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Introduction to the Modeling and Analysis of Complex Systems

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270 CHAPTER 14. CONTINUOUS FIELD MODELS II: ANALYSISh<strong>and</strong> side. But this non-au<strong>to</strong>nomy can be easily eliminated by replacing x with a newstate variable y that satisfies∂y= 0,∂t(14.4)y(x, 0) = x. (14.5)In <strong>the</strong> following, we will continue <strong>to</strong> use x instead <strong>of</strong> y, just <strong>to</strong> make <strong>the</strong> discussion easier<strong>and</strong> more intuitive.To find an equilibrium state <strong>of</strong> this system, we need <strong>to</strong> solve <strong>the</strong> following:0 = D∇ 2 c eq + sin x (14.6)= D d2 c eq+ sin x (14.7)dx2 This is a simple ordinary differential equation, because <strong>the</strong>re are no time or additionalspatial dimensions in it. You can easily solve it by h<strong>and</strong> <strong>to</strong> obtain <strong>the</strong> solutionc eq (x) = sin xD + C 1x + C 2 , (14.8)where C 1 <strong>and</strong> C 2 are <strong>the</strong> constants <strong>of</strong> integration. Any state that satisfies this formularemains unchanged over time. Figure 14.1 shows such an example with D = C 1 = C 2 = 1.Exercise 14.1 Obtain <strong>the</strong> equilibrium states <strong>of</strong> <strong>the</strong> following continuous fieldmodel in a 1-D space:∂c/∂t = D∇ 2 c + 1 − x 2 (14.9)As we see above, equilibrium states <strong>of</strong> a continuous field model can be spatially heterogeneous.But it is <strong>of</strong>ten <strong>the</strong> case that researchers are more interested in homogeneousequilibrium states, i.e., spatially “flat” states that can remain stationary over time. This isbecause, by studying <strong>the</strong> stability <strong>of</strong> homogeneous equilibrium states, one may be able<strong>to</strong> underst<strong>and</strong> whe<strong>the</strong>r a spatially distributed system can remain homogeneous or selforganize<strong>to</strong> form non-homogeneous patterns spontaneously.Calculating homogeneous equilibrium states is much easier than calculating generalequilibrium states. You just need <strong>to</strong> substitute <strong>the</strong> system state functions with constants,

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