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Center for Partial Differential Equations, ECNU No. 2013-02 Diffusion and Advection: some PDE models in Spatial Ecology Lecture notes from Program on Nonlinear Equations in Population Biology, Center for PDE, ECNU, mid April-June, 2013 Yuan Lou The Ohio State University, USA.lou@math.ohio-state.edu The Center receives funding from Cente for PDE 500 Dongchuan Road Administration Building 12th floor Minhang Campus, East China Normal University Shanghai, 200241, China Email: admin@cpde.ecnu.edu.cn DIFFUSION AND ADVECTION: SOME PDE MODELS IN SPATIAL ECOLOGY Yuan Lou Abstract. This series of lectures will focus on the dynamics of some reaction-diffusion advection models from spatial ecology. Mathematically we are interested in the effect of diffusion and advection on population dynamics in spatially heterogeneous environment. Biologically we are interested in understanding the evolution of dispersal; i.e., loosely speaking, to investigate what kind of dispersal strategies are optimal. LECTURE1 1. Logistic model (1.1) dN =rN(1−N) dt K r : intrinsic growth rate (no unite); K: carrying capacity (same unit as population size). Discrete-time model N =N(t):populationsizeattimet,t = 0,1,2,··· t Geometric growth N =RN t+1 t R=Nt+1 = offspring ♯, ♯ : numbers Nt parents ♯ r = lnR General model N =f(N) t+1 t Beverton-Holt model (1.2) N = RNt t+1 1+R−1N K t K: population size where the parent vs offspring ratio 1991 Mathematics Subject Classification. Primary: 35B44, 35K57; Secondary: 35B30, 35K51. Key words and phrases. Diffusion, Advection, Logistic, Lotka-Volterra, Spatial Ecology. 1 2 YUANLOU For geometric model, Nt = 1 Nt+1 R What is the next level of models in terms of complexity? Nt =linear function of N N t t+1 =line passing through (K,1) and (0, 1 ). R Then we get (1.2). Change (1.2), RhN N = t , h > 0. t+h 1+Rh−1N K t N −N 1[ RhN ] t+h t = t −N h h 1+Rh−1N t [ K t ] 1 (Rh −1)N − Rh−1N2 = t K t h 1+Rh−1N [ K t ] Rh−1 (1−Nt)N N = K t →lnRN(1− ),ash→0. h 1+Rh−1N t K K t Remark 1.1. Two species model R1N1(t) N(t+1)= 1 1+α N (t)+β N (t) 1 1 1 2 R2N2(t) N(t+1)= . 2 1+α N (t)+β N (t) 2 1 1 2 which is equivalent to N(t) 1+α N (t)+β N (t) 1 1 1 1 2 = N(t+1) R 1 1 N(t) 1+α N (t)+β N (t) 2 2 1 1 2 N(t+1) = R . 2 2 Corresponding continuous-time model dN 1 =lnR (1−C N −D N ) dt 1 1 1 1 2 dN 2 =lnR (1−C N −D N ), dt 2 2 1 2 2 where C ,D , i = 1,2 depend upon α ,β i = 1,2. i i i i DIFFUSION AND ADVECTION: SOME PDE MODELS IN SPATIAL ECOLOGY 3 2. Diffusion models of single species −→ n (2.1) ut = ∇·[d(x)∇u]+ b ·∇u+uf(x,u), x ∈ Ω ⊂ R , t > 0. u(x,t) : density at location x and time t. −→ d(x) > 0,smooth, b = (b1,b2,··· ,bn) Holder continuous. Boundary condition: −→ (2.2) −→ ∇u· n =0 on ∂Ω where n is the outward unit normal vector. Obvious, u ≡ 0 is a steady state of (2.1) Stability of u ≡ 0: It is determined by the smallest eigenvalue (denoted by σ1). −→ (2.3) ∇·[d(x)∇φ]+ b ·∇φ+f(x,0)φ+σφ=0, in Ω −→ ∇φ· n =0 on ∂Ω. Proposition 2.1. If σ > 0, then u ≡ 0 is locally stable; 1 If σ < 0, then u ≡ 0 is unstable. 1 Proof. Sub-solution: Consider σ1 < 0. Set u(x) = εφ1(x) where ε > 0, φ1 > 0 is an eigenfunction of σ1. Recall −→ u =∇·[d(x)∇u]+ b ·∇u+uf(x,u). t It suffices to show: −→ ut ≤ ∇·[d(x)∇u]+ b ·∇u+uf(x,u) −→ ⇔0≤ε∇·[d∇φ1]+εb ·∇φ1+εφ1f(x,εφ1) ⇔0≤−f(x,0)φ −σ φ +φ f(x,εφ ) 1 1 1 1 1 ⇔0≤[f(x,εφ )−f(x,0)]−σ . 1 1 The last inequality holds for 0 < ε << 1 since σ < 0. 1 Remark 2.1. { −→ n ut = ∇·[d(x)∇u]+ b ·∇u+uf(x,u), x ∈ Ω ⊂ R , t > 0, u(x,0) = εφ1 (sub−solution). By maximum principles, u(x,t) is increasing in t for every x ⇒ u ≡ 0 is unstable. Exercise: To check, if σ < 0, u ≡ 0 is locally stable (construct super-solution). 1
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