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Flat convergence : ウィキペディア英語版 | Flat convergence In mathematics, flat convergence is a notion for convergence of submanifolds of Euclidean space. It was first introduced by Hassler Whitney in 1957, and then extended to "integral currents" by Federer and Fleming in 1960. It forms a fundamental part of the field of geometric measure theory. The notion was applied to find solutions to Plateau's problem. In 2001 the notion of an integral current was extended to arbitrary metric spaces by Ambrosio and Kirchheim. ==Integral currents== A ''k''-dimensional current ''T'' is a multilinear real-valued operator on smooth ''k''-forms. For example, given a Lipschitz map from a manifold into Euclidean space, ''F'': ''N''''k'' → R''N'', one has an integral current ''T''(''ω'') defined by integrating the pullback of the differential ''k''-form, ''ω'', over ''N''. Currents have a notion of boundary (which is the usual boundary when ''N'' is a manifold with boundary) and a notion of mass, ''M''(''T''), (which is the volume of the image of ''N''). An integer rectifiable current is defined as a countable sum of currents formed in this respect. An integral current is an integer rectifiable current whose boundary has finite mass. It is a deep theorem of Federer-Fleming that the boundary is then also an integral current.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Flat convergence」の詳細全文を読む
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