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Kinetic Theory and Phase Change

Kinetic Theory and Phase Change. Kinetic Theory Comparison with Ideal Gas RMS velocity examples PVT Diagrams Phase Changes Vapor Pressure and Humidity Examples. Ideal Gas Animation. Gas/piston animation (Java animation) (Flash animation) Note

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Kinetic Theory and Phase Change

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  1. Kinetic Theory and Phase Change • Kinetic Theory • Comparison with Ideal Gas • RMS velocity examples • PVT Diagrams • Phase Changes • Vapor Pressure and Humidity • Examples

  2. Ideal Gas Animation • Gas/piston animation (Java animation) (Flash animation) • Note • Molecule collides with wall, gives it a little Impulse. (F Δt) • No more impulse until it makes round trip, then hits again. (box size) • N molecules with average velocity • Molecules moving equally in x, y, z directions

  3. Kinetic Theory • A little Physics 103 • Change in x-momentum for molecule hitting wall: • Time for molecule to travel 2l and hit again: • Average force during this time: • Average force of N molecules: • Average x-velocity-squared = 1/3 average total-velocity-squared • Pressure is thus: V is volume

  4. Kinetic Theory Results - 1 • Previous page • Multiply by volume and rearrange like kinetic energy • Result • P inversely proportional to V • PV proportional to N • PV proportional to

  5. Ideal Gas Law - #molecules version • Ideal Gas Law PV = nRT • Using #molecules: PV = NkT • N = nNA (N number of molecules) • k= R/NA (NA Avagadro’s number) • P in Pascals (no alternative units) • V in m3 • T in K° • Boltzman’s constant • k = R/NA = 1.38e-12 J/K

  6. Kinetic Theory Results - 2 • Comparing Kinetic Theory • With Ideal Gas Law • Gives • 4. Average Kinetic Energy

  7. Kinetic Theory Examples • Root-mean-square velocity • Example 13-16 - Average translational KE at 37°C • Example 13-17 - rmsspeed of O2 and N2 at 20°C Mass N2 RMS velocity N2

  8. PV diagrams • Pressure vs. Volume at constant Temperature • Plot pressure vs. volume curves at constant temperature. • Different PV curves for different temperatures. (T “parameter”) • Different PV curves for different # moles. (usually constant) • Can plot in 3-D PVT diagram with 3rd temperature axis.

  9. PV diagrams with phase change* • Pressure vs. Volume at constant Temperature. • At high temperatures PV varies normally (ideal gas). • As temperature is lowered PV becomes distorted. • As temperature is lowered further, liquid forms (critical point). • As temperature is lowered below critical point, liquid-vapor phase coexist *Non-ideal gas

  10. 3-D PVT Diagrams with Phase Change • Trace PV line at constant temperature (red) • Trace PT line at constant pressure (blue)

  11. 3-D PVT diagram projections • PV diagram is projection to the right • PT diagram is projection to the left

  12. PT diagrams (Phase diagrams) • Pressure vs. Temperature at constant Pressure. • Below 0.006 atm water sublimes directly from solid to vapor with increasing temperature. (vapors love vacuums!) • At 0.006 atm, solid/liquid/vapor water coexists at 0.01°C (triple point). • From 0.006 to 1.0 atm, water melts above 0°C, boils below 100 °C. (Rocky Mountain pressure cooker!) • At 1.0 atm water melts at 0°C, boils at 100°C (for us folks at sea level). • From 1.0 to 218 atm, water boils between 100°C to 374°C. • Above 374°C water doesn’t exist as liquid at any pressure (critical point). Gases - Low Pressures, high temperatures Solids - High pressures, low temperatures Liquids - In between

  13. Vapor pressure • Partial pressure of water vapor in equilibrium with liquid water. • Saturated Vapor Pressure (maximum PP) varies with temperature. • Relative Humidity

  14. Problem 67 • What is the partial pressure of water on a day when the temperature is 25°C and the relative humidity is 40% ? • SVP from table • Relative Humidity

  15. Problem 69 • If the humidity in a room of volume 680 m3 at 25°C is 80%, what mass of water can still evaporate from an open pan? • SVP from table • Using Ideal Gas for partial pressures • 80% of 865 moles evaporated, 20% left • Mass of 173 moles water

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