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Turbulence Measurements in: Natural Convection Boundary Layer Swirling Jet by Abolfazl Shiri Thesis Supervisor William K. George Turbulence Measurements in: Swirling ... – PowerPoint PPT presentation

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Title: Turbulence Measurements in:


1
Turbulence Measurements in
Natural Convection Boundary Layer
Swirling Jet
by Abolfazl Shiri Thesis Supervisor William K.
George
2
Turbulence Measurements in
Natural Convection Boundary Layer
Swirling Jet
  • Why we did these two experiments?
  • They were both turbulent flows and we aimed to
    measure the turbulence parameters.
  • There is a lack of reliable experimental data in
    both flows.
  • The velocity measurement method in both
    experiments was laser Doppler anemometry.
  • Both have axisymmetric nature which simplifies
    the three-dimensionality of the flow.
  • Doing a related experimental study while
    designing and installing the other experimental
    facility.

3
Swirling Jet Experiment
  • What is a jet flow?

Jet flow represent a class of free shear flows
that evolve in the absence of walls.
Free Shear Flows
Jets
Wakes
Shear Layer Flows
Plumes
4
Anatomy of the Jet Flow
  • Regions
  • Potential core ( X/D 1 )
  • Mixing layer
  • Developing flow ( X/D 20 )
  • Self-preserving flow
  • Characteristic velocity scale Uc(x)
  • Characteristic jet width d1/2(x)

Asymptotic behaviour of flow at self-preserving
region
5
Entrainment
Jet mass flow
  • Self-preserved region
  • When the mass entrained by the
  • turbulence overwhelms the
  • added mass at the source of jet.
  • Main application of jet flows in industry for
    mixing due to entrainment.
  • Laboratory jets cant be categorized as
    universal self-similar, point-source of momentum
    jets.
  • Virtual origin (x0) and jet growth rate (dd/dx)
    are the parameters characterizing the initial
    condition.
  • Azimuthal velocity component (swirl) modifies
    the initial condition.

6
Swirling Jet Flow
  • Two cases of low and moderate swirl (S 0.15
    0.25) were compared with a non-swirling jet.
  • Geometry of the nozzle and the velocity profile
    at the nozzle changes the initial condition.
  • How the additional swirl effects the nozzle
    velocity profile?

Not a top-hat anymore!
7
Jet Facility
  • 1 inch jet nozzle diameter
  • Six injectors for tangential flow derived by
    different blower
  • 3.5m X 3.5m X 10m enclosure
  • Solid-body rotation for tangential velocity
    distribution
  • Reynolds number at nozzle 40,000
  • Same facility which used in Hussein, Capp
    George 1994 for axisymmetric jets study.
  • Brought from university of Buffalo by George and
    modified to add the swirl components.

8
Summary of the Swirling Jet Experiment
  • The far swirling jet is self-similar (like the
    non-swirling jet).
  • For S lt 0.2, the effect of initial swirl is
    negligible.
  • There is no considerable effect of swirl on
    growth rate, consistent with the theory.
  • The change in the virtual origin of these jets
    are slight (consistent with the relatively low
    swirl number)
  • The role of each term (production, advection,
    diffusion and dissipation) is similar in both
    swirling and non-swirling jet.

9
Natural Convection Experiment
Conduction
Very Slow Process
Forced Convection
Convection
Heat Transfer Modes

Natural Convection
No need for a medium to tranfer the heat
  • Natural convection flows are among the least
    well undersood.
  • Although they are the most commonly occuring
    method of convective heat transfer, there is a
    lack of controlled and reliable experimental
    studies because of the difficulties.

Radiation
10
Natural Convection Applications
Natural-draft cooling tower
Reactor heat exchanger
Radiator
Heat-sink
11
Some Definitions
For vertical surface, transition to turbulence at
RaL ? 109
For a wall at T70 C in air, transition starts at
L ? 0.6 m
12
Theory of the NCBL
  • Turbulent natural convection boundary layer flow
    next to a cylindrical surface
  • Axisymmetric flow homogeneous in tangential
    direction.
  • Newtonian, Incompressible flow.
  • Temperature gradient in the flow cause the
    density, viscosity and other thermodynamics
    properties variation.
  • Buoyancy as the source of momentum.

To simplify the momentum and energy equations of
the flow
Inner layer ? Viscous and conduction terms are
dominating Outer layer ? Viscous and conduction
terms are negligible
B.L. equation separation
? For an acceptable seperation between the scales
we need a really big Grashof number flow...
This was primary reason for the large experimetal
facility at Chalmers.
13
Experimental Rig
  • Previous experiments
  • Most of the experiments were carried out next to
    a vertical flat plate Tsuji Nagano (1988)
  • Measurements on vertical cylinder by Persson
    Karlsson (1996) were problematic
  • Low Grashof number
  • Boundary conditions were not controlled.

New experimental facility was built to modify
the rig used by Persson Karlsson
14
Experimental Rig Schematic
15
Measurement Methods
Laser Doppler Anemometry (LDA)
Velocity measurement
Thermocouple
mean temperature
Temperature measurement
Cold-wire thermometry
instantaneous temperature
16
Temperature Measurement Errors
  • Prongs temperature gradient.
  • Wall temperature measurement errors.
  • Calibration uncertainities.
  • Temperature measurement errors in very low
    velocity fluids.

17
Summary of the NCBL Experiment
  • The experiments were carried out in three
    different heights 1.5m, 3m and 4m corresponding
    to the Rayleigh numbers Ra 1.0 1010 , 7
    1010 and 1.7 1011 respectively.
  • Simultaneous two components velocity and
    temperature measured across boundary layer in
    turbulent region.
  • Temperature measurement methods were not
    suitable for this flow, but lack of any other
    alternative method with the necessary accuracy
    forced us to use them, considering the short
    comings.
  • A comprehensive theoritical foundation was
    established for future investigations.

18
In Memory of
  • Professor Rolf Karlsson
  • (1945 2005)
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