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Title: Lecture of : the Reynolds equations of turbulent motions


1
Lecture of the Reynolds equations of turbulent
motions
JORDANIAN GERMAN WINTER ACCADMEY
Prepared by Eng. Mohammad Hamasha Jordan
University of Science Technology
2
  • Most of the research on turbulent flow analysis
    is the
  • past century has used the concept of time
    averaging.
  • Applying time averaging to the basic equations
    of
  • motion yield Reynolds equations.
  • Reynolds equations involve both mean and
  • fluctuating quantities.
  • Reynolds equations attempt to model fluctuating
  • terms by relating them to the mean properties
    or
  • gradients.
  • Reynolds equations form the basis of the most
  • engineering analyses of turbulent flow.

3
  • assume
  • Fluid is in a randomly unsteady turbulent state.
  • Worked with the time-averaged or mean equations
  • of motion.
  • So any variable is resolve into mean value
    plus
  • fluctuating value

  • Where T is large compared to relevant period of
  • fluctuation.

4
  • Itself may vary slowly with time as the
  • following figure

fig 1
5
  • Lets assume the turbulent flow is incompressible
    flow with constant transport properties with
    significant fluctuations in velocity, pressure
    and temperature.
  • The variables will be formed as following

equ.. 1
  • From the basic integral Equation

6
  • incompressible continuity equation

equ...2
  • Substitute in u, v, w from equ 1 and take the
    time average of entire equation

equ .3
  • This is Reynolds-averaged basic differential
    equation for turbulent mean
  • continuity.
  • Subtract equ 3 from equ 2 but do not take time
    average, this gives

equ4
7
  • equations 3 and 4 does not valid for fluid with
    density fluctuating
  • ( compressible fluid ).
  • Now use non linear Navier-Stokes equation

equ5
  • Convective- acceleration term

equ.6
8
  • substitute equ 2 in to equ 5

equ..7
  • the momentum equation is complicated by new term
    involving
  • the turbulent inertia tensor .
  • This new term is never negligible in any
    turbulent flow and is the
  • source of our analytic difficulties.
  • time-averaging procedure has introduced nine new
    variables (the tensor components) which can
    be defined only through (unavailable) knowledge
    of the detailed turbulent structure.

9
  • The components of are related not only
    to fluid physical
  • properties but also to local flow conditions
    (velocity,
  • geometry, surface roughness, and upstream
    history).
  • there is no further physical laws are available
    to resolve this
  • dilemma.
  • Some empirical approaches have been quite
    successful,
  • though rather thinly formulated from
    nonrigorous postulates.

10
  • A slight amount of illumination is thrown upon
    Eq. 7 if it is
  • rearranged to display the turbulent inertia
    terms as if they
  • were stresses, which of course they are not.
    Thus we write

equ..8
  • This is Reynolds-averaged basic differential
    equation for turbulent mean
  • momentum.

equ..9
Turbulent
Laminar
  • mathematically, then, the turbulent inertia terms
    behave as if the
  • total stress on the system were composed of
    the Newtonian
  • Viscous Stresses plus an additional or
    apparent turbulent-
  • stress tensor .
  • is called turbulent shear.

11
  • Now consider the energy equation (first law of
    thermodynamics)
  • for incompressible flow with constant
    properties

equ..10
  • Taking the time average, we obtain the
    mean-energy equation

equ..11
  • This is Reynolds-averaged basic differential
    equation for turbulent mean
  • thermal energy.

equ..12
equ..13
Turbulent
Laminar
12
  • By analogy with our rearrangement of the momentum
    equation, we
  • have collected conduction and turbulent
    convection terms into a
  • sort of total-heat-flux vector qi which
    includes molecular flux plus
  • the turbulent flux .
  • The total-dissipation term is obviously
    complex in the general
  • case. In two-dimensional turbulent-boundary-la
    yer flow (the most
  • common situation), the dissipation reduces
    approximately to

equ..14
  • Reynolds equations can not be achieve without
    additional relation or
  • empirical modeling ideas

13
The Turbulence Kinetic-Energy Equations
14
  • Many attempts have been made to add "turbulence
    conservation
  • relations to the time-averaged continuity,
    momentum, and energy
  • equations.
  • the most obvious single addition would be a
    relation for the
  • turbulence kinetic energy K of the
    fluctuations, defined by

equ.15
15
  • A conservation relation for K can be derived by
    forming the mechanical energy
  • equation, i.e., the clot product of u and the
    ith momentum equation. then, we
  • subtract the instantaneous mechanical energy
    equation from its time-averaged
  • value. The result is the turbulence
    kinetic-energy relation for an incompressible
  • fluid

equ.16
16

17
The Reynolds stress equation
18
II
III
I
IV
V
19
  • Here the roman numerals denote (I) rate of change
    of Reynolds stress,
  • (II) generation of stress, (III) dissipation,
    (IV) pressure strain effects,
  • and (V) diffusion of Reynolds stress.

20
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