Metal is made of tiny bits. 

Metal is made of tiny bits. 

These lines can make metal strong. They also change how heat and power move. Sometimes, these lines can cause rust.
Some boundaries are small. They happen when bits are slightly bent. Other boundaries are big. They happen when bits are very different.
These lines can move. They move when things get hot.
It is neat to look at metal closely! 
Most metals are made of many tiny parts. We call these parts grains or crystallites. 

Boundaries can be small or large. We call small ones low-angle boundaries. These happen when grains are only slightly tilted. They are made of tiny mistakes in the pattern called dislocations.
These boundaries can even move. This often happens when the metal gets hot. When boundaries move, the grains can grow larger.
Many metals are made of many tiny parts called grains or crystallites. 

Boundaries work in different ways depending on how the grains are tilted. If the grains are only slightly tilted, it is a low-angle grain boundary. These are made of many dislocations, which are tiny wedges of atoms.
Scientists have learned a lot about these tiny structures over time. Long ago, some people thought high-angle boundaries were like a layer of liquid. This idea was later changed after the invention of electron microscopy. This new tool let scientists see the actual grain structure directly. They discovered that boundaries are actually made of specific structural units. These units depend on how the two grains are tilted against each other. Scientists use a special math system called CSL theory to describe them.
There are many specific details that help describe these boundaries. In CSL theory, scientists look at how many atoms are shared between grains. For example, a boundary with a value of Σ3 shares one atom for every three atoms. 

Understanding these boundaries helps us make much stronger materials. For instance, making the grains smaller can improve a metal's strength. This is known as the Hall-Petch relationship. Boundaries can also move when a material gets hot. This movement can cause the grains to grow larger.
In materials science, a grain boundary is the interface where two grains, or crystallites, meet within a polycrystalline material. 

Scientists categorize these boundaries based on the degree of misorientation between the two grains. A low-angle grain boundary (LAGB), also called a subgrain boundary, occurs when the misorientation is less than about 15 degrees. These boundaries are composed of an array of dislocations. A dislocation is essentially a half-plane of atoms that acts like a wedge. When a single grain is bent by an external force, the energy from that bending can be reduced by inserting a dislocation. As the grain bends further, more dislocations are added, forming a wall that splits the grain into two sub-grains.
There are different ways these dislocations can arrange themselves. In a tilt boundary, the rotation axis is parallel to the boundary plane. This can be imagined as a single crystal being gradually bent. In a twist boundary, the misorientation occurs around an axis perpendicular to the boundary plane. This type of boundary incorporates two sets of screw dislocations. These dislocations might form a square network if they are orthogonal. In other cases, they may interact to form a complex hexagonal structure. Most real-world boundaries are mixed types, containing different dislocations to find the best fit between neighbors.
When deformation continues, the density of these dislocations increases. The spacing between them decreases until their cores begin to overlap. At this point, the ordered nature of the boundary breaks down. The boundary is then considered a high-angle grain boundary (HAGB), with a misorientation greater than 15 degrees. High-angle boundaries are much more disordered than low-angle ones. They feature large areas of poor fit and a more open structure.
Historically, scientists held different views about these structures. It was once believed that high-angle boundaries were a form of amorphous or liquid layer between grains. However, this model could not explain the observed strength of the boundaries. After the invention of electron microscopy, researchers gained the ability to see the grain structure directly. This evidence forced scientists to discard the liquid layer hypothesis. We now know that a boundary consists of structural units. These units depend on the misorientation of the grains and the plane of the interface.
To understand the fit between grains, scientists use Coincidence Site Lattice (CSL) theory. This theory describes the degree of fit, represented by the Greek letter sigma (Σ). The value of Σ is the reciprocal of the ratio of coincidence sites to the total number of sites. For example, if Σ=3, then one out of every three atoms is shared between the two lattices. Boundaries with low Σ values, such as coherent twin boundaries (Σ3) or high-mobility boundaries (Σ7), have special properties. 
Energy and volume are also vital to characterizing these interfaces. The energy of a low-angle boundary depends on the degree of misorientation. This relationship is described by the Read–Shockley equation. 
Finally, grain boundaries can move, which impacts how materials change over time. This movement is called boundary migration. High-angle boundaries move by the transfer of atoms between neighboring grains. This process depends on temperature, the structure of the boundary, and the presence of impurity atoms. Low-angle boundaries move more slowly, often through a process called dislocation climb. This movement is limited by the diffusion of solutes in the bulk. Engineers can manage this by using particles to inhibit grain growth through a process called Zener pinning.
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