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Slow translational instabilities of spike patterns in the one-dimensional Gray-Scott model

机译:一维Gray-Scott模型中尖峰模式的平移缓慢

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Slow translational instabilities of symmetric k-spike equilibria for the one-dimensional singularly perturbed two-component Gray-Scott (GS) model are analyzed. These symmetric spike patterns are characterized by a common value of the spike amplitude. The GS model is studied on a finite interval in the semi-strong spike-interaction regime, where the diffusion coefficient of only one of the two chemical species is asymptotically small. Two distinguished limits for the GS model are considered: the low feed-rate regime and the intermediate regime. In the low feed-rate regime it is shown analytically that k—1 small eigenvalues, governing the translational stability of a symmetric k-spike pattern, simultaneously cross through zero at precisely the same parameter value at which k—1 different asymmetric k-spike equilibria bifurcate off of the symmetric k-spike equilibrium branch. These asymmetric equilibria have the general form SBB ... BS (neglecting the positioning of the B and S spikes in the overall spike sequence). For a one-spike equilibrium solution in the intermediate regime it is shown that a translational, or drift, instability can occur from a Hopf bifurcation in the spike-layer location when a reaction-time parameter τ is asymptotically large as ε → 0. Locally, this instability leads to small-scale oscillations in the spike-layer location. For a certain parameter range within the intermediate regime such a drift instability for the GS model is shown to be the dominant instability mechanism. Numerical experiments are performed to validate the asymptotic theory.
机译:分析了一维奇摄动两分量Gray-Scott(GS)模型的对称k尖峰平衡的慢平移不稳定性。这些对称的尖峰图案的特征在于尖峰幅度的共同值。 GS模型是在半强尖峰相互作用机制中的有限间隔上进行研究的,其中两种化学物质中只有一种的扩散系数渐近较小。考虑了GS模型的两个明显的局限性:低进给率状态和中间状态。在低进给率状态下,分析表明,控制对称k尖峰图形平移稳定性的k-1个小特征值,在恰好是k-1个不同的非对称k尖峰的相同参数值处同时穿越零平衡分叉出对称的k峰平衡分支。这些不对称平衡的一般形式为SBB ... BS(忽略了整个尖峰序列中B和S尖峰的位置)。对于中间状态下的一峰平衡解决方案,研究表明,当反应时间参数τ渐近变大为ε→0时,在峰形层位置的Hopf分叉会发生平移或漂移不稳定性。 ,这种不稳定性会导致尖峰层位置发生小规模的振荡。对于中间范围内的某个参数范围,这种GS模型的漂移不稳定性被证明是主要的不稳定性机理。进行数值实验以验证渐近理论。

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