不平衡格劳伯-川崎动力学的等速界面流

T. Funaki, P. Meurs, S. Sethuraman, K. Tsunoda
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摘要

我们推导了格劳伯-川崎动力学的水动力极限。川崎部分很简单,描述了具有硬核排他性相互作用的粒子的独立运动。它以扩散的时空尺度加速。格劳伯部分描述了粒子的诞生和死亡。它被设置为支持两个级别的粒子密度,并优先选择其中一个。它也在时间上加速,但速度比川崎部分要慢。在这种标度下,极限粒子密度立即取两个有利密度值中的任意一个。分离这两个值的界面以恒定的速度演变(惠更斯原理)。在最近的四篇论文中也推导出了类似的水动力极限。这些论文的关键区别在于,我们考虑了格劳伯动力学,它对两个有利的密度值之一有偏好。因此,我们在较短的时间尺度上观察到极限动力学,其演化与之前四篇论文中得到的平均曲率流不同。虽然我们的证明中有几个步骤可以采用这些论文,但对界面传播的证明是新的。
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Constant-speed interface flow from unbalanced Glauber-Kawasaki dynamics
We derive the hydrodynamic limit of Glauber-Kawasaki dynamics. The Kawasaki part is simple and describes independent movement of the particles with hard core exclusive interactions. It is speeded up in a diffusive space-time scaling. The Glauber part describes the birth and death of particles. It is set to favor two levels of particle density with a preference for one of the two. It is also speeded up in time, but at a lesser rate than the Kawasaki part. Under this scaling, the limiting particle density instantly takes either of the two favored density values. The interface which separates these two values evolves with constant speed (Huygens' principle). Similar hydrodynamic limits have been derived in four recent papers. The crucial difference with these papers is that we consider Glauber dynamics which has a preferences for one of the two favored density values. As a result, we observe limiting dynamics on a shorter time scale, and the evolution is different from the mean curvature flow obtained in the four previous papers. While several steps in our proof can be adopted from these papers, the proof for the propagation of the interface is new.
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