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Algorithms IV · software · air pollution effects
Unstable or Neutral - Crossover Between Momentum and Buoyancy For cases with stack gas temperature greater than or equal to ambient temperature, it must be determined whether the plume rise is dominated by momentum or buoyancy. The crossover temperature difference, (DT)c, is determined as follows: for Fb < 55, (DT)c=0.0297 Ts(vs/ds2)1/3 (9) and for Fb >= 55, (DT)c=0.00575 Ts(vs2/ds)1/3 (10) If DT, exceeds or equals (DT)c, plume rise is assumed to be buoyancy dominated, otherwise plume rise is assumed to be momentum dominated. Unstable or Neutral - Buoyancy Rise For situations where DT exceeds (DT)c as determined above, buoyancy is assumed to dominate. The distance to final rise, xf, is assumed to be 3.5x*, where x* is the distance at which atmospheric turbulence begins to dominate entrainment. The value of xf is calculated as follows: for Fb < 55: xf=49Fb5/8 (11) and for Fb >= 55: xf=119Fb2/5 (12) The final effective plume height, he (m), is determined as for Fb < 55: he=hs+(21.425 Fb3/4/us) (13) and for Fb = 55: he=hs+(38.71 Fb3/5/us) (14) Unstable or Neutral - Momentum Rise For situations where the stack gas temperature is less than or equal to the ambient air temperature, the assumption is made that the plume rise is dominated by momentum. If DT is less than (DT)c, the assumption is also made that the plume rise is dominated by momentum. The plume height is calculated as: he=hs+3ds(vs/us) (15) Briggs suggests that this equation is most applicable when vs/us is greater than 4.
software · air pollution effects DISPER software solutions: This application has been used in great number of environmental reports, air pollution courses and air pollution studies in the last years. We currently have users in more than 10 countries.
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