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Session 4, Unit 7 Plume Rise

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The wind speed u is adjusted to the stack height. For non-neutral conditions ... Gifford-Slade method (total dispersion parameters) Huber-Snyder method ... – PowerPoint PPT presentation

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Title: Session 4, Unit 7 Plume Rise


1
Session 4, Unit 7Plume Rise
2
Qualitative Descriptions
  • Plume rise ?h
  • Hhs ?h
  • Driving forces
  • Buoyancy
  • Momentum
  • Different phases
  • Initial phase
  • Thermal phase
  • Breakup phase
  • Diffusion phase

3
Qualitative Descriptions
  • Influencing factors
  • When there is no downwash
  • Exit velocity
  • Stack diameter
  • Stack gas temperature
  • Ambient temperature
  • Wind speed
  • Atmospheric stability
  • Wind shear
  • Downwash

4
Holland Plume Rise Formula
  • Simple
  • More suitable for power plant
  • For neutral conditions
  • The wind speed u is adjusted to the stack height.
  • For non-neutral conditions

5
Briggs Plume Rise Formulas
  • More complicated
  • Buoyancy flux parameter
  • Momentum flux parameter

6
Briggs Plume Rise Formulas
  • Determination of buoyancy dominated or momentum
    dominated plumes
  • Calculate (?T)c
  • For unstable or neutral (A-D)
  • For Fb lt55
  • For Fb?55
  • For stable (E,F)
  • If ?T (Ts-Ta) ? (?T)c , its buoyancy dominated
  • If ?T (Ts-Ta) lt (?T)c , its momentum dominated

7
Briggs Plume Rise Formulas
  • For buoyancy dominated plume under unstable or
    neutral conditions (A-D)
  • x distance at which atmospheric turbulence
    begins to dominate entrainment
  • For Fb?55 m4/sec3, x34 Fb2/5
  • For Fblt55 m4/sec3, x14 Fb5/8
  • xfdistance to the final rise, m
  • xf3.5x
  • Final plume rise

8
Briggs Plume Rise Formulas
  • For buoyancy dominated plume under stable
    conditions (E and F)
  • Stability parameter, s
  • Default values for
  • 0.02 K/m for E stability
  • 0.035 K/m for F stability

9
Briggs Plume Rise Formulas
  • Final plume rise
  • Distance to final rise

10
Briggs Plume Rise Formulas
  • For momentum dominated plume under unstable or
    neutral conditions (A-D)
  • For momentum dominated plume under stable
    conditions (E,F)
  • Calculate both and use the lower one.

11
Briggs Plume Rise Formulas
  • Gradual rise
  • Distance lt distance to final rise (i.e., xltxf)
    and Buoyancy dominated plume

12
Briggs Plume Rise Formulas
  • Distance lt distance to final rise (i.e., xltxf)
    and momentum dominated plume
  • Jet entrainment coefficient
  • Unstable conditions (A-D)

13
Briggs Plume Rise Formulas
  • Xdownwind distance with max value of
  • Xmax49Fb5/8 for 0ltFblt55 m4/sec3
  • xmax119Fb2/5 for Fbgt 55 m4/sec3
  • Stable conditions (E,F)
  • with

14
Briggs Plume Rise Summary
15
Buoyancy Induced Dispersion
  • Air entrainment due to boiling-like action
    enlarges the plume
  • Small impact on ground level concentration in
    most cases
  • The impact can be reflected in ?
  • Initial plume size
  • Effective dispersion coefficients

16
Session 4, Unit 8Averaging Time, Multiple
Sources, and Receptors
  • Chimney, Building, and Terrain Effects

17
Averaging Time
  • The concentration calculated from the Gaussian
    equations should represent the averaging time
    that is consistent with the averaging time of ?
  • Short-term ? 1 month
  • Long-term gt 1 month

18
Averaging Time
  • If longer averaging time is desired, use the
    following power law
  • P0.17-0.75, suggested value is 0.17

19
Crosswind Averaging
  • Integrate y from -? to ?
  • Average over a sector

20
Crosswind Averaging
  • Average over a sector considering distribution of
    wind speeds and stability classes
  • ISCLT3 and STAR

21
Crosswind Averaging
  • Smoothing transition from sector to sector
  • Weighted smoothing function, WS
  • Smoothed average concentration

22
Multiple Sources
  • The max from each source do not exactly overlap
  • Use of multiple stack factor
  • More accurate method modeling with a consistent
    coordinate system

23
Receptors
  • Receptor grid
  • Cartesian coordinate system
  • Polar coordinate system
  • Single stack, but the origin of the coordinate
    system is not at the stack base
  • Multiple stacks
  • Presentation of results
  • Concentration isopleths

24
Example Calculation
  • Chapter 10

25
Chimney Effects
  • Stack tip downwash
  • Low pressure behind stack
  • u is at the stack top level
  • No plume rise (plume sink)
  • Avoid stack tip downwash

26
Building Effects
  • General description
  • Expanded meaning of building
  • Reduce building effects rule of thumb
  • hsgt2.5hb
  • Too conservative for tall thin buildings

27
Briggs Procedure to Minimize Downwash
  • Five steps
  • Correction for stack induced downwash
  • Correction for building effects
  • Determine if plume is entrained in the cavity.
    If entrained, treat it as a ground level source
  • Buoyancy effect
  • Calculate downwind concentration

28
Cavity
  • Description
  • Cavity length
  • Short buildings (L/H?2)
  • L affects cavity length xr
  • Long buildings (L/Hgt2)
  • L does not affect cavity length xr

29
Cavity
  • Max cavity width
  • Its location long x direction
  • Max height

30
Cavity
  • Concentrations within cavity

31
Wake Downwind of Cavity
  • Treated as a ground level source
  • Turner method (virtual source)
  • Gifford method
  • Gifford-Slade method (total dispersion
    parameters)
  • Huber-Snyder method

32
Sources Downwind of Buildings
  • Briggs method
  • Beyond 3?b ? no building effect
  • Within 3?b ? treat them as ground level sources

33
Complex Terrain
  • Definition
  • Simple terrain
  • Complex terrain
  • Intermediate terrain
  • Plume behavior in complex terrain

34
Complex Terrain
  • Modeling approaches
  • Briggs
  • Egan
  • Bowne
  • Modified dispersion coefficients
  • ISC3 (COMPLEX 1) to be discussed later

35
GEP Stack Height
  • Definition
  • Greater of
  • 65 m
  • HGH1.5L (for stacks in existance on Jan 12,
    1979, HG2.5H)
  • Structures to be considered within 5L
  • In modeling analyses, no credit is given for
    stack height above the GEP
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