Presentation Slides for Chapter 16 of Fundamentals of Atmospheric Modeling 2 nd Edition Mark Z. Jacobson Department of Civil & Environmental Engineering.

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Presentation transcript:

Presentation Slides for Chapter 16 of Fundamentals of Atmospheric Modeling 2 nd Edition Mark Z. Jacobson Department of Civil & Environmental Engineering Stanford University Stanford, CA March 30, 2005

Mass Flux To and From a Single Drop Rate of change of mass (g) of single pure liquid water drop (16.1) Integrate from drop surface to infinity(16.2) Energy change at drop surface due to conduction(16.3)

Mass Flux To and From a Single Drop Integrate from drop surface to infinite radius(16.4) Relate change in mass and energy at surface(16.5) Combine (16.4) and (16.5) and assume steady state(16.6)

Mass Flux To and From a Single Drop Combine equation of state at saturation with Clausius Clapeyron equation to obtain(16.7)

Mass Flux To and From a Single Drop Integrate from infinite radius to drop surface(16.8) Simplify assuming T≈ T r (16.9) Substitute (16.6) into (16.9) --> (16.10)

Mass Flux to and From a Single Drop Substitute (16.2) into (16.10)(16.11) Rearrange --> Mass-flux form of growth equation(16.12) (16.2) (16.10)

Mass Flux to and From a Single Drop Mass-flux form of growth equation(16.12) Rewrite equation for trace gases and particle sizes (16.13)

Fluxes to and From a Single Drop Change in mass as a function of change in radius(16.14) Radius-flux form of growth equation(16.15)

Fluxes to and From a Single Drop Change in mass as a function of change in volume Volume-flux form of growth equation(16.16)

Gas Diffusion Coefficient Molecular diffusion Movement of molecules due to their kinetic energy, followed by collision with other molecules and random redirection. Uncorrected gas diffusion coefficient (cm 2 s -1 )(16.17)

Collision Diameters and Diffusion Coefficients of Several Gases Table 16.1 CollisionDiffusion Diametercoefficient Gas( m)(cm 2 s -1 ) ____________________________________________ Air Ar CO H NH O H 2 O

Corrected Gas Diffusion Coefficient (16.18)

Corrected Gas Diffusion Coefficient Correction for collision geometry, sticking probability(16.19) Mass accommodation (sticking) coefficient,  q,i Fractional number of gas collisions with particles that results in the gas sticking to the surface. From Knudsen number for condensing vapor(16.20)

Corrected Gas Diffusion Coefficient Mean free path of a gas molecule(16.23) Ventilation factor (16.24) Corrects for enhanced vapor transfer to a large-particle surface due to eddies sweeping vapor to the surface

Corrected Gas Diffusion Coefficient Particle Reynolds number Gas Schmidt number(16.25)

Corrected Thermal Conductivity Corrected thermal conductivity of air (16.26) Correction to conductivity for collision geometry and sticking probability(16.27)

Corrected Thermal Conductivity Knudsen number for energy(16.28) Thermal mean free path(16.29)

Corrected Thermal Conductivity Thermal accommodation (sticking) coefficient Fraction of molecules bouncing off surface of a drop that have acquired temperature of drop ≈ 0.96 for water.(16.30) Ventilation factor (16.31) Corrects for enhanced energy transfer to drop surface due to eddies

Corrected Saturation Vapor Pressure Curvature (Kelvin) effect Increases saturation vapor pressure over small drops. Solute effect (Raoult’s Law) The saturation vapor pressure of a solvent containing solute is reduced to that of the pure solvent multiplied by the mole fraction of the solvent in solution. Radiative cooling effect Decreases saturation vapor pressure over large drops

Curvature and Solute Effects Fig Saturation ratio

Curvature Effect Saturation vapor pressure over a curved, dilute surface relative to that over a flat, dilute surface(16.33) Note that exp(x)≈1+x for small x

Curvature Effect Surface tension of water containing dissolved organics(16.34) Surface tension of water containing dissolved inorganic ions (16.35)

Solute Effect Vapor pressure over flat water surface with solute relative to that without solute (Raoult's Law)(16.36) Relatively dilute solution: n w >>n s (16.37) Number of moles of solute in solution

Solute Effect Number of moles of liquid water in a drop(16.38) Combine terms --> solute effect(16.39)

Köhler Equation Combine curvature and solute effects --> Sat. ratio at equilibrium (16.40) Simplify Köhler equation(16.42) Set Köhler equation to zero -->(16.43) Critical radius for growth and critical saturation ratio

Table 16.2 Critical radii / supersaturations for water drops containing sodium chloride or ammonium sulfate at 275 K Köhler Equation Sodium chlorideAmmonium sulfate Solute mass (g)r* (  m)S*-1 (%)r* (  m)S*-1 (%) 00∞ 0∞

Radiative Cooling Effect Saturation vapor pressure over a drop that radiatively heats/cools relative to one that does not(16.44) Radiative cooling rate (W)(16.45)

Overall Equilibrium Saturation Ratio Overall equilibrium saturation ratio for liquid water(16.46) Equilibrium saturation ratio for gases other than liquid water (16.47)

Flux to Drop With Multiple Components Volume of a single particle in which one species is growing (16.48) Time derivative of (16.47)(16.50) Mass of a single particle in which one species is growing (16.49) since

Flux to Drop With Multiple Components Combine (16.50) and (16.48) with (16.16) (16.51) Rate of change in volume of one component in one multicomponent particle

Flux to a Population of Drops Volume as a function of volume concentration Substitute volumes into (16.49)(16.52)

Flux to a Population of Drops Partial pressure in terms of mole concentration(16.53) Vapor pressure in terms of mole concentration(16.53)

Flux to a Population of Drops Combine (16.52) with (16.53)(16.54) Effective diffusion coefficient(16.55)

Flux to a Population of Drops Simplify effective diffusion coefficient for non-water gases(16.56) Corresponding gas-conservation equation(16.57)

Matrix of Partial Derivatives for Growth ODEs (16.58) v q,1,t v q,2,t v q,3,t v q,4,t v q,1,t v q,2,t v q,3,t v q,4,t

Partial Derivatives For Matrix (16.58) (16.60) (16.61) (16.62)

Table 16.3 Condensation between gas phase and 16 size bins: N B + 1 = 17 Effect of Sparse-Matrix Reductions When Solving Growth ODEs WithoutWith Quantity ReductionsReductions Order of matrix1717 Initial fill-in28949 Final fill-in28949 Decomp Decomp Backsub Backsub

Analytical Predictor of Condensation (APC) Solution For Solving Growth Assume radius in growth term constant during time step Define mass transfer coefficient(16.64) Change in particle volume concentration(16.63)

APC Solution Volume concentration of a component(16.66) Effective surface vapor mole concentration(16.65) Uncorrected surface vapor mole concentration

APC Solution (16.68) Substitute conversions into (16.63) and (16.57)(16.67) Integrate (16.67) for final aerosol concentration (16.69)

APC Solution Mole balance equation(16.70) Substitute (16.69) into (16.70)(16.71) Aerosol mole concentration (16.69)

Fig Comparison of APC growth solution, when h = 10 s, with an exact solution. Both solutions lie almost on top of each other. APC Growth Simulation dv (  m 3 cm -3 ) / d log 10 D p

Solving Homogen. Nucl. with Cond. Sum nucleation, condensation transfer rates in first bin(16.73) Homog. nucleation rate converted to mass transfer rate(16.74) Final number concentration in first bin after nucleation(16.74)

Fig Homogeneous Nucleation with Condensation Simultaneously dn (No. cm -3 ) / d log 10 D p

Fig Growth plus coagulation pushes particles to larger sizes than does growth alone or coagulation alone Effect of Coagulation on Condensation dn (No. cm -3 ) / d log 10 D p

Fig Growth plus coagulation pushes particles to larger sizes than does growth alone or coagulation alone Effect of Coagulation on Condensation dv (  m 3 cm -3 ) / d log 10 D p

Fig Comparison of full-moving (FM) with moving-center (MC) results for growth-only and growth plus coagulation cases shown in Fig. 16.4(a) Growth With Different Size Structures dn (No. cm -3 ) / d log 10 D p

Ice Crystal Growth Rate of mass growth of a single ice crystal(16.76)

Ice Crystal Growth Electrical capacitance of crystal (cm)(16.77) a c,i = length of the major semi-axis (cm) b c,i = length of the minor semi-axis (cm)

Ice Crystal Growth Effective saturation vapor pressure over ice Ventilation factor for falling oblate spheroid crystals(16.78) x= x q,i for ventilation of gas x= x h,i for ventilation of energy