In geometry, inversive geometry is the study of inversion, a special way of changing shapes on a flat surface. Inversion takes circles or straight lines and turns them into other circles or lines, while keeping the angles between them the same. This helps solve many tough geometry problems that are easier to understand after an inversion is used.
The idea of inversion was discovered by several people around the same time. Steiner found it in 1824, Quetelet in 1825, Bellavitis in 1836, Stubbs and Ingram between 1842 and 1843, and Kelvin in 1845. Inversion can also be expanded to work in spaces with more than two dimensions.
Inversion in a circle
The inverse of a point in geometry is a special way to find a new point related to a given circle. Imagine you have a point P and a circle with center O and radius r. The inverse point P' lies on the same line from O through P, but its distance from O is such that the product of the distances OP and OP' equals r squared. This means points closer to the center move farther away, and points farther away move closer.
Inversion has many interesting properties. For example, a line not passing through the center of the circle becomes a circle that does pass through the center, and a circle passing through the center becomes a line not passing through the center. Inversion also keeps angles the same size but can change their direction. These properties make inversion useful for solving many geometry problems more easily.
In three dimensions
In three dimensions, inversion works similarly to the two-dimensional case but uses spheres instead of circles. When you invert a point in 3D space using a reference sphere, the point moves along a straight line from the center of the sphere to a new position. This keeps angles the same, just like in two dimensions.
In three dimensions, spheres invert to other spheres. If a sphere passes through the center of the reference sphere, it turns into a flat plane. Planes that pass through the center also become spheres. This idea helps solve many tough geometry problems by making them easier to understand.
Axiomatics and generalization
One of the first people to study the basics of inversive geometry was Mario Pieri in 1911 and 1912. Edward Kasner wrote his thesis on the "Invariant theory" of the inversion group.
Later, the rules of inversive geometry were seen as a special type of structure where certain shapes are called "blocks." In incidence geometry, any flat area with one extra point forms something called a Möbius plane, also known as an inversive plane. There are versions of these planes that have a limited number of points and others that go on forever. A way to model the Möbius plane using normal flat shapes is called the Riemann sphere.
Invariant
The cross-ratio between four points stays the same even after an inversion. This special property helps solve tricky geometry problems more easily. When you flip or turn shapes using inversion, some measurements change, but the cross-ratio remains unchanged.
Relation to Erlangen program
The transformation called inversion in a circle was invented by L. I. Magnus in 1831. Since then, this mapping has become important in higher mathematics. Through applying circle inversion, students of transformation geometry can understand the significance of Felix Klein's Erlangen program, which grew out of models of hyperbolic geometry.
Combining two inversions in circles that share the same center results in a similarity or homothetic transformation, known as dilation. This dilation is defined by the ratio of the radii of the two circles.
Inversive geometry also connects to complex numbers and the Möbius group, which includes transformations like translation and rotation. The addition of reciprocation—based on circle inversion—helps create the unique properties of Möbius geometry. However, inversive geometry is broader, also including basic circle inversion and conjugation mappings.
In higher dimensions
In higher dimensions, inversive geometry uses a special transformation called inversion. This transformation changes the position of points in space using a sphere. By flipping the position of points based on their distance from the center of the sphere, we can create new shapes and movements.
This idea can help us understand movements like stretching, sliding, or turning objects in space. When we combine these movements, we get special kinds of maps that keep angles the same. These maps are very important in studying shapes and spaces.
Anticonformal mapping property
The circle inversion map is called "anticonformal" because it keeps the sizes of angles between lines and curves the same but flips the direction they face. This is different from a "conformal" map, which keeps both the size and direction of angles.
In math, this means the special grid of numbers (called a Jacobian) for this map is a simple stretch or shrink of a mirror flip. For complex numbers, the basic circle inversion map uses the mirror image of the normal inverse map, making it anticonformal instead of conformal.
Hyperbolic geometry
The (n − 1)-sphere can be described by a special kind of equation. When we use a process called inversion, some of these spheres stay exactly the same. These special spheres are important in a model of hyperbolic geometry called the Poincaré disk model.
Inversion in the unit sphere keeps certain spheres unchanged and swaps points inside the sphere with points outside. This helps us understand how angles and shapes behave in hyperbolic geometry, showing that distances and angles in this model match those in hyperbolic space.
Images
This article is a child-friendly adaptation of the Wikipedia article on Inversive geometry, available under CC BY-SA 4.0.
Images from Wikimedia Commons. Tap any image to view credits and license.
Safekipedia