Weak and Strong Solutions of the 3D Navier–Stokes Equations and Their Relation to a Chessboard of Convergent Inverse Length Scales
Using the scale invariance of the Navier–Stokes equations to define appropriate space-and-time-averaged inverse length scales associated with weak solutions of the 3 D Navier–Stokes equations, on a periodic domain V = [ 0 , L ] 3 an infinite ‘chessboard’ of estimates for these inverse length scales...
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Veröffentlicht in: | Journal of nonlinear science 2019-02, Vol.29 (1), p.215-228 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Using the scale invariance of the Navier–Stokes equations to define appropriate space-and-time-averaged inverse length scales associated with weak solutions of the 3
D
Navier–Stokes equations, on a periodic domain
V
=
[
0
,
L
]
3
an infinite ‘chessboard’ of estimates for these inverse length scales is displayed in terms of labels
(
n
,
m
)
corresponding to
n
derivatives of the velocity field in
L
2
m
(
V
)
. The
(
1
,
1
)
position corresponds to the inverse Kolmogorov length
R
e
3
/
4
. These estimates ultimately converge to a finite limit,
R
e
3
, as
n
,
m
→
∞
, although this limit is too large to lie within the physical validity of the equations for realistically large Reynolds numbers. Moreover, all the known time-averaged estimates for weak solutions can be rolled into one single estimate, labelled by
(
n
,
m
)
. In contrast, those required for strong solutions to exist can be written in another single estimate, also labelled by
(
n
,
m
)
, the only difference being a factor of 2 in the exponent. This appears to be a generalization of the Prodi–Serrin conditions for
n
≥
1
. |
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ISSN: | 0938-8974 1432-1467 |
DOI: | 10.1007/s00332-018-9484-8 |