Fluid Dynamics
Fluid Dynamics is the English version of the leading Russian journal Izvestia RAN, Mekhanika Zhidkosti i Gaza. It publishes original articles in the field of classical fluid and plasma dynamics, biomechanics of continuous media, flow in electro-magnetic fields, dynamics of multiphase and chemically reactive flow, including flow in porous media.
The journal publishes theoretical and experimental investigations. Numerical research should focus on new mechanical results with a short description of the numerical method itself.
The manuscripts are peer reviewed by two experts. In accordance with the "Statute of Scientific Journals of the Russian Academy of Sciences", the Editorial Board has the exclusive right to accept or reject manuscripts. According to the rules of our journal, authors will not be informed of the reasons for rejection. Papers are published free of charge to the authors and no fee is paid to them.
Media registration certificate: ПИ № ФС 77 – 82144 от 02.11.2021
Information about the Fluid Dynamics see also at the websites
Ағымдағы шығарылым
№ 4 (2025)
Articles
HYDROELASTIC WAVES IN A POROUS ICE PLATE
Аннотация
3-16
ENSTROPHY DYNAMICS FOR FLOW PAST A SOLID BODY WITH NO-SLIP BOUNDARY CONDITION
Аннотация
17-29
SEICHE OSCILLATIONS IN LAKE ONEGA
Аннотация
The results of numerical modeling of barotropic seiche oscillations in Lake Onega are presented. The model is based on a linearized system of shallow water equations on a rotating sphere without taking into account the dissipative terms. The spatial approximation of the equations is performed on an irregular triangular grid. The use of a computational grid with high spatial resolution in solving the spectral-difference eigenvalue problem made it possible to obtain a good correspondence between the calculated periods and the measured ones. Spatial distributions of the amplitude and phase of the first seven modes of natural oscillations of the model Lake Onega are constructed with periods of 13 h 20 min, 11 h 30 min, 6 h 30 min, 5 h 14 min, 4 h 38 min, 4 h 24 min and 4 h 10 min. The analysis showed the importance of taking into account the relatively shallow Svyatula bay. If this bay is excluded from the computational domain, the modes with periods of 13 h 20 min and 11 h 30 min are replaced by one mode with an intermediate period of 12 h 30 min.
30-42
ESTIMATE OF POSITION OF LAMINAR-TURBULENT TRANSITION OF SUPERSONIC BOUNDARY LAYER ON A FLAT PLATE WITH STREAMWISE SLOTS
Аннотация
43-49
INFLUENCE OF GEOMETRY AND FUEL INJECTION ON THERMOACOUSTIC INSTABILITIES IN A SUPERSONIC CAVITY
Аннотация
50-65
FLUID DISPLACEMENT FROM A LAYERED RESERVOIR IN THE GRAVITY FIELD
Аннотация
66-81
DIRECT NUMERICAL SIMULATION OF TURBULENCE ONSET IN SUPERSONIC BOUNDARY LAYER OVER A PARABOLIC PROFILE
Аннотация
82-94
NUMERICAL SIMULATION OF SUBSONIC TWISTED JETS OF HIGH-ENTHALPY AIR AT OPERATING PARAMETERS OF THE VGU-4 HF PLASMATRON
Аннотация
95-104
TURBULENT FLOW IN A NARROW CHANNEL WITH A SINGLE-ROW STACK OF INCLINED TRENCH DIMPLES ON ONE WALL
Аннотация
The results of an experimental study of flow aerodynamics in a narrow channel with a rectangular cross-sectional height of H = 20 mm and an aspect ratio of AR = 7.5 are presented. The channel surface contains a system of elongated trench dimples with a cylindrical cross-section. The dimples have a width of D/H = 0.75, a relative depth of Δ/D = 0.22, and a length of L/D = 7 calibers. They are positioned at a fixed angle of φ = 45°, to the longitudinal axis of the channel. The package contained a total of seven dimples, with a constant spacing of h/D = 2. The Reynolds number, calculated from the hydraulic diameter, was constant at Rech = 3.9 · 104 in the experiments measuring velocity components and velocity fluctuations. Hydraulic losses were measured over a wide range of Reynolds numbers, from Rech = 1.9 · 104 to Rech = 1.1 · 105. The experiments measured velocity components and their fluctuations in the longitudinal and transverse directions for a channel with dimples on one wall, and the hydraulic resistance of a channel with dimples on one and two opposite walls. It was found that the longitudinal velocity profiles Uz differ significantly depending on the position within the dimple for all the dimples studied. A boundary layer separation zone forms at the inlet of the dimple, where the flow enters. The extent of this zone along the dimple does not exceed one caliber, and further along the dimple, no negative values of the velocity Uz are observed. As one moves along the dimple, the intensity of the vortex motion of the gas inside significantly weakens. A similar flow structure was previously observed by the authors (Thermophysics and Aeromechanics. 2022. V. 29. No. 6. P. 935) in a single trench dimple with the same geometric parameters.
105-116
MEASUREMENT OF THE RADIATION HEAT FLUX GENERATED BY THE SHOCK WAVE FRONT IN THE DIRECTION OF ITS MOVEMENT
Аннотация
117-124
ADAPTATION OF SHALLOW WATER VORTEX MOTIONS TO CYCLOSTROPHIC BALANCE
Аннотация
125-133
ICE FORMATION PROCESS SIMULATION ON AIRCRAFT HEATED SURFACES
Аннотация
134-148

