Abstract
There is abundant experimental, theoretical and computational evidence
that
certain constrained turbulent fluid systems self-organize into large-scale
structures.
Examples include two-dimensional (geostrophic) fluids, guiding-centre plasmas
and
pure-electron plasmas, as well as two- and three-dimensional magnetofluids
such as
reversed-field pinches and spheromaks. The theoretical understanding of
relaxation
phenomena is divided into two quite different constructs: selective decay
and
maximal entropy. Theoretical foundations of both of these principles are
largely due
to Montgomery and his collaborators. In this paper, selective decay and
maximal
entropy theories of turbulent relaxation of fluids are reviewed and experimental
evidence is presented. Experimental evidence from both 2D fluids and from
3D
magnetofluids is consistent with the selective decay hypothesis. However,
high-resolution computational evidence strongly suggests that formation
of
large-scale
structures is dictated by maximal-entropy principles rather than selective
decay.
Publisher
Cambridge University Press (CUP)
Cited by
22 articles.
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