Ore condition

Ore condition

In mathematics, especially in the area of algebra known as ring theory, the Ore condition is a condition introduced by Øystein Ore, in connection with the question of extending beyond commutative rings the construction of a field of fractions, or more generally localization of a ring. The right Ore condition for a domain R, and any pair a, b of non-zero elements, is the requirement that the sets aR and bR should intersect in more than the element 0. The left Ore condition is defined similarly. A domain that satisfies the right Ore condition is called a right Ore domain.


Contents

Application

Since it is well known that each integral domain is a subring of a field of fractions (via an embedding) in such a way that every element is of the form rs−1 with s nonzero, it is natural to ask if the same construction can take a noncommutative domain and associate a division ring (a noncommutative field) with the same property. It turns out that the answer is sometimes "no", that is, there are domains which do not have an analogous "right division ring of fractions".

For every right Ore domain R, there is a unique (up to natural R-isomorphism) division ring D containing R as a subring such that every element of D is of the form rs−1 for r in R and s nonzero in R. Such a division ring D is called a ring of right fractions of R, and R is called a right order in D. The notion of a ring of left fractions and left order are defined analogously, with elements of D being of the form s−1r.

It is important to remember that the definition of R being a right order in D includes the condition that D must consist entirely of elements of the form rs−1. Any domain satisfying one of the Ore conditions can be considered a subring of a division ring, however this does not automatically mean R is a left order in D, since it is possible D has an element which is not of the form s−1r. Thus it is possible for R to be a right-not-left Ore domain. Intuitively, the condition that all elements of D be of the form rs−1 says that R is a "big" R-submodule of D. In fact the condition ensures RR is an essential submodule of DR. Lastly, there is even an example of a domain in a division ring which satisfies neither Ore condition (see examples below).

Another natural question is: "When is a subring of a division ring right Ore?" One characterization is that a subring R of a division ring D is a right Ore domain if and only if D is a flat left R-module (Lam 2007, Ex. 10.20).

A different, stronger version of the Ore conditions is usually given for the case where R is not a domain, namely that there should be a common multiple

c = au = bv

with u, v not zero divisors. In this case, Ore's theorem guarantees the existence of an over-ring called the (right or left) classical ring of quotients.

Examples

Commutative domains are automatically Ore domains, since for nonzero a and b, ab is nonzero in aRbR. Right Noetherian domains, such as right principal ideal domains, are also known to be right Ore domains. Even more generally, Alfred Goldie proved that a domain R is right Ore if and only if RR has finite uniform dimension. It is also true that right Bézout domains are right Ore.

A subdomain of a division ring which is not right or left Ore: If F is any field, and G = \langle x,y \rangle\, is the free monoid on two symbols x and y, then the monoid ring F[G]\, does not satisfy any Ore condition, but it is a free ideal ring and thus indeed a subring of a division ring, by (Cohn 1995, Cor 4.5.9).

Multiplicative sets

The Ore condition can be generalized to other multiplicative subsets, and is presented in textbook form in (Lam 1999, §10) and (Lam 2007, §10). A subset S of a ring R is called a right denominator set if it satisfies the following three conditions for every a,b in R, and s, t in S:

  1. st in S; (The set S is multiplicatively closed.)
  2. aSsR is not empty; (The set S is right permutable.)
  3. If sa = 0, then there is some u in S with au = 0; (The set S is right reversible.)

If S is a right denominator set, then one can construct the ring of right fractions RS−1 similarly to the commutative case. If S is taken to be the set of regular elements (those elements a in R such that if b in R is nonzero, then ab and ba are nonzero), then the right Ore condition is simply the requirement that S be a right denominator set.

Many properties of commutative localization hold in this more general setting. If S is a right denominator set for a ring R, then the left R-module RS−1 is flat. Furthermore, if M is a right R-module, then the S-torsion, torS(M) = { m in M : ms = 0 for some s in S }, is an R-submodule isomorphic to Tor1(M,RS−1), and the module MR RS−1 is naturally isomorphic to a module MS−1 consisting of "fractions" as in the commutative case.

References

  • Cohn, P.M. (1961), "On the embedding of rings in skew fields", Proc. London Math. Soc. 11: 511–530, doi:10.1112/plms/s3-11.1.511, MR25#100 
  • Cohn, P.M. (1995) Skew fields, Theory of general division rings, Cambridge University Press, ISBN 0-521-43217-0
  • Lam, Tsit-Yuen (1999), Lectures on modules and rings, Graduate Texts in Mathematics No. 189, Berlin, New York: Springer-Verlag, ISBN 978-0-387-98428-5 
  • Lam, Tsit-Yuen (2007), Exercises in modules and rings, Problem Books in Mathematics, Berlin, New York: Springer-Verlag, ISBN 978-0-387-98850-4; 978-0-387-98850-4, MR2278849 
  • Stenström, Bo (1971), Rings and modules of quotients, Lecture Notes in Mathematics, Vol. 237, Berlin: Springer-Verlag, pp. vii+136 

External links


Wikimedia Foundation. 2010.

Игры ⚽ Нужно решить контрольную?

Look at other dictionaries:

  • Ore's theorem — For Ore s theorem in ring theory, see Ore condition. Ore s theorem is a result in graph theory proved in 1960 by Norwegian mathematician Øystein Ore. It gives a sufficient condition for a graph to be Hamiltonian, essentially stating that a graph… …   Wikipedia

  • Ore Kadal — Directed by Shyamaprasad Produced by Vindhayan Written by …   Wikipedia

  • Ore Mountains — For other similarly named ranges, see Ore Mountains (disambiguation). Ore Mountains Erzgebirge Krušné hory Range …   Wikipedia

  • Øystein Ore — Øystein Ore, né et mort à Oslo (7 octobre 1899 13 août 1968), est un mathématicien norvégien. Sommaire 1 Vie 2 Œuvre 3 Livres écrits par Ore 4 Voir aussi …   Wikipédia en Français

  • Øystein Ore — Born October 7, 1899(1899 10 07) Oslo, Norway Died August 13, 1968(1968 08 13) (a …   Wikipedia

  • Kambalda type komatiitic nickel ore deposits — Kambalda type nickel ore deposits are a class of magmatic nickel copper ore deposit in which the physical processes of komatiite volcanology serve to enrich, concentrate and deposit nickel bearing sulfide within the lava flow environment of an… …   Wikipedia

  • Christ Church, Ore — Christ Church The church from the east …   Wikipedia

  • Red-lead ore — Red Red, a. [Compar. {Redder} ( d?r); superl. {Reddest}.] [OE. red, reed, AS. re[ a]d, re[ o]d; akin to OS. r[=o]d, OFries. r[=a]d, D. rood, G. roht, rot, OHG. r[=o]t, Dan. & Sw. r[ o]d, Icel. rau[eth]r, rj[=o][eth]r, Goth. r[ a]uds, W. rhudd,… …   The Collaborative International Dictionary of English

  • Kidney ore — Kidney Kid ney (k[i^]d n[y^]), n.; pl. {Kidneys} (k[i^]d n[i^]z). [OE. kidnei, kidnere, from Icel. koi[eth]r belly, womb (akin to Goth. gipus, AS. cwi[thorn] womb) + OE. nere kidney; akin to D. nier, G. niere, OHG. nioro, Icel. n[=y]ra, Dan. nyre …   The Collaborative International Dictionary of English

  • List of mathematics articles (O) — NOTOC O O minimal theory O Nan group O(n) Obelus Oberwolfach Prize Object of the mind Object theory Oblate spheroid Oblate spheroidal coordinates Oblique projection Oblique reflection Observability Observability Gramian Observable subgroup… …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”