foliation$29178$ - definizione. Che cos'è foliation$29178$
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Cosa (chi) è foliation$29178$ - definizione

MATHEMATICAL CONCEPT
Regular foliation; Kronecker foliation; Foliation theory

Foliation         
·noun The process of forming into a leaf or leaves.
II. Foliation ·noun The manner in which the young leaves are dispo/ed within the bud.
III. Foliation ·noun The act of beating a metal into a thin plate, leaf, foil, or lamina.
IV. Foliation ·noun The act of coating with an amalgam of tin foil and quicksilver, as in making looking-glasses.
V. Foliation ·noun The enrichment of an opening by means of foils, arranged in trefoils, quatrefoils, ·etc.; also, one of the ornaments. ·see Tracery.
VI. Foliation ·noun The property, possessed by some crystalline rocks, of dividing into plates or slabs, which is due to the cleavage structure of one of the constituents, as mica or hornblende. It may sometimes include slaty structure or cleavage, though the latter is usually independent of any mineral constituent, and transverse to the bedding, it having been produced by pressure.
foliation         
[?f??l?'e??(?)n]
¦ noun chiefly Geology the process of splitting into thin sheets or laminae.
Foliated         
WIKIMEDIA DISAMBIGUATION PAGE
Foliations; Foliated
·adj Spread over with an amalgam of tin and quicksilver.
II. Foliated ·Impf & ·p.p. of Foliate.
III. Foliated ·adj Containing, or consisting of, foils; as, a foliated arch.
IV. Foliated ·adj Having leaves, or leaflike projections; as, a foliated shell.
V. Foliated ·adj Characterized by being separable into thin plates or folia; as, graphite has a foliated structure.
VI. Foliated ·adj Laminated, but restricted to the variety of laminated structure found in crystalline schist, as mica schist, ·etc.; schistose.

Wikipedia

Foliation

In mathematics (differential geometry), a foliation is an equivalence relation on an n-manifold, the equivalence classes being connected, injectively immersed submanifolds, all of the same dimension p, modeled on the decomposition of the real coordinate space Rn into the cosets x + Rp of the standardly embedded subspace Rp. The equivalence classes are called the leaves of the foliation. If the manifold and/or the submanifolds are required to have a piecewise-linear, differentiable (of class Cr), or analytic structure then one defines piecewise-linear, differentiable, or analytic foliations, respectively. In the most important case of differentiable foliation of class Cr it is usually understood that r ≥ 1 (otherwise, C0 is a topological foliation). The number p (the dimension of the leaves) is called the dimension of the foliation and q = np is called its codimension.

In some papers on general relativity by mathematical physicists, the term foliation (or slicing) is used to describe a situation where the relevant Lorentz manifold (a (p+1)-dimensional spacetime) has been decomposed into hypersurfaces of dimension p, specified as the level sets of a real-valued smooth function (scalar field) whose gradient is everywhere non-zero; this smooth function is moreover usually assumed to be a time function, meaning that its gradient is everywhere time-like, so that its level-sets are all space-like hypersurfaces. In deference to standard mathematical terminology, these hypersurface are often called the leaves (or sometimes slices) of the foliation. Note that while this situation does constitute a codimension-1 foliation in the standard mathematical sense, examples of this type are actually globally trivial; while the leaves of a (mathematical) codimension-1 foliation are always locally the level sets of a function, they generally cannot be expressed this way globally, as a leaf may pass through a local-trivializing chart infinitely many times, and the holonomy around a leaf may also obstruct the existence of a globally-consistent defining functions for the leaves. For example, while the 3-sphere has a famous codimension-1 foliation discovered by Reeb, a codimension-1 foliation of a closed manifold cannot be given by the level sets of a smooth function, since a smooth function on a closed manifold necessarily has critical points at its maxima and minima.