Chapter 15 Part 4 — Temperature & Maxwell–Boltzmann Theory
Overview: Three Key Themes about Temperature
The instructor groups the closing content of Chapter 15 into three theoretical pillars to remember:
Translational (particle-to-particle) collisions as the microscopic mechanism for heat transfer.
Temperature is a macro-scale average—it represents the statistical behavior of trillions of particles whose individual speeds follow a Maxwell–Boltzmann (normal/Gaussian) distribution.
Because speeds vary, spontaneous phase changes occur, producing vapor–liquid (or solid) dynamic equilibria and a measurable vapor pressure in a closed system.
Humor opener: “The guy who froze himself to absolute zero is 0 K now.” (Wordplay: 0 K ≠ “OK”).
1. Translational Collisions & Heat Transfer
Definition: “Translational” means particles physically move from point A → B, colliding and transferring momentum/energy.
Conservation of momentum governs each collision:
Fast (hot) particles lose kinetic energy on impact.
Slow (cold) particles gain kinetic energy.
Interface focus: Heat flow is analyzed primarily at the boundary where two objects touch; internal collisions merely redistribute energy within each body.
Thermodynamic equilibrium:
Reached when average kinetic energies (temperatures) of both objects equalize.
Individual atoms/molecules still display a spread of speeds—only the mean equalizes.
Review link: Ties back to earlier thermodynamics segment covered earlier in the year.
2. Temperature as a Macro-Scale Average & Maxwell–Boltzmann Distributions
Macro vs. micro:
Temperature ≙ average kinetic energy of an enormous ensemble; it is not the speed of any single particle.
Symbolically,
Maxwell–Boltzmann (M–B) Distribution characteristics:
Bell-shaped/Gaussian: Majority of particles lie within ≈1 σ of the mean speed.
Extremes exist: A few very fast or very slow particles reside in the distribution tails.
Phase comparison (same substance):
Solid → narrow, lower-speed peak.
Liquid → broader, slightly faster peak.
Gas → broadest, highest-speed peak; wide variety of speeds.
Even within a solid some particles can exceed speeds of many gas particles—yet they are statistically rare.
Mass comparison (different substances at same T):
From if is fixed (same T), then (inverse relationship).
Lighter molecules move faster & show wider spread than heavier ones at identical temperatures.
3. Spontaneous Phase Change & Dynamic Equilibrium (Vapor Pressure)
Evaporation mechanism:
Occurs at the liquid surface when two very fast molecules collide, giving one enough to overcome intermolecular forces (IMFs) and escape.
Only surface molecules can escape; deeper molecules are caged by particles above them.
Condensation mechanism:
A very slow gas-phase molecule may strike the surface without enough to rebound, thus re-entering the liquid.
Dynamic equilibrium in a closed container:
Rate(evaporation) = Rate(condensation).
Macroscopically, liquid level appears unchanged; microscopically, particles continuously interchange.
Vapor pressure:
The pressure exerted by gas molecules in equilibrium with their liquid/solid.
Volatility describes how much must evaporate before equilibrium is reached; low-IMF liquids (acetone, alcohol) reach a higher vapor pressure quickly; high-IMF liquids (water) do so slowly.
Open system: Evaporated particles disperse; equilibrium with the entire atmosphere is effectively impossible → the liquid eventually disappears.
Ranking Particle Speeds by Molar Mass: Worked Examples
General rule at a fixed : lighter molar mass ⇒ greater average velocity ⇒ wider speed range.
Example 1 (given in lecture)
Substance | M (g·mol⁻¹) | Relative speed |
|---|---|---|
70.906 | slowest | |
44.009 | medium | |
31.998 | fastest | |
Written as increasing velocity: \text{Cl}2 < \text{CO}2 < \text{O}_2. |
Example 2 (practice problem)
Substance | M (g·mol⁻¹) | Ranking |
|---|---|---|
17.031 | ||
16.043 | ||
4.002 | ||
Increasing velocity: \text{NH}3 < \text{CH}4 < \text{He} (He is fastest, NH₃ slowest among the three). |
Temperature Scales & Absolute Zero
Degree vs. Kelvin:
Degrees C (°C) & Degrees F (°F) are relative scales (“degrees” indicate comparison to some reference).
Kelvin (K) is absolute: 0 K = absolute zero (no translational motion).
Absolute zero estimated at (graphical extrapolation; unattained in lab—only approached).
Conversion: (commonly rounded) or (more precise).
Memory aid: “Degrees-C plus two-seven-three.”
Sig-fig caution (addition rule):
Example: 16 °C → K (answer limited to ones place because 16 °C has no tenths).
The Kelvin scale is mandatory for gas-law calculations (Boyle, Charles, Gay-Lussac, etc.).
Practical Illustration: Uneven Heating of a Glass Beaker
When a beaker sits on a hot plate:
Glass in direct contact with boiling water gets hot quickly.
Glass rim above water heats slowly because energy must percolate through particle collisions within the glass wall.
Lab tip: Safely grasp a beaker above the liquid level; never where glass contacts the fluid.
Quick Reference Equations and Statistical Notes
Kinetic energy of a particle: .
Average kinetic energy (temperature): .
Inverse mass–velocity relationship at constant : .
1 σ on a Maxwell–Boltzmann curve typically contains ≈66 % of particles.
Vapor pressure equilibrium condition (closed system): .
Common qualitative vocabulary:
Volatility: readiness to evaporate (high volatility ⇒ high vapor pressure; weak IMFs).
Dynamic equilibrium: forward & reverse processes occurring at equal rates, producing no net macroscopic change.
End of Chapter 15, Part 4. Minimal math here; heavier computation resumes in Chapter 18.