11.2
Crystals show symmetry because their atoms are arranged in a regular, repeating pattern in three dimensions.
A symmetry operation moves parts of a crystal without changing its overall appearance.
One of the simplest symmetry operations is translation. In translation, every point in the structure moves by the same distance in the same direction, reproducing the repeating lattice.
Other common symmetry operations include rotation, reflection, and inversion. Rotation turns the structure around an axis by a specific angle without changing its appearance. Reflection forms a mirror image across a plane. Inversion moves each point through a central point to an equivalent position on the opposite side.
The geometric feature about which a symmetry operation is performed is called a symmetry element. For instance, a line represents a rotation axis, a plane represents a mirror plane, and a point represents a center of inversion.
Crystals may also contain combined symmetry elements. For example, a screw axis combines rotation with translation along the same axis.
Similarly, a glide plane combines reflection with translation parallel to the plane.
Crystal symmetry operations are isometric transformations that map objects onto indistinguishable copies while preserving distances, angles, and volumes. The simplest symmetry operation is translation, which shifts the entire infinite crystal lattice parallelly by a translation vector.
Crystallographic rotations involve rotations by an angle of 2π/n around an axis without changing the positions of points on the axis. It is called the rotational axis of the symmetry, denoted by n. The combination of rotation and translation along the same axis is a roto-translation, resulting in a screw axis.
A symmetry operation with respect to a point is the inversion, forming the center of symmetry or inversion center, while a symmetry operation with respect to a plane is a reflection leading to the plane of symmetry.
The roto-inversion axis, represented as 'n̅,' involves a 2π/n rotation coupled with inversion at a point on the same axis, while roto-reflection is a rotation with an angle of 2π/n around an axis followed by reflection across a plane perpendicular to the same axis. The glide plane results from the combination of the reflection across a plane and translation parallel to the plane.
A crystal can have multiple planes or axes of symmetry, but only one center of symmetry. The sum of these symmetries, referred to as the crystal's elements of symmetry, varies from crystal to crystal; for instance, a cubic crystal like NaCl has 23 such elements.
Crystals show symmetry because their atoms are arranged in a regular, repeating pattern in three dimensions.
A symmetry operation moves parts of a crystal without changing its overall appearance.
One of the simplest symmetry operations is translation. In translation, every point in the structure moves by the same distance in the same direction, reproducing the repeating lattice.
Other common symmetry operations include rotation, reflection, and inversion. Rotation turns the structure around an axis by a specific angle without changing its appearance. Reflection forms a mirror image across a plane. Inversion moves each point through a central point to an equivalent position on the opposite side.
The geometric feature about which a symmetry operation is performed is called a symmetry element. For instance, a line represents a rotation axis, a plane represents a mirror plane, and a point represents a center of inversion.
Crystals may also contain combined symmetry elements. For example, a screw axis combines rotation with translation along the same axis.
Similarly, a glide plane combines reflection with translation parallel to the plane.
From Chapter 11:
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