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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.
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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;
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If σ < 0, then u ≡ 0 is unstable.
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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.
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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).
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