In General > s.a. chaos.
* Idea: An eddy-like state of fluid motion where the inertial-vortex
forces of the eddies are larger than any of the other forces that tend to damp
the
eddies out.
* History: The first
serious study began with Reynolds, who proposed that its onset is due to instabilities
in the laminar flow, that can be characterized
(in a classical fluid) by the Reynolds number; This is now thought to be too
simplistic; Reaching the critical value for R is only a sufficient
condition, and there are some flows that do not have a critical Reynolds number;
Very
little is understood from first principles.
* Goal: There is no consensus
even on what finding a solution to the problem means; According to engineers,
finding mean velocity profiles, wall
stresses,
and p gradients (use statistical theory, from O Reynolds on); For
physicists,
understanding the non-linear processes and the details of motions
at various
scales.
* Basic concepts: Randomness, eddy viscosity, cascade, scaling.
* And chaos: The approach
to turbulence has been shown to be chaotic for certain systems, following the
predictions of Ruelle & Takens (1971),
and contrary to the Landau-Hopf theory; Turbulent flow itself is thought to
be chaotic, but this cannot be experimentally tested.
* Characteristics: Apparently
random local eddies and whirlpools; Diffusion; Dissipation.
* Motivation: Lots of energy spent in overcoming the drag caused by
turbulence.
Reynolds Number
* Idea: A dimensionless
parameter that measures non-linearity in the Navier-Stokes equation and characterizes
the conditions for laminar flow or turbulence
in terms
of speed of flow, density, viscosity and diameter of the pipe; The
number of active degrees of freedom in turbulent flow is about R 9/4 per L3.
$ Def: The number R := UL/
mol =
(typical flow velocity) (typical length scale) / (kinematic molecular viscosity).
* Values: For small R,
the flow is laminar; As R increases,
instabilities set in; For large R, there is full turbulence (in real
life,
mol is
usually of the order of 10–2–10–1 cm2/sec).
@ References: Reynolds PTRS(1895),
reprint PRS(95).
Related Topics > s.a. magnetism [megnetohydrodynamic
turbulence]; sound [analog
metric viewpoint]; Transport.
* Superfluid turbulence: Shows quantized vortices (& Onsager,
Feynman).
* Magnus effect: A turbulence
and viscosity effect; For a moving ball, a region of turbulence develops downstream;
If the ball spins, the region is
asymmetric, more on the side of the trailing edge, and exerts a force on
the ball in the same direction as the Bernoulli effect; Applications:
Golf balls, it explains why dimples are effective.
@ Superfluid turbulence: Donnelly SA(88)nov; > s.a. Superfluids.
@ Magnus effect: Nathan AJP(08)feb [and flight of baseball].
@ Applications: Leung & Gibson ap/03/CJOL
[in geophysics and astrophysics]; Ghosh et al PRS(05)
[enhancing particle coalescence].
@ Quantum fluids: Fisher & Pickett pw(06)apr;
Vinen & Donnelly PT(07)apr.
@ Other topics: Ruelle 95 [and chaos]; Gurarie ht/95 [and
statistical physics, field theory]; Canuto & Dubovikov IJMPA(97)
[new approach]; Gotoh & Nakano JSP(03)
[role of p]; Galanti & Tsinober
PLA(04)
[ergodicity]; Choi et al mp/04 [wave
turbulence, rev]; Leubner et al ap/06/AiG
[astrophysical plasma fluctuations,
non-extensive entropy]; Lück et al PLA(06)
[coherence length].
References
@ Historical: Reynolds PTRS(1883); Darrigol HSPBS(02) [XIX century];
Eyink & Sreenivasan RMP(06) [Onsager].
@ Intros, reviews: Deissler RMP(84);
Dwoyer et al ed-85; Frisch & Orszag PT(90)jan;
Kadanoff PT(95)sep; L'vov & Procaccia
PW(96); Gawedzki cd/96 [intro];
Gibson AMR(96)ap/99 [review];
Nelkin AJP(00)RL;
Bernard cm/00-ln;
Tabeling PRP(02)
[2D]; Barenghi pw(04)dec;
Falkovich & Sreenivasan PT(06)apr
[universal properties].
@ Texts: Mathieu & Scott 00; Davidson 04 [r PT(05)oct].
@ Scaling: Gawedzki ht/97;
Falkovich et al RMP(01);
Carbone et al RNC(04);
Bershadskii JSP(07)
[finite-size corrections]; Flandoli et al CMP(08).
@ Systems: Naulin et al PLA(04) [plasma, statistical]; Zakharov et al
PRP(04) [1D waves].
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Send feedback and suggestions to bombelli at olemiss.edu – Modified
13 jun 2008