

FRACTAL GEOMETRY
A modern mathematical theory that radically departs from traditional Euclidean
Geometry, fractal geometry describes objects that are selfsimilar, or scale symmetric.
This means that when such objects are magnified, their parts are seen to bear an exact resemblance to the whole, the likeness continuing with the parts of the parts and so on to infinity.
Fractals, as these shapes are called, also must be devoid of translational symmetry  that is, the smoothness associated with Euclidean lines, planes, and spheres. Instead a rough, jagged quality is maintained at every scale at which an object can be examined.
The nature of fractals is reflected in the word itself, coined by mathematician Benoit B. Mandelbrot from the Latin verb frangere, "to break," and the related adjective fractus, "irregular and fragmented."
The simplest fractal is the cantor Bar Set, named after the 19thcentury German mathematician Georg cantor.
One may be constructed by dividing a line in 3 parts and removing the middle part.
The procedure is repeated indefinitely, first on the 2 remaining parts, then on on 4 parts produced by that operation, and so on, until the object has an infinitely large number of parts each of which is infinitely small.
Fractals are not relegated exclusively to the realm of mathematics. If the definition is broadened a bit, such objects can be found virtually everywhere in the natural world.
The difference is that "natural" fractals are randomly, statistically, or stochastically rather than exactly scale symmetric.
The rough shape revealed at one length scale bears only an approximate resemblance to that at another, but the length scale being used is not apparent just by looking at the shape.
Moreover, there are both upper and lower limits to the size range over which the fractals in nature are indeed fractal.
Above and below that range, the shapes are either rough (but not selfsimilar) or smoothin other words, conventionally Euclidean.
Whether natural or mathematical, all fractals have particular fractal dimensions. These are not the same as the familiar Euclidean dimensions, measured in discrete whole integers1, 2, or 3but a different kind of quantity.
Usually noninteger, a fractal dimension indicates the extent to which the fractal object fills the Euclidean dimension in which it is embedded.
A natural fractal of fractal dimension 2.8, for example, would be a spongelike shape nearly 3dimensional in appearance.
A natural fractal of fractal dimension 2.2 would be a much smoother object that just misses being flat.
Background
The roots of fractal geometry can be traced to the late 19th century, when mathematicians started to challenge Euclid's principles.
Fractional dimensions were not discussed until 1919, however, when the German mathematician Felix Hausdorff put forward the idea in connection with the smallscale structure of mathematical shapes.
As completed by the Russian mathematician A. S. Besicovitch, Hausdorff's dimensionality was a forerunner of fractal dimensionality. Other mathematicians of the time, however, considered such strange shapes as "pathologies" that had no significance.
This attitude persisted until the mid20th century and the work of Mandelbrot, a Polishborn French mathematician who moved to the United States in 1958.
His 1961 study of similarities in large and smallscale fluctuations of the stock market was followed by work on phenomena involving nonstandard scaling, including the turbulent motion of fluids and the distribution of galaxies in the universe.
A 1967 paper on the length of the English coast showed that irregular shorelines are fractals whose lengths increase with increasing degree of measurable detail.
By 1975, Mandelbrot had developed a theory of fractals, and publications by him and others made fractal geometry accessible to a wider audience. The subject began to gain importance in the sciences.
Mandelbrot later also investigated another fractal terrain, that of shapes distorted in some way from one length to another.
These fractals are now called nonlinear, since the relationships between their parts is subject to change.
They retain some degree of selfsimilarity, but it is a local rather than global characteristic in them.
The general definition of the word fractal may thus need further refinement, to indicate more precisely which shapes should be included and which excluded by the term.
The most intriguing of the nonlinear fractals thus far has been the mathematical set named after Mandelbrot by the American mathematicians John Hubbard and Adrien Douady.
The more the set is magnified, the more its unpredictability increases, until unpredictability comes to dominate the budlike shape that is the set's major element of stability.
The set has become the source of stunning color computer Graphics images.
It is also important in mathematics because of its centrality to dynamical system theory.
An entire Mandelbrot set is actually a catalog of dynamical mathematical objectsthat is, objects generated through an iterative process called Julia sets.
These derive from the work done by a French mathematician, Gaston Julia, on the iteration of nonlinear transformations in a complex plane.
Impact on the Sciences
Scientists have begun to investigate the fractal character of a wide range of phenomena. Researchers are interested in doing so for the practical reason that behavior on a fractal shape may differ markedly from that on a Euclidean shape.
Physics is by far the discipline most affected by fractal geometry.
In condensedmatter, or solidstate physics, for example, the socalled "percolation cluster" model used to describe critical phenomena involved in phase transitions and in mixture of atoms with opposing properties is clearly fractal.
This has implications, as well, for a host of attributes, including electrical conductivity. The percolation cluster model may also apply to the atomic structure of glasses, gels, and other amorphous materials, and their fractal nature may give them unique heattransport properties that could be exploited technologically.
Another major area of condensedmatter physics to invoke the concept of selfsimilarity is that of kinetic growth, in which particles are gradually added to a structure in such a way that once they stick, they neither come off nor rearrange themselves.
In the case of the simplest model of kinetic growth, the most important physical phenomenon to which it applies appears to be the fingering of a lessviscous fluid (water) through a more viscous fluid (oil) lodged in a porous substance (limestone and other kinds of rock).
A more complex model explains the growth of colloidal agglomerates.
Mathematical physics, for its part, has a particular interest in nonlinear fractals.
When dynamical systemsthose that change their behavior over timebecome chaotic, or totally unpredictable, physicists describe the route they take with such fractals.
called strange attractors, these objects are not real physical entities but abstractions that exist in "phase space," an expanse with as many dimensions as physicists need to describe dynamical physical behavior.
One point in phase space represents a single measurement of the state of a dynamical system as it evolves over time.
When all such points are connected, they form a trajectory that lies on the surface of a strange attractor.
Most physicists who study chaos do so with carefully controlled laboratory setups of turbulent fluid flow.
Individual strange attractors have been identified for different kinds of turbulent fluid flow, suggesting the existence of numerous routes to chaos.
Although not concerned with fractals to the same extent as physics, other sciences have discovered them.
In biology, the anomolous thermal relaxation rate of ironcontaining proteins has been explained as resulting from the fractal shape of the linear polymer chain that comprises all proteins. The distribution pattern of atoms on the protein surface, a different aspect of protein structure, also appears to be fractal.
Many more fractals have been detected in geology, including both random exterior surfacesragged mountains and valleysand interior fractal surfaces in the brittle crust, such as California's famous San Andreas fault.
Earthquake processes for small tremorsthose of magnitude 6 or lessappear to be fractal in time as well as space, since these quakes occur in selfsimilar clusters rather than at regular intervals.
Meteorology provides a different kind of spacetime fractal: the contour of the area over which tropical rain falls is selfsimilar, and the amount of rain that falls varies in a selfsimilar fashion over time.
Finally, on the interface of science and art, computergraphics specialists, using a recursive splitting technique, have produced striking new fractal images of great statistical complexity.
Landscapes made this way have been used as backgrounds in many motion pictures; trees and other branching structures have been used in still lifes and animations.
 Grolier Encyclopedia
Back to top





