solute effect curvature effect sum of both curves (terms) relative humidity near drop

10
S o lu te E ffe ct C u rv at u re Ef f e ct S u m o f b o t h C u r v e s ( t e r m s ) Relative Humidity Near Drop

Upload: leon-kelly

Post on 21-Jan-2016

232 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Solu

te E

ffec

t

Curvature Effect

Sum

of

both

Cur

ves

(ter

ms)

Rel

ativ

e H

umid

ity N

ear

Dro

p

Page 2: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Equilibrium (Saturation) Curve e Near Drop = e of Environment

(particle doesn’t change size)

Rel

ativ

e H

umid

ity N

ear

Dro

p

Page 3: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

p

e Near Drop < e of Environment(drop grows by condensation)

Page 4: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

e Near Drop > e of Environment(drop shrinks by evaporation)

Rel

ativ

e H

umid

ity N

ear

Dro

p

e Near Drop < e of Environment(drop grows by condensation)

Page 5: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

p

e Near Drop > e of Environment(drop shrinks by evaporation)

e Near Drop < e of Environment(drop grows by condensation)

If the RH increases a bit (move drop vertically),the drop will be supersaturated with respect to theequilibrium curve and will move to the right (grow) until it hits the curve again – and then it stops growing and re-establishes equilibrium.

If the drop increases in size for some reason at constant RH (move drop to the right), it will become sub-saturated with respect to the equilibrium curve and will shrink back to its original size (hit the equilibrium curve).

Page 6: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

pIf the RH increases a bit (move drop vertically),the drop will be supersaturated with respect to theequilibrium curve and will move to the right (grow) until it hits the curve again – and then it stops growing and re-establishes equilibrium.

If the drop increases in size for some reason at constant RH (move drop to the right), it will become sub-saturated with respect to the equilibrium curve and will shrink back to its original size (hit the equilibrium curve).

e Near Drop > e of Environment(drop shrinks by evaporation)

e Near Drop < e of Environment(drop grows by condensation)

Page 7: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

p

}

Solute Effect(effective for small drops)

e Near Drop > e of Environment(drop shrinks by evaporation)

e Near Drop < e of Environment(drop grows by condensation)

Page 8: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

pIf the RH increases a bit (move drop vertically), the drop will be supersaturated with respect to theequilibrium curve and will grow (move to right). However, when it does so, it never reaches equilibrium with the environment again (never touches the curve), so the drop will simply continue to grow without bound (in reality it reaches a finite size because it competes with other drops for a finite amount of vapor).

The peak in the Kohler Curve is called the critical radius or activation radius.

e Near Drop > e of Environment(drop shrinks by evaporation)

e Near Drop < e of Environment(drop grows by condensation)

Page 9: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

p }Curvature Effect

(effective for bigger drops;they appear flat)

e Near Drop > e of Environment(drop shrinks by evaporation)

e Near Drop < e of Environment(drop grows by condensation)

Page 10: Solute Effect Curvature Effect Sum of both Curves (terms) Relative Humidity Near Drop

Rel

ativ

e H

umid

ity N

ear

Dro

p