Chemistry – Chapter 7 Notes: Phase Changes, Energetics & Intro Gas Concepts
Chapter Scope and Learning Goals
- Chapter 7 focuses on:
- Changes of state (phase transitions) in matter.
- Energy transfer accompanying each transition.
- Properties of gases and an introduction to the gas laws (to be covered later).
- Gas mixtures and Dalton’s law of partial pressures (preview only).
- Key skills to master:
- Identify and classify six fundamental phase changes.
- Relate kinetic energy (KE), intermolecular forces (IMF), and temperature to the physical state of a substance.
- Distinguish endothermic vs. exothermic processes.
- Use thermodynamic quantities (heat of fusion, heat of vaporization, specific heat) as conversion factors.
- Interpret and sketch heating curves and cooling curves.
Three States of Matter – Quick Review
- Solid
- Particles tightly packed, fixed positions, vibrational motion only.
- Highest IMF, lowest KE.
- Liquid
- Particles close but able to slide/flow.
- Intermediate IMF and KE.
- Gas
- Particles far apart, move independently.
- Lowest IMF, highest KE.
Six Fundamental Phase Changes
- Melting (Fusion)
- Solid → Liquid.
- Example: Ice cube melts on a hot day.
- Freezing (Solidification)
- Liquid → Solid.
- Example: Water freezing in a freezer.
- Vaporization / Evaporation / Boiling
- Liquid → Gas.
- Example: Puddle water evaporates in summer.
- Condensation
- Gas → Liquid.
- Example: Water vapor condenses on a cold glass.
- Sublimation
- Solid → Gas (skips liquid phase).
- Example: Dry ice (solid CO₂) turning into vapor cloud.
- Deposition
- Gas → Solid (skips liquid phase).
- Example: Frost or snowfall (water vapor → ice crystals).
Molecular-Level Explanation of Phase Changes
- Every particle (atom, molecule, ion) possesses kinetic energy (KE=21mv2) that increases with temperature.
- Simultaneously, particles attract one another via intermolecular forces (potential energy, PE).
- Physical state is a balance:
- Low KE + strong IMF ⇒ solid.
- Moderate KE + moderate IMF ⇒ liquid.
- High KE + weak IMF ⇒ gas.
- During a phase change
- Temperature remains constant because energy is used to disrupt (or form) IMF, not to increase KE.
- Covalent (intramolecular) bonds are NOT broken → phase change is a physical, not chemical, transformation.
Types of Intermolecular Forces (IMF)
- Dispersion (London) Forces
- Present in all substances; only force in non-polar molecules.
- Weakest; strength increases with molar mass/size.
- Dipole–Dipole Forces
- Require permanent molecular dipole (polar molecules).
- Intermediate strength.
- Hydrogen Bonding (H-bonding)
- Special strong dipole force when H is directly bonded to N, O, or F.
- Strongest of the three.
IMF vs. Physical Properties – Examples
- Ethanol (polar, O–H present)
- Exhibits hydrogen bonding → stronger IMF.
- Liquid at room temperature.
- Propane (non-polar, only dispersion)
- Much weaker IMF.
- Gas at room temperature.
- General trend:
- Stronger IMF ⇒ higher melting point (m.p.) and boiling point (b.p.).
- Non-polar gases (e.g., N₂, O₂) have very low m.p./b.p.; polar substances (e.g., H₂O, NH₃) have higher values.
Energy Classification of Phase Changes
- Endothermic (heat absorbed from surroundings)
- Melting, Vaporization, Sublimation.
- \text{q} > 0 for the system; surroundings cool down.
- Exothermic (heat released to surroundings)
- Freezing, Condensation, Deposition.
- \text{q} < 0 for the system; surroundings warm up.
Compressibility of Gases
- Gases are highly compressible.
- Applying external pressure can force gas particles closer, enabling condensation (gas → liquid) without cooling.
- Practical relevance: liquefied petroleum gas (LPG), aerosol cans, refrigeration cycles.
Characteristic Temperatures (at 1 atm)
- Melting Point (m.p.)
- Temperature where solid ↔ liquid equilibrium exists.
- Boiling Point (b.p.)
- Temperature where vapor pressure equals external pressure (1 atm ⇒ normal b.p.).
- Both are physical (not chemical) properties; useful for identification and purity checks.
Heating Curve – Water Example
- Axes: heat added (x) vs. temperature (y).
- Regions:
- A (Solid Ice): −30∘C→0∘C, temp rises.
- B (Melting Plateau): 0∘C, temp constant, ice → water.
- C (Liquid Water): 0∘C→100∘C, temp rises.
- D (Boiling Plateau): 100∘C, temp constant, water → steam.
- E (Superheated Steam): >100∘C, temp rises again.
- Key insight: Horizontal segments = phase changes (temperature constant while heat disrupts or forms IMF).
Thermodynamic Quantities for Phase Change
- Heat of Fusion (ΔHfus)
- Energy required to melt 1 g (or 1 mol) at the m.p.
- For H₂O: ΔHfus=80cal g−1 (common reference value).
- Heat of Vaporization (ΔHvap)
- Energy required to vaporize 1 g (or 1 mol) at the b.p.
- For H₂O: ΔHvap=539cal g−1.
- ΔH<em>vap>ΔH</em>fus because all IMF must be overcome to enter gas phase.
Using ΔH<em>fus and ΔH</em>vap as Conversion Factors
- Format: ΔHx(=gcal) or molkJ.
- Example Problem: Heat to vaporize 10 g H₂O at 100∘C
- q=10g×539gcal=5.39×103cal (5390 cal).
Temperature Change (No Phase Change) – Specific Heat
- Specific Heat (c): heat needed to raise 1 g of substance by 1∘C.
- Common units: cal g−1∘C−1 or J g−1∘C−1.
- Heat equation ("q-equation"):
q=mcΔT
where:
- q = heat (cal or J).
- m = mass (g).
- c = specific heat.
- ΔT=T<em>final−T</em>initial (∘C).
Worked Examples
- Paraffin Wax
- m=10g,c=0.60g∘Ccal,ΔT=30−20=10∘C
- q=10×0.60×10=60cal.
- Liquid Water
- m=45g,c=1.00g∘Ccal,ΔT=32−23=9∘C
- q=45×1.00×9=405cal.
Typical Conceptual & Multiple-Choice Insights
- Greatest potential energy (strongest IMF) exists in the solid state.
- During vaporization, IMF are disrupted; covalent bonds remain intact.
- Endothermic vs. exothermic:
- Deposition, condensation, freezing are all exothermic.
- Correct identification of ΔHvap:
- It is the heat added when a substance evaporates at its boiling point (not when it melts, condenses, or sublimes).
- Heating curve recognition:
- Phase changes occur where temperature line is flat (constant).
Ethical & Real-World Relevance
- Understanding phase change energetics underpins refrigeration, climate science (snowfall vs. rain), medicinal cryopreservation, and energy budgeting in chemical engineering.
- Comprehending gas compressibility is critical for safe cylinder storage and aerosol technology.
Key Equations & Numbers to Memorize
- Heat equation (temperature change): q=mcΔT.
- Energy for melting: q=mΔHfus.
- Energy for vaporization: q=mΔHvap.
- Typical water values (1 atm):
- m.p.=0∘C,b.p.=100∘C.
- c(l)=1.00g∘Ccal(4.184g∘CJ).
- ΔH<em>fus=80cal g−1,ΔH</em>vap=539cal g−1.
Study Tips & Connections
- Always specify the phase and temperature before applying q=mΔHx or q=mcΔT.
- Combine steps for multi-stage problems: cooling, freezing, further cooling ⇒ sum of individual q values.
- Link back to Chapter 1 (matter & IMF) and upcoming gas-law chapters (relationship between P, V, T for gases and Dalton’s law of partial pressures).
- Practice drawing heating/cooling curves for different substances, labeling each plateau with correct ΔH value.