Javascript must be enabled to continue!
A Complex-Lamellar Description Of Boundary Layer Transition
View through CrossRef
Flow transition is important, in both practical and phenomenological terms. However, there is currently no method for identifying the spatial locations associated with transition, such as the start and end of intermittency. The concept of flow stability and experimental correlations have been used, however, flow stability only identifies the location where disturbances begin to grow in the laminar flow and experimental correlations can only give approximations as measuring the start and end of intermittency is diffcult. Therefore, the focus of this work is to construct a method to identify the start and end of intermittency, for a natural boundary layer transition and a separated flow transition. We obtain these locations by deriving a complex-lamellar description of the velocity field that exists between a fully laminar and fully turbulent boundary condition. Mathematically, this complex-lamellar decomposition, which is constructed from the classical Darwin-Lighthill-Hawthorne drift function and the transport of enstrophy, describes the flow that exists between the fully laminar Pohlhausen equations and Prandtl's fully turbulent one seventh power law. We approximate the difference in enstrophy density between the boundary conditions using a power series. The slope of the power series is scaled by using the shape of the universal intermittency distribution within the intermittency region. We solve the complex-lamellar decomposition of the velocity field along with the slope of the difference in enstrophy density function to determine the location of the laminar and turbulent boundary conditions. Then from the difference in enstrophy density function we calculate the start and end of intermittency. We perform this calculation on a natural boundary layer transition over a flat plate for zero pressure gradient flow and for separated shear flow over a separation bubble. We compare these results to existing experimental results and verify the accuracy of our transition model.
Title: A Complex-Lamellar Description Of Boundary Layer Transition
Description:
Flow transition is important, in both practical and phenomenological terms.
However, there is currently no method for identifying the spatial locations associated with transition, such as the start and end of intermittency.
The concept of flow stability and experimental correlations have been used, however, flow stability only identifies the location where disturbances begin to grow in the laminar flow and experimental correlations can only give approximations as measuring the start and end of intermittency is diffcult.
Therefore, the focus of this work is to construct a method to identify the start and end of intermittency, for a natural boundary layer transition and a separated flow transition.
We obtain these locations by deriving a complex-lamellar description of the velocity field that exists between a fully laminar and fully turbulent boundary condition.
Mathematically, this complex-lamellar decomposition, which is constructed from the classical Darwin-Lighthill-Hawthorne drift function and the transport of enstrophy, describes the flow that exists between the fully laminar Pohlhausen equations and Prandtl's fully turbulent one seventh power law.
We approximate the difference in enstrophy density between the boundary conditions using a power series.
The slope of the power series is scaled by using the shape of the universal intermittency distribution within the intermittency region.
We solve the complex-lamellar decomposition of the velocity field along with the slope of the difference in enstrophy density function to determine the location of the laminar and turbulent boundary conditions.
Then from the difference in enstrophy density function we calculate the start and end of intermittency.
We perform this calculation on a natural boundary layer transition over a flat plate for zero pressure gradient flow and for separated shear flow over a separation bubble.
We compare these results to existing experimental results and verify the accuracy of our transition model.
Related Results
The vertical distribution of PM2.5 and boundary-layer structure during winter haze in Nanjing
The vertical distribution of PM2.5 and boundary-layer structure during winter haze in Nanjing
<p>At the end of November 2018, a heavy air pollution event was recorded by many meteorological stations in the Yangtze River Delta (YRD), China. The local PM2.5 conc...
A Complex-Lamellar Description Of Boundary Layer Transition
A Complex-Lamellar Description Of Boundary Layer Transition
Flow transition is important, in both practical and phenomenological terms. However, there is currently no method for identifying the spatial locations associated with transition, ...
Getting Nosy: Olfactory Rosette Morphology and Lamellar Microstructure of Two Chondrichthyan Species
Getting Nosy: Olfactory Rosette Morphology and Lamellar Microstructure of Two Chondrichthyan Species
Synopsis
To smell, fish rely on passive water flow into their olfactory chambers and through their olfactory rosettes to detect chemical signals in their aquatic env...
Lamellar Structure in Melted-Slowly Cooled Vinylidene Fluoride/Trifluoroethylene (86/14) mol% Copolymer
Lamellar Structure in Melted-Slowly Cooled Vinylidene Fluoride/Trifluoroethylene (86/14) mol% Copolymer
Lamellar structure, and its thermally induced changes in melted-slowly cooled vinylidene fluoride/trifluoroethylene (86/14) mol% copolymer were studied by scanning electron microsc...
Fertility Transition Across Major Sub-Saharan African Cities: The Role of Proximate Determinants
Fertility Transition Across Major Sub-Saharan African Cities: The Role of Proximate Determinants
Abstract
Background
Sub-Saharan Africa’s fertility transition has lagged behind other regions despite rapid urbanization, resulting in persistently high fertility rates. S...
Penetrative convection in Nocturnal ABL: Numerical Simulations
Penetrative convection in Nocturnal ABL: Numerical Simulations
<p>After the sunset, under calm and clear sky conditions, aerosol laden surface air-layer, cools rapidly due to radiative cooling<sup>[1, 2, & 3...
Large-eddy simulation and parametrization of turbulence decay in atmospheric boundary layer
Large-eddy simulation and parametrization of turbulence decay in atmospheric boundary layer
<p>Various types of one-dimensional RANS (Reynolds-Averaged Navier-Stokes) parametrizations are widely used in modern weather and climate models for replicating atmos...
Exploring the biomineral morphology of crossed-lamellar bivalve shells as a water temperature proxy
Exploring the biomineral morphology of crossed-lamellar bivalve shells as a water temperature proxy
<p>Bivalve shells serve as excellent high-resolution archives of marine paleoclimate. Recently, ultrastructural features of the shells were investigated as potential ...

