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Viscous flows with flat free boundaries. / Pukhnachev, V. V.; Zhuravleva, E. N.
в: European Physical Journal Plus, Том 135, № 7, 554, 01.07.2020.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Viscous flows with flat free boundaries
AU - Pukhnachev, V. V.
AU - Zhuravleva, E. N.
N1 - Publisher Copyright: © 2020, Società Italiana di Fisica and Springer-Verlag GmbH Germany, part of Springer Nature. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.
PY - 2020/7/1
Y1 - 2020/7/1
N2 - Two problems with a free boundary for the Navier–Stokes equations are considered. In the first problem, the fluid occupies a horizontal strip whose lower boundary is a motionless wall and whose upper boundary is a straight-line free boundary parallel to the wall. In the second problem, the fluid motion is rotationally symmetric. Here, the flow domain is a horizontal layer bounded by a solid plane and a parallel flat free surface. In both problems, the vertical velocity and pressure are independent of the longitudinal coordinates. In the first problem, there are three modes of motion: stabilization to a quiescent state with increasing time, blowup of the solution within a finite time, and intermediate self-similar mode in which the layer thickness unlimitedly increases with time. The same situation occurs in the second problem if the solid surface bounding the layer does not move. However, its rotation can prevent the solution collapse.
AB - Two problems with a free boundary for the Navier–Stokes equations are considered. In the first problem, the fluid occupies a horizontal strip whose lower boundary is a motionless wall and whose upper boundary is a straight-line free boundary parallel to the wall. In the second problem, the fluid motion is rotationally symmetric. Here, the flow domain is a horizontal layer bounded by a solid plane and a parallel flat free surface. In both problems, the vertical velocity and pressure are independent of the longitudinal coordinates. In the first problem, there are three modes of motion: stabilization to a quiescent state with increasing time, blowup of the solution within a finite time, and intermediate self-similar mode in which the layer thickness unlimitedly increases with time. The same situation occurs in the second problem if the solid surface bounding the layer does not move. However, its rotation can prevent the solution collapse.
UR - http://www.scopus.com/inward/record.url?scp=85087902175&partnerID=8YFLogxK
U2 - 10.1140/epjp/s13360-020-00552-z
DO - 10.1140/epjp/s13360-020-00552-z
M3 - Article
AN - SCOPUS:85087902175
VL - 135
JO - European Physical Journal Plus
JF - European Physical Journal Plus
SN - 2190-5444
IS - 7
M1 - 554
ER -
ID: 24766799