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=12mv2)\bigl(KE\,=\,\tfrac12 m v^2\bigr) 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): 30C0C-30\,^{\circ}\text{C} \to 0\,^{\circ}\text{C}, temp rises.
    • B (Melting Plateau): 0C0\,^{\circ}\text{C}, temp constant, ice → water.
    • C (Liquid Water): 0C100C0\,^{\circ}\text{C} \to 100\,^{\circ}\text{C}, temp rises.
    • D (Boiling Plateau): 100C100\,^{\circ}\text{C}, temp constant, water → steam.
    • E (Superheated Steam): >100C100\,^{\circ}\text{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\Delta H_{fus})
    • Energy required to melt 1 g (or 1 mol) at the m.p.
    • For H₂O: ΔHfus=80cal g1\Delta H_{fus}=80\,\text{cal g}^{-1} (common reference value).
  • Heat of Vaporization (ΔHvap\Delta H_{vap})
    • Energy required to vaporize 1 g (or 1 mol) at the b.p.
    • For H₂O: ΔHvap=539cal g1\Delta H_{vap}=539\,\text{cal g}^{-1}.
  • ΔH<em>vap>ΔH</em>fus\Delta H<em>{vap} > \Delta H</em>{fus} because all IMF must be overcome to enter gas phase.

Using ΔH<em>fus\Delta H<em>{fus} and ΔH</em>vap\Delta H</em>{vap} as Conversion Factors

  • Format: ΔHx(=calg)\Delta H_{x}\bigl(=\frac{\text{cal}}{\text{g}}\bigr) or kJmol\frac{\text{kJ}}{\text{mol}}.
  • Example Problem: Heat to vaporize 10 g H₂O at 100C100\,^{\circ}\text{C}
    • q=10g×539calg=5.39×103calq = 10\,\text{g} \times 539\,\tfrac{\text{cal}}{\text{g}} = 5.39\times10^{3}\,\text{cal} (5390 cal).

Temperature Change (No Phase Change) – Specific Heat

  • Specific Heat (cc): heat needed to raise 1 g of substance by 1C1\,^{\circ}\text{C}.
  • Common units: cal g1C1\text{cal g}^{-1}\,^{\circ}\text{C}^{-1} or J g1C1\text{J g}^{-1}\,^{\circ}\text{C}^{-1}.
  • Heat equation ("q-equation"): q=mcΔTq = m\,c\,\Delta T where:
    • qq = heat (cal or J).
    • mm = mass (g).
    • cc = specific heat.
    • ΔT=T<em>finalT</em>initial\Delta T = T<em>{final}-T</em>{initial} (C)\,(^{\circ}\text{C}).

Worked Examples

  1. Paraffin Wax
    • m=10g,  c=0.60calgC,  ΔT=3020=10Cm = 10\,\text{g},\; c = 0.60\,\tfrac{\text{cal}}{\text{g}\,^{\circ}\text{C}},\; \Delta T = 30-20 = 10\,^{\circ}\text{C}
    • q=10×0.60×10=60calq = 10 \times 0.60 \times 10 = 60\,\text{cal}.
  2. Liquid Water
    • m=45g,  c=1.00calgC,  ΔT=3223=9Cm = 45\,\text{g},\; c = 1.00\,\tfrac{\text{cal}}{\text{g}\,^{\circ}\text{C}},\; \Delta T = 32-23 = 9\,^{\circ}\text{C}
    • q=45×1.00×9=405calq = 45 \times 1.00 \times 9 = 405\,\text{cal}.

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\Delta H_{vap}:
    • 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=mcΔTq = m\,c\,\Delta T.
  • Energy for melting: q=mΔHfusq = m\,\Delta H_{fus}.
  • Energy for vaporization: q=mΔHvapq = m\,\Delta H_{vap}.
  • Typical water values (1 atm):
    • m.p.=0C,  b.p.=100Cm.p. = 0\,^{\circ}\text{C},\; b.p. = 100\,^{\circ}\text{C}.
    • c(l)=1.00calgC  (4.184JgC)c_{(l)} = 1.00\,\tfrac{\text{cal}}{\text{g}\,^{\circ}\text{C}} \;\bigl(4.184\,\tfrac{\text{J}}{\text{g}\,^{\circ}\text{C}}\bigr).
    • ΔH<em>fus=80cal g1,  ΔH</em>vap=539cal g1\Delta H<em>{fus} = 80\,\text{cal g}^{-1},\; \Delta H</em>{vap} = 539\,\text{cal g}^{-1}.

Study Tips & Connections

  • Always specify the phase and temperature before applying q=mΔHxq = m\,\Delta H_{x} or q=mcΔTq = m c \Delta T.
  • Combine steps for multi-stage problems: cooling, freezing, further cooling ⇒ sum of individual qq 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\Delta H value.