. Moreover, if the evolution of a quantum state ψ=ψ(t,x) is governed by a Schrödinger-type equation

    itψ+22ψ=Hψ, (1.2)

    where H is a potential function, then by writing (1.2) in its real and imaginary parts, we obtain the Hamilton-Jacobi equation of the density ρ and the phase function S,

    {tρ+div(ρS)=0tS+12|S|2+H=22Δρρ.

    As a consequence, the position density ρ and the momentum density J associated to ψ formally satisfy the quantum hydrodynamic (QHD) system

    {tρ+divJ=0tJ+div(JJρ)+ρxH=22ρ(ρρ), (1.3)

    and the physical observables ρ and J are also called the hydrodynamic data associated to ψ. For the Schrödinger equation (1.2), the natural energy functional is defined by

    E(t)=Rd22|ψ|2+H|ψ|2dx, (1.4)

    which has the corresponding hydrodynamic formulation as

    E(t)=Rd22|ρ|2+|J|22ρ+ρHdx. (1.5)

    The QHD system is extensively used in physics to describe a compressible, inviscid fluid where quantum effects appear at macroscopic / mesoscopic scales and thus they need to be taken into account also in the hydrodynamical description. It is for instance the case when studying phenomena in superfluidity [15], Bose-Einstein condensation [23] or in the modeling of semiconductor devices at nanoscales [13].

    The main problem of the Madelung transformation (1.1) is that the phase function S usually fails to be well-defined when vacuum regions {ρ=0} exist. It is straightforward to see that the phase function S may experience high oscillation or blow-up as the density ρ approaching 0, which leads to lost of information of the phase function at vacuum boundaries. Moreover, even though the velocity field v=S is irrotational outside vacuum, its circulations on closed curves around a vacuum region are actually quantized [12,19], namely for any Lipschitz closed curve γ strictly away from vacuum points, it should follows

    t0v(γ(t))˙γ(t)dt2πZ. (1.6)

    In [1,2] the authors overcome the difficulty of defining the hydrodynamic data (ρ,J) when vacuum regions may exist by means of the polar decomposition approach (see Proposition 7, or the overview [3]). In this way it is possible to consider (ρ,J) of any given wave function, which are defined almost everywhere and satisfy a generalized irrotationality condition.

    In this present paper we are going to provide the method of wave function lifting to reconstruct a complex wave function from given distribution of particle density ρ, which may contain vacuum regions, and momentum density J under suitable conditions, and discuss the uniqueness of the lifted wave function. More explicitly, we will consider hydrodynamic data (ρ,J) given in the following three cases: 1-dimensional data with general vacuum regions, multi-dimensional quantum vortex data satisfying the quantised vorticity condition (1.6), and solutions of the QHD system (1.3) without vacuum. The first two results are reviews of the wave function lifting arguments in [4,5], and we discuss further the source of non-uniqueness of the wave function lifting in this paper. The last result is our recent extension of the wave function lifting method to the dynamics of quantum fluids governed by QHD models (1.3).

    In our construction of wave function, we find that the only possible source of the non-uniqueness of the lifted wave function is the lost of information at vacuum boundary. Therefore in the cases such that the connected components of non-vacuum regions are strictly separated (namely they can be contained in disjoint open neighbourhoods), as the 1-dimensional problem considered in this paper, the answer to the Pauli problem is usually negative—there are infinitely many wave functions associated to the same hydrodynamic data. However, we also show that those lifted wave functions are only differed by piece-wise constant phase shifts (see Lemma 13). On the other hand, for hydrodynamic data such that the position density ρ is continuous and the non vacuum region is connected (for example the case of pointwise quantum vortices), since there is no problem of crossing vacuum boundaries, the lifted wave function is unique upto constant rotations, which gives a positive answer to the Pauli problem.

    We start with the wave function lifting result in dimension d=1 for finite energy hydrodynamic data given by functional (1.5). To consider the momentum density in vacuum regions, let us introduce the hydrodynamic state (ρ,Λ) (see Definition 5 or [1,2]), and the momentum density is given by J=ρΛ. In our results we further require Λ=0 almost everywhere in vacuum regions, which is called the physical compatibility condition of hydrodynamic state. This condition is equivalent to say that the energy density vanishes in large vacuum regions, which is a physically reasonable condition, and is guaranteed for all Schrödinger generated data by Lemma 6.

    Theorem 1. Let (ρ,Λ) be a hydrodynamic state. There exists an associated wave function ψH1x(R) in the sense of the Definition 5, if and only if (ρ,Λ) satisfies

    (1) there exists a constant 0<M1< such that

    ρH1x(R)+ΛL2x(R)M1;

    (2) Λ=0 almost everywhere in {ρ=0}.

    Furthermore, we have

    xψ=(xρ+iΛ)ϕ,
    ψH1x(R)1C(M1),

    where ϕP(ψ) is a polar factor of ψ defined in (2.1).

    For any piecewise constant phase shift

    Θ=exp(ijθj1(aj,bj)),θj[0,2π), (1.7)

    where {(aj,bj)}j is a disjoint decomposition of the non-vacuum region {ρ>0}, we have ΘψH1x(R) and Θψ is also a wave function associated to (ρ,Λ). On the other hand, if ˜ψ is another wave function associated to (ρ,Λ), then there exists a phase shift ˜Θ of form (1.7) such that ˜ψ=˜Θψ.

    The lifting result of wave functions in space H2x is established for (ρ,J) with L2x bounded generalised chemical potential λ (see Definition 9, in 1-D space we omit the subscript), which is abbreviated as GCP states in this paper.

    Theorem 2. Let (ρ,Λ) be a hydrodynamic state. There exists a wave function ψH2(R), associated to (ρ,Λ) in the sense of Definition 5, if and only if

    (ρ,Λ) is a GCP state in the sense of Definition 10;

    the kinetic energy density k=22(xρ)2+12Λ2 is continuous.

    Moreover, let us assume

    ρH1x(R)+ΛL2x(R)M1,1{ρ>0}xJ/ρL2x(R)+λL2x(R)M2, (1.8)

    for some constants M1,M2<, where λ is defined in (2.8), it follows that

    ψH2x(R)C(1M1+2M2). (1.9)

    In the 2-dimensional case, we additionally assume the continuity of density ρ, which is essential to give a proper definition to the point vacuum and can not be inferred by the finite energy assumption and Sobolev embedding in multi-dimension. It is also needed to provide a local lower bound on the density when strictly away from the vacuum. Nevertheless, in the physical and mathematical literature the most widely studied quantum vortex structures (1.6) fall in this framework, see for example [7,20,24], and in the Theorem, we formulate the quantised vorticity condition in a distributional differential form (1.12). This result can also be extended to the case of simple vortex lines in 3-dimensional case, see Proposition 10.

    Theorem 3. Let (ρ,Λ) be a finite energy hydrodynamic state satisfying the bound

    ρH1(R2)+ΛL2(R2)M1. (1.10)

    Let us further assume that ρ is continuous with isolated point vacuum (consequently V={x;ρ(x)=0} is at most countable)

    V={x(α)}αAR2,infαβ|x(α)x(β)|>0, (1.11)

    and the velocity v satisfies the quantised vorticity condition

    {vM(R2),v=2παAkαδx(α),kαZ. (1.12)

    Then there exists a wave function ψH1(R2) such that

    ρ=|ψ|,Λ=Im(ˉϕψ),

    where ϕP(ψ) is a polar factor defined in (2.1). The lifted wave function is unique upto constant rotation eiθ, θ[0,2π).

    If we furthermore assume that ρ,JL1loc(R2) and (ρ,Λ) satisfy also the bounds

    λjL2(R2)+xjJjρL2(R2)M2,j=1,2, (1.13)

    where λj's are the generalised chemical potential given by Definition 9, then ψH2(R2) and we have

    ψH2x(R2)C(1M1+2M2).

    Our results establish the equivalence between hydrodynamic states and the corresponding wave functions ψ in H1x and H2x, and we also refer to the recent paper [6], where the wave function lifting method of ψH1x is considered for general spaces (X,d,ν) with metric d and measure ν. In [6], the velocity v is interpreted as a cotangent vector filed in L2(TX), and the quantised vorticity condition is extended in the integral form

    t0v(γ(t))˙γ(t)dt2πZ,

    for almost every closed curve γ on X. However, in general spaces usually one can not expect the uniqueness of lifted wave functions.

    Let us remind that the previous results do not provide correspondence between the dynamics of Schrödinger equations and the QHD models. For given a hydrodynamic solution (ρ,J), one can construct its associated wave function ψ(t,) by Theorem 1 to Theorem 3 at each fixed time t. But to make ψ a solution to the corresponding Schrödinger equation, more delicate construction is required. In the last result, we restrict us to the non-vacuum case and extend the wave function lifting result to the dynamical case for GCP solutions of the QHD system (1.3), which provides the equivalence of the dynamics of QHD models (1.3) and Schrödinger equations (1.2).

    Theorem 4. Let (ρ,J) be a GCP solution (see Definition 12) of (1.3) on [0,T)×Rd with potential HLtL1loc,x, such that ρ is strictly positive on any compact set, then there exists a unique (upto constant phase shifts) wave function ψLt([0,T),H2x(Rd)) associated to (ρ,J) in the sense of Definition 5 for almost every t[0,T). Moreover, ψ is a weak solution of the Schrödinger equation (1.2).

    If the corresponding Scrödinger equation has satisfactory well-posedness result, as a consequence of Theorem 4 one immediately obtains the well-possedness of the QHD model for non-vacuum solutions. However, this correspondence generally does not hold true if vacuum regions exist. For example, the cubic nonlinear Schrödinger equation H=|ψ|2 has well-known well-posedness theory, while the uniqueness of the corresponding QHD system for initial data with quantized vorticity is still an open problem. If the condition of quantized vorticity is not required, [10] (multi-D) and [18] (1-D) provide the non-uniqueness results of finite energy weak solutions.

    The rest of this paper is structured in the following way: In Section Section 2 we will give the definitions and recall some preliminary results, including the polar decomposition approach. In Section Section 3 we construct the lifted wave function for 1-dimensional hydrodynamic data (Theorems 1 and 2) which may contain general vacuum regions, while multi-dimensional data satisfying the quantised vorticity condition are considered in Theorem 3 in Section Section 4. Last, in Section Section 5 we prove Theorem 4, namely for a given solution of the QHD system (1.3) without vacuum region, there exists a unique (upto constant rotations) lifted wave function, which is also a solution to the corresponding Schrödinger equation (1.2).

    Notations and definitions will be fixed in this section and are used through this paper. The standard notation for Lebesgue and Sobolev norms are given by

    ||f||Lpx=(Rd|f(x)|pdx)1p,
    ||f||Wk,px=kj=0||jf||Lpx,

    and we denote Hkx=Hk(Rd)=Wk,2(Rd). The mixed Lebesgue norm of functions f:ILr(Rd) is defined as

    ||f||LqtLrx=(I||f(t)||qLrxdt)1q=(I(Rd|f(x)|rdx)qrdt)1q,

    where I[0,) is a time interval, and the explicit dependence on I is omitted in this paper. The mixed Sobolev norm LqtWk,rx is defined analogously. Last, often letters as C and M are used to denote positive constants, which may change line to line.

    Now we recall the method of polar decomposition to define the hydrodynamic state associated to a given quantum state ψ possibly containing vacuum regions. Given any function ψH1x(Rd), we can define the set of polar factors as

    P(ψ)={ϕLx(Rd) | ϕLx1, ρϕ=ψ a.e.}, (2.1)

    where ρ:=|ψ|.

    Definition 5. Let ΩRd be an open set. Given a wave function ψH1x(Ω), we say that (ρ,Λ) is the hydrodynamic state associated to ψ if

    ρ=|ψ|andΛ=Im(ˉϕψ), (2.2)

    where ϕP(ψ) is a polar factor of ψ, and the momentum density of ψ is defined by

    J=ρΛ.

    In general the polar factor of a wave function ψ is not unique, due to the possible appearance of vacuum regions. Nevertheless, Λ=Im(ˉϕψ) is well defined, as a consequence of the following Sard type lemma (see e.g., Theorem 6.19 in [16] for a general statement).

    Lemma 6. Let ΩRd be an open set, g:ΩR be in H1x(Ω), and

    B=g1({0})={xΩ : g(x)=0}.

    Then g(x)=0 for almost every xB.

    We stress that, in view of the lemma above, Λ satisfy the physical compatibility condition

    Λ=0a.e. on {ρ=0}. (2.3)

    Furthermore, (ρ,Λ) enjoy the following properties.

    Proposition 7 (Polar factorization [1,2]). Let ψH1x(Rd) and (ρ,Λ) be a hydrodynamic state associated to ψ, then we have (ρ,Λ)H1x(Rd)×L2x(Rd), and

    2Re(¯ψψ)=2ρρ+ΛΛ,a.e.inRd. (2.4)

    Moreover the following identity is satisfied in the sense of distributions

    J=2ρΛ. (2.5)

    Remark 8. The identity (2.5) is called the generalised irrotationality condition introduced by the authors of [1,2]. Formally it is easy to compute that (2.5) is equivalent to

    ρv=0,

    therefore (2.5) can be seen as an extension of the irrotationality property of the phase velocity v=S to the case when vacuum regions are present.

    By taking the trace of (2.4), we have

    2|ψ|2=2|ρ|2+|Λ|2=2|ρ|2+|J|2ρ,

    therefore ρ and Λ together characterise the ˙H1x regularity of ψ. Following the energy functional (1.5) and the terminology of hydrodynamic theory, we define the kinetic energy density function to be

    k=22|ψ|2=22|ρ|2+12|Λ|2. (2.6)

    Let us also recall the space of hydrodynamic functions corresponding to H2x wave functions, which is introduced by [4,5]. To define the new space, we start by considering the following chemical potential

    μ=22ρρ+12|v|2+H. (2.7)

    Formally it is possible to interpret μ as the first variation of the total energy functional (1.5) with respect to the position density [14],

    μ=δEδρ.

    Obviously, the chemical potential μ cannot be used to carry out a satisfactory mathematical analysis when vacuum regions exist. For this reason it will be more convenient to consider the following "generalized chemical potential" λj.

    Definition 9. Let

    (ρ,Λ)[H1x(Rd)Cx(Rd)]×L2x(Rd;Rd),

    such that Λ satisfies (2.3) and ρL1loc(R). Then we define the generalized chemical potential λj, j=1,2,,d, to be the measurable function given by

    λj={222xjρ+12Λ2jρin {ρ>0},0elsewhere, (2.8)

    where Λj is the j-th component of Λ.

    In what follows we provide the definition of bounded generalized chemical potential hydrodynamic states, namely those states where λj can be rigorously characterized.

    Definition 10 (GCP states). We say that the pair (ρ,Λ) is a state with bounded generalized chemical potential (GCP state, in short) if:

    ρH1x(Rd)Cx(Rd) and ΛL2x(Rd;Rd);

    Λ=0 a.e. on {ρ=0};

    ρ,JL1loc,x(Rd), where (ρ,J)=((ρ)2,ρΛ);

    ● the following bounds are satisfied

    1{ρ>0}xjJ/ρL2x(Rd)+λjL2x(Rd)C,j=1,2,,d,

    where λ is defined as in (2.8).

    Now we extend the hydrodynamic spaces defined above to solutions of the QHD system (1.3). Since we consider hydrodynamic functions with relatively low regularity, we need to introduce the definition of general weak solutions of (1.3). Preliminary, we first rewrite the quantum pressure term as

    22ρ(ρρ)=24div(ρ2logρ)=24ρ2div(ρρ). (2.9)

    We can now give the definition of weak solutions to the QHD system.

    Definition 11 (Weak solutions). Let ρ0,J0L1loc(Rd), we say the pair (ρ,J) is a finite energy weak solution to the Cauchy problem for (1.3) with initial data ρ(0)=ρ0, J(0)=J0, in the space-time slab [0,T)×Rd if there exist ρL2loc(0,T;H1loc(Rd)), ΛL2loc(0,T;L2loc(Rd)) such that

    (ⅰ) ρ=(ρ)2,J=ρΛ;

    (ⅱ) ηC0([0,T)×Rd),

    T0Rdρtη+Jηdxdt+Rdρ0(x)η(0,x)dx=0; (2.10)

    (ⅲ) ζC0([0,T)×Rd;Rd),

    T0RdJtζ+ΛΛ:ζρζxH+2ρρ:ζ+24ρΔdivζdxdt+RdJ0(x)ζ(0,x)dx=0; (2.11)

    () (generalized irrotationality condition) for almost every t(0,T)

    J=2ρΛ, (2.12)

    holds in the sense of distributions.

    The weak solutions of finite energy and GCP weak solutions are given by the following definition.

    Definition 12. Let (ρ,J) be a weak solution to the QHD system (1.3) as in the Definition 11. We say that (ρ,J) is a finite energy weak solution, if we have supt[0,T)E(t)<, where E(t) is the energy functional defined by (1.5).

    Moreover, we say (ρ,J) is a GCP weak solution if for almost every t[0,T), the corresponding hydrodynamic state (ρ,Λ)(t) is a GCP state as in Definition 10, and satisfies the uniform bound

    tρL(0,T;L2(Rd))+dj=1λjL(0,T;L2(Rd))I0<.

    In this section we establish the method of wave function lifting in dimension d=1. We first prove Theorem 1, which gives sufficient and necessary conditions for a hydrodynamic data (ρ,Λ) to have an associated wave function ψH1(R).

    Proof of the lifting part of Theorem 1. Let ψH1x(R) be associated to (ρ,Λ), then by means of the polar factorization in Proposition 7 we have that both conditions (1) and (2) are fulfilled.

    To prove the converse statement, we consider δn(x)=1ne|x|2/2, which is locally strictly positive and converges to 0 as n. We define the following approximating hydrodynamical quantities

    ρn=ρ+δn,Λn=Jρn=ρρnΛ,

    then it is straightforward to check that the sequence {(ρn,Λn)} also satisfies a uniform bound as in condition (1),

    ρnH1x(R)ρH1x(R)+δnH1x(R)C(1M1),

    and since ρn(x)>ρ(x) for every xR, we have |Λn(x)||Λ(x)| a.e. and consequently

    ΛnL2x(R)ΛL2x(R).

    By we have ρnρ in H1x(R). Moreover, the physical compatibility condition (2) holds also for Λn. Hence ρn(x)ρ(x) and Λn(x)Λ(x) a.e. in R. Then the dominated convergence theorem yields ΛnΛ in L2x(R). Furthermore, since ρn(x)>0 it is possible to define the approximating velocity field

    vn=Λnρn.

    Notice that, since by definition ρn is uniformly bounded away from zero on compact intervals, we have vnL1loc(R), hence it makes sense to define the phase

    Sn(x)=x0vn(x)dx

    and consequently the wave function

    ψn(x)=ρn(x)eiSn(x).

    Let us remark that ψn is uniquely defined, up to a constant phase shift. We now show that the sequence ψn has a limit ψH1x(R) satisfying |ψ|=ρ, Im(ˉϕxψ)=Λ, where ϕP(ψ). Since xψn=eiSn(xρn+iΛn), we have

    ψn2H1x=xρn2H1x+Λn2L2xC(M1),

    thus, up to subsequences, ψnψ in H1. On the other hand, we also have ρnρ in H1, ΛnΛ in L2 and moreover eihSnϕ weakly* in Lx, for some ϕLx. It is straightforward to check that ϕP(ψ), indeed we have ψn=ρneihSnρϕ=ψ in L2x(R). Furthermore

    xψn=eiSn(xρn+iΛn)ϕ(xρ+iΛ),inL2x(R)

    so that xψ=ϕ(xρ+iΛ) and hence (ρ,Λ) are the hydrodynamical quantities associated to ψ in the sense of the Definition 5.

    Now we begin to discuss the uniqueness and stability properties of the wave function lifting given in Theorem 1 in H1x(R). Actually the wave function associated to a finite energy hydrodynamic data can not be uniquely determined because of the arbitrary phase shifts allowed on each connected component of {ρ>0}. In the next lemma, we show that this is the only source of non-uniqueness. Since this lemma is also used in later contents for multi-dimensional cases, we present it here in a general form.

    Lemma 13. Let ΩRd be a connected open set and ψ1, ψ2H1x(Ω) be two wave functions associated to the same hydrodynamic data (ρ,Λ)[H1x(Ω)C1x(Ω)]×L2x(Ω). Furthermore we assume that ρ>0 on Ω.

    Then there exists a constant phase shift θ[0,2π), such that

    ψ2=eiθψ1. (3.1)

    Proof. By our assumption and the polar factorization, we have

    ψj=ρϕjandψj=(ρ+iΛ)ϕj,j=1,2,

    where ϕjP(ψj), j=1,2. Since ρ>0 on Ω, the polar factor ϕj is uniquely defined by

    ϕj=ψjρ,

    then we can define function f=ψ1/ψ2H1(Ω). A direct computation shows that

    f=1ψ22[ρϕ2(ρ+iΛ)ϕ1ρϕ1(ρ+iΛ)ϕ2]=0,a.e. inΩ.

    Since Ω is open and connected, the function f=ψ1/ψ2 is a constant C on Ω, which satisfies

    |C|=|ψ1||ψ2|=1,

    therefore formula (3.1) holds true.

    Before stating the next results, here we collect some elementary properties of Sobolev functions that will be used later. Let g be a function in H1x(a,b) and H1x(b,c), then gH1x(a,c) if and only if g is continuous at point b, and in this case we have

    xg2L2x(a,c)=xg2L2x(a,b)+xg2L2x(b,c).

    Then let us consider gH1x(Ω), where ΩR is an open set. The continuity of g allows us to decompose the set {x;g(x)0} into disjoint open intervals, i.e.,

    {x;g0}=j(aj,bj),g(aj)=g(bj)=0. (3.2)

    The next lemma shows that we can introduce arbitrary constant phase shift on each component (aj,bj), without breaking the H1 regularity of g.

    Lemma 14. Let gH1x(Ω) and let ΘLx(Ω) be a piecewise constant phase shift given by the formula

    Θ=exp(ijθj1(aj,bj)),θj[0,2π), (3.3)

    where (aj,bj)'s are the components of {g0} as in (3.2). Then we have ΘgH1x(Ω), and

    x(Θg)=Θxg. (3.4)

    Proof. The proof of the lemma follows a standard argument of weak derivative. We take ηCc(Ω) to be a test function and consider the weak derivative x(Θg):

    Ωηx(Θg)dx=ΩΘgxηdx=jbjajeiθjgxηdx.

    On each interval (aj,bj) by integration by parts and g(aj)=g(bj)=0, we obtain

    Ωηx(Θg)dx=jbjajeiθjηxgdx.

    Furthermore the vanishing derivative Lemma 6 implies xg=0 a.e. outside {x;g(x)0}=j(aj,bj), therefore we can conclude

    Ωηx(Θg)dx=ΩηΘxgdx,

    namely x(Θg)=ΘxgL2x(Ω), which finishes the proof of the lemma.

    A direct consequence of Lemmas 13 and 14 is the non-uniqueness of wave function lifting for given hydrodynamic data at H1 level, and the only source of non-uniqueness is the arbitrary phase shifts allowed on the components of the non-vacuum regions. More precisely, let ψH1x(R) be a wave function associated to (ρ,Λ) in the sense of the Definition 5, then for any piecewise phase shift function Θ of the form (3.3), by formula (3.4) it is straightforward to check that ΘψH1x(R) is another wave function associated to the same hydrodynamic data, whose polar factors are P(Θψ)=ΘP(ψ).

    Another application of Lemma 14 is the following Proposition 15. We can show that even though the lifted wave functions do not enjoy general stability property, there is at least one wave function associated to the limiting hydrodynamic data, which can be attained as a strong limit in H1x(R) of a subsequence of associated wave functions with well-chosen phase shift.

    Proposition 15. Given a sequence of hydrodynamic data {(ρn,Λn)} which converges to (ρ0,Λ0) in H1x(R)×L2x(R), let us assume {ψn} and ψ0 are wave functions associated to {(ρn,Λn)} and (ρ0,Λ0), respectively.

    Then there exists a subsequence ψnk and a piecewise constant phase shift Θ given by the formula (3.3) on the connected components of {ψ00}, such that

    limnkψnkΘψ0H1x(R)=0.

    Proof. For the case that ρ00, the proposition is trivial. Therefore we assume ρ0 is not identically 0.

    By Lemma 14, for any phase shift Θ given by (3.3), we have Θψ0H1x(R) with

    x(Θψ0)=Θxψ0.

    By the polar decomposition provided by Proposition 7, we have

    ψn=ρnϕnandxψn=(xρn+iΛn)ϕn (3.5)

    with a polar factor ϕnP(ψn). Since ϕnLx1, then up to a subsequence {ϕnk} converges weakly* to some ˜ϕ0 in Lx(R). We define ˜ψ0=ρ0˜ϕ0. Since (ρn,Λn) converges strongly to (ρ0,Λ0) in H1x(R)×L2x(R), by passing to the limit as nk in (3.5) we obtain

    ψnk=ρnkϕnkρ0˜ϕ0=˜ψ0,inL2x(R),

    and

    xψnk=(xρnk+iΛnk)ϕnk(xρ0+iΛ0)˜ϕ0,inL2x(R).

    Consequently, ˜ψ0 is a weak limit of ψnk, with ˜ψ0H1x(R) and

    x˜ψ0=(xρ0+iΛ0)˜ϕ0.

    Moreover the polar factorization of ψnk and ˜ψ0 implies

    ψnk2H1x(R)=ρnk2H1x(R)+Λnk2L2x(R)ρ02H1x(R)+Λ02L2x(R)=˜ψ02H1x(R),

    then by the weak convergence and the convergence of norms we obtain ψnk˜ψ0 in H1x(R). Since ˜ψ0 is a wave function associated to (ρ0,Λ0), by Lemma 13 on each component (aj,bj) of {ψ00}, there exist a unitary eiθj such that

    ˜ψ0=eiθjψ0on(aj,bj).

    Let

    Θ=eijθj1(aj,bj),

    then we have ˜ψ0=Θψ0 on R.

    Now we are going to prove Theorem 2, which states the wave function lifting at the H2 level. One should notice that Sobolev regularity for the wave function does not correspond to further regularity for the hydrodynamical quantities. For example if we consider ψ(x)=x on [1,1], then ψCx, but on the other hand ρ is only Lipschitz, with 2xρ=δ0. In fact, the same example is considered in more details in [8], which shows that Sobolev regularity above 32 is not preserved, but regularity below 32 is preserved. Considering a wave function ψH2x will require further information on the energy density and on the generalised chemical potential λ given by Definition 9 (in 1-D we omit the subscript of λ1). Another important fact we should emphasise when considering a wave function lifting ψH2x(R) is that xψ should be a continuous function. As mentioned before, ψ should have well designed phase shifts on all the connected components of the set {ρ>0}, such that xψ have no jump discontinuity at vacuum boundaries.

    In order to prove Theorem 2, we first state the following lemma, which shows the connection between the hydrodynamic quantities λ, xJρ1{ρ>0} and the H2x regularity of the associated wave function ψ.

    Lemma 16. (1) If the hydrodynamic state (ρ,Λ) is given through an associated wave function ψH2x(R), then (ρ,Λ) is a GCP state and the identities

    xJρ1{ρ>0}=Im(ˉϕ2xψ),λ=22Re(ˉϕ2xψ), (3.6)

    hold true in L2(R), where ϕP(ψ) is a polar factor of ψ.

    (2) Let us assume that (ρ,Λ) is a GCP state and let ψH1x(R) be a wave function associated to (ρ,Λ), then ψH2x(aj,bj), for all connected components (aj,bj) of the set {ρ>0} as given in (3.2), and we have

    22xψ=[2λ+ixJρ]ϕinL2x(aj,bj). (3.7)

    Proof. Let us consider (ρ,Λ) given through an associated wave function ψH2x(R), then it follows from Theorem 1 that (ρ,Λ)H1x(R)×L2x(Λ). Moreover, by the definition of the hydrodynamic quantities ρ=|ψ|2, J=Im(ˉψxψ), we have on the set {ρ>0}={|ψ|>0}

    Im(ˉϕ2xψ)=xIm(ˉψxψ)|ψ|=xJρ.

    Moreover, by using the definition (2.8) for λ, on the set {|ψ|>0} we have

    22Re(ˉϕ2xψ)=22|ψ|[xRe(ˉψxψ)|xψ|2]=22ρ[122xρ(xρ)22Λ2]=222xρ+Λ22ρ=λ.

    Let us emphasize that the previous computations are rigorous since ψH2x(R) and {|ψ|>0} is an open set. By Lemma 6 we have 2xψ=0 a.e. in {ρ=0}, thus identities (3.6) hold almost everywhere on R.

    To prove the converse statement, we assume (ρ,Λ) to be a GCP state, and let ψH1x(R) be a wave function associated to (ρ,Λ). By using the polar factorization, it follows that

    ψ=ρϕ,xψ=(xρ+iΛ)ϕ,

    where ϕP(ψ). Since |ψ|>0 on (aj,bj), the polar factor ϕP(ψ) is uniquely defined, ϕ=ψ|ψ|, and a direct computation gives

    xϕ=1|ψ|(xψx|ψ|ψ|ψ|)=iΛρϕ.

    Using the identities above and the definition of hydrodynamic quantities, we obtain

    [2λ+ixJρ]ϕ=(22xρ+ixΛ+ixρΛρΛ2ρ)ϕ=x[(xρ+iΛ)ϕ]=2x(xψ).

    Thus we prove the identity (3.7), and by using the bounds of λ and xJρ given in the Definition 10 of GCP state, it follows that ψH2x(aj,bj).

    The previous lemma shows that the condition

    1{ρ>0}xJ/ρL2x(R)+λL2x(R)M2,

    on the hydrodynamic state allows to improve on the regularity of the wave function ψ on the connected components of {ρ>0}. However, in general ψ is not in H2x(R), since xψ may possibly experience jump discontinuities at vacuum boundaries, due to the fact that the H1 regularity allows for arbitrary phase shifts on connected components. On the other hand, H2 regularity requires compatibility conditions of the phase shift at vacuum boundaries. We will show that, by additionally assuming the continuity of kinetic energy density k, it is possible to provide an appropriate choice of the phase shifts on every connected component, which will enable us to construct another wave function ˜ψH2x(R) associated to the same hydrodynamical quantities. More precisely, starting from ψ, we will construct a ˜ψH2x(R) such that ˜ψ=Θψ, where Θ is a piecewise phase shift of the form

    Θ=exp(ijθj1(aj,bj)),θj[0,2π). (3.8)

    The main difficulty of our construction lies in the accumulation points of vacuum boundaries. To overcome this difficulty, we need the next lemma which shows that under the assumption of Theorem 2, the kinetic energy density k vanishes at the accumulation points of vacuum boundaries, and k is indeed a function in the space H1x(R).

    Lemma 17. Let (ρ,Λ) be a GCP hydrodynamic state and let us assume that the kinetic energy density k is continuous. If ˜x is an accumulation point of vacuum boundaries j{aj,bj}, then k(˜x)=0.

    Proof. By using Theorem 1, there exists a ψH1x(R) associated to (ρ,Λ), and the kinetic energy density is given by

    k=22|xψ|2.

    In particular, the continuity of k implies that |xψ| is also a continuous function. To prove Lemma 17, it is sufficient to show |xψ| vanishes at the accumulation points of vacuum boundaries.

    Let us consider an accumulation point ˜x of the vacuum boundaries j{aj,bj}, namely there exists a sequence of intervals {(ajn,bjn)}n such that (ajn,bjn)˜x as n. On each (ajn,bjn), we take xjn=12(ajn+bjn), and we claim xψ(xjn)0 as n. If the claim holds, by the continuity of |xψ| we obtain |xψ(˜x)|=0.

    The claim xψ(xjn)0 can be proved by contradiction. Indeed, let us assume that

    lim infn|xψ(xjn)|>c>0.

    Since ajn and bjn are vacuum boundary points, namely ψ(ajn)=ψ(bjn)=0, then we have

    0=bjnajnxψ(y)dy.

    Moreover by the property (2) of Lemma 16, we have ψH2x(ajn,bjn), so we can decompose the integral as

    0=bjnajn[xψ(xjn)+yxjn2xψ(s)ds]dy=xψ(xjn)ljn+bjnajnyxjn2xψ(s)dsdy,

    where ljn=bjnajn. By using the identity (3.7) and the bounds (1.8), it follows that

    2xψL2x(ajn,bjn)22λL2x+1xJρ1{ρ>0}L2xC(2M2),

    then we have

    |bjnajnyxjn2xψ(s)dsdy|l32jn2xψL2x(ajn,bjn)l32jnC(2M2).

    For n large enough one has |xψ(xjn)|>c and l12jnC(2M2)<c2 since ljn0 as n, hence it follows that

    0|xψ(xjn)ljn||bjnajnyxjn2xψ(s)dsdy|>c2ljn>0,

    which is a contradiction.

    Now we are ready to prove Theorem 2.

    Proof of Theorem 2. Let us consider the hydrodynamic data (ρ,Λ) given through an associated wave function ψH2(R), then by the property (1) of Lemma 16 we know that (ρ,Λ) is a GCP state. Moreover, by Sobolev embedding, k=22|xψ|2 is a continuous function.

    Now we assume that (ρ,Λ) is a GCP state, and decompose the non vacuum regions into disjoint intervals,

    {ρ>0}=j(aj,bj),ρ(aj)=ρ(bj)=0. (3.9)

    Lemma 16 shows that on all the connected components (aj,bj) of {ρ>0} we have ψH2x(aj,bj), and the identity (3.7) holds true in L2x(aj,bj). However as discussed before, to obtain a H2 wave function defined on the whole R, we need to overcome the possible jump discontinuity at vacuum boundaries. The additionally assumption on the continuity of energy density allows us to provide an well-designed choice of the phase shifts on every connected component and to construct another wave function ˜ψH2x associated to the same hydrodynamical quantities. More precisely, starting from ψ, we will construct a piecewise phase shift function Θ of the form

    Θ=exp(ijθj1(aj,bj)),θj[0,2π), (3.10)

    such that ˜ψ=Θψ belongs to H2x(R).

    Before the construction of Θ, we first give some discussion on vacuum boundaries j{aj,bj}. Let {˚aj} denote the isolated vacuum points, namely ρ(˚aj)=0 and ρ>0 on (˚ajϵ,˚aj+ϵ){˚aj} for some small ϵ>0. Then we define the set

    W={ρ>0}j{˚aj}.

    By the continuity of ρ and the definition of ˚aj, it is straightforward to see that W is an open set, consequently it can be represented as disjoint open intervals

    W=j(ˉaj,ˉbj),

    where ˉaj,ˉbjj{aj,bj}j{˚aj}. The set j{aj,bj}j{˚aj} consists of the following two types of vacuum boundary points. The first type is the boundary of large vacuum intervals, where by definition of ˚aj's we have |ψ|2=ρ0 on (ˉajϵ,ˉaj) or on (ˉbj,ˉbj+ϵ) for some ε>0, and by the continuity of |xψ| we have |xψ(ˉaj)|=|xψ(ˉbj)|=0. The second type is the accumulation point of vacuum boundaries, where |xψ| also vanishes as proved in Lemma 17.

    Let us fix an interval (ˉaj,ˉbj) and let {˚ajk}K2k=K1 denote the vacuum points in (ˉaj,ˉbj). By our construction, the only possible accumulation points of {˚ajk} are ˉaj and ˉbj, hence we can assume ˚ajk<˚ajk+1 for all k.

    The phase shift function Θ on (ˉaj,ˉbj) is constructed through the following strategy. We start from a fixed (˚aj0,˚aj1) and set θj0=0, namely Θ=1 on (˚aj0,˚aj1). To extend the definition of Θ to (˚aj1,˚aj2), we notice that the intervals (˚ajk,˚ajk+1) are connected components of the set {ρ>0}. Thus by Lemma 16 we have the H2 regularity of ψ on (˚aj0,˚aj1) and (˚aj1,˚aj2), which implies the the left and right side limits xψ(˚aj1) and xψ(˚a+j1) exist. On the other hand, the continuity of the kinetic energy density k implies |xψ|=12k is continuous, hence we have |xψ(˚aj1)|=|xψ(˚a+j1)|. Therefore we can choose a θj1[0,2π) such that (Θxψ)(˚aj1)=eiθj1xψ(˚a+j1) (θj1=0 if |xψ| vanishes at ˚aj1), and we define Θ=eiθj1 on (˚aj1,˚aj2). By repeating this process inductively, we extend the definition of Θ to the whole (ˉaj,ˉbj). Moreover we have ΘxψH1(˚ajk,˚ajk) and our construction ensures the continuity of Θxψ at all point vacuum ˚ajk. Thus by the elementary property of Sobolev functions, it follows that ΘxψH1x(ˉaj,ˉbj), and by Lemmas 14 and 16 we have the identity

    2x(Θxψ)=[22xρΛ2ρ+ixJρ]ΘϕinL2(ˉaj,ˉbj),ϕP(ψ). (3.11)

    To this point we have constructed the phase shift function Θ on W=j(ˉaj,ˉbj), and we extend Θ to the whole R by defining Θ=1 on Wc, thus Θ has the form (3.8) as required, and we define ˜ψ=Θψ. By Lemma 14 we have x˜ψ=Θxψ, and ˜ψH1x(R) is also a wave function associated to (ρ,Λ) which satisfies

    x˜ψ=(xρ+iΛ)Θϕ. (3.12)

    Now we prove x˜ψ=ΘxψH1x(R). Let ηCc(R) be an arbitrary test function, then we have

    Rηx(Θxψ)dr=R(Θxψ)xηdr.

    By the vanishing derivative Lemma 6, it follows that xψ=0 a.e. outside the set W, therefore

    Rηx(Θxψ)dr=W(Θxψ)xηdx=jˉbjˉaj(Θxψ)xηdx.

    Since ΘxψH1x(ˉaj,ˉbj), we can write

    ˉbjˉaj(Θxψ)xηdx=ˉbjˉajηx(Θrψ)dx+η(ˉbj)(Θxψ)(ˉbj)η(ˉaj)(Θxψ)(ˉaj),

    where the boundary terms vanish since xψ(ˉaj)=xψ(ˉbj)=0 as we have shown before. By using the identity (3.11) and the bounds for GCP states in Definition 10, we obtain

    |2Rηx(Θxψ)dx|ηL2x(R)(22xρΛ2ρL2x(W)+rJρL2x(W))C(M2)ηL2x(R).

    Thus we conclude x˜ψ=ΘxψH1x(R). Moreover again by the Sard type Lemma 6, we have x(Θxψ)=0 almost everywhere on the set {ρ=0}={ψ=0}, therefore the identity

    22x˜ψ=2x(Θxψ)=[22xρΛ2ρ+ixJρ]1{ρ>0}Θϕ (3.13)

    holds true in L2x(R), and the bound (1.9) for the wave function ˜ψ follows directly.

    One of the main obstacles for multi-dimensional problems is the topology of the vacuum region {ρ=0}. First, while in one space dimension the energy estimate and the Sobolev embedding yield the position density to be continuous, which consequently implies that {ρ=0} is a closed set, in the multidimensional cases we loose this topological information and in general it is not possible to characterize the structure of the vacuum region with the same methods of the 1-D case. Moreover, for d2 an extra structural property of the quantum vortex discussed in Section Section 1 needs to be taken into account. Therefore we first focus on the wave function lifting method in two-dimensional space, and we assume that the position density ρ=ρ(x), xR2, is continuous such that V={x;ρ(x)=0} consists of isolated points, namely there exists an at most countable set A of indices, such that

    V={x(α)}αAR2,infαβ|x(α)x(β)|>0. (4.1)

    Moreover a quantization condition for the vorticity is required, as explained in the discussion of quantum vortices presented in Section Section 1. More precisely, let v=J/ρ be the velocity field, which is well-defined almost everywhere, then the quantised vorticity condition (1.6) is restated in the sense of distribution as

    {vM(R2),v=2παAkαδx(α),kαZ, (4.2)

    where M(R2) is the space of measures, and δx(α) is the Dirac-delta function supported at x(α) for αA. This condition is connected to the Bohr-Sommerfeld quantization rule in quantum theory.

    Remark 18. A straightforward consequence of the wave function lifting is that the quantized vorticity condition (4.2) implies the generalized irrotationality condition

    J=2ρΛ,for a.e.xR2. (4.3)

    More precisely, given a hydrodynamic state (ρΛ) satisfying the assumptions of Theorem 3, then we know that there exists an associated wave function ψH1x(R2), then as a consequence of the polar factorization Proposition 7, we further have that the hydrodynamic state (ρ,Λ) satisfy the identity (4.3), where J=ρΛ. On the other hand, the reverse implication from (4.3) to (4.2) does not hold, see e.g., [6].

    Now we are at the point to prove the wave function lifting proposition in the two dimensional case. We will use the notion of difference quotients (see [11]), namely for any function fL1loc(R2) and direction hR2, |h|>0, we define

    Dhf(x)=f(x+h)f(x)|h|. (4.4)

    As |h|0, the difference quotient Dhf will approximate the derivative of f in the direction h.

    We remark that in the cases of quantum vortices, the non-vacuum region is a connected set, therefore as a direct consequence of Lemma 13, the lifted wave function is unique upto constant rotation.

    Proof of Theorem 3. We restrict to the simplest case, when the vacuum is a single point, and without loss of generality we assume V={0}. In this case the quantised vorticity condition becomes

    {vM(R2),v=2kπδ0,kZ. (4.5)

    For isolated vacuum points, the proof follows essentially the same idea.

    To construct a wave function we take a sequence of smooth mollifier {χϵ} such that supp(χϵ)Bϵ(0), where Br(x) is the ball centred at x with radius r. We define

    vϵ(x)=vχϵ(x)=v(),χϵ(x),

    so that

    vϵ=(v)χϵ=2kπδ0χϵ=2kπχϵ.

    Let us fix an arbitrary x0Bϵ(0), we can take a piecewise smooth curve γ(x) connecting x0 and x, strictly away from Bϵ(0). In this way, for any xBϵ(0), the approximating polar factor ϕϵ can be defined as

    ϕϵ(x)=exp(iγ(x)vϵ(y)dl(y))

    and we extend the definition of ϕϵ continuously to xBϵ(0) by setting ϕϵ(x)=ϕϵ(ϵx/|x|).

    We claim that the above definition of ϕϵ is independent of the choice of curve γ. Indeed, for any two curves γ1 and γ2 connecting x0 and x, we can patch them into a piecewise smooth closed curve ˜γ. Denote Ω the domain inside ˜γ, then we have two cases: Bϵ(0)Ω or Bϵ(0)Ω=. In either case by Stokes' theorem

    γ1vϵ(y)dl(y)γ2vϵ(y)dl(y)=˜γvϵ(y)dl(y)=Ωvϵ(y)dy=2kπ or 0,

    where k is the integer given in (4.5), thus we have

    exp(iγ1vϵ(y)dl(y))=exp(iγ2vϵ(y)dl(y)).

    The polar factors {ϕϵ} have uniform Lx bound 1, therefore up to subsequences we have ϕϵϕ in Lx(R2) with ϕLx1. The lifted wave function is defined by ψ=ρϕ. Obviously ψL2x(R2), then we are going to show ψH1x(R2).

    For this purpose, we only need to show the L2 norm of the difference quotient Dhϕ defined in (4.4) has a uniform bound, namely

    DhψL2x(R2)C

    for some constant C and all hR2 with |h|0 small. We have

    DhψL2x(R2)=DhψL2x(B|h|(0))+DhψL2x(B|h|(0)c).

    For the part near the vacuum point 0, we simply bound it by

    DhψL2x(B|h|(0))=1|h|ψ(+h)ψ()L2x(B|h|(0))2|h|ρLx(B1(0))|B|h|(0)|12=2πρLx(B1(0)),

    which is uniformly bounded since ρ is continuous.

    Then we consider the norm away from the vacuum. For any relatively compact open set UB|h|(0)c and for any ϵ<|h|, we have explicit representation

    ϕϵ=exp(iγvϵ(y)dl(y)),ϕϵ=ivϵϕϵ.

    By the continuity of ρ, we have infxU{ρ(x)}=α>0 and the velocity field v=Λ/ρL2x(U). Moreover, vϵv in L2x(U) and ϕ=limε0ϕε, then it follows

    ϕϵ=ivϵϕϵivϕ=ϕin L2x(U). (4.6)

    Thus we obtain that in L2x(U)

    ψ=(ρ+iρv)ϕ=(ρ+iΛ)ϕ

    with uniform L2x bound

    ψL2x(U)=ρL2x(U)+ΛL2x(U)M1.

    By using a sequence of relatively compact sets U invading Bc, we get

    ψL2x(Bh(0)c)1M1,

    and we conclude ψH1x(R2). Furthermore, the above argument implies that for a.e. xR2 we have

    ψ=(ρ+iΛ)ϕ, (4.7)

    which proves the polar factorization (2.2).

    Further let us assume the condition (1.13), then we are able to show that ψH2(R2). The proof uses difference quotients as in the previous case, but here it requires further small technicalities since ψLx.

    Let us consider a relatively compact set U, strictly away from the vacuum point 0. By (4.6) and (4.7) it follows that for j=1,2,

    [(22xjρΛ2jρ)+ixjJjρ]ϕ=(22xjρ+ixjΛj+ixjρvjΛjvj)ϕ=xj[(xjρ+Λj)ϕ]=2xj(xjψ)

    in the sense of distribution. Therefore the condition (1.13) and Definition 9 of λj imply 2xjψL2x(U) satisfying the uniform bound

    2xjψL2x(U)2M2. (4.8)

    Now we again take the smooth mollifier {χϵ} such that supp(χϵ)Bε(0), and we define the smooth approximating wave function ψε=ψχε. It follows (4.8) that for any relatively compact open set U such that dist(U,0)>ε, we have

    2xjψεL2x(U)2xjψL2x(Uε)2M2, (4.9)

    where Uε is the εneighbourhood of the set U. For xjψε, j=1,2, by using the polar factorization we can decompose it as xjψε=|xjψε|ϕεj, where the polar factor ϕεj=xjψε/|xjψε| when |xjψε|0. In this case direct computation shows

    xjϕεj=iIm(xj¯ψε2xjψε)|xjψε|2ϕεj, (4.10)

    and by the same argument as polar factorization we have

    |2xjψε|2=(xj|xjψε|)2+(Im(xj¯ψε2xjψε)|xjψε|)2. (4.11)

    To apply the theory of difference quotients, instead of xjψε and xjψ, we will consider the L cut-off functions {fεj,n} and fj,n defined by

    fεj,n=min{|xjψε|,n}ϕεj,j=1,2,fj,n=min{|xjψ|,n}ϕj,ϕjP(xjψ).

    By using the fact

    |fεj,nfj,n||xjψεxjψ|,

    and xjψεxjψ in L2x(R2), it follows fεj,nfj,n in L2(R2) as ε0.

    Now we consider the difference quotient of fj,n in the direction ej, where

    e1=(1,0)ande2=(0,1),

    and we let hj=|h|ej for |h|0 small, and we have

    Dhjfj,nL2x(R2)=Dhjfj,nL2x(B|h|(0))+Dhjfj,nL2x(B|h|(0)c).

    For the part near the vacuum, it can be simply controlled by

    Dhjfj,nL2x(B|h|(0))2πfj,nLx2πn.

    The part away from the vacuum is treated again by considering a relatively compact open sets UB|h|(0)c. By definition |fεj,n||xjψε|, and since 2xjψεL2x(U) for all ε<|h|, the xjderivative of the truncated function fεj,n also belongs to L2x(U). Moreover by using (4.10) and (4.11), for |jψε|>n we have

    |xjfεj,n|2=|xj(nϕεj)|2=(nIm(xj¯ψε2xjψε)|xjψε|2)2(Im(xj¯ψε2xjψε)|xjψε|)2|2xjψε|2,

    and xjfεj,n=2xjψε in the case |xjψε|n. Therefore by using (4.9), we have the uniform bound

    xjfεj,nL2x(U)2xjψεL2x(U)2M2.

    By passing to the limit as ε0, we obtain

    xjfj,nL2x(U)2M2 (4.12)

    for any relatively compact open set U strictly away from 0, hence it also works on B|h|(0)c. Therefore the theory of difference quotient shows xjfj,nL2(R2) and we have the bound

    xjfj,nL2x(R2)2M2+2πn.

    Notice that even though the bound of xjfj,nL2 obtained above depends on n, as long as we have xjfj,nL2(R2), a zero measure set has no effect on the L2 norm of xjfj,n. Thus by choosing a sequence of open set U invading R2{0} in (4.12), we obtain that

    xjfj,nL2x(R2)2M2,j=1,2.

    On the other hand, it is straightforward to see that fj,n converges to xjψ strongly as n by construction. Therefore we conclude 2xjψL2x(R2) for j=1,2, with the bound

    2xjψL2x(R2)2M2.

    It implies ψL2x(R2) and we have

    ψL2x(R2)22M2,

    then by standard argument we can conclude that ψH2x(R2) satisfies the bound

    ψH2x(R2)C(1M1+2M2).

    The wave function lifting argument can also be extended to a simple example of 3D hydrodynamic data, where we assume planar symmetry of the data and the vorticity to be concentrated in a finite number of vortex lines. This is a typical example of the vortex structure of quantum flows in 3D space [22]. More precisely, we consider hydrodynamic data (ρ(x),J(x)), x=(x1,x2,x3)R3 and JR3, of the following form:

    ρ(x)=ρ1(x1,x2)ρ2(x3)andJ(x)=(J1(x1,x2)ρ2(x3),0)=ρΛ, (4.13)

    where ρ,ρjR and J1R2. The data (ρ,J) is essentially a product of a 2D data (ρ1,J1) and a 1D data (ρ2,0). We assume (ρ1,J1)=((ρ1)2,ρ1Λ1) has pointwise vacuum and quantised vorticity, namely we assume ρ1 to be continuous with vacuum structure (1.11), and the velocity field v1=J1/ρ1 to satisfy the quantized vorticity condition (1.12). The regularity of (ρ1,J1) is characterised by the bounds (1.10) and (1.13), and we assume ρ2Hsx(R) with s=1 or 2.

    Under the above assumptions, we can state the following proposition as an extension of the wave function lifting argument to 3D data.

    Proposition 19. Let (ρ,J) be a hydrodynamic data as in (4.13), with (ρ1,J1) satisfying the conditions (1.11) and (1.12). Furthermore let us assume that (ρ1,J1) satisfy the mass and energy bounds (1.10) and ρ2H1x(R). Then there exists a wave function ψH1x(R3) such that

    ρ=|ψ|,Λ=Im(ˉϕψ),

    where ϕP(ψ) is a polar factor defined in (2.1).

    If we furthermore assume the bounds (1.13) on (ρ1,J1) and ρ2H2(R), then ψH2x(R3) and

    ψH2x(R3)C(1M1+2M2).

    In the last section we will extend the wave function lifting method to GCP weak solutions of QHD system (1.3) given by Definition 10. For existence results of GCP solutions, we refer to [4,5] for polynomial potential H=ργ1, γ>1. We also restrict ourselves to the case of non-vacuum solutions to avoid the difficulty involving the structure of vacuum regions and the dynamics of system (1.3).

    In the previous results, the lifted wave function ψ associated to given hydrodynamic data (ρ,J) is constructed at every fixed time, which can be rotated by any constant phase shift. However, to recover the dynamics of the corresponding Schrödinger equation, the evolution of the phase function should also be considered in the scheme of wave function lifting, which is solved by a space-time gradient equation involving the velocity v and the chemical potential μ, as we will see in the next lemma.

    Lemma 20 (Phase function). Let (ρ,J) be a GCP solution of (1.3) on [0,T)×Rd with potential HLtL1loc,x, such that ρ is strictly positive on any compact set. Then there exists a unique (upto constant phase shifts in space-time) phase function S(LtH1loc,xW1,tL1loc,x)([0,T)×Rd), which can be explicitly written as

    S(t,x)=S+Ul(0,x)v0(y)dlydx+Ul(x,x)v(t,y)dlydxUt0μ(s,x)dsdx, (5.1)

    where S[0,2π) and U=(12,12)d.

    Proof. By Lemma 16, for (ρ,J) generated by a wave function ψ such that |ψ|=ρ is strictly positive on any compact set, we have

    v=Im(ψψ),μ=22ρρ+12|v|2+H=22Re(ψψ)+H,

    which imply vLt([0,T),L2loc,x(Rd)) and μLt([0,T),L1loc,x(Rd)). On the other hand, by Madelung transformation (1.1), the phase function S, formally given by S=1ilog(ψ|ψ|), of ψ should satisfy a space-time gradient equation

    {S=v,tS=μ,S(0,0)=S. (5.2)

    Therefore we should define the phase function S to be the unique solution of the space-time gradient Eq (5.2). For locally strictly positive density, the generalised irrotationality condition (2.5) reduces to

    v=0

    in the sense of distribution, and the equation for momentum density in (1.3) can be written as

    tv=22(ρρ)12|v|2H=μ, (5.3)

    which exactly combine to the solvability condition of the gradient Eq (5.2).

    To rigorously define the phase function S in hydrodynamic functions, we again use the smooth mollifiers {χϵ} and define

    vϵ(x)=vχϵ(x),μϵ(x)=μχϵ(x),

    which also satisfy the "irrotationality" conditions

    vε=0,tvε=με. (5.4)

    Then we define the approximating phase function to be

    Sε(t,x;x)=S+l(0,x)vε,0(y)dly+l(x,x)vε(t,y)dlyt0με(s,x)ds,

    where xRd is an arbitrary point, and the curve l(x,y) of integration is given by

    l(x,y)=dj=1{(y1,,yj1,z,xj+1,,xd);z(min{xj,yj},max{xj,yj})},

    namely the piecewise straight lines parallel to frame axises connecting x and y. It is straightforward to check that the approximating phase function Sε solves the mollification of Eq (5.2), namely

    {Sε=vSε,tSε=με,Sε(0,0)=Sε.

    However, for weak solutions (ρ,J), the velocity v and the chemical potential μ are merely Lebesgue functions in LtL1loc,x, therefore we can not directly take the limit ε0 in Sε(t,x;x). On the other hand, due to the irrotationality condition (5.4), the choice of x has no influence on the definition of Sε(t,x;x), thus we can take the average of Sε(t,x;x) with respect to xU=(12,12)d, which allows us to give the hydrodynamic definition of the approximating phase function Sε independent of x as

    Sε(t,x)=S+Ul(0,x)vε,0(y)dlydx+Ul(x,x)vε(t,y)dlydxUt0με(s,x)dsdx.

    By take the limit ε0, we obtain the explicit formulation of the phase function S as (5.1). The regularity of S is a direct consequence of (5.1) and vLt([0,T),L2loc,x(Rd)),μLt([0,T),L1loc,x(Rd)).

    Remark 21. If we replace the local positivity of ρ and the irrotationality condition v=0 with the quantised vorticity condition (4.2), and assume that the velocity and the chemical potential satisfy

    vLt([0,T),L1x,loc(Rd)),μM([0,T)×Rd),

    where M([0,T)×Rd) is the space of Radon measures, then we can extend Lemma 20 to the cases of quantum vortex. However, so far assumptions above for v and μ, and the structure of quantum vortex, are not proven to be preserved along general GCP weak solutions, due to the lack of estimates of v and μ when vacuums exist. Therefore we restrict ourselves to the case of non-vacuum.

    Now we can proof the main theorem of this section.

    Proof of Theorem 4. Following the assumption of Theorem 4, we can define a wave function

    ψ=ρeiS,

    where S is the phase function of (ρ,J) given by Lemma 20. By Eq (5.2), it is straightforward to compute that ψ is an wave function associated to (ρ,J) in the sense

    ρ=|ψ|2,J=Im(ˉψψ).

    Therefore by Theorem 2 or Theorem 3, we have ψLt([0,T),H2x(Rd)). Moreover, by the continuity equation of ρ and (5.2), we can compute that

    tψ=(tρ+iρtS)eiS=[divJ2ρ+iρμ]eiS.

    Recall that

    divJ=Im(ˉψψ),
    μ=22Re(ψψ)+H,

    then it follows that

    tψ=[2Im(ˉψψ)2ρ+i22Re(ψψ)iH]ρeiS=[22Im(ψψ)+i22Re(ψψ)iH]ψ=i222ψiHψ,

    which shows ψ is a solution of the corresponding Schrödinger equation. The uniqueness of the lifted wave function is a direct consequence of Lemma 13 and the local positivity of |ψ|.

    In this paper, we consider the Pauli problem to construct a quantum state from given distribution of position density ρ and momentum density J of particles, and the uniqueness of the associated quantum state.

    In the following cases: 1-dimensional data with general vacuum regions, multi-dimensional quantum vortex data satisfying the quantised vorticity condition (1.6), and solutions of the QHD system (1.3) without vacuum, we provide the wave function lifting method to construct a complex wave function ψ as a quantum state associated to given (ρ,J) in the sense of

    ρ=|ψ|2,J=Im(ˉψψ),

    where (ρ,J) belongs to the finite energy space or the GCP space (see Definition 10), and the wave function ψ has corresponding regularity in H1x or H2x.

    Concerning the uniqueness problem, we prove that in general the lifted wave function is not unique if the connected components of the non-vacuum region {ρ>0} are strictly separated by open neighbourhoods. However, we also show that the only resource of non-uniqueness is the lost of information on vacuum boundaries, and any two lifted wave functions associated to the same (ρ,J) are only differed by a piecewise constant phase shift function of the form

    Θ=exp(ijθj1Ωj),θj[0,2π),

    where Ωj's are the connected components of {ρ>0}.

    The authors declare they have not used Artificial Intelligence (AI) tools in the creation of this article.

    The authors declare no conflicts of interest.



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