RS Fellow - EPSRC grant (2016): Spatial fragmentations

当大的东西被分解成更小的碎片时--比如地震中的岩石--碎片的具体破裂程度可能取决于一系列参数，比如它们的大小、形状和结构。例如，又长又薄的石块可能比紧凑的石块破裂得更快。一个被称为碎片化过程的数学概念也描述了随着时间的推移随机分解成越来越小的碎片的对象的集合。然而，关于如何破裂的规则可能会相当严格：一块如何断裂，以及它断裂的速度，只取决于它的大小。这使我们能够给出关于这些过程的很好的数学结果，但对于理解真实对象并不是很有用。在这个项目中，我们建议研究一个简单的碎片模型，其中块破裂的速度取决于它们的形状和大小。我们从一个正方形开始，经过一段时间后，它分裂成两个随机大小的矩形。然后，这两个矩形执行相同的操作：每个矩形都等待一段时间，然后一分为二。但他们等待的时间取决于他们的身高和宽度的比例。事实上，就像岩石的例子一样，细长的碎片可能比粗略的方形碎片破裂得更快。其目的是，这项工作将是理解更复杂的碎片化系统的第一步，在这些碎片化系统中，拆分规则可能非常复杂。但即使是我们计划研究的相对简单的物体，也被用作被称为马氏体雪崩的现实生活过程的模型。这些描述了杂质在晶体原子结构中形成的方式--例如，当金属熔化，然后快速冷却以增加其强度时。

When something big gets broken up into smaller pieces - for example rocks in an earthquake - how exactly the pieces break might depend on a whole host of parameters, such as their size, shape and structure. For example, long, thin pieces of rock are likely to break more quickly than compact blocks. A mathematical concept called a fragmentation process also describes a collection of objects that break up randomly into smaller and smaller pieces as time passes. However, the rules of how the breaking up happens can be quite restrictive: how a piece breaks, and how quickly it breaks, is only allowed to depend on its size. This allows us to give nice mathematical results about these processes but is not very useful for understanding real objects. In this project we propose to study a simple model of fragmentation where how quickly blocks break does depend on their shape as well as their size. We begin with a square, which after some time breaks up into two randomly-sized rectangles. These two rectangles then do the same: each of them waits some time and then splits into two. But the time they wait before doing so depends on the ratio of their height to their width. In fact, exactly as in the rocks example, long thin pieces are likely to break more quickly than roughly square pieces. The aim is that this work will be a first step towards understanding more complex fragmentation systems, where the break-up rules might be very complicated. But even the relatively simple object that we plan to study has been used as a model for real-life processes called martensitic avalanches. These describe the way in which impurities form in crystalline atomic structures - such as when metals are melted and then cooled quickly in order to increase their strength.