Electronic Journal of Differential Equations, Vol. 2015 (2015), No. 261, pp. 1–14. ISSN: 1072-6691. URL: http://ejde.math.txstate.edu or http://ejde.math.unt.edu ftp ejde.math.txstate.edu WELL-POSEDNESS AND BLOWUP CRITERION OF GENERALIZED POROUS MEDIUM EQUATION IN BESOV SPACES XUHUAN ZHOU, WEILIANG XIAO, TAOTAO ZHENG Abstract. We study the generalized porous medium equation of the form ut + νΛβ u = ∇ · (u∇P u) where P is an abstract operator. We obtain the local well-posedness in Besov spaces for large initial data, and show the solution becomes global if the initial data is small. Also, we prove a blowup criterion for the solution. 1. Introduction In this article, we study the equation in Rn of the form ut + νΛβ u = ∇ · (u∇P u); u(0, x) = u0 . (1.1) Here u = u(t, x) ia a real-valued function, represents a density or concentration. The dissipative coefficient ν > 0 corresponds to the viscous case, while ν = 0 corresponds to the inviscid case. The fractional operator Λβ is defined by Fourier transform as (Λβ u)∧ = |ξ|β û, and P is an abstract operator. The general form of equation (1.1) has good suitability in many cases. The simplest case ν = 0, P u = u comes from a model in groundwater infiltration, that is, ut = ∆u2 (see [2, 33]). We call (1.1) generalized porous medium equation (GPME) inspired by Caffarelli and Vázquez [12], in which they introduced the fractional porous medium flow (FPME) when ν = 0 and P u = Λ−2s u, 0 < s < 1. When P u = Λ−2 u, it is the mean field equation, which is first studied by Lin and Zhang [28]. Some results on the well-posedness and regularity on those equations can be seen [7, 8, 13, 14, 30, 31, 34, 39] and the references therein. Another similar model occurs in the aggregation equation, which is an important equation arising in physics, biology, chemistry, population dynamics, etc.([15, 10, 21, 32]). In this model, the operator P is a convolution operator with kernel K; that is, P u = K ∗ u. The typical kernels are |x|γ , see [9, 22, 27], and −e−|x| , see [3, 6, 25, 26]. For more results on this equation, we refer to [4, 5, 11, 23, 24] and 2010 Mathematics Subject Classification. 35K15, 35K55, 35Q35, 76S05. Key words and phrases. Generalized porous medium equation; well-posedness; blowup criterion; Besov spaces. c 2015 Texas State University. Submitted June 25, 2015. Published October 7, 2015. 1 2 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 the references therein. Besides, if we rewrite the equation (1.1) with same initial data as ut + νΛβ u + v · ∇u = −u(∇ · v); (1.2) v = −∇P u, then it is a kind of special transport type equation. Furthermore, if we assume that v is divergence-free vector function (∇ · v = 0), the form (1.2) can contain the 2 − D quasi-geostrophic (Q-G) equation [17, 18, 19, 35]. In this article we study the well-posedness of equation (1.1) in homogenerous Besov spaces under a general condition s+σ . k∇P ukḂ s ≤ CkukḂp,q (1.3) p,q It is widespread adopted in the case of FPME, Q-G equation, or aggregation equation with its usual kernel |x|γ and it plays somewhat key role in the well-posedness and regularity of those equations in Besov spaces or Sobolev spaces. Based on the ideas used in [29, 36, 37, 38], we prove the following theorem. Theorem 1.1. Assume P satisfies (1.3), β ∈ (0, 2], p ≥ 1 and σ + 1 < β < n +σ−β p σ +n min(2/p, 1). Then for any initial data u0 ∈ Ḃp,1 problem (1.1) admits a unique solution n +σ−β p u ∈ C([0, T ); Ḃp,1 n +σ−β+1 p ∩ Ḃp,1 n +σ−β+1 p ∩ Ḃp,1 n +σ p ) ∩ L1 ([0, T ); Ḃp,1 n , the Cauchy +σ+1 p ∩ Ḃp,1 ). Moreover, if T ∗ denotes the maximal time of existence of u, (i) there exists a constant C0 > 0 such that if ku0 k ∞; R T∗ (ii) if T ∗ < ∞, then 0 ku(t)kḂ n/p+σ+1 dt = ∞. n +σ−β+1 p Ḃp,1 < C0 , then T ∗ = p,1 Remark 1.2. In the case of aggregation equation, Wu and Zhang [36] proved a similar result under the condition ∇K ∈ W 1,1 , β ∈ (0, 1). Corresponding to their case we prove same result for σ = 0, that is ∇K ∈ L1 , β ∈ (1, 2), and also a similar result for σ = −1; that is, ∇K ∈ Ẇ 1,1 , β ∈ (0, 1). Throughout this article, C denotes a positive constant that may differ line by line, the notation A . B means A ≤ CB, and A ∼ B denotes A . B and B . A. 2. Preliminaries Let us recall some basic knowledge on Littlewood-Paley theory and Besov spaces. Let S (Rn ) be the Schwartz class and S 0 be its dual space. Given f ∈ S (Rn ), we use its Fourier transform Ff = fˆ as Z −n/2 ˆ f = (2π) e−ix·ξ f (x)dx. Rn Let ϕ ∈ and Cc∞ (Rn ) be a radial real-valued smooth function such that 0 ≤ ϕ(ξ) ≤ 1 supp ϕ ⊂ {ξ ∈ Rn : 3 8 ≤ |ξ| ≤ }, 4 3 X j∈Z ϕ(2−j ξ) = 1 for any ξ 6= 0. EJDE-2015/261 POROUS MEDIUM EQUATION IN BESOV SPACES 3 We denote ϕj (ξ) = ϕ(2−j ξ) and P the set of all polynomials. Setting h = F −1 ϕ, we define the frequency localization operators as follows: Z X ∆j u = ϕ(2−j D)u = 2jn h(2j y)u(x − y)dy, Sj f = ∆k u. Rn k≤j−1 Definition 2.1. For s ∈ R, p, q ∈ [1, ∞], we define the homogeneous Besov space s Ḃp,q as X 1/q s Ḃp,q = {f ∈ S 0 /P : kf kḂ s = 2jsq k∆j f kqLp < ∞}. p,q j∈Z Here the norm changes normally when p = ∞ or q = ∞. Definition 2.2. In this paper, we need two kinds of mixed time-space norm defined as follows: For s ∈ R, 1 ≤ p, q ≤ ∞, I = [0, T ), T ∈ (0, ∞], and X a Banach space with norm k · kX where 1/r Z kf (τ, ·)krX dτ , kf (t, x)kLr (I;X) := I X 1/q . 2jsq k∆j f kqLr (I;Lp ) kf (t, x)kLr (I;Ḃ s ) := p,q j∈Z By Minkowski’ inequality, there holds s s Lr (I; Ḃp,q ) ,→ Lr (I; Ḃp,q ), if r ≤ q, s s Lr (I; Ḃp,q ) ,→ Lr (I; Ḃp,q ), if r ≥ q. (2.1) Now we state some basic properties about the homogeneous Besov spaces. Proposition 2.3 ([1]). For s ∈ R, 1 ≤ p, q ≤ ∞, the following hold: (i) Let β ∈ R, we have the equivalence of norms: kΛβ f kḂ s ∼ kf kḂp,q s+β . p,q (ii) (iii) s−n(1/p −1/p2 ) . If p1 ≤ p2 , q1 ≤ q2 , then Ḃps1 ,q1 ,→ Ḃp2 ,q2 1 Let 1 ≤ p, q ≤ ∞, s1 , s2 < np when q > 1 (or s1 , s2 ≤ n p when q = 1), and s1 + s2 > 0, there holds kuvk s1 +s2 − n p Ḃp,q s1 kvk s2 , ≤ CkukḂp,q Ḃp,q where C > 0 be a constant depending on s1 , s2 , p, q, n. Lemma 2.4 (Bernstein’s inequalities [17]). Set B to be a ball and C to be an annulus, and let 1 ≤ p ≤ q ≤ ∞, α ∈ ({0} ∪ N)n , then the following estimates hold: (i) If supp fb ∈ 2j B, β + |α| ≥ 0, then kΛβ Dα f kLq ≤ C2j(β+|α|+n(1/p−1/q)) kf kLp . (ii) If supp fb ∈ 2j C, then C2j(β+|α|) kf kLp ≤ kΛβ Dα f kLp ≤ C 0 2j(β+|α|) kf kLp , where C ≤ C 0 are positive constants independent of j. Lemma 2.5 ([1]). Let C ba an annulus. If supp fb ⊂ 2j C, then positive constant c > 0 exists such that for any t > 0, there holds β jβ ke−tΛ f kLp ≤ Ce−ct2 kf kLp . 4 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 Lemma 2.6 ([29]). Let s ∈ R and 1 ≤ p ≤ p1 ≤ ∞. Set Rj := (Sj−1 v − v) · ∇∆j u − [∆j , v · ∇]u. There exists a constant C = C(n, s) such that X 0 2js kRj kLp ≤ C kSj 0 −1 ∇vkL∞ 2j s k∆j 0 ukLp |j−j 0 |≤4 0 X + 2j−j k∆j 0 ∇vkL∞ 2js k∆j ukLp j 0 ≥j−3 X + 2(j−j 00 )(s−1− pn ) j 0 pn 2 1 1 00 k∆j 0 ∇vkLp1 2j s k∆j 00 ukLp |j 0 −j|≤4 j 00 ≤j 0 −2 X + (j−j 0 )(s+n min( p1 , p10 )) j 0 pn 2 2 1 1 0 (2j−j k∆j 0 ∇vkLp1 j 0 ≥j−3 |j 00 −j 0 |≤1 00 + k∆j 0 ∇ · vkLp1 )2j s k∆j 00 ukLp . Now we recall a priori estimates needed in our proof. Consider the transportdiffusion equation ∂t u + v · ∇u + νΛβ u = f, u(0, x) = u0 (x). (2.2) Lemma 2.7 ([29]). Let 1 ≤ r1 ≤ r ≤ ∞, 1 ≤ p ≤ p1 ≤ ∞ and 1 ≤ q ≤ ∞. Assume s ∈ R satisfies the following conditions: n n (or s ≤ , if q = 1), s<1+ p1 p1 n n n n s > − min ( , 0 ) (or s > −1 − min ( , 0 ), if div u = 0). p1 p p1 p There exists a positive constant C = C(n, β, s, p, p1 , q) such that for any smooth solution u of (2.2) with ν ≥ 0, the following a priori estimate holds: ν 1/r kukLr Ḃ s+β/r ≤ CeCZ(T ) ku0 kḂ s + ν 1/r1 −1 kf kLr1 Ḃ s−β+β/r1 , T where Z(T ) = RT 0 p,q p,q T p,q k∇v(t)kḂ n/p1 ∩L∞ dt. p1 ,∞ 3. Local and global well-posedness In this section we prove our main theorem. We first rewrite (1.1) as ut + Λβ u + v · ∇u = u(∆P u); v = −∇P u; u(0, x) = u0 . Step 1: Approximate solutions. In this step we construct approximate equaβ tions, and prove the boundedness of the approximate solutions. Set u0 = e−tΛ u0 (x) m+1 and let u be the solution of the linear equation um+1 + Λβ um+1 + v m · ∇um+1 = um (∆P um ); t v m = −∇P um ; u m+1 (0, x) = u0 . (3.1) EJDE-2015/261 n POROUS MEDIUM EQUATION IN BESOV SPACES +σ−β p Set X = Ḃp,1 n +σ−β+1 p ∩ Ḃp,1 n +σ p and Y = Ḃp,1 n +σ+1 p ∩ Ḃp,1 5 . It is easy to show u0 ∈ L∞ (R+ ; X) ∩ L1 (R+ ; Y ). Now by induction, we deduce um belongs to the same spaces. In fact, by Lemma 2.7 kum+1 kL∞ Ḃ n/p+σ−β+1 + kum+1 kL1 Ḃ n/p+σ+1 p,1 T .e c RT 0 p,1 T k∇v m (t)k m dt n/p Ḃp,∞ ∩L∞ m ku0 kḂ n/p+σ−β+1 p,1 + ku (∆P u )kL1 Ḃ n/p+σ−β+1 p,1 T c .e RT 0 k∇v m (t)k n/p dt Ḃp,1 (3.2) ku0 kḂ n/p+σ−β+1 p,1 + kum kL∞ Ḃ n/p+σ−β+1 k∆P um kL1 Ḃ n/p p,1 T ckum k .e T n/p+σ+1 L1 Ḃp,1 T p,1 ku0 kḂ n/p+σ−β+1 p,1 + kum kL∞ Ḃ n/p+σ−β+1 kum kL1 Ḃ n/p+σ+1 . p,1 T T p,1 Similarly, we conclude that kum+1 kL∞ Ḃ n/p+σ−β + kum+1 kL1 Ḃ n/p+σ T ckum k .e p,1 T n/p+σ+1 L1 Ḃp,1 T p,1 ku0 kḂ n/p+σ−β + kum kL∞ Ḃ n/p+σ−β kum kL1 Ḃ n/p+σ+1 . p,1 m Thus for all m ∈ N , we have u T ∞ + p,1 1 (3.3) p,1 T + ∈ L (R ; X) ∩ L (R ; Y ). Step 2: Uniform estimates. We prove the key uniform estimates during this step. Set uj := ∆j u, fj := ∆j (um ∆P um ). Then we can obtain Claim 3.1. There exists T1 ≤ T , such that for all t ∈ [0, T1 ] X jβ 1/r kum+1 kLr Ḃ s+β/r . 1 − e−ctr2 2js ku0,j kLp t p,1 j∈Z + XZ j∈Z t 2js kfj kLp + kRj kLp dτ, 0 where Rj := (Sj−1 v m − v m ) · ∇um+1 − [∆j , v m · ∇]um+1 . j We postpone the proof of this claim to the appendix. Taking s = np + σ − β + 1 and ρ large enough such that σ + 1 + β/ρ ≤ β. Then by Proposition 2.3 with s1 = n/p + σ + 1 − β + β/r, s2 = n/p − β/r, there holds XZ t 2j(n/p+σ+1−β) kfj kLp dτ . kum kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ . j∈Z t 0 p,1 t p,1 Taking ρ large enough and using Lemma 2.6 with s = n/p + 1 + σ − β, p1 = p, XZ t 2j(n/p+σ+1−β) kRj kLp dτ j∈Z 0 . kum+1 kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ . t p,1 t p,1 6 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 Hence for r ≥ 1 and ρ large enough, we have kum+1 kLr Ḃ n/p+σ+1−β+β/r t p,1 X jβ 1/r . 1 − e−ctr2 2j(n/p+σ+1−β) ku0,j kLp (3.4) j∈Z + kum kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ t p,1 t p,1 + kum+1 kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ . t p,1 t p,1 0 jβ Now by (3.4) with r = ρ and the fact that 1 − e−ctρ 2 for ρ large, 1/ρ0 jβ ≤ 1 − e−ctρ2 1/ρ kum+1 kLρ Ḃ n/p+σ+1−β+β/ρ + kum+1 kLρ0 Ḃ n/p+σ+1−β/ρ t p,1 t p,1 X −ctρ2jβ 1/ρ j(n/p+σ+1−β) . 1−e 2 ku0,j kLp j∈Z + kum kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ t m+1 + ku p,1 t p,1 m kLρ Ḃ n/p+σ+1−β+β/ρ ku kLρ0 Ḃ n/p+σ+1−β/ρ . t p,1 t p,1 By Lebesgue dominated convergence theorem, for ρ < ∞, we have X jβ 1/ρ 1 − e−ctρ2 2j(n/p+σ+1−β) ku0,j kLp = 0. lim+ t7→0 j∈Z Now we set X jβ 1/ρ T = sup t > 0 : c 1 − e−ctρ2 2j(n/p+σ+1−β) ku0,j kLp ≤ η , j∈Z for some η > 0 sufficiently small. By definition of u0 , ∀t ≤ T , we have ku0 kLρ Ḃ n/p+σ+1−β+β/ρ ≤ η, t p,1 ku0 kLρ0 Ḃ n/p+σ+1−β/ρ ≤ η. t p,1 Choosing η small enough such that cη ≤ 1/2, ku1 kLρ Ḃ n/p+σ+1−β+β/ρ + ku1 kLρ0 Ḃ n/p+σ+1−β/ρ ≤ 3η. t p,1 t (3.5) p,1 If we assume that (3.5) holds for um and further take η small enough such that 3cη ≤ 1/3, we obtain kum+1 kLρ Ḃ n/p+σ+1−β+β/ρ + kum+1 kLρ0 Ḃ n/p+σ+1−β/ρ ≤ 3η. t p,1 t (3.6) p,1 Thus by induction, we prove the uniform boundedness (3.6) for some suitable η and jβ jβ 1/ρ , we have ∀t ≤ T . Let r = 1 in (3.4), since 1 − e−ct2 ≤ 1 − e−ctρ2 X jβ 1/ρ kum+1 kL1 Ḃ n/p+σ+1 . 1 − e−ctρ2 2j(n/p+σ+1−β) ku0,j kLp t p,1 j∈Z + kum kLρ Ḃ n/p+σ+1−β+β/ρ kum kLρ0 Ḃ n/p+σ+1−β/ρ t m+1 + ku p,1 t p,1 m kLρ Ḃ n/p+σ+1−β+β/ρ ku kLρ0 Ḃ n/p+σ+1−β/ρ . t p,1 t p,1 This and (3.6) imply kum+1 kL1 Ḃ n/p+σ+1 ≤ η + 18cη 2 ≤ 3η. t p,1 (3.7) EJDE-2015/261 POROUS MEDIUM EQUATION IN BESOV SPACES n/p+σ+1−β Next we prove that um are uniformly bounded in L∞ t Ḃp,1 7 . In fact, by (3.2) 1 kum+1 kL∞ Ḃ n/p+σ+1−β ≤ ce1/3 ku0 kḂ n/p+σ+1−β + e1/3 kum kL∞ Ḃ n/p+σ+1−β . t t p,1 p,1 p,1 3 By induction, we conclude kum kL∞ Ḃ n/p+σ+1−β t p,1 1 − ( 13 e1/3 )m 1/3 ce ku0 kḂ n/p+σ+1−β p,1 1 − 13 e1/3 1/3 (3ce + 1)ku0 kḂ n/p+σ+1−β . p,1 ≤ ≤ + em/3 0 ku kL∞ Ḃ n/p+σ+1−β t p,1 3m (3.8) n/p+σ+1−β Thus approximate solutions are uniformly bounded in the space L∞ T Ḃp,1 n/p+σ+1 L1T Ḃp,1 ∩ . Now we return to (3.3) and by the uniform estimate (3.7) kum+1 kL∞ Ḃ n/p+σ−β + kum+1 kL1 Ḃ n/p+σ T ckum k .e p,1 T n/p+σ+1 L1 Ḃp,1 T p,1 ku0 kḂ n/p+σ−β + kum kL∞ Ḃ n/p+σ−β kum kL1 Ḃ n/p+σ+1 p,1 T p,1 T p,1 (3.9) 1 ≤ ce1/3 ku0 kḂ n/p+σ−β + e1/3 kum kL∞ Ḃ n/p+σ−β . t p,1 p,1 3 Hence, similarly to (3.8), by induction again, kum kL∞ Ḃ n/p+σ−β ≤ (3ce1/3 + 1)ku0 kḂ n/p+σ−β . t p,1 p,1 Substituting this into (3.9) we conclude kum kL1 Ḃ n/p+σ ≤ (4ce1/3 + 1)ku0 kḂ n/p+σ−β . t p,1 p,1 1 Thus we conclude that (u )m∈N is uniformly bounded in L∞ T X ∩ LT Y . m Step 3: Strong convergence. Let (m, k) ∈ N2 , m > k and um,k = um − uk , v m,k = v m − v k . Then um,k satisfies the equation um+1,k+1 + Λβ um+1,k+1 + v k · ∇um+1,k+1 t = um,k (∆P um ) + uk (∆P um,k ) − v m,k · ∇um+1 ; v m,k = −∇P um,k ; um+1,k+1 (0, x) = 0. Set U m+1,k+1 (T ) = kum+1,k+1 kLρ Ḃ n/p+σ−β/ρ0 +kum+1,k+1 kLρ0 Ḃ n/p+σ−β/ρ . Applying T T p,1 p,1 Lemma 2.7 with s = n/p + σ − β, there holds U m+1,k+1 (T ) ck∇v k k .e n/p L1 Ḃp,1 T kum,k (∆P um )kL1 Ḃ n/p+σ−β T (3.10) p,1 + kuk (∆P um,k )kL1 Ḃ n/p+σ−β + kv m,k · ∇um+1 kL1 Ḃ n/p+σ−β . T p,1 T p,1 Now applying Proposition 2.3 with s1 = n/p − β/ρ, s2 = n/p + σ − β/ρ0 , kv m,k · ∇um+1 kL1 Ḃ n/p+σ−β . kum,k kLρ0 Ḃ n/p+σ−β/ρ kum+1 kLρ Ḃ n/p+σ+1−β/ρ0 . T p,1 T p,1 T p,1 8 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 Similarly, for ρ large enough such that σ + 1 + β/ρ ≤ β, we conclude U m+1,k+1 (T ) . e ck∇v k k n/p L1 Ḃp,1 T kum,k kLρ0 Ḃ n/p+σ−β/ρ kum+1 kLρ Ḃ n/p+σ+1−β/ρ0 T p,1 T p,1 + kuk kLρ Ḃ n/p+σ+1−β/ρ0 kum,k kLρ0 Ḃ n/p+σ−β/ρ + ku k p,1 T p,1 T m,k 0 n/p+σ−β/ρ Lρ T Ḃp,1 m ku kLρ Ḃ n/p+σ+1−β/ρ0 T p,1 ≤ cηU m,k (T ). Choosing η small enough such that cη < 1 and by induction, we conclude that {um } 0 n/p+σ−β/ρ0 n/p+σ−β/ρ is a Cauchy sequence in LρT Ḃp,1 ∩ LρT Ḃp,1 . So um hence converges strongly to some u in it. Now by taking r = 1 and r = ∞ in (3.4), respectively, and by passing to the limit into the approximation equation, we can get a solution 1 to in L∞ T X ∩ LT Y . 1 Step 4: Uniqueness. Let u1 , u2 ∈ L∞ T X ∩ LT Y be two solutions of (1.1) with the same initial data. Let u1,2 = u1 − u2 , then ∂t u1,2 + Λβ u1,2 + v2 · ∇u1,2 = u1,2 (∆P u1 ) + u2 (∆P u1,2 ) − v1,2 · ∇u1 ; v1,2 = −∇P u1,2 ; u1,2 (0, x) = 0. According to Lemma 2.7, ku1,2 kL∞ Ḃ n/p+σ−β p,ρ t .e cku2 k n/p+σ+1 L1 t Ḃp,1 ku1,2 (∆P u1 )kLρ Ḃ n/p+σ−2β+β/ρ p,ρ t + ku2 (∆P u1,2 )kLρ Ḃ n/p+σ−2β+β/ρ + kv1,2 · ∇u1 kLρ Ḃ n/p+σ−2β+β/ρ . t p,ρ t p,ρ By a similar argument as in Step 3, we have ku1,2 kρ ∞ n/p+σ−β Lt Ḃp,ρ cρku2 k n/p+σ+1 L1 Ḃp,1 T Z t ku1,2 kρ ∞ n/p+σ−β ku1 (τ )kρ n/p+σ+1−β+β/ρ Lτ Ḃp,ρ Ḃp,ρ 0 ρ + ku2 (τ )k n/p+σ+1−β+β/ρ dτ. .e Ḃp,ρ s s Since the inclusion Ḃp,1 ⊂ Ḃp,ρ holds for any ρ ∈ [1, ∞]. Thus the Minkowski’s inequality and Gronwall’s inequality give that u1 = u2 , ∀t ∈ [0, T ]. Step 5: Continuity in time. For all t, t0 ∈ [0, T ), we have ku(t) − u(t0 )kḂ n/p+σ−β p,1 X X j(n/p+σ−β) p. ≤ 2 kuj (t) − uj (t0 )kLp + 2 2j(n/p+σ−β) kuj kL∞ T L j>N j≤N Since u ∈ n/p+σ−β L∞ , T Ḃp,1 for any > 0, we can choose N large enough such that X p ≤ . 2j(n/p+σ−β) kuj kL∞ T L 4 j>N EJDE-2015/261 POROUS MEDIUM EQUATION IN BESOV SPACES 9 On the other hand, X X p 2j(n/p+σ−β) kuj (t) − uj (t0 )kLp ≤ |t − t0 | 2j(n/p+σ−β) k∂t uj kL∞ T L j≤N j≤N 0 ≤ |t − t |2N β k∂t ukL∞ Ḃ n/p+σ−2β . p,1 T Now write ut = −Λβ u − v · ∇u + u(∆P u) and v = −∇P u. Obviously, we have kΛβ ukL∞ Ḃ n/p+σ−2β ≤ kukL∞ Ḃ n/p+σ−β . p,1 T T p,1 Applying Proposition 2.3 with s1 = n/p − β, s2 = n/p + σ − β, kv · ∇ukL∞ Ḃ n/p+σ−2β ≤ kukL∞ Ḃ n/p+σ−β kukL∞ Ḃ n/p+σ+1−β . p,1 T p,1 T p,1 T Similarly, we have ku(∆P u)kL∞ Ḃ n/p+σ−2β ≤ kukL∞ Ḃ n/p+σ−β kukL∞ Ḃ n/p+σ+1−β . T 0 Nβ Thus for |t − t | ≤ (2 p,1 p,1 T k∂t ukL∞ Ḃ n/p+σ−2β )−1 2 , p,1 T T p,1 we conclude ku(t) − u(t0 )kḂ n/p+σ−β ≤ . p,1 Hence u ∈ n/p+σ−β C([0, T ); Ḃp,1 ). n/p+σ+1−β Similarly we obtain u ∈ C([0, T ); Ḃp,1 ). Step 6: Blowup criterion. We give a blowup criterion as follows: Proposition 3.2. Let T ∗ denote the maximal time of existence of a solution u in C([0, T ∗ ); X) ∩ L1 ([0, T ∗ ); Y ). If T ∗ < ∞, then Z T∗ ku(t)kḂ n/p+σ+1 dt = ∞. p,1 0 R T∗ Proof. Supposing T ∗ < ∞ and 0 ku(t)kḂ n/p+σ+1 dt < ∞, and using Lemma 2.7 p,1 with ρ = ∞, we have kukL∞ Ḃ n/p+σ+1−β . e T∗ c R T∗ 0 ku(t)k n/p+σ+1 dt Ḃp,1 ku0 kḂ n/p+σ+1−β p,1 p,1 Z + 0 T ∗ ku(t)kḂ n/p+σ+1−β ku(t)kḂ n/p+σ+1 dt . p,1 p,1 Hence by Gronwall’s inequality we have kukL∞ Ḃ n/p+σ+1−β . e T∗ c R T∗ 0 ku(t)k n/p+σ+1 dt Ḃp,1 p,1 ku0 kḂ n/p+σ+1−β < ∞. (3.11) ku0 kḂ n/p+σ−β < ∞. (3.12) p,1 By a similar argument there also holds kukL∞ Ḃ n/p+σ−β . e T∗ c R T∗ 0 ku(t)k n/p+σ+1 dt Ḃp,1 p,1 p,1 From Step 5, for all t, t0 ∈ [0, T ∗ ), we have ku(t) − u(t0 )kX → 0 as t → t0 . This means that u(t) satisfies the Cauchy criterion at T ∗ . So there exists an element u∗ in X such that u(t) → u∗ in X as t → T ∗ . Now set u(T ∗ ) = u∗ and consider the 10 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 equation with initial data u∗ . By the well-posedness we obtain a solution existing on a larger time interval than [0, T ∗ ), which is a contradiction. Step 7: Global solution. To obtain global well-posedness for small initial data, it is sufficient to bound Z t ku(τ )kḂ n/p+σ+1 dτ. F (t) := p,1 0 Lemma 2.7 gives kukL1 Ḃ n/p+σ+1 . e t cF (t) Z ku0 kḂ n/p+σ+1−β + p,1 p,1 0 t ku(τ )kḂ n/p+σ+1−β ku(τ )kḂ n/p+σ+1 dτ . p,1 p,1 A similar argument with (3.11) gives kukL∞ Ḃ n/p+σ+1−β . ecF (t) ku0 kḂ n/p+σ+1−β . t p,1 p,1 Hence we conclude F (t) ≤ CeCF (t) (1 + F (t))ku0 kḂ n/p+σ+1−β . p,1 Since F (t) is continuous and F (0) = 0, we obtain that: if the initial data satisfies e−C ku0 kḂ n/p+σ+1−β < 1+C , then p,1 2 F (t) ≤ CeC (1 + C)ku0 kḂ n/p+σ+1−β . p,1 By the blow-up criterion, the solution is global. 4. Appendix We now give the proof of Claim 3.1. We list some lemmas which will be used in our proof. Lemma 4.1 ([20]). Let v be a smooth vector field, and ψt be the solution to Z t ψt (x) = x + v(τ, ψτ (x))dτ. 0 Then for all t ∈ R+ , the flow ψt is a C 1 diffeomorphism over Rn and there holds k∇ψt±1 kL∞ ≤ eV (t) , k∇ψt±1 − IdkL∞ ≤ eV (t) − 1, Z t k∇2 ψt±1 kL∞ ≤ eV (t) k∇2 v(τ )kL∞ eV (τ ) dτ, 0 where V (t) = Rt 0 k∇v(τ )kL∞ dτ . Lemma 4.2 ([20]). Let χ ∈ S (Rn ). There exists a constant C = C(χ, n) such that for all C 2 diffeomorphism ψ over Rn with inverse φ, and for all u ∈ S 0 , p ∈ [1, +∞], (j, j 0 ) ∈ Z2 , 0 kχ(2−j D)(∆j u ◦ ψ)kLp 1/p ≤ CkJφ kL∞ k∆j ukLp (2−j kDJφ kL∞ kJψ kL∞ + 2j 0 −j kDφkL∞ ). EJDE-2015/261 POROUS MEDIUM EQUATION IN BESOV SPACES 11 Lemma 4.3 ([16]). Let v ∈ L1loc (R+ ; Lip) be a fixed vector field. For j ∈ Z, set β uj = ∆j u, ψj be the flow of the regularized vector field Sj−1 v. Then for u ∈ Ḃp,∞ with β ∈ [0, 2), p ∈ [1, ∞], there holds β kΛβ (uj ◦ ψj ) − (Λβ uj ) ◦ ψj kLp ≤ CeCV (t) V 1− 2 (t)2jβ kuj kLp , and when β = 2, kΛ2 (uj ◦ ψj ) − (Λ2 uj ) ◦ ψj kLp ≤ CeCV (t) V (t)22j kuj kLp , Rt where V (t) = 0 k∇v(τ )kL∞ dτ and C = C(β, p) > 0. Proof of Claim 3.1. Applying ∆j to (3.1) we have ∂t um+1 + Sj−1 v m · ∇um+1 + Λβ um+1 = fj + Rj , j j j (4.1) where Rj := (Sj−1 v m − v m ) · ∇um+1 − [∆j , v m · ∇]um+1 . Let ψj be the flow of the j m regularized vector field Sj−1 v . Denote ūj := uj ◦ ψj , then (4.1) becomes ∂t ūm+1 + Λβ ūm+1 = f¯j + R̄j + Gj , j j (4.2) where Gj := Λβ (um+1 ◦ ψj ) − (Λβ um+1 ) ◦ ψj . j j Applying ∆k on the equivalent integral equation of (4.2), we have k∆k ūm+1 (t)kLp j kβ . e−ct2 k∆k u0,j kLp Z t kβ + e−c(t−τ )2 k∆k f¯j kLp + k∆k R̄j kLp + k∆k Gj kLp dτ. (4.3) 0 Lemma 4.3 implies k∆k Gj (t)kLp . ecV (t) V 1−β/2 (t)2jβ kum+1 kLp , j with V (t) = Rt 0 k∇v m (τ )kL∞ dτ . From Bernstein inequality and Lemma 4.1 k∆k f¯j kLp . 2−k k∇∆k f¯j kLp . 2−k k(∇fj ) ◦ ψj kLp k∇ψj kL∞ . 2j−k ecV (t) kfj kLp . A similarly argument implies k∆k R̄j (t)kLp . 2j−k ecV (t) kRj kLp . Taking the Lr norm over [0, t] on (4.3) and plugging the above estimates give kβ 2j(s+β/r) k∆k ūm+1 kLrt Lp . 2(j−k)β/r (1 − e−ctr2 )1/r 2js k∆k u0,j kLp j + 2j(s+β/r) 2(j−k)β ecV (t) V 1−β/2 (t)kum+1 kLrt Lp j (4.4) Z t + 2(j−k)(1+β/r) ecV (t) 2js kfj kLp + kRj kLp dτ. 0 Let M0 ∈ Z to be fixed later. Decomposing um+1 = Sj−M0 ūm+1 ◦ ψj−1 + j j X ∆k ūm+1 ◦ ψj−1 . j k≥j−M0 For all t ∈ [0, T ], there holds kum+1 kLrt Lp . ecV (t) kSj−M0 ūm+1 kLrt Lp + j j X k≥j−M0 k∆k ūm+1 kLrt Lp . j (4.5) 12 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 By Lemma 4.1 and Lemma 4.2, kSj−M0 ūm+1 kLrt Lp . ecV (t) ecV (t) − 1 + 2−M0 kum+1 kLrt Lp . j j (4.6) 0 Since ∆k u0,j = 0 for |k − j| ≥ 2 and ecV (t) − 1 + 2−M0 . e−c V (t) 2−M0 , multiplying (4.5) by 2j(s+β/r) and using (4.4) and (4.6), we obtain jβ 1/r 2j(s+β/r) kum+1 kLrt Lp . ecV (t) 2M0 β/r 1 − e−ctr2 2js ku0,j kLp j + ecV (t) 2j(s+β/r) 2−M0 + 2M0 β V 1−β/2 (t) kum+1 kLrt Lp j Z t + ecV (t) 2M0 (1+β/r) 2js kfj kLp + kRj kLp dτ. 0 Now we choose M0 to be the unique integer such that 2c2−M0 ∈ (1/8, 1/4] and T1 ≤ T be the largest real number such that 2−M0 β 2 cV (T1 ) ≤ min ln 2, ( β/2 ) 2−β . 8c Thus for t ∈ [0, T1 ], Z t jβ 1/r m+1 j(s+β/r) −ctr2 js 2 kuj kLrt Lp . 1 − e 2 ku0,j kLp + 2js kfj kLp + kRj kLp dτ. 0 1 Taking the l -norm we conclude that kum+1 kLr Ḃ s+β/r t . X j∈Z p,1 jβ 1 − e−ctr2 1/r 2js ku0,j kLp + XZ j∈Z t 2js kfj kLp + kRj kLp dτ. 0 4.1. Acknowledgments. This research was supported by the NNSF of China under grant 11271330. References [1] H. 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Zhou, W. Xiao, J. Chen; Fractional porous medium and mean field equations in Besov spaces, Electron. J. Differential Equations, 2014 (2014), 1-14. 14 X. ZHOU, W. XIAO, T. ZHENG EJDE-2015/261 Xuhuan Zhou Department of Mathematics, Zhejiang University, Hangzhou 310027, China E-mail address: zhouxuhuan@163.com Weiliang Xiao chool of Applied Mathematics, Nanjing University of Finance and Economics, Nanjing 210023, China E-mail address: xwltc123@163.com Taotao Zheng Department of Mathematics, Zhejiang University of Science and Technology, Hangzhou 310023, China E-mail address: taotzheng@126.com