1 / 10

Solute Effect

Curvature Effect. Relative Humidity Near Drop. Sum of both Curves (terms). Solute Effect. Equilibrium (Saturation) Curve e Near Drop = e of Environment (particle doesn’t change size). Relative Humidity Near Drop. e Near Drop < e of Environment (drop grows by condensation).

artemas-kristy
Download Presentation

Solute Effect

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

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

  2. Equilibrium (Saturation) Curve e Near Drop = e of Environment (particle doesn’t change size) Relative Humidity Near Drop

  3. e Near Drop < e of Environment (drop grows by condensation) Relative Humidity Near Drop

  4. e Near Drop < e of Environment (drop grows by condensation) Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation)

  5. 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). e Near Drop < e of Environment (drop grows by condensation) Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation)

  6. 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). e Near Drop < e of Environment (drop grows by condensation) Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation)

  7. e Near Drop < e of Environment (drop grows by condensation) Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation) } Solute Effect(effective for small drops)

  8. If 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 grows by condensation) Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation)

  9. e Near Drop < e of Environment (drop grows by condensation) } Relative Humidity Near Drop e Near Drop > e of Environment (drop shrinks by evaporation) Curvature Effect(effective for bigger drops; they appear flat)

  10. Relative Humidity Near Drop

More Related