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TEMPERATURE LAPSE RATE THE STANDARD ATMOSPHERE

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For 45, the (sin )-1 correction becomes increasingly inaccurate. ... virtual source below the ground at (x0, y0, -z0) that is the mirror image of the ... – PowerPoint PPT presentation

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Title: TEMPERATURE LAPSE RATE THE STANDARD ATMOSPHERE


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PLUME RISE
  • H h ??h
  • h physical stack height, ?
  • ?h plume rise due to thermal buoyancy and
    momentum
  • Correlations of various complexity exist between
    plume rise, stack temperature, stack velocity,
    atmospheric conditions etc. (e.g. Hollands,
    equation 6.35 de Nevers)

3
PLUME RISE - HOLLANDS EQUATION
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PLUME RISE - BUOYANCY AND MOMENTUM FLUXES
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Table 4-6 Wark, Warner Davis
  • Equations for calculating final plume rise

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STACK TIP DOWNWASH
  • For Vs lt 1.5 us
  • (Vs stack gas velocity, us wind velocity at stack
    height)
  • Note that maximum downwash correction is 3 stack
    diameters

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BUILDING DOWNWASH AND WAKE EFFECTS
  • Figs. 3-19 and 3-20 demonstrate these. Special
    treatments are included in models.
  • BUILDING DOWNWASH - Simple rule of thumb
  •   downwash unlikely to be a problem if
  • hs ? hb 1.5 Lb
  •  hs stack height
  • hb building height
  • Lb the lesser of either building height or
    maximum projected building width.
  • Good Engineering Practice (GEP) rule for stack
    design.
  •  

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LINE SOURCES - Infinite line source
  • Can be handled in principle as one dimensional
    dispersion from a point source.
  • For wind perpendicular to line source
  • q emission per unit time per unit distance

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Oblique wind and finite line source
  • For wind at an angle of ? with the line source,
    the strength is effectively increased by a
    factor of
  • (sin ? )-1
  • For a finite line source we must consider the end
    effects, the resulting concentration will be less
    than that for an infinite line source under the
    same conditions.
  • Examples 4-9 and 4-10 (Wark, Warner Davis)
    demonstrate the application of the infinite line
    source case to CO concentrations near a highway.

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COMPLICATIONS
  • For ? lt 45, the (sin ? )-1 correction becomes
    increasingly inaccurate.
  • The dispersion due to vehicle induced turbulence
    and thermal buoyancy due to heat release from
    the vehicles are important factors
  • The P-G-T dispersion coefficients were originally
    observed in flat grass terrain, most highways of
    interest have some roughness effects associated
    with them (bridge, below grade. above grade etc.)

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CALINE
  • series of models developed to provide better
    estimations of motor vehicle pollutant
    concentrations near highways and arteries.
  • Main features
  • - Finite line segment approach
  • - Mixing zone concept to incorporate traffic
    induced dispersion
  • - New dispersion data near highways,
    adjustments for averaging time and surface
    roughness included for P-G-T coefficients

17
3 DIMENSIONAL DISPERSION MODEL
  • Similar to heat conduction equation in 3-d
  • Solution for instantaneous release of X g of
    pollutant at t 0 and x y z 0

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PUFF RELEASE
  • Solution for instantaneous release of X g of
    pollutant at t 0 and (x0, y0, z0)
  • Using ? instead of K, we get

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PUFF RELEASE
  • To consider ground reflection we add a virtual
    source below the ground at (x0, y0, -z0) that is
    the mirror image of the real source above the
    ground.

Virtual source to account for reflection
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  • At z 0 (cwith reflection ) 2(cwithout
    reflection )
  • Not as simple at other z.

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PUFF RELEASE
  • Say we release a puff at ground level (z00)
  • The center of the plume (y00) is travelling in
    the x direction with windspeed u, i.e. x0 ut
  • Ground-level concentration (z0) along the center
    line of the plume, y0 , will be given by

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PUFF RELEASE
  • Ground-level concentration will be at a maximum
    for xx0 i.e

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Decay of pollutants in the atmosphere
  • The mass balances we have used so far assume
    conservative pollutants no generation or
    consumption terms.
  • For a reactant being consumed by a first order
    reaction in a batch reactor

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Decay of pollutants in the atmosphere
  • The time spent in the atmosphere after release
    x/u
  • Thus, first order decay in the atmosphere can be
    modelled simply by

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ATMOSPHERIC TURBULENCE AND SAMPLING TIME
  • The time scale for atmospheric turbulence can be
    quite long, of the order of many minutes.
  • Field observations of dispersion coefficients are
    specific to the sampling (averaging) time used
    (typically 10 minutes)
  • Estimates of corrections for other sampling
    periods can be made

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  • From Air Dispersion Modelling Guideline for
    Ontario, Guidance for Demonstrating Compliance
    with The Air Dispersion Modelling Requirements
    set out in Ontario Regulation 419/05, Air
    pollution Local Air Quality, made under the
    Environmental Protection Act, July 2005.
  • Available at http//www.ene.gov.on.ca/envision/ai
    r/regulations/localquality.htm
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