Differential and Integral Equations Volume 19, Number 6 (2006), 627–668 QUANTITATIVE UNIQUENESS FOR TIME-PERIODIC HEAT EQUATION WITH POTENTIAL AND ITS APPLICATIONS K-D. Phung Yangtze Center of Mathematics, Sichuan University, Chengdu 610064, China G. Wang Department of Mathematics, Wuhan University, Wuhan 430072, China The Center for Optimal Control and Discrete Mathematics Huazhong Normal University, Wuhan 730079, China (Submitted by: Viorel Barbu) Abstract. In this paper, we establish a quantitative unique continuation property for some time-periodic linear parabolic equations in a bounded domain Ω. We prove that for a time-periodic heat equation with particular time-periodic potential, its solution u(x, t) satisfies u(·, 0)L2 (Ω) ≤ C u(·, 0)L2 (ω) where ω ⊂ Ω. Also we deduce the asymptotic controllability for the heat equation with an even, timeperiodic potential. Moreover, the controller belongs to a finite dimensional subspace and is explicitly computed. 1. Introduction and main results Throughout this paper, Ω is a connected bounded domain in Rd , d ≥ 1, with a boundary ∂Ω of class C 2 , ω is a non-empty open subset of Ω. Let 1 > 0 be the first eigenvalue of the operator −Δ with the Dirichlet boundary condition (i.e., the smallest strictly positive eigenvalue of −Δ in H01 (Ω)). Let T > 0 be a real number; we denote by .∞ the usual norm in L∞ (Ω×(0, T )). In this paper, we study an infinite-dimensional system generated by the following parabolic equation ∂t y − Δy + ay = f in Ω × (0, +∞), (1.1) y = 0 on ∂Ω × (0, +∞), Accepted for publication: February 2006. AMS Subject Classifications: 35B10, 93B07, 93B60. The first author thanks the support of the NCET od China under grant NCET-04-0882, and the NSF of China under grants 10371084 and 10525105. 627 628 K-D. Phung and G. Wang with an even, T -periodic, bounded potential a = a(x, t) ∈ L∞ (Ω × R) satisfying 1 ≤ a∞ and a(x, t + T ) = a(x, t) = a(x, −t) in Ω × R. (1.2) We assume that y(·, 0) = y o ∈ L2 (Ω) and f = f (x, t) ∈ L1loc (0, +∞; L2 (Ω)), so that (1.1) admits a unique solution y = y(x, t) ∈ C([0, +∞); L2 (Ω)). Let {G(t, s)}0≤s≤t<+∞ be the T -periodic evolutionary process on L2 (Ω), such that t G(t, r)f (·, r)dr, (1.3) y(·, t) = G(t, s)y(·, s) + s for all 0 ≤ s ≤ t, where the T -periodicity of G(t, s) means G(t + T, s + T ) = G(t, s). Notice that any bounded function in L∞ (Ω × (0, T /2)) can be extended to be an even, T -periodic potential a ∈ L∞ (Ω × R). Here, we are only interested in the case where (a∞ − 1 ) ≥ 0 and a is not positive, because if (a∞ − 1 ) < 0 or a ≥ 0, then the system (1.1) is clearly stable when f = 0. The Poincaré map is usually defined by G(T + t, t). We restrict our attention on the operator G(T, 0) G(T, 0) : L2 (Ω) −→ L2 (Ω) y(·, 0) −→ y(·, T ). (1.4) It is well known that G(T, 0) is compact by the smoothing action of the diffusion. Since a is even and T -periodic, we see that G(T, 0) is self-adjoint. Consequently, there is a complete orthonormal set in L2 (Ω) formed of eigenfunctions (zjo )j≥1 of G(T, 0) corresponding to eigenvalues (λj )j≥1 , where λj = λj (T ) depends on T , λj ∈ R, λj → 0 as j → +∞. Thus, we may arrange the eigenfunctions so that the sequence {|λj |}j≥1 is non-increasing, · · · ≤ |λm+1 | ≤ |λm | ≤ · · · ≤ |λ1 |. Clearly, λj = 0 from the backward uniqueness property for the linear parabolic equation. Furthermore, we will see that for all T > 0 and for all even, T -periodic, bounded potentials a, any eigenvalue λj (T ) of G(T, 0) satisfies 1 + ln |λj (T )| ≤ a∞ . T (1.5) The first result of the paper is as follows. Theorem 1. There exist two constants co ∈ (0, 1) and C > 0, both only depending on ω and Ω, such that if we choose the time-periodicity T ∈ (0, co ] Quantitative uniqueness for time-periodic heat equation 629 and an even, T -periodic potential a ∈ L∞ (Ω × R) such that 1 ≤ a∞ ≤ 1 co 1/4 , T then any eigenfunction zjo of G(T, 0) in L2 (Ω), corresponding to the eigenvalue λj (T ) with |λj (T )| ≥ 1, satisfies Ω G(t, 0)zjo (x)2 dx ≤ eCa4/3 ∞ ω G(t, 0)zjo (x)2 dx for all t ≥ 0. The knowledge of the eigencouple of the Poincaré map plays a key role in the study of periodic parabolic systems (see [14], [15]). Theorem 1 implies clearly that the eigenfunctions zjo of the Poincaré map corresponding to the eigenvalues λj with |λj | ≥ 1 have the unique continuation property. It is classical in control theory for linear partial differential equations that the unique continuation property is linked with the approximate controllability and, more precisely, a quantitative uniqueness result yields an estimate of the cost of the approximate control (see e.g. [12]). Here, our second theorem establishes an asymptotic controllability (or open loop stabilizability) for the heat equation with time-periodic potential. Theorem 2. There exist two constants co ∈ (0, 1) and C > 0, both only depending on Ω and ω, such that if we choose the time-periodicity T ∈ (0, co ] and an even, T -periodic potential a ∈ L∞ (Ω × R) such that 1 ≤ a∞ ≤ 1 co 1/4 , T and if there exists m > 0 such that · · · ≤ |λm+1 (T )| < 1 ≤ |λm (T )| = · · · = |λ2 (T )| = |λ1 (T )| , 630 K-D. Phung and G. Wang then for each initial data y o ∈ L2 (Ω), the control function fc ∈ C([0, T ]; L2 (Ω)) satisfying ⎧ (i) ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ (ii) ⎪ ⎪ ⎨ fc (x, T − t) = σj (t)G(t, 0)zjo (x), j=1,··,m ⎛ ⎞ σ1 (t) −1 ⎜ . ⎟ o o ⎜ . ⎟ = −1 G(t, 0)z (x)G(t, 0)z (x)dx κ j T ω ⎝ . ⎠ 1≤κ,j≤m σm (t) ⎛ ⎞ ⎪ ⎪ y o (x)G(T, 0)z1o (x)dx ⎪ Ω ⎪ ⎪ ⎜ ⎟ ⎪ .. ⎪ ⎟, ⎪ ×⎜ ⎪ . ⎝ ⎠ ⎪ ⎪ ⎪ o o ⎪ ⎪ y (x)G(T, 0)z (x)dx m ⎪ Ω ⎪ T 4/3 ⎩ (iii) 0 fc (·, s)L2 (ω) ds ≤ eCa∞ e(a∞ −1 )T y o L2 (Ω) , implies that the solution y = y(x, t) ∈ C([0, +∞); L2 (Ω)) of the following heat equation with potential a and control function fc , ⎧ ⎨ ∂t y − Δy + ay = fc · 1|ω×(0,T ) in Ω × (0, +∞), y = 0 on ∂Ω × (0, +∞), ⎩ y(·, 0) = y o in Ω, satisfies, for all t ≥ T , y(·, t)L2 (Ω) ≤ Cm e−γt y o L2 (Ω) , where 4/3 2eC (a∞ +a∞ T ) − ln |λm+1 (T )| . > 0 and Cm = γ= T |λm+1 (T )|2 The notion of asymptotic controllability is standard in the nonlinear control theory of finite-dimensional systems (see e.g. [7]). Here, (i) says that our control has a finite-dimensional structure (see also [4], [5]). (ii) implies that the operator associating the initial data with the control function is linear which gives a kind of robustness property of our control. (iii) gives us an explicit expression of the cost of the control, from which we see easily that we can act a control on the equation in a very short time T , but as a payment, evenness and T -periodicity for the potential a are required. From the following property of the Poincaré map, G(nT, 0)zjo = (λj )n zjo (1.6) for all n ∈ N, it is clear that if all eigenvalues λj satisfy |λj | < 1, then the system (1.1) is stable without control. On the other hand, if the modulus of some eigenvalues of G(T, 0) are bigger than one, then the equation Quantitative uniqueness for time-periodic heat equation 631 (1.1) with f = 0 is unstable. We call such eigenvalues unstable eigenvalues. Theorem 2 amounts to saying that if all unstable eigenvalues have the same absolute value then the equation (1.1) with f = fc · 1|ω×(0,T ) can be stabilized by a control fc in a finite-dimensional subspace of L2 (Ω) spanned by (zjo )j=1,··· ,m which are the eigenfunctions of G(T, 0) corresponding to the unstable eigenvalues. So it is important to study the unique continuation of the eigenfunctions of G(T, 0) corresponding to the unstable eigenvalues. This is why we restrict our attention in Theorem 1 to the case where |λj | ≥ 1. The unique continuation property or more precisely the number of zeros of a one-dimensional parabolic equation is well described in [1] which leads to the study of the asymptotic behaviour of the periodic 1d quasilinear parabolic equation [3], or to the consideration of the structural stability of the periodic 1d semilinear heat equation [6]. In order to get Theorem 1 and Theorem 2, we need a more general unique continuation result in bounded domains Ω ⊂ Rd , d ≥ 1, described as follows. Theorem 3. There exist two constants co ∈ (0, 1) and C > 0, both only depending on Ω and ω, such that for all T ∈ (0, co ], β ≥ 0 and q ∈ L∞ (Ω × (0, T )) satisfying co 1/4 , 1 + β ≤ q∞ ≤ 1 T we have 4/3 |u(x, 0)|2 dx ≤ eCq∞ Ω where u ∈ tion C([0, T ]; L2 (Ω)) |u(x, 0)|2 dx, ω solves the following T -periodic linear heat equa- ⎧ ⎨ ∂t u − Δu + βu + qu = 0 in Ω × (0, T ), u = 0 on ∂Ω × (0, T ), ⎩ u(·, 0) = u(·, T ) in Ω. Strong unique continuation for the heat equation with potential in bounded domains Ω ⊂ Rd , d ≥ 1, has been widely studied, (see for instance [10], [11] and references therein). In [17], one obtains that any solution v of the linear heat equation with time-independent Lipschitz continuous potential such that v(·, to ) = 0 in ω, for some to ∈ (0, T ), satisfies v = 0 in Ω × (0, T ). The idea of the proof in [17] is to transform the solution v to a solution of an elliptic equation where the unique continuation property for elliptic operators can be used (see also [8]). Here we are interested in the unique continuation and its quantification of the linear time-periodic heat equation with time-dependent potential. The basic technique used here is to combine 632 K-D. Phung and G. Wang some properties of time-periodic solutions of the heat equation with a kind of global Carleman estimate for an elliptic operator. This paper is organized as follows. In Section 2, we give an introduction of the Poincaré map and some related preliminary results, then we prove Theorem 1. In Section 3 and Section 4, we give the proofs of Theorem 2 and Theorem 3 respectively. In Section 5, we point out some related results for a particular case where the potential depends only on time. Finally, in the Appendix, we give the proof of the Global Carleman inequality we need. 2. The Poincaré map Let a be an even, T -periodic, bounded function in L∞ (Ω × R); more precisely a(x, t + T ) = a(x, t) = a(x, −t) in Ω × R. We consider the following heat equation with the potential a = a(x, t), ∂t y − Δy + ay = f in Ω × (s, +∞), (2.1) y = 0 on ∂Ω × (s, +∞), where s ≥ 0 and f ∈ L1loc (0, +∞; L2 (Ω)). Let y ∈ C([s, +∞); L2 (Ω)) be the mild solution of (2.1) and G(t, s) be the T -periodic evolutionary process generated by −Δ + aI in L2 (Ω). More precisely, {G(t, s)}0≤s≤t<+∞ is a family of bounded linear operators from L2 (Ω) to itself, such that ⎧ ⎪ (i) G(t, t) = I for all t ≥ 0, ⎪ ⎪ ⎪ ⎪ ⎪ ⎨(ii) G(t, r)G(r, s) = G(t, s) for all 0 ≤ s ≤ r ≤ t, (iii) The map (t, s) → G(t, s)g is continuous for every fixed g ∈ L2 (Ω), ⎪ ⎪ ⎪ (iv) G(t + T, s + T ) = G(t, s) for all 0 ≤ s ≤ t, ⎪ ⎪ ⎪ ⎩(v) G(t, s) ≤ e(a∞ −1 )(t−s) for all 0 ≤ s ≤ t. (2.2) Thus, the mild solution y of equation (2.1) can be written in the following form t y(·, t) = G(t, s)y(·, s) + G(t, r)f (·, r)dr (2.3) s for all 0 ≤ s ≤ t. Now, we are going to focus our attention on the Poincaré map G(T, 0) and obtain some properties in our case. Since a is even and T -periodic, we get that G(T, 0) is self-adjoint. Indeed, let pT ∈ L2 (Ω) and p ∈ C([0, T ]; L2 (Ω)) be the solution of ⎧ ⎨ −∂t p − Δp + ap = 0 in Ω × (0, T ), p = 0 on ∂Ω × (0, T ), (2.4) ⎩ T in Ω, p(·, T ) = p Quantitative uniqueness for time-periodic heat equation then for all y o ∈ L2 (Ω), o y (x)p(x, 0)dx = [G(T, 0)y o (x)] pT (x)dx; Ω 633 (2.5) Ω that is, (2.6) G∗ (T, 0)pT (x) = p(x, 0). On the other hand, because a(x, T − t) = a(x, t), the solution w(x, t) = p(x, T − t) solves ⎧ ∂t w − Δw + aw = 0 in Ω × (0, T ), ⎪ ⎪ ⎨ w = 0 on ∂Ω × (0, T ), (2.7) w(·, 0) = pT in Ω, ⎪ ⎪ ⎩ w(·, T ) = p(·, 0) in Ω. Finally, for all pT ∈ L2 (Ω), G∗ (T, 0)pT (x) = G(T, 0)pT (x). (2.8) L2 (Ω), we deduce that there As G(T, 0) is a compact self-adjoint operator on is a complete orthonormal set in L2 (Ω) formed by the eigenfunctions (zjo )j≥1 of G(T, 0) with corresponding eigenvalues λj = λj (T ) ∈ R, which converge to 0 as j → +∞. Thus, we can arrange the eigenfunctions so that the sequence {|λj |}j≥1 is non-increasing. Now we are able to give some properties of the eigencouple (zjo , λj (T )) associated to the compact self-adjoint operator G(T, 0). Lemma 2-1. For all s ∈ [0, T ] and φ ∈ L2 (Ω), o φ(x)G(T − s, 0)zj (x)dx = G(T, s)φ(x)zjo (x)dx. Ω Ω It follows immediately from Lemma 2-1 that for all s ∈ [0, T ], G(T − s, 0)zjo (x) G(s, 0)zio (x) dx = δij . λj Ω (2.8) Lemma 2-2. As soon as the time-periodicity T > 0 and an even, T -periodic potential a ∈ L∞ (Ω × R) are chosen, then any eigenvalue λj (T ) of G(T, 0) satisfies ln |λj (T )| 1 + ≤ a∞ . T Note that in particular, under the hypothesis of Theorem 1, the eigenvalues λj (T ) have to satisfy co 1/4 ln |λj (T )| 1 + . (2.9) ≤ a∞ ≤ 1 T T 634 K-D. Phung and G. Wang 2.1. Proof of Lemma 2-1. Let g = g(x, t) ∈ C([s, T ]; L2 (Ω)) be the solution of ⎧ ⎨ ∂t g − Δg + ag = 0 in Ω × (s, T ), g = 0 on ∂Ω × (s, T ), (2.10) ⎩ g(·, s) = φ in Ω, and zj = zj (x, t) ∈ C([0, T ]; L2 (Ω)) be the solution of ⎧ ⎨ ∂t zj − Δzj + azj = 0 in Ω × (0, T ), zj = 0 on ∂Ω × (0, T ), ⎩ zj (·, 0) = zjo in Ω. (2.11) Now, from the relation a(·, T − t) = a(·, t), we obtain that the function t → Ω g(x, t)zj (x, T − t)dx is constant. Indeed, d g(x, t)zj (x, T − t)dx dt Ω ∂t g(x, t)zj (x, T − t)dx + g(x, t) − (∂t zj )(x, T − t) dx = Ω Ω −(−Δ + a(x, t))g(x, t)zj (x, T − t)dx = Ω g(x, t)(−Δ + a(x, t))zj (x, T − t)dx = 0. (2.12) + Ω Consequently, for all t ∈ [s, T ], g(x, s)zj (x, T − s)dx = g(x, t)zj (x, T − t)dx = g(x, T )zjo (x)dx. Ω Ω Ω (2.13) That completes the proof of Lemma 2-1. 2.2. Proof of Lemma 2-2. Let ln |λj (T )| β = ∈R T and u = u(x, t) ∈ C([0, 2T ]; L2 (Ω)) be the solution of ⎧ + au = 0 in Ω × (0, 2T ), ⎨ ∂t u − Δu + βu u = 0 on ∂Ω × (0, 2T ), ⎩ u(·, 0) = zjo in Ω. By an energy method, we have the following equality 1d 2 2 |u(x, t)| dx + |∇u(x, t)| dx + β |u(x, t)|2 dx 2 dt Ω Ω Ω (2.14) (2.15) Quantitative uniqueness for time-periodic heat equation 635 a(x, t) |u(x, t)|2 dx = 0. + (2.16) Ω Also, notice that u(x, t) = e−βt zj (x, t) = e−βt G(t, 0)zjo (x) = 0 and u(·, 2T ) = u(·, 0) From (2.16) and (2.17), we get 1 + β − a ∞ 0 2T in Ω. (2.17) |u(x, t)|2 dx ≤ 0. (2.18) Ω Consequently, ln |λj (T )| 1 + β = 1 + ≤ a∞ . T This is the desired inequality. (2.19) 2.3. Proof of Theorem 1. For |λj (T )| ≥ 1, we have that ln |λj (T )| ≥0 T and u(x, t) = e−βt zj (x, t) ∈ C([0, 2T ]; L2 (Ω)) satisfies ⎧ ⎨ ∂t u − Δu + βu + au = 0 in Ω × (0, 2T ), u = 0 on ∂Ω × (0, 2T ), ⎩ u(·, 2T ) = u(·, 0) in Ω. β= (2.20) (2.21) Now, we apply Theorem 3 for the 2T -periodic solution u of (2.21) with q = a ∈ L∞ (Ω × (0, 2T )) satisfying co 1/4 ln |λj (T )| (2.22) ≤ a∞ ≤ 1 1 + T 2T to obtain 2 Ca4/3 ∞ |u(x, 0)| dx ≤ e |u(x, 0)|2 dx. (2.23) Ω ω It follows by translation in time and by the 2T -periodicity of u that for all t ∈ [0, 2T ], 2 Ca4/3 ∞ |u(x, t)| dx ≤ e |u(x, t)|2 dx. (2.24) Ω ω Consequently, we obtain that for all t ∈ [0, 2T ], G(t, 0)zjo (x)2 dx ≤ eCa4/3 G(t, 0)zjo (x)2 dx. ∞ Ω Hence, if we choose co in Theorem 1 to be we complete the proof of Theorem 1. (2.25) ω co 2 in Theorem 3 and the same C, 636 K-D. Phung and G. Wang 3. The asymptotic controllability problem In this section, we prove Theorem 2. Recall that if (a∞ − 1 ) < 0, then the system (1.1) is already stable with f = 0. We consider the solution of the following heat equation with a potential a = a(x, t) ∈ L∞ (Ω × R) satisfying a(x, t + T ) = a(x, t) = a(x, −t) in Ω × R and (a∞ − 1 ) ≥ 0, ⎧ ⎨ ∂t y − Δy + ay = fc · 1|ω×(0,T ) in Ω × (0, +∞), (3.1) y = 0 on ∂Ω × (0, +∞), ⎩ y(·, 0) = y o in Ω, where y o ∈ L2 (Ω) and fc ∈ C([0, T ]; L2 (Ω)). It is clear that for all integers n ≥ 1, we have nT o y(·, nT ) = G(nT, 0)y + G(nT, s) fc (·, s) · 1|ω×(0,T ) ds. (3.2) 0 (zjo , λj (T )) Let G(T, 0), then be the eigencouple of the compact self-adjoint operator o y = Ω j≥1 y o (x)zjo (x)dx zjo . (3.3) It follows from Lemma 2-1 that for any s ∈ [0, T ], G(T, s) fc (x, s) · 1|ω×(0,T ) G(T, s)(fc (x, s) · 1|ω×(0,T ) )zjo (x)dx zjo (x) = = j≥1 Ω j≥1 Ω fc (x, s) · 1|ω×(0,T ) G(T − s, 0)zjo (x)dx zjo (x). (3.4) By (3.3), (3.4) and by the periodicity of G(t, s), we infer o G(nT, 0)y = y o (x)zjo (x)dx G(nT, 0)zjo Ω j≥1 = j≥1 and λnj Ω y o (x)zjo (x)dx zjo (3.5) G(nT, s) fc (x, s) · 1|ω×(0,T ) = G(nT, T )G(T, s) fc (x, s) · 1|ω×(0,T ) = fc (x, s) · 1|ω×(0,T ) G(T − s, 0)zjo (x)dx G(nT, T )zjo (x) j≥1 Ω Quantitative uniqueness for time-periodic heat equation = j≥1 = j≥1 1|(0,T ) · fc (x, s)G(T − ω λn−1 1|(0,T ) · j ω s, 0)zjo (x)dx 637 G((n − 1)T, 0)zjo (x) fc (x, s)G(T − s, 0)zjo (x)dx zjo (x). (3.6) We conclude from (3.5) and (3.6) that y(x, nT ) = j≥1 λnj Yj (T )zjo (x) for all integers n ≥ 1, where T 1 o o y (x)zj (x)dx + fc (x, s)G(T − s, 0)zjo (x)dxds. (3.7) Yj (T ) = λj 0 ω Ω Recall that we have arranged the eigenfunctions so that {|λj |}j≥1 is a nondecreasing sequence. Let m > 0 be such that |λj | ≤ |λm+1 | < 1 for all j ≥ m + 1 and 1 ≤ |λm | ≤ |λj | for all j = 1, · · · , m. Now we decompose y(x, nT ) as follows y(x, nT ) = y1,m (x, nT ) + y2,m (x, nT ), where y1,m (x, nT ) = (3.8) λnj Yj (T )zjo (x) (3.9) λnj Yj (T )zjo (x). (3.10) j=1,··· ,m and y2,m (x, nT ) = j≥m+1 Note that y1,m is the projection of y in the subspace of L2 (Ω) spanned by the eigenfunctions (zjo )j=1,··· ,m of G(T, 0) corresponding to the unstable eigenvalues (λj )j=1,···,m while y2,m is the projection of y in the subspace of L2 (Ω) spanned by the eigenfunctions (zjo )j≥m+1 of G(T, 0) corresponding to the stable eigenvalues (λj )j≥m+1 . Next, we estimate respectively 2 2 Ω |y2,m (x, nT )| dx and Ω |y1,m (x, nT )| dx. It follows first from (3.10) that |y2,m (x, nT )|2 dx = |λj |2n |Yj (T )|2 Ω j≥m+1 = j≥m+1 zjo (x) 2 |λj | y(x, T ) dx . λj Ω 2n Indeed, because of the evenness and T -periodicity of a, we have T G(T − s, 0)zjo (x) fc (x, s) dxds λj ω 0 (3.11) 638 K-D. Phung and G. Wang T = Ω 0 G(T − s, 0)zjo (x) dxds λj ∂t y(x, s) − Δy(x, s) + a(x, T − s)y(x, s) zjo (x) = y(x, T ) dx − λj Ω Ω y o (x)zjo (x)dx. (3.12) As |λj | ≤ |λm+1 | < 1 for all j ≥ m + 1, we deduce from (3.11) that 2 |y2,m (x, nT )|2 dx ≤ |λm+1 |2(n−1) y(x, T )zjo (x)dx Ω j≥m+1 ≤ |λm+1 |2(n−1) Ω |y(x, T )|2 dx. (3.13) Ω On the other hand, we have |y1,m (x, nT )|2 dx = Ω |λj |2n |Yj (T )|2 j=1,··· ,m by (3.9) where T 1 1 o o y (x)zj (x)dx + fc (x, s)G(T − s, 0)zjo (x)dx ds. Yj (T ) = T Ω λj ω 0 (3.14) Now we are in position to construct a control function fc = fc (x, s) ∈ C([0, T ]; L2 (Ω)) such that for all x ∈ Ω, for all s ∈ [0, T ], σi (s)G(s, 0)zio (x), (3.15) fc (x, T − s) = i=1,···,m where σi = σi (s) ∈ C([0, T ]) and 1 1 o o y (x)zj (x)dx + fc (x, s)G(T − s, 0)zjo (x)dx = 0 (3.16) T Ω λj ω for all j = 1, · · · , m, which implies Ω |y1,m (x, nT )|2 dx = 0. By (3.15) and (3.16), it suffices to obtain {σi (s)}i=1,··· ,m by solving the following linear system λj σi (s) zi (x, s)zj (x, s)dx = − y o (x)zjo (x)dx; (3.17) T Ω ω i=1,··· ,m that is, ⎡ ··· ⎢ .. .. ⎣ . . ω z1 (x, s)zm (x, s)dx · · · ω z1 (x, s)z1 (x, s)dx ⎞ σ1 (s) ⎥⎜ ⎟ .. .. ⎦⎝ ⎠ . . σm (s) ω zm (x, s)zm (x, s)dx ω zm (x, s)z1 (x, s)dx ⎤⎛ Quantitative uniqueness for time-periodic heat equation ⎛ =− 1⎜ ⎝ T Ωy o (x)z 1 (x, T )dx .. . 639 ⎞ ⎟ ⎠ (3.18) o Ω y (x)zm (x, T )dx where zj = zj (x, t) ∈ C([0, +∞); L2 (Ω)) is the solution of ⎧ ⎨ ∂t zj − Δzj + azj = 0 in Ω × (0, +∞), zj = 0 on ∂Ω × (0, +∞), ⎩ zj (·, 0) = zjo in Ω. (3.19) The existence of suchσi (s) ∈ C([0, T ]) can be proved if and only if for all o o s ∈ [0, T ], the matrix is invertible. ω G(s, 0)zi (x)G(s, 0)zj (x)dx 1≤i,j≤m G(s, 0)zio (x)G(s, 0)zjo (x)dx . By contra!1≤i,j≤m diction, we assume that M (s) = ω zi (x, s)zj (x, s)dx 1≤i,j≤m is a not invertible matrix for some s ∈ [0, T ] fixed. Then the lines of M (s) are linearly in dependent which implies that {zi (x, s)}i=1,··· ,m are linearly dependentm−1 2 L (ω). Hence there exists μ1 (s), · · · , μm−1 (s) a non-zero vector in R such that 3.1. Invertibility of ω μ1 (s)z1 (·, s) + · · · + μm−1 (s)zm−1 (·, s) − zm (·, s) = 0 in ω. (3.20) However, by the assumption that |λm+1 | < 1 ≤ |λm | = · · · = |λ2 | = |λ1 |, it follows that the function κs (x, t) = μ1 (s)z1 (x, t) + · · · + μm−1 (s)zm−1 (x, t) − zm (x, t) satisfies ⎧ ⎨ ∂t κs − Δκs + aκs = 0 in Ω × (0, 2T ), κs = 0 on ∂Ω × (0, 2T ), ⎩ κs (·, 2T ) = |λ1 |2 κs (·, 0) in Ω. (3.21) (3.22) ln|λ1 | Let u(x, t) = e− T t κs (x, t), then u ∈ C([0, 2T ]; L2 (Ω)) solves ⎧ 1| ⎨ ∂t u − Δu + ln|λ T u + au = 0 in Ω × (0, 2T ), u = 0 on ∂Ω × (0, 2T ), ⎩ u(·, 2T ) = u(·, 0) in Ω. (3.23) By Theorem 3, there exists a constant c1 > 0 such that if we choose a ∈ L∞ (Ω × R) such that c1 1/4 1 ≤ a∞ ≤ 1 , (3.24) 2T 640 K-D. Phung and G. Wang and noting that 1 + ln |λ1 | ≤ a∞ T and ln |λ1 | ≥ 0, T (3.25) which follows from Lemma 2-2 and the fact that |λ1 | ≥ 1, then the solution u = u(x, t) of (3.23) satisfies u(·, 0) = 0 in ω =⇒ u(·, 0) = 0 in Ω. (3.26) It follows by translation in time and by the 2T -periodicity of u that u(·, s) = 0 in ω =⇒ u(·, s) = 0 in Ω. (3.27) So κs (·, s) = 0 in Ω and o o − zm = 0 in Ω. (3.28) μ1 (s)z1o + · · · + μm−1 (s)zm−1 ! This contradiction shows that the matrix ω zi (x, s)zj (x, s)dx 1≤i,j≤m is invertible for all s ∈ [0, T ] and ⎞ ⎡ ⎤−1 ⎛ z (x, s)z (x, s)dx · · · z (x, s)z (x, s)dx σ1 (s) 1 1 m 1 ω ω ⎟ ⎢ ⎥ ⎜ .. .. .. .. ⎠=⎣ ⎦ ⎝ . . . . z1 (x, s)zN (x, s)dx · · · zm (x, s)zm (x, s)dx σm (s) ⎞ ω ⎛ ω1 o − T Ω y (x)z1 (x, T )dx ⎟ ⎜ .. (3.29) ×⎝ ⎠. . 1 o − T Ω y (x)zm (x, T )dx Consequently, if we take the control function fc ∈ C([0, T ]; L2 (Ω)) in equation (3.1) as fc (x, t) = σi (T − t)zi (x, T − t), (3.30) i=1,··· ,m then the corresponding solution y ∈ C([0, +∞); L2 (Ω)) satisfies y(·, nT )L2 (Ω) = y2,m (·, nT )L2 (Ω) ≤ |λm+1 |(n−1) y(·, T )L2 (Ω) ≤ |λm+1 |(n−1) y o L2 (Ω) e(a∞ −1 )T (3.31) T + |λm+1 |(n−1) fc (·, s)L2 (ω) e(a∞ −1 )(T −s) ds, 0 for all integers n ≥ 1, where λm+1 is the first eigenvalue such that |λm+1 | < 1. Quantitative uniqueness for time-periodic heat equation 641 3.2. Estimate of fc (·, s)L2 (ω) . It follows from (3.31) that we would like T to compute 0 fc (·, s)L2 (ω) e(a∞ −1 )(T −s) ds. We have ⎞ ⎛ σ (s) 1 ⎟ ⎜ .. σ1 (s) · · · σm (s) · zi (x, s)zj (x, s)dx ⎠ ⎝ . 1≤i,j≤m ω σm (s) ⎞ ⎛ o y (x)z1 (x, T )dx Ω ⎜ 1 ⎟ .. σ1 (s) · · · σm (s) · ⎝ =− (3.32) ⎠, . o T Ω y (x)zm (x, T )dx or equivalently 2 1 σi (s)zi (x, s) dx = − y o (x) T ω Ω i=1,··· ,m which implies "2 " " " σi (s)zi (·, s)" 2 " i=1,··· ,m σi (s)zi (x, T )dx, (3.33) i=1,··· ,m " " 1 o " " σi (s)zi (·, T )" 2 y L2 (Ω) " T L (ω) L (Ω) i=1,··· ,m " " σi (s)G(T, s)zi (·, s)" 2 ≤ " 1 o " ≤ y L2 (Ω) " T i=1,··· ,m " 1 o " ≤ y L2 (Ω) "G(T, s) T L (Ω) " " σi (s)zi (·, s)" i=1,··· ,m ≤ " 1 o " y L2 (Ω) e(a∞ −1 )(T −s) " T L2 (Ω) " " σi (s)zi (·, s)" i=1,··· ,m L2 (Ω) Now we claim that there exists a constant c > 0 such that " " " " " " " " σi (s)zi (·, s)" 2 ≤ c" σi (s)zi (·, s)" " i=1,··· ,m L (Ω) i=1,··· ,m . L2 (ω) (3.34) . Indeed, since |λm+1 | < 1 ≤ |λm | = · · · = |λ2 | = |λ1 |, the function κs (x, t) = σi (s)zi (x, t) (3.35) (3.36) i=1,··· ,m satisfies ⎧ ⎨ ∂t κs − Δκs + aκs = 0 in Ω × (0, 2T ), κs = 0 on ∂Ω × (0, 2T ), ⎩ κs (·, 2T ) = |λ1 |2 κs (·, 0) in Ω. (3.37) 642 K-D. Phung and G. Wang ln|λ1 | Let u(x, t) = e− T t κs (x, t), then u ∈ C([0, 2T ]; L2 (Ω)) satisfies ⎧ 1| ⎨ ∂t u − Δu + ln|λ T u + au = 0 in Ω × (0, 2T ), u = 0 on ∂Ω × (0, 2T ), ⎩ u(·, 2T ) = u(·, 0) in Ω. (3.38) By Theorem 3, there exists a constant c1 > 0, which is the same as that in (3.24), such that if we choose a ∈ L∞ (Ω × R) satisfying (3.24) and note (3.25) then the following estimate holds 2 Ca4/3 ∞ |u(x, 0)| dx ≤ e |u(x, 0)|2 dx, (3.39) Ω ω where C > 0 is a constant which depends only on ω and Ω. It follows by translation in time and by the 2T -periodicity of u solution of (3.38) that for all s ∈ [0, T ], 2 Ca4/3 ∞ |u(x, s)| dx ≤ e |u(x, s)|2 dx, (3.40) Ω which implies ω 2 Ca4/3 ∞ |κs (x, s)|2 dx |κs (x, s)| dx ≤ e Ω or equivalently " " " " σi (s)zi (·, s)" " i=1,··· ,m (3.41) ω L2 (Ω) " 4/3 " ≤ eCa∞ " i=1,··· ,m " " σi (s)zi (·, s)" L2 (ω) , (3.42) as desired. By (3.42) and (3.34) we get " " 4/3 1 " " σi (s)zi (·, s)" 2 ≤ y o L2 (Ω) e(a∞ −1 )(T −s) eCa∞ . (3.43) " T L (ω) i=1,··· ,m Now we conclude that if we take co = all a ∈ L∞ (Ω × R) satisfying c1 2 where c1 is given in (3.39) then for co 1/4 , (3.44) T we may take the control function fc ∈ C([0, T ]; L2 (Ω)) of the form (3.15) with estimates T T 1 Ca4/3 a∞ −1 (T −s) o ∞ y 2 fc (·, s)L2 (ω) ds ≤ e e ds L (Ω) T 0 0 4/3 (3.45) ≤ eCa∞ e a∞ −1 T y o L2 (Ω) 1 ≤ a∞ ≤ 1 Quantitative uniqueness for time-periodic heat equation and 0 T 643 4/3 fc (·, s)L2 (ω) e(a∞ −1 )(T −s) ds ≤ eCa∞ e2(a∞ −1 )T y o L2 (Ω) , (3.46) so that the corresponding solution y ∈ C([0, +∞); L2 (Ω)) of (3.1) satisfies (3.31). 3.3. Exponential decay of the solution. Now we turn to obtaining the 4/3 exponential decay of the solution. Let CT,a = 1 + eCa∞ e(a∞ −1 )T . By (3.31) and (3.46), it follows that y(·, nT )L2 (Ω) ≤ |λm+1 |(n−1) CT,a e(a∞ −1 )T y o L2 (Ω) (3.47) for all integers n ≥ 1. For any t ≥ T , we may write t = nT + σ where n ≥ 1 and 0 ≤ σ < T . Since y(·, t) = G(t, nT )y(·, nT ), it follows from (3.47) that y(·, t)L2 (Ω) = y(·, nT )L2 (Ω) e(a∞ −1 )(t−nT ) ≤ y(·, nT )L2 (Ω) e(a∞ −1 )T 1 1 ≤ exp − (n + 1) ln CT,a e2(a∞ −1 )T y o L2 (Ω) , |λm+1 (T )| |λm+1 (T )|2 (3.48) which implies CT,a e2(a∞ −1 )T o t 1 y L2 (Ω) y(·, t)L2 (Ω) ≤ exp − ln T |λm+1 (T )| |λm+1 (T )|2 (3.49) for all t ≥ T , and completes the proof of Theorem 2. 4. The quantitative unique continuation for time-periodic heat equation with potential In this section, we shall show Theorem 3 by dividing the proof into three steps. In the first step, we study the solutions u locally in ω×{t = 0} then, in the second step, we apply a global Carleman inequality for elliptic operators where time t ∈ (0, T ) is seen as a parameter. In the last step, we conclude the proof of Theorem 3 by choosing an adequate time T . 4.1. Step 1: Local property of u near t = 0. The goal of this subsection is to prove the following result: 644 K-D. Phung and G. Wang Lemma 4-1. There exist a non-empty open subset ω of ω and a constant Cω > 1 depending only on ω and Ω such that for all T > 0 and integers M ≥ 2, we have M d 2 2q∞ t 2+ M |u(x, t)| dx ≤ e t |u(x, 0)|2 dx Cω (M + 2) ω Ω 1 − C (M + 2)2 tM d ω 2q∞ t (M + 2) M |u(x, 0)|2 dx +e 1 − Cω (M + 2)2 t ω for all t ∈ (0, T ), where the solution u solves the following linear heat equation with potential ⎧ ⎨ ∂t u − Δu + βu + qu = 0 in Ω × (0, T ), u = 0 on ∂Ω × (0, T ), ⎩ u(·, 0) ∈ L2 (Ω). Proof of Lemma 4-1. Let xo ∈ Rd and ro > 0; we denote $ # B(xo , r) = #x ∈ Rd : |x − xo | ≤ ro , $ D(xo , r) = x ∈ Rd : |xi − xoi | ≤ ro , for all i = 1, · · · , d . (4.1) Without loss of generality, we suppose that there exists r > 0 such that D(0, 2r) ⊂ ω. Then B(xo , r) ⊂ ω for all xo ∈ [−r, r]d . Let N ≥ 4 be an arbitrary but fixed integer; we have B(xo , r/N ) ⊂ B(xo , 2r/N ) ⊂ · · · ⊂ B(xo , r) ⊂ ω. (4.2) Let us define a sequence of smooth functions Φn ∈ C0∞ (B(xo , nr/N )) for n = 2, · · · , N such that ⎧ 0 ≤ Φn ≤ 1, ⎨ Φn = 1 in B(xo , (n − 1)r/N ), (4.3) ⎩ |∇Φn | ≤ 2N/r. The construction of such a sequence Φn is standard. Let Φ ∈ C0∞ (B(xo , ro )); multiplying the equation in Lemma 4-1 by Φ2 u, we get the usual energy equality 1d 2 2 |Φu(x, t)| dx + |Φ∇u(x, t)| dx + β |Φu(x, t)|2 dx (4.4) 2 dt Ω Ω Ω = − q(x, t) |Φu(x, t)|2 dx − 2 Φ(x)∇u(x, t) · ∇Φ(x)u(x, t)dx, Ω Ω Quantitative uniqueness for time-periodic heat equation 645 from which, after some calculation involving the Cauchy-Schwarz inequality, we infer 1d |Φu(x, t)|2 dx (4.5) 2 dt B(xo ,ro ) ≤ q∞ |Φu(x, t)|2 dx + ∇Φ2L∞ (B(xo ,ro )) |u(x, t)|2 dx. B(xo ,ro ) B(xo ,ro ) Multiplying (4.5) by e−2q∞ t , we obtain d |Φu(x, t)|2 dx e−2q∞ t dt B(xo ,ro ) 2 |u(x, t)|2 dx e−2q∞ t . ≤ 2 ∇ΦL∞ (B(xo ,ro )) (4.6) B(xo ,ro ) Taking Φ = Φn and ro = nr/N in (4.6), using (4.3), it follows that d gn (t) ≤ 8(N/r)2 gn+1 (t) dt for all n = 2, · · · , N − 1, where |Φn u(x, t)|2 dx e−2q∞ t . gn (t) = (4.8) Integrating (4.7) over (0, t), we obtain that for all n = 2, · · · , N − 1, t gn+1 (τ )dτ + gn (0). gn (t) ≤ 8(N/r)2 (4.9) (4.7) B(xo ,nr/N ) 0 By induction, we deduce that for n = 0, · · · , N − 3, t j 2 n+1 n t gn+3 (τ )dτ + g2 (t) ≤ 8(N/r) 8(N/r)2 t gj+2 (0). (4.10) 0 j=0,··· ,n By (4.8), (4.3) and (4.10), after some computation, we have 2 −2q∞ t |u(x, t)| dx e ≤ |u(x, t)|2 dx e−2q∞ t √ o o D(x ,r/(N d)) B(x ,r/N ) ≤ |Φ2 u(x, t)|2 dx e−2q∞ t ≤ g2 (t) B(xo ,2r/N ) ≤ (8(N/r)2 )N −2 tN −3 t gN (τ )dτ + 0 ≤ (8(N/r)2 )N −2 tN −3 t 0 B(xo ,r) (8(N/r)2 t)j gj+2 (0) j=0,··· ,N −3 |ΦN u(x, τ )|2 dxe−2q∞ τ dτ 646 K-D. Phung and G. Wang + 2 j (8(N/r) t) j=0,··· ,N −3 2 N −2 N −3 ≤ (8(N/r) ) B(xo ,(j+2)r/N ) t |u(x, τ )|2 dxe−2q∞ τ dτ t 0 1 − (8(N/r)2 t)N −2 + 1 − 8(N/r)2 t |Φj+2 u(x, 0)|2 dx Ω |u(x, 0)|2 dx. (4.11) ω On the other hand, it is easy to check that for all τ ∈ (0, T ), 2 −2q∞ τ |u(x, τ )| dx e ≤ |u(x, 0)|2 dx, Ω (4.12) Ω which together with (4.11) implies 2 2q∞ t 2 N −2 N −2 |u(x, t)| dx ≤ e (8(N/r) ) t |u(x, 0)|2 dx √ D(xo ,r/(N d)) + e2q∞ t (8(N/r)2 t)N −2 1 − 1 − 8(N/r)2 t Ω |u(x, 0)|2 dx. (4.13) ω Now, we break the rectangle [0, √rd ]d ⊂ Rd into N d small rectangles Dj , j = 1, · · · , N d , having the same shape, by dividing each interval [0, √rd ] into % N small pieces (i.e., [0, √rd ] = [k N r√d , (k + 1) N r√d ] and [0, √rd ]2 = k=0,··,N −1 % % k N r√d , (k + 1) N r√d × k N r√d , (k + 1) N r√d , ...). k=0,··,N −1 k=0,··· ,N −1 It is clear that meas Dj1 ∩ Dj2 = 0 for j1 = j2 and also 2 |u (x, t)| dx = |u (x, t)|2 dx. (4.14) d 0, √r d Dj j=1,··,N d One can check that for each Dj , j = 1, · · · , N d , r Dj ⊂ D xo , k √ , N d (4.15) √ if xo = (xo1 , · · · , xod ) ∈ [−r, r]d with xoi , j = 1, · · · , d, equals k(r/N d) for some k = 0, · · · , N − 1, which implies by (4.14) that 2 d 2q∞ t 2 N −2 (8(N/r) t) |u(x, 0)|2 dx d |u(x, t)| dx ≤ N e 0, √r d + N d e2q∞ t 1 − (8(N/r)2 t)N −2 1 − 8(N/r)2 t ω Ω |u(x, 0)|2 dx. (4.16) Quantitative uniqueness for time-periodic heat equation 647 Let M = N − 2 ≥ 2; we have M d 2 2q∞ t 8 2+ M |u(x, t)| dx ≤ e (M + 2) t |u(x, 0)|2 dx r2 √r [0,1]d Ω d 8 M (M + 2)2 t d 1 − r2 + e2q∞ t (M + 2) M |u(x, 0)|2 dx. (4.17) 1 − r82 (M + 2)2 t ω Lemma 4-1 follows. 4.2. Step 2: Observability estimate for periodic-parabolic solutions. The goal of this section is to prove the following observability inequality: Theorem 4-1. Let ω be a non-empty open subset of ω. There exists a constant c > 0 such that for all T > 0, β ≥ 0 and q ∈ L∞ (Ω × (0, T )), we have T e2q∞ T 2 4/3 2/3 |u(x, 0)| dx ≤ |u(x, t)|2 dxdt exp c(1 + β + q∞ ) T Ω ω 0 where u ∈ C([0, T ]; L2 (Ω)) solves the following T -periodic in time linear heat equation with potential ⎧ ⎨ ∂t u − Δu + βu + qu = 0 in Ω × (0, T ), u = 0 on ∂Ω × (0, T ), ⎩ u(·, 0) = u(·, T ) in Ω. As we know, for initial condition problems of parabolic equations, the constant of observability grows in an exponentially fast way of order e1/T (see [12]). However, Theorem 4-1 shows that the constant of observability √ explodes for small time only in a polynomially fast way of order 1/ T for parabolic equations with time-periodic conditions. In order to prove Theorem 4-1, we need the following propositions. Proposition 4-1. Let ωo be a non-empty open subset of Ω. There exist a smooth function ϕ = ϕ(x) ≥ 1 and a constant c > 0, such that for all T > 0, β ≥ 0, q ∈ L∞ (Ω × (0, T )) and θ ≥ c 1 + β 2/3 + q4/3 ∞ , we have d 1 1 2 2θϕ(x) e |∇u(x, t)| dx + β e2θϕ(x) |u(x, t)|2 dx dt 2 Ω 2 Ω e2θϕ(x) |∇ϕ(x)|2 |u(x, t)|2 dx − θ2 Ω 1 2 2θϕ(x) 2 + e |∇u(x, t)| dx + θ e2θϕ(x) |u(x, t)|2 dx c Ω Ω 648 K-D. Phung and G. Wang ≤c θ 2θϕ(x) e 2 |∇u(x, t)| dx + θ ωo 3 2θϕ(x) e 2 |u(x, t)| dx ωo for almost every t ∈ (0, T ), where u = u(x, t) solves the following linear heat equation with potential ⎧ ⎨ ∂t u − Δu + βu + qu = 0 in Ω × (0, T ), u = 0 on ∂Ω × (0, T ), ⎩ u(·, 0) ∈ H 2 (Ω) ∩ H01 (Ω). Proposition 4-2. (Global Carleman inequality for the operator Δ − β) Let ωo be a non-empty open subset of Ω. There exist a smooth function ϕ = ϕ(x) ≥ 1 and a constant c > 0, such that for all β ≥ 0, q ∈ L∞ (Ω), 4/3 q L∞ (Ω) and w ∈ H 2 (Ω) ∩ H01 (Ω), we have θ > c 1 + β 2/3 + "2 " " " "2θ∇ϕ · ∇(eθϕ w) − qeθϕ w" 2 L (Ω) 1 2θϕ(x) 2 3 + e |∇w(x)| dx + θ e2θϕ(x) |w(x)|2 dx θ c Ω Ω " "2 " θϕ " 2θϕ(x) 2 3 ≤ "e (Δ − β)w" 2 c θ e |∇w(x)| dx + θ e2θϕ(x) |w(x)|2 dx . L (Ω) ωo ωo The proof of Proposition 4-2 is given in the Appendix. Proof of Proposition 4-1. We apply Proposition 4-2 to the solution u of the linear heat equation with potential, then we deduce that there exist a smooth function ϕ = ϕ(x) ≥ 1 and a constant c > 0, such that for all β ≥ 0, 4/3 , we have q ∈ L∞ (Ω × (0, T )), and θ > c 1 + β 2/3 + q∞ " " " "2 "2θ∇ϕ · ∇ eθϕ u(·, t) − q(·, t)eθϕ u(·, t)" 2 L (Ω) 1 + e2θϕ(x) |∇u(x, t)|2 dx + θ3 e2θϕ(x) |u(x, t)|2 dx θ c Ω Ω " "2 " θϕ " ≤ "e (Δ − β)u(·, t)" 2 L (Ω) 2θϕ(x) 2 3 +c θ e |∇u(x, t)| dx + θ e2θϕ(x) |u(x, t)|2 dx (4.18) ωo ωo for almost every t ∈ (0, T ). On the other hand, we multiply equation −∂t u + (Δ − β)u − qu = 0 by e2θϕ (Δ − β)u and integrate it over Ω to get 1 d 1d 2 2θϕ(x) e |∇u(x, t)| dx + β e2θϕ(x) |u(x, t)|2 dx 2 dt Ω 2 dt Ω Quantitative uniqueness for time-periodic heat equation " "2 " " + "eθϕ (Δ − β)u(·, t)" 2 L (Ω) = q(x, t)u(x, t)(Δ − β)u(x, t)e2θϕ(x) dx Ω ∂t u(x, t)2θ∇ϕ(x) · ∇u(x, t)e2θϕ(x) dx − Ω q(x, t)u(x, t)(Δ − β)u(x, t)e2θϕ(x) dx = Ω ∂t u(x, t)eθϕ(x) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx − Ω ∂t u(x, t)eθϕ(x) 2θ∇ϕ(x) · (θ∇ϕ(x)eθϕ(x) )u(x, t)dx + 649 (4.19) Ω which implies, with Ξ(t) = Ω e2θϕ(x) |∇u(x, t)|2 dx + β Ω e2θϕ(x) |u(x, t)|2 dx − 2θ2 Ω |∇ϕ(x)|2 e2θϕ(x) |u(x, t)|2 dx, "2 " 1d " " θϕ Ξ(t) + "e (Δ − β)u(·, t)" 2 2 dt L (Ω) − q(x, t)u(x, t)(Δ − β)u(x, t)e2θϕ(x) dx Ω (4.20) = − ∂t u(x, t)eθϕ(x) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx. Ω Replacing ∂t u by (Δ − β) u − qu in the right-hand side of (4.20), we deduce that "2 " 1d " " Ξ(t) + "eθϕ (Δ − β)u(·, t)" 2 2 dt L (Ω) + eθϕ(x) (Δ − β)u(x, t) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx Ω eθϕ(x) (Δ − β)u(x, t) −q(x, t)eθϕ(x) u(x, t) dx + Ω q(x, t)u(x, t)eθϕ(x) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx. (4.21) = Ω By the Cauchy-Schwarz inequality, the right-hand side of (4.21) is bounded by q(x, t)u(x, t)eθϕ(x) 2θ∇ϕ(x) · θ∇ϕ(x)eθϕ(x) u(x, t)dx Ω 650 K-D. Phung and G. Wang q(x, t)u(x, t)eθϕ(x) 2θ∇ϕ(x) · eθϕ(x) ∇u(x, t)dx Ω " "2 " " ≤ 2θ2 q∞ ∇ϕ2L∞ (Ω) "eθϕ u" 2 L (Ω) " " " " " " θϕ " " + 2θ q∞ ∇ϕL∞ (Ω) "e u" 2 "eθϕ ∇u" 2 . + L (Ω) L (Ω) (4.22) Then, we conclude by (4.21) and (4.22) that " "2 1d " " Ξ(t) + "eθϕ (Δ − β)u(·, t)" 2 2 dt L (Ω) + eθϕ(x) (Δ − β)u(x, t) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx Ω + eθϕ(x) (Δ − β)u(x, t) −q(x, t)eθϕ(x) u(x, t) dx Ω " " " θϕ "2 2 2 ≤ 2θ q∞ ∇ϕL∞ (Ω) "e u" 2 L (Ω) " " " " " " " " + 2θ q∞ ∇ϕL∞ (Ω) "eθϕ u" 2 "eθϕ ∇u" 2 . (4.23) L (Ω) L (Ω) Consequently, there exists a constant c > 0 such for all β ≥ 0 and q ∈ L∞ (Ω × (0, T )), we have "2 " 1d " " Ξ(t) + "eθϕ (Δ − β)u(·, t)" 2 2 dt L (Ω) + eθϕ(x) (Δ − β)u(x, t) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx Ω θϕ(x) θϕ(x) e (Δ − β)u(x, t) −q(x, t)e u(x, t) dx + Ω e2θϕ(x) |∇u(x, t)|2 dx + θ2 e2θϕ(x) |u(x, t)|2 dx (4.24) ≤ c q∞ Ω Ω for almost every t ∈ (0, T ). By (4.18) and (4.24), we get "2 θϕ 1" " " θϕ 2θ∇ϕ · ∇ e u(·, t) − q(·, t)e u(·, t) " " 2 2 L (Ω) 1 θ + e2θϕ(x) |∇u(x, t)|2 dx + θ3 e2θϕ(x) |u(x, t)|2 dx 2c Ω Ω c e2θϕ(x) |∇u(x, t)|2 dx + θ3 e2θϕ(x) |u(x, t)|2 dx − θ 2 ωo ωo Quantitative uniqueness for time-periodic heat equation "2 1" " " θϕ e (Δ − β)u(·, t) " 2 " 2 L (Ω) " "2 1d 1" " ≤− Ξ(t) − "eθϕ (Δ − β)u(·, t)" 2 2 dt 2 L (Ω) − eθϕ(x) (Δ − β)u(x, t) 2θ∇ϕ(x) · ∇ eθϕ(x) u(x, t) dx Ω eθϕ(x) (Δ − β)u(x, t) −q(x, t)eθϕ(x) u(x, t) dx − Ω e2θϕ(x) |∇u(x, t)|2 dx + θ2 e2θϕ(x) |u(x, t)|2 dx + c q∞ 651 ≤ Ω (4.25) Ω from which it follows that "2 1" " θϕ " "e (Δ − β)u(·, t) + 2θ∇ϕ · ∇ eθϕ u(·, t) − q(·, t)eθϕ u(·, t)" 2 2 L (Ω) 1d 1 + e2θϕ |∇u(x, t)|2 dx + θ2 e2θϕ |u(x, t)|2 dx Ξ(t) + θ 2 dt 2c Ω Ω 2 2θϕ 2 2θϕ e |∇u(x, t)| dx + θ e |u(x, t)|2 dx ≤ c q∞ Ω Ω c 2 2θϕ 3 e |∇u(x, t)| dx + θ e2θϕ |u(x, t)|2 dx . (4.26) + θ 2 ωo ωo + 4c c q∞ in (4.26), we deduce that the By taking θ ≥ c 1 + β 2/3 + q4/3 ∞ inequality 1d 2 2θϕ(x) 2 e |∇u(x, t)| dx + θ e2θϕ(x) |u(x, t)|2 dx Ξ(t) + c 2 dt Ω Ω c 2 2θϕ(x) 3 2θϕ(x) e |∇u(x, t)| dx + θ e |u(x, t)|2 dx (4.27) ≤ θ 2 ωo ωo holds for all θ ≥ c1 1 + β 2/3 + q4/3 where c1 > 0 is large enough. This ∞ completes the proof of Proposition 4-1. Proof of Theorem 4-1. Throughout the proof of Theorem 4-1, c denotes several positive constants only depending on the geometry. By integrating the estimate in Proposition 4-1 over (0, T ), we get T T 2 2θϕ(x) 2 e |∇u(x, t)| dxdt + θ e2θϕ(x) |u(x, t)|2 dxdt (4.28) 0 Ω T ≤c θ 0 2θϕ(x) e ωo Ω 0 2 |∇u(x, t)| dxdt + θ 3 0 T ωo e2θϕ(x) |u(x, t)|2 dxdt , 652 K-D. Phung and G. Wang thanks to the T -periodicity of u. With an adequate choice of θ > c 1+β 2/3 + in (4.28), it follows that, denoting Cβ,q = exp c(1 + β 2/3 + q4/3 q4/3 ∞ ∞ ) , T T T 2 2 |u(x, t)| dxdt ≤ Cβ,q |u(x, t)| dx + |∇u(x, t)|2 dx . 0 Ω 0 0 ωo ωo (4.29) By the usual energy method (i.e., an equality like (4.4)), we also have T T 2 |∇u(x, t)| dxdt ≤ (c + q∞ ) |u(x, t)|2 dx (4.30) 0 ω 0 ωo ⊂ ω, using the T -periodicity of u. for some ωo ⊂ ω Consequently, for all T > 0, β ≥ 0 and q ∈ L∞ (Ω × (0, T )), T T |u(x, t)|2 dxdt ≤ exp c(1+β 2/3 +q4/3 ) |u(x, t)|2 dx. (4.31) ∞ 0 Ω 0 ω where u solves the following T -periodic in time linear heat equation with potential ⎧ ∂ u − Δu + βu + qu = 0 in Ω × (0, T ), ⎪ ⎪ ⎨ t u = 0 on ∂Ω × (0, T ), (4.32) u(·, 0) = u(·, T ) in Ω, ⎪ ⎪ ⎩ u(·, 0) ∈ H 2 (Ω) ∩ H01 (Ω). By density of H 2 (Ω) ∩ H01 (Ω) in L2 (Ω), this last estimate is also true for solutions u with initial data in L2 (Ω). On the other hand, we recall that 2 2q∞ t 2q∞ T e |u(x, T )| dx ≤ e |u(x, t)|2 dx (4.33) Ω and 1 2q∞ T T ≤ −1 = e 2 q∞ Ω T e2q∞ t dt. (4.34) 0 Finally, it follows from (4.33), (4.34) and (4.31) that e2q∞ T T 2 2 |u(x, 0)| dx = |u(x, T )| dx ≤ |u(x, t)|2 dxdt T Ω Ω Ω 0 T e2q∞ T |u(x, t)|2 dxdt. (4.35) ≤ exp c(1 + β 2/3 + q4/3 ∞ ) T ω 0 This completes the proof of Theorem 4-1. Quantitative uniqueness for time-periodic heat equation 653 4.3. Step 3: Choice of T . Now we are able to conclude the proof of Theorem 3 as follows. By integrating over (0, T ) the estimate in Lemma 4-1, we have M d 1 T |u(x, t)|2 dx ≤ e2q∞ T Cω (M + 2)2+ M T |u(x, 0)|2 dx T 0 ω Ω M 2 1 − Cω (M + 2) T d |u(x, 0)|2 dx. (4.36) + e2q∞ T (M + 2) M 1 − Cω (M + 2)2 T ω Combining the latter with Theorem 4-1, we deduce that there exists a constant c > 1 such that for all T > 0, q ∈ L∞ (Ω × (0, T )) and integers M ≥ 2, we have, denoting Cβ,q = exp c(1 + β 2/3 + q4/3 ∞ ) , M 2 2+d/M 4q∞ T |u(x, 0)| dx ≤ Cβ,q e T |u (x, 0)|2 dx Cω (M + 2) Ω 4q∞ T + Cβ,q e d/M (M + 2) 1 − Cω (M + 2)2 T M Ω 1 − Cω (M + 2)2 T |u (x, 0)|2 dx. ω (4.37) From this we infer that there exists a constant c > 1 such that for all T > 0, β ≥ 0 and q ∈ L∞ (Ω × (0, T )) satisfying 1 + β ≤ q∞ , the inequality M 2 c(1+T )q4/3 2+d/M ∞ Cω (M + 2) |u(x, 0)| dx ≤ e T |u(x, 0)|2 dx Ω Ω M 2 c(1+T )q4/3 d/M 1 − Cω (M + 2) T ∞ (M + 2) |u(x, 0)|2 dx (4.38) +e 1 − Cω (M + 2)2 T ω holds for all integers M ≥ 2. First we choose an integer M ≥ 2 so that 1 + d + 2c ≤ M + 1, (4.39) M < 2 q4/3 ∞ 4/3 1 which can be done because q∞ ≥ 1 . By (4.39), it follows that 1 + 2c q4/3 ∞ ≤ M. 1 + d ≤ M, (4.40) By (4.40) and (4.38), we infer M 2 3 M −1+c(T −1)q4/3 ∞ Cω (2M ) T |u (x, 0)| dx ≤ e |u (x, 0)|2 dx Ω c(1+T )q4/3 ∞ +e (2M ) 1 − Cω (2M )2 T 2 M 1 − Cω (2M ) T Ω ω |u (x, 0)|2 dx. (4.41) 654 K-D. Phung and G. Wang Next, we choose T > 0, so that T ≤ 1 eCω 4q4/3 ∞ 1+d +2c 4/3 1 3 < 1 eCω (2M )3 ≤ 1, which can be done because of (4.39). Then by (4.41), we get 4/3 2 −1 2 2cq∞ 2 |u(x, 0)| dx ≤ e |u(x, 0)| dx + e (2M ) |u(x, 0)|2 dx, (4.42) Ω Ω ω which gives 4/3 2 e2cq∞ 4/3 1 + d |u(x, 0)| dx ≤ + 2c |u(x, 0)|2 dx. (4.43) 4 q∞ 4/3 1 − e−1 Ω ω 2 1 Now let co = eCω 4 1 1+d +2c 4/3 1 3 , then by (4.43), we conclude that if 1 + β ≤ 41 1/4 q∞ and q∞ ≤ 1 cTo , then there exists a constant C > 0 such that 2 Cq4/3 ∞ |u(x, 0)| dx ≤ e |u(x, 0)|2 dx, (4.44) Ω ω where the solution u ∈ satisfies the following T -periodic in time linear heat equation with potential ⎧ ⎨ ∂t u − Δu + βu + qu = 0 in Ω × (0, T ), u = 0 on ∂Ω × (0, T ), (4.45) ⎩ u(·, 0) = u(·, T ) in Ω. C([0, T ]; L2 (Ω)) The proof of Theorem 3 is now completed. 5. The autonomous case Let us denote by i , with 0 < 1 < 2 ≤ 3 ≤ · · · , and by ei for i ≥ 1, the eigenvalues and eigenfunctions of −Δ in H01 (Ω). Recall here that (ei )i≥1 forms an orthonormal basis of the Hilbert space L2 (Ω). Let a = a(t) ∈ L∞ (R) be an even, T -periodic potential. From a Galerkin − st a(τ )dt Δ(t−s) method, G(t, s) can be explicitly expressed by G(t, s) = e e and one can check easily that the eigencouple (zjo , λj ) of the compact selfadjoint operator G(T, 0) satisfies λj = e−j T − T 0 a(τ )dτ zjo = ej . Furthermore, we obtain the following asymptotic controllability result. Quantitative uniqueness for time-periodic heat equation 655 Theorem 5-1. Suppose that a = a(t) ∈ L∞ (R) is a space-independent potential satisfying (i) a(t + T ) = a(t) = a(−t) in R, T (ii) 1 ≤ − T1 0 a(t)dt < 2 ; then for all initial data y o ∈ L2 (Ω) ,the control function f ∈ L1 (0, T ; L2 (Ω)) given by 1 −1 t−TT−t a(τ )dτ Ω y o (x)e1 (x)dx e1 (x) f (x, t) = − e 2 T ω |e1 (x)| dx implies that the solution y = y(x, t) ∈ C([0, +∞); L2 (Ω)) of the following heat equation with potential a = a(t), ⎧ ⎨ ∂t y − Δy + ay = f · 1|ω×(0,T ) in Ω × (0, +∞), y = 0 on ∂Ω × (0, +∞), ⎩ y(·, 0) = y o in Ω, satisfies for all t ≥ T , 1 T C aα/2 +a∞ T ∞ a(τ )dτ t y o L2 (Ω) y(t)L2 (Ω) ≤ e exp − 2 + T 0 and 0 T Caα/2 ∞ f (s)L2 (ω) ds ≤ e a∞ −1 T e y o L2 (Ω) , where C > 0 is a constant which only depends on the geometry and α ≥ 0. More precisely, α = 23 for general non-empty subdomains ω ⊂ Ω and α = 0 under the geometrical control condition of the work of Bardos-LebeauRauch (i.e., Ω ⊂ Rd , d ≥ 1, is of class C ∞ , there is no infinite order of contact between the boundary ∂Ω and the bicharacteristics of ∂t2 − Δ, and all generalized bicharacteristic ray of ∂t2 − Δ meets ω × (0, Tc ) for some 0 < Tc < +∞). Note that no hypotheses on T > 0 are required with a space- independent potential which satisfies a∞ − 1 ≥ 0 thanks to (ii). We omit details of the proof here. For general non-empty subdomains ω ⊂ Ω, we apply Theorem A (see Appendix) to get a quantification of the unique continuation property for the eigenfunction of −Δ in H01 (Ω) and deduce α = 23 . When the geometrical control condition of the work of Bardos-Lebeau-Rauch [2] is satisfied, then we apply the observability estimate for the wave equation for a fixed frequency and deduce α = 0. 656 K-D. Phung and G. Wang If the even, T -periodic bounded potential a = a(t) depends only on the time t, then G(T, 0) is a positive operator and the first eigenvalue is of multiplicity one (see the Krein-Rutman theorem in e.g. [15]). We do not know if such a result is still true for a potential a = a(x, t) depending on space and time. Observe that here no positivity hypotheses on the potential or on the initial data are imposed as in [15] or as in [9]. 6. Appendix: Global Carleman inequality for the operator (Δ − β) Carleman estimates are widely used in applied problems (see [16] for inverse problems or e.g. [13], [12], [18] for controllability problems). In what follows, we present the proof of the global Carleman inequality for the operator (Δ − β) that we have used (see Proposition 4-2 or Theorem A below). In our inequality in Theorem A, the presence of the first term in the left-hand side plays a key role. Theorem A. Let Ω be a bounded connected domain in Rd , d ≥ 1, with a boundary ∂Ω of class C 2 , and ωo be a non-empty open subset of Ω. Then there exist a smooth function ϕ = ϕ(x) ≥ 1 and a constant C > 0, such that 4/3 2/3 + for all β ∈ R, for all q ∈ L∞ (Ω), for all θ > C 1 + |β| q L∞ (Ω) , for all w ∈ H 2 (Ω) ∩ H01 (Ω), we have " "2 " " "2θ∇ϕ · ∇(eθϕ w) − qeθϕ w" 2 L (Ω) 1 3 θ + e2θϕ(x) |w(x)|2 dx + θ e2θϕ(x) |∇w(x)|2 dx C Ω Ω "2 " " " θϕ " ≤ "e (Δ − β)w L2 (Ω) 3 2θϕ(x) 2 +C θ e |w(x)| dx + θ e2θϕ(x) |∇w(x)|2 dx . ωo ωo 2 1/2 6.1. An equality with weight. We denote . = the usual (·) dx 2 norm in L (Ω) associated to the scalar product (·, ·) = (·, ·)dx. From now on, we shall omit all xs in the functions of x. Let θ > 0, ϕ = ϕ(x) ∈ C 2 (Rd ) be arbitrary but given. We shall prove first that the function v(x) = eθϕ(x) w(x) where w ∈ H 2 (Ω) ∩ H01 (Ω) satisfies Quantitative uniqueness for time-periodic heat equation the following ⎧ " "2 " " 2 ⎪ 2 (∇ϕ)2 v − βv ⎪ Δv − θΔϕv + θ − q v " " + 2θ∇ϕ∇v + qv ⎪ ⎪ ⎪ ⎪ ⎪ +2(boundary terms) ⎪ ⎪ 2 ⎪ ⎪ 2 3 ∇ϕ∇ (∇ϕ)2 v 2 ⎪ ⎪ i ϕ(∂i v) + 2θ ⎨ +4θ i ∂ +4θ ij ϕ∂i v∂j v i j=i ∂" " ⎪ 2 ⎪ " " ⎪ " + 2θ2 div(Δϕ∇ϕ)v 2 ⎪ = "eθϕ (Δ − β)w ⎪ ⎪ ⎪ ⎪ 2 (∇ϕ)2 v − βv ⎪ − qv qv ⎪ Δv − θΔϕv + θ −4θ ∇ϕ q v∇v − 2 ⎪ ⎪ ⎪ ⎩ +2θβ Δϕv 2 + 2θ Δϕ(∇v)2 − 2θ3 Δϕ(∇ϕ)2 v 2 , ⎧ ⎪ 2θβ Δϕv 2+ 2θ Δϕ(∇v)2 − 2θ3 Δϕ(∇ϕ)2 v2 ⎨ − qv = −2θ Δϕv Δv − θΔϕv + θ2 (∇ϕ)2 v − βv ⎪ 2 2 ⎩ 2 2 2 2 q v + θ Δ ϕv −2θ (Δϕ) v − 2θ Δϕ and 657 (A1) (A2) boundary terms = −θ (∂n v)2 ∂n ϕ. (A3) ∂Ω Proof of (A1). We shall start with computation of all derivatives of v = as the sum of P1 v and P2 v where eθϕ w and then write the term eθϕ (Δ − β)w P1 is a differential operator of order 1 and P2 is a differential operator of order 2 given below; after that we calculate Ω (P2 v + P1 v)2 dx where the term Ω (P2 v, P1 v)dx plays a key role. One can check easily that Δv = Δeθϕ w + 2∇eθϕ ∇w + eθϕ Δw = θΔϕv − θ2 (∇ϕ)2 v + 2θ∇ϕ∇v + eθϕ Δw and P2 v + P1 v = eθϕ (Δ − β)w, (A4) (A5) where P1 v = −2θ∇ϕ∇v + qv (6.1) − qv. P2 v = Δv − θΔϕv + θ (∇ϕ) v − βv 2 2 Then we have " θϕ " " " "2 = "Δv − θΔϕv + θ2 (∇ϕ)2 v − βv − qv "2 "e (Δ − β)w + −2θ∇ϕ∇v + qv2 + 2(P2 v, P1 v). (A6) (A7) 658 K-D. Phung and G. Wang However, a direct calculation leads us to − qv, −2θ∇ϕ∇v + qv (P2 v, P1 v) = Δv − θΔϕv + θ2 (∇ϕ)2 v − βv 2 3 Δϕ∇ϕv∇v − 2θ ∇ϕ(∇ϕ)2 v∇v (A8) = −2θ ∇ϕ∇vΔv + 2θ + 2θβ ∇ϕv∇v + 2θ ∇ϕ q v∇v + (P2 v, qv) 2 2 2 = −2θ ∂i ϕ∂i v∂i v − 2θ ∂i ϕ∂i v ∂j v + θ Δϕ∇ϕ∇(v 2 ) i i j=i 2 −θ q v∇v + (P2 v, qv) ∇ϕ(∇ϕ) ∇(v ) + θβ ∇ϕ∇(v ) + 2θ ∇ϕ = −θ ∂i ϕ∂i (∂i v)2 − 2θ ∂j (∂i ϕ∂i v∂j v) 3 2 2 i + 2θ i i ∂ij ϕ∂i v∂j v + θ j=i j=i i j=i div(Δϕ∇ϕ)v 2 − θ3 div (∇ϕ(∇ϕ)2 )v 2 3 2 2 2 q v∇v + (P2 v, qv). div ∇ϕ(∇ϕ) v − θβ Δϕv + 2θ ∇ϕ +θ + θ2 div (Δϕ∇ϕ)v 2 ∂i ϕ∂i (∂j v)2 − θ2 From this we get by integration by parts − qv, −2θ∇ϕ∇v + qv = (boundary terms) Δv − θΔϕv + θ2 (∇ϕ)2 v − βv 2 2 ∂i ϕ(∂i v) + 2θ ∂ij ϕ∂i v∂j v − θ ∂i2 ϕ(∂j v)2 +θ − θ2 + 2θ i div(Δϕ∇ϕ)v 2 + θ3 i j=i div ∇ϕ(∇ϕ)2 v 2 − θβ i j=i Δϕv 2 ∇ϕ q v∇v + (P2 v, qv). Then by (A7) and (A9), we infer " "2 " "2 " " θϕ " − qv " "e (Δ − β)w " − "Δv − θΔϕv + θ2 (∇ϕ)2 v − βv " + −2θ∇ϕ∇v + qv2 − qv, −2θ∇ϕ∇v + qv = 2 Δv − θΔϕv + θ2 (∇ϕ)2 v − βv (A9) Quantitative uniqueness for time-periodic heat equation = 2(boundary terms) + 2θ + 4θ i + 2θ 3 ∂i2 ϕ(∂i v)2 (A10) i ∂ij ϕ∂i v∂j v − 2θ i j=i div ∇ϕ(∇ϕ)2 v 2 − 2θβ 659 ∂i2 ϕ(∂j v)2 j=i − 2θ 2 div(Δϕ∇ϕ)v 2 2 Δϕv + 4θ ∇ϕ q v∇v + 2(P2 v, qv) or equivalently P2 v2 + 2θ∇ϕ∇v − qv2 + 2(boundary terms) ∂i2 ϕ(∂i v)2 + 2θ3 div ∇ϕ(∇ϕ)2 v 2 + 4θ ∂ij ϕ∂i v∂j v + 2θ i i j=i " "2 " θϕ " 2 2 = "e (Δ − β)w" + 2θ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v − 4θ ∇ϕ + 2θ ∂i2 ϕ(∂j v)2 + 2θβ Δϕv 2 . (A11) i By adding 2θ j=i 2 2 i ∂i ϕ(∂i v) on both sides of (A11) and noting that div ∇ϕ(∇ϕ)2 = ∇ϕ∇ (∇ϕ)2 + Δϕ(∇ϕ)2 , we get P2 v2 + 2θ∇ϕ∇v − qv2 + 2(boundary terms) 2 2 3 2 2 ∂i ϕ(∂i v) + 2θ ∂ij ϕ∂i v∂j v ∇ϕ∇ (∇ϕ) v + 4θ + 4θ i i j=i " "2 " " = "eθϕ (Δ − β)w q v∇v − 2(P2 v, qv) " + 2θ2 div(Δϕ∇ϕ)v 2 − 4θ ∇ϕ ∂i2 ϕ(∂j v)2 + 2θβ Δϕv 2 + 2θ i + 2θ j=i ∂i2 ϕ(∂i v)2 − 2θ 3 Δϕ(∇ϕ)2 v 2 i " "2 " θϕ " 2 2 = "e (Δ − β)w" + 2θ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v − 4θ ∇ϕ + 2θβ Δϕv 2 + 2θ Δϕ(∇v)2 − 2θ3 Δϕ(∇ϕ)2 v 2 , (A12) as desired. 660 K-D. Phung and G. Wang Proof of (A2). By integration by parts and the fact that v ∈ H 2 (Ω) ∩ H01 (Ω), it follows that 2θ Δϕ∇v∇v = −2θ ΔϕvΔv − 2θ v∇Δϕ∇v 2 = −2θβ Δϕv − 2θ Δϕv(Δ − β)v − 2θ v∇Δϕ∇v 1 2 = −2θβ Δϕv − 2θ ∇Δϕ ∇(v 2 ) 2 ! − 2θ Δϕv P2 v + θΔϕv − θ2 (∇ϕ)2 v + qv (A13) or equivalently 2θβ Δϕv 2 + 2θ Δϕ(∇v)2 − 2θ3 Δϕ(∇ϕ)2 v 2 2 2 2 2 = −2θ ΔϕvP2 v − 2θ q v + θ Δ2 ϕv 2 , (Δϕ) v − 2θ Δϕ (A14) as desired. Proof of (A3). By (A8) and (A9) we can check that boundary terms = −θ ∂i ∂i ϕ(∂i v)2 − 2θ i ∂Ω j=i i j=i ∂Ω i i 2 ∂i ∂i ϕ(∂j v)2 − θ3 div (∇ϕ(∇ϕ)2 )v 2 2 ∂i ϕ(∂i v) ni − 2θ ∂i ϕ∂i v∂j vnj div (Δϕ∇ϕ)v ∂Ω +θ ∂j (∂i ϕ∂i v∂j v) + θ + θ2 = −θ i 2 ∂i ϕ(∂j v) ni + θ i j=i (Δϕ∇ϕ)v · n − θ 2 2 ∇ϕ(∇ϕ)2 v 2 · n. 3 ∂Ω j=i (A15) ∂Ω Since v ∈ H 2 (Ω) ∩ H01 (Ω), we deduce from (A15) that boundary terms = −θ ∂i ϕ(∂i v)2 ni − 2θ ∂Ω ∂Ω i j=i i ∂i ϕ∂i v∂j vnj + θ ∂Ω i j=i ∂i ϕ(∂j v)2 ni Quantitative uniqueness for time-periodic heat equation = −2θ ∂Ω ∂Ω i ∂Ω = −2θ ∂Ω = −2θ i ∂Ω j=i ∂i ϕ∂i v∂j vnj + θ j ∇ϕ∇v∂n v + θ ∂Ω ∂i ϕ(∂i v)2 ni i ∂Ω ∂i ϕ∂i v∂j vnj j=i ∂i ϕ(∂j v)2 ni + θ i i +θ ∂i ϕ(∂i v) ni − 2θ 2 661 i ∂i ϕ(∂j v)2 ni j (∇v)2 ∂n ϕ. (A16) ∂Ω Since v|∂Ω = 0, ∇v = (∇v · n)n and then we have 2 2 (∂n v) ∂n ϕ + θ (∇v) ∂n ϕ = −θ boundary terms = −2θ ∂Ω ∂Ω ∂Ω (∂n v)2 ∂n ϕ. (A17) This completes the proof of (A3). 6.2. Choice of the weight function. We shall prove that with a particular choice of ϕ = ϕ(x) ≥ 1 there exists a constant C > 0 such that for all β ∈ R, 4/3 2/3 + q L∞ (Ω) , the estimate for all q ∈ L∞ (Ω), and θ > C 1 + |β| "2 " 2 1 3 " θϕ θϕ " θϕ 2 (e w) + θ θ ∇(eθϕ w) "2θ∇ϕ∇(e w) − qe w" + C Ω Ω " "2 3 2 " θϕ " " +C θ ∇(eθϕ w) ≤ "e (Δ − β)w (eθϕ w)2 + θ (A18) ωo holds for all w ∈ H 2 (Ω) ∩ ωo H01 (Ω). Proof of (A18). We study the particular case that ϕ(x) = eρψ(x) , where ρ > 0 and ψ is a smooth non-negative function. One can check that Δϕ = ρ2 (∇ψ)2 ϕ + ρΔψϕ (A19) and 2ϕ 2 ψϕ = ρ(∂i ϕ)2 ∂j ψ + ∂i ϕρ∂ij ∂i ϕ∂ij 2 2 2 2 2 ψϕ. ∂i ϕ∂j ϕ∂ij ϕ = ρ (∂j ψ) (∂i ϕ) ϕ + ρ∂i ϕ∂j ϕ∂ij Next we compute ∇ϕ∇ (∇ϕ)2 = i ∂i ϕ∂i (∇ϕ)2 . Since 2 ∂j ϕ∂ij ϕ ∂i ϕ∂i (∇ϕ)2 = 2∂i ϕ∇ϕ∇∂i ϕ = 2∂i2 ϕ(∂i ϕ)2 + 2∂i ϕ j=i (A20) ! ! 2 = 2 ρ2 (∂i ψ)2 ϕ + ρ∂i2 ψϕ (∂i ϕ)2 + 2∂i ϕ ∂j ϕ ρ2 ∂i ψϕ∂j ψ + ρ∂ij ψϕ j=i 662 K-D. Phung and G. Wang ! = 2 ρ2 (∂i ψ)2 ϕ + ρ∂i2 ψϕ (∂i ϕ)2 + 2∂i ϕ (ρ∂j ψϕ)(ρ∂i ψϕ)ρ∂j ψ + 2∂i ϕ j=i 2 ∂j ϕρ∂ij ψϕ ! = 2 ρ2 (∂i ψ)2 ϕ + ρ∂i2 ψϕ (∂i ϕ)2 j=i 2 + 2ρ ∂i ϕ = 2ρ2 (∂j ψ)2 ϕ∂i ϕ + 2∂i ϕ j=i 2 ∂j ϕρ∂ij ψϕ j=i 2 (∂j ψ)2 ϕ(∂i ϕ)2 + 2ρ ∂i2 ψϕ(∂i ϕ)2 + ∂i ϕ ∂j ϕ∂ij ψϕ , j (A21) j=i it follows that ∇ϕ∇ (∇ϕ)2 = 2ρ2 (∇ψ)2 ϕ(∇ϕ)2 2 + 2ρ ∂j ϕ∂ij ψ ϕ. ∂i2 ψ (∂i ϕ)2 + ∂i ϕ i (A22) j=i On the other hand, by (A1) and (A2), we infer P2 v2 + 2θ∇ϕ∇v + qv2 + 2(boundary terms) 2 2 3 2 2 + 4θ ∂i ϕ(∂i v) + 2θ ∂ij ϕ∂i v∂j v ∇ϕ∇ (∇ϕ) v + 4θ i i j=i " "2 " 2 2 " = "eθϕ (Δ − β)w + 2θ − 4θ ∇ϕ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v " 2 2 2 2 − 2θ ΔϕvP2 v − 2θ (Δϕ) v − 2θ Δϕ q v + θ Δ2 ϕv 2 (A23) which together with (A22) gives P2 v2 + 2θ∇ϕ∇v − qv2 + 2 (boundary terms) 2 ϕ ∂i ψ∂j ψ∂i v∂j v (∂i ψ)2 (∂i v)2 + + 4θρ i + 4θρ ϕ i + 4θ3 ρ i ∂i2 ψ(∂i v)2 + j=i ∂i2 ψ(∂i ϕ)2 + ∂i ϕ j=i 2 ∂ij ψ∂i v∂j v j=i 3 2 + 4θ ρ (∇ψ)2 (∇ϕ)2 ϕv 2 2 ∂j ϕ∂ij ψ ϕv 2 " "2 " " = "eθϕ (Δ − β)w q v∇v − 2(P2 v, qv) " + 2θ2 div(Δϕ∇ϕ)v 2 − 4θ ∇ϕ Quantitative uniqueness for time-periodic heat equation − 2θ ΔϕvP2 v − 2θ 2 (Δϕ) v − 2θ 2 2 663 2 Δϕ qv + θ Δ2 ϕv 2 (A24) or equivalently P2 v2 + 2θ∇ϕ∇v − qv2 + 2(boundary terms) 2 2 3 2 + 4θρ ∂i ψ∂i v + 4θ ρ ϕ (∇ψ)2 (∇ϕ)2 ϕv 2 (6.2) i " "2 " θϕ " 2 2 = "e (Δ − β)w" + 2θ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v − 4θ ∇ϕ 2 2 2 2 − 2θ ΔϕvP2 v − 2θ (Δϕ v − 2θ Δϕ q v + θ Δ2 ϕv 2 2 − 4θρ ϕ ∂i2 ψ(∂i v)2 + ∂ij ψ∂i v∂j v i − 4θ3 ρ i j=i ∂i2 ψ(∂i ϕ)2 + ∂i ϕ 2 ∂j ϕ∂ij ψ ϕv 2 . (A25) j=i Next we compute the term 2θρ2 (∇ψ)2 ϕ(∇v)2 . To this end, we observe by (A2) that 2 ! 2 2 2θ ρ (∇ψ) ϕ + ρΔψϕ (∇v) = 2θ Δϕ(∇v)2 2 3 Δϕ(∇ϕ)2 v 2 = −2θβ Δϕv + 2θ − 2θ ΔϕvP2 v − 2θ2 (Δϕ)2 v 2 − 2θ Δϕ q v 2 + θ Δ2 ϕv 2 2 ! ρ (∇ψ)2 ϕ + ρΔψϕ (∇ϕ)2 v 2 = −2θβ Δϕv 2 + 2θ3 − 2θ ΔϕvP2 v − 2θ2 (Δϕ)2 v 2 − 2θ Δϕ q v 2 + θ Δ2 ϕv 2 (A26) which implies 2 2 2 2 3 2 (∇ψ) ϕ(∇v) = −2θρ Δψϕ(∇v) + 2θ ρ (∇ψ)2 (∇ϕ)2 ϕv 2 2θρ 3 2 2 2 + 2θ ρ Δψ(∇ϕ) ϕv − 2θ ΔϕvP2 v − 2θ (Δϕ)2 v 2 2 + θ Δ2 ϕv 2 . − 2θ Δϕ( q + β)v (A27) 664 K-D. Phung and G. Wang Finally, it follows from (A25) and (A27) that P2 v2 + 2θ∇ϕ∇v − qv2 + 2(boundary terms) + 4θρ2 ∂i ψ∂i v 2 ϕ i + 4θ3 ρ2 (∇ψ)2 (∇ϕ)2 ϕv 2 + 2θρ2 (∇ψ)2 ϕ(∇v)2 " "2 " θϕ " 2 2 = "e (Δ − β)w" + 2θ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v − 4θ ∇ϕ β 2 2 2 2 v − θ Δ2 ϕv 2 (Δϕ) v + 2θ Δϕ q + − 2 2θ ΔϕvP2 v + 2θ 2 2 ∂ij ψϕ∂i v∂j v (A28) − 4θρ ∂i2 ψϕ(∂i v)2 + i − 4θ3 ρ ∂i2 ψ(∂i ϕ)2 + ∂i ϕ i − 2θρ j=i 2 ∂j ϕ∂ij ψ ϕv 2 j=i Δψϕ(∇v)2 + 2θ3 ρ2 (∇ψ)2 (∇ϕ)2 ϕv 2 + 2θ3 ρ or equivalently P2 v2 + 2θ∇ϕ∇v − qv2 + 2(boundary terms) + 4θρ2 2 2 2 ∂i ψ∂i v 2 ϕ i 3 2 Δψ(∇ϕ)2 ϕv 2 2 (∇ψ) (∇ϕ) ϕv + 2θρ (∇ψ)2 ϕ(∇v)2 + 2θ ρ " "2 " θϕ " 2 2 = "e (Δ − β)w" + 2θ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v − 4θ ∇ϕ β 2 2 2 2 (Δϕ) v + 2θ Δϕ q + − 2 2θ ΔϕvP2 v + 2θ v − θ Δ2 ϕv 2 2 2 ∂i2 ψϕ(∂i v)2 + ∂ij ψϕ∂i v∂j v − 4θρ i − 4θ3 ρ − 2θρ j=i ∂i2 ψ(∂i ϕ)2 + ∂i ϕ i Δψϕ(∇v)2 + 2θ3 η 2 ∂j ϕ∂ij ψ ϕv 2 j=i Δψϕ(∇ϕ)2 v 2 . (A29) Now, we choose ψ such that ψ ∈ C 2 (Ω), ψ(x) > 0 in Ω, ψ(x) = 0 on ∂Ω and |∇ψ(x)| > 0 ∀x ∈ Ω \ωo , (A30) Quantitative uniqueness for time-periodic heat equation 665 where ωo ⊂ ω is an arbitrary fixed subdomain of Ω such that ωo ⊂ ω. The existence of such a function ψ was proved in [13]. Then the boundary terms (A3) are non-negative. More precisely, for all ρ > 0, θ > 0, boundary terms = −θ (∂n v)2 (ρ∂n ψ)ϕ ≥ 0. (A31) ∂Ω By (A30), (A31) and (A29), there exists a constant C > 0, such that for all ρ > 0 there is a constant Cρ > 0 such that for all θ > 0, we have 1 3 2 2 2 2 2 2 P2 v + 2θ∇ϕ∇v − qv + (∇ϕ) ϕv + θρ ϕ(∇v)2 θ ρ C Ω\ωo Ω\ωo ≤ P2 v2 + 2θ∇ϕ∇v − qv2 2 2 + 2(boundary terms) + 4θρ ∂i ψ∂i v ϕ i + 2θ3 ρ2 (∇ψ)2 (∇ϕ)2 ϕv 2 + 2θρ2 (∇ψ)2 ϕ(∇v)2 " "2 " 2 2 " = "eθϕ (Δ − β)w + 2θ − 4θ ∇ϕ q v∇v − 2(P2 v, qv) div(Δϕ∇ϕ)v " β q + )v 2 − Δ2 ϕv 2 − 2θ 2 ΔϕvP2 v + 2θ (Δϕ)2 v 2 + 2 Δϕ( 2 2 ∂ij ψϕ∂i v∂j v ∂i2 ψϕ(∂i v)2 + − 4θρ i − 4θ3 ρ − 2θρ j=i ∂i2 ψ(∂i ϕ)2 + ∂i ϕ i Δψϕ(∇v)2 + 2θ3 ρ 2 ∂j ϕ∂ij ψ ϕv 2 j=i Δψϕ(∇ϕ)2 v 2 . (A32) Using the Cauchy-Schwarz inequality in (A32), we get 1 3 2 P2 v2 + 2θ∇ϕ∇v − qv2 + (∇ϕ)2 ϕv 2 + θρ2 ϕ(∇v)2 θ ρ C Ω\ωo Ω\ωo "2 " " " q 2L∞ Cρ v 2 + (∇v)2 ≤ "eθϕ (Δ − β)w " + θ2 Cρ v 2 + θ2 1 2 2 2 2 + 2 q L∞ v + P2 v + θ q L∞ + |β| Cρ v + θCρ v 2 (A33) 2 + Cθρ ϕ(∇v)2 + Cθ3 ρ (∇ϕ)2 ϕv 2 + Cθρ ϕ(∇v)2 + Cθ3 ρ ϕ(∇ϕ)2 v 2 . 666 K-D. Phung and G. Wang Finally, we obtain that, (recall that ϕ ≥ 1) for all ρ > 1, for all θ > 1, 1 1 (∇ϕ)2 ϕv 2 + θ ϕ(∇v)2 P2 v2 + 2θ∇ϕ∇v − qv2 + ρ2 θ3 2 C Ω\ωo Ω\ωo "2 " " + " q L∞ + q 2L∞ Cρ v 2 ≤ "eθϕ (Δ − β)w " + θ2 1 + |β| + Cρ θ3 (∇ϕ)2 ϕv 2 + θ ϕ(∇v)2 "2 " " 2 2 " 1 + | β| + q C + 2θ v2 ≤ "eθϕ (Δ − β)w " ρ L∞ 3 2 2 + Cρ θ (∇ϕ) ϕv + θ ϕ(∇v)2 ωo ωo 3 2 2 (A34) (∇ϕ) ϕv + θ ϕ(∇v)2 , + Cρ θ Ω\ωo Ω\ωo where C > 0 is a constant independent of ρ and θ. Now we may choose and fix ρ > 1 large enough in (A34) to get 1 3 2 2 2 2θ∇ϕ∇v − qv + (∇ϕ) ϕv + θ ϕ(∇v)2 θ C Ω\ωo Ω\ωo "2 " " " θϕ 2 2 2 v + v2 ≤ "e (Δ − β)w" + θ 1 + |β| + q L∞ C Ω\ωo ωo (A35) (∇ϕ)2 ϕv 2 + θ ϕ(∇v)2 , + C θ3 ωo ωo where C > 0 is a constant independent of θ. Then by (A35), using properties + of ψ, we may choose θ large enough so that θ3/2 > C1 1 + |β| q 2L∞ (Ω) to get 1 3 2 2 θ v +θ (∇v)2 2θ∇ϕ∇v − qv + C2 Ω\ωo Ω\ωo "2 " " " θϕ 3 2 2 (A36) (∇ϕ) ϕv + θ ϕ(∇v)2 , ≤ "e (Δ − β)w" + C2 θ ωo ωo where C1 and C2 are two constants independent of θ. Finally, we have proved that there exists a constant C > 0 such that for 4/3 2/3 + all β ∈ R, q ∈ L∞ (Ω) and θ > C 1 + |β| q L∞ (Ω) , the following estimate holds 1 3 2 2 v + θ (∇v)2 θ 2θ∇ϕ∇v − qv + C Ω Ω Quantitative uniqueness for time-periodic heat equation " "2 " θϕ " ≤ "e (Δ − β)w" + C θ3 2 2 v +θ ωo (∇v) 667 . (A37) ωo 4/3 2/3 + q L∞ (Ω) , Thus, coming back to the function w, for all θ > C 1 + |β| " "2 2 1 3 " " (eθϕ w)2 + θ θ ∇(eθϕ w) "2θ∇ϕ∇(eθϕ w) − qeθϕ w" + C Ω Ω " "2 2 " θϕ " 3 θϕ 2 θϕ " +C θ ≤ "e (Δ − β)w (e w) + θ ∇(e w) , (A38) ωo ωo which completes the proof of (A18). Finally, we deduce from (A38), "2 " 1 3 " θϕ θϕ " θϕ 2 (e w) + θ (eθϕ ∇w)2 θ "2θ∇ϕ∇(e w) − qe w" + C Ω Ω " "2 " " (A39) ≤ "eθϕ (Δ − β)w (eθϕ w)2 + θ (eθϕ ∇w)2 , " + C θ3 ωo ωo which implies Theorem A. This closes the Appendix on the global Carleman inequality for the operator Δ − β where β ∈ R. Acknowledgment. This work was supported by the grant of Key Lab of Hubei Province, China. 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