FACTOID # 113: In Denmark, more than 50% of the tax collected is personal income tax. In the Netherlands, personal income tax makes up less than 15%.
 
 Home   Encyclopedia   Statistics   Countries A-Z   Flags   Maps   Education   Forum   FAQ   About 
 
WHAT'S NEW
RECENT ARTICLES
More Recent Articles »
 

FACTS & STATISTICS    Simple view

  1. Select countries to view: (hold down Control key and click to select several)

     

     

    Compare:

     

     

  1. Select fact or statistic: (* = graphable)

     

     

     

  2. (OPTIONAL) Compare to statistic: (both need to be graphable)

     

     

     

  3. View result as:

     

       
(OR) SEARCH ALL encyclopedia, stats & forums:   

Encyclopedia > Free magma

In abstract algebra, a magma (also called a groupoid) is a particularly basic kind of algebraic structure. Specifically, a magma consists of a set M equipped with a single binary operation M × MM. A binary operation is closed by definition, but no other axioms are imposed on the operation.


The term magma for this kind of structure was introduced by Bourbaki; however, the term groupoid is a very common alternative. Unfortunately, the term groupoid also refers to an entirely different kind of algebraic concept described at Groupoid.

Contents

Types of magmas

Magmas are not often studied as such; instead there are several different kinds of magmas, depending on what axioms one might require of the operation. Commonly studied types of magmas include

Free magma

A free magma on a set X is the "most general possible" magma generated by the set X (that is there are no relations or axioms imposed on the generators; see free object). It can be described, in terms familiar in computer science, as the magma of full binary trees with leaves labelled by elements of X. The operation is that of joining trees at the root. It therefore has a foundational role in syntax.


See also: free semigroup, free group.


More definitions

A magma (S, *) is called

  • medial if it satisfies the identity xy * uz = xu * yz (i.e. (x * y) * (u * z) = (x * u) * (y * z) for all x, y, u, z in S),
  • left semimedial if it satisfies the identity xx * yz = xy * xz,
  • right semimedial if it satisfies the identity yz * xx = yx * zx,
  • semimedial if it is both left and right semimedial,
  • left distributive if it satisfies the identity x * yz = xy * xz,
  • right distributive if it satisfies the identity yz * x = yx * zx,
  • autodistributive if it is both left and right distributive,
  • commutative if it satisfies the identity xy = yx,
  • idempotent if it satisfies the identity xx = x,
  • unipotent if it satisfies the identity xx = yy,
  • zeropotent if it satisfies the identity xx * y = yy * x = xx,
  • alternative if it satisfies the identities xx * y = x * xy and x * yy = xy * y,
  • power-associative if the submagma generated by any element is associative,
  • a semigroup if it satisfies the identity x * yz = xy * z (associativity),
  • a semigroup with left zeros if it satisfies the identity x = xy,
  • a semigroup with right zeros if it satisfies the identity x = yx,
  • a semigroup with zero multiplication if it satisfies the identity xy = uv,
  • a left unar if it satisfies the identity xy = xz,
  • a right unar if it satisfies the identity yx = zx,
  • trimedial if any triple of its (not necessarily distinct) elements generates a medial submagma,
  • entropic if it is a homomorphic image of a medial cancellation magma.

See also

External links

  • Jezek page (http://adela.karlin.mff.cuni.cz/~jezek/)
  • Definition list (http://adela.karlin.mff.cuni.cz/~jezek/medial/16.jpg) J.Jezek and T.Kepka: Medial groupoids Rozpravy CSAV, Rada mat. a prir. ved 93/2 (1983), 93 pp
  • Definition list (http://adela.karlin.mff.cuni.cz/~jezek/medial/17.jpg) but old groupoid for magma
  • medial groupoid (http://www.math.usf.edu/~eclark/algctlg/medial_gpds.html) groupoid = magma
  • A Catalogue of Algebraic Systems / John Pedersen  (http://www.math.usf.edu/~eclark/algctlg/) no broken links
  • Mathematical Structures: medial groupoids (http://math.chapman.edu/cgi-bin/structures.pl?Medial_groupoids) groupoid = magma
  • operations (http://ocean.ucc.ie/~cjvdb1/html/binops.shtml)
  • mathworld: Groupoid (http://mathworld.wolfram.com/Groupoid.html)

  Results from FactBites:
 
Magma (algebra) - Wikipedia, the free encyclopedia (606 words)
The term magma for this kind of structure was introduced by Bourbaki; however, the term groupoid is a very common alternative.
Magmas are not often studied as such; instead there are several different kinds of magmas, depending on what axioms one might require of the operation.
A free magma on a set X is the "most general possible" magma generated by the set X (that is there are no relations or axioms imposed on the generators; see free object).
Free object - Wikipedia, the free encyclopedia (446 words)
These are rather simpler than free groups: the free monoid on a set X, is the monoid of all finite strings using X as alphabet, with operation concatenation of strings.
As that example suggests, free objects look like constructions from syntax; and we can reverse that to some extent by saying that major uses of syntax can be explained and characterised as free objects, in a way that makes apparently heavy 'punctuation' explicable (and more memorable).
Free objects are created by a left adjoint G to F: for a set X the free object on X as 'generators' is G(X).
  More results at FactBites »


 

COMMENTARY     


Share your thoughts, questions and commentary here
Your name
Your comments
Please enter the 5-letter protection code

Want to know more?
Search encyclopedia, statistics and forums:

 


Lesson Plans | Student Area | Student FAQ | Reviews | Press Releases |  Feeds | Contact
The Wikipedia article included on this page is licensed under the GFDL.
Images may be subject to relevant owners' copyright.
All other elements are (c) copyright NationMaster.com 2003-5. All Rights Reserved.
Usage implies agreement with terms.