BackChemistry 1770 Final Study Guide: Gases and Intermolecular Forces
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Chapter 10 - Gases
Deep Time and Atmospheric Temperature
The concept of deep time refers to understanding Earth's history over hundreds of thousands of years. Scientists estimate past atmospheric temperatures using ice cores.
Ice Core Analysis: Glaciers form from layers of snow that compress into ice over time. The top layers are younger, while deeper layers are older.
Age Determination: The age of ice is determined by its depth in the glacier; deeper ice is older.
Gas Trapping: Air bubbles trapped in ice contain ancient atmospheric gases, allowing temperature estimation.
Role of Gas Velocity Distribution (Boltzmann Distribution)
Boltzmann Distribution: Describes the spread of molecular speeds in a gas.
Temperature: Higher temperatures increase average molecular speed.
Isotopes: Heavier isotopes move slower; their distribution helps infer past temperatures.
Kinetic Molecular Theory
The kinetic molecular theory explains the behavior of gases based on molecular motion.
Postulates:
Gas particles are in constant, random motion.
Collisions are elastic; no energy is lost.
Volume of gas particles is negligible compared to container volume.
No intermolecular forces act between particles.
Average kinetic energy is proportional to temperature.
Distribution of Speeds: Lighter molecules move faster; higher temperatures broaden the speed distribution.
Comparison: At the same temperature, lighter gases have higher average speeds than heavier gases.
Pressure
Definition: Pressure is the force exerted per unit area.
Formula:
Units: Common units include atm, Pa, mmHg, and torr.
Conversions: 1 atm = 101,325 Pa = 760 mmHg = 760 torr
Combined Gas Law
The combined gas law relates pressure, volume, and temperature for a fixed amount of gas.
Formula:
Historical Gas Laws: If one variable is constant, the equation simplifies to Boyle's, Charles's, or Gay-Lussac's law.
Ideal Gas Law
Formula:
Variables: P = pressure, V = volume, n = moles, R = gas constant, T = temperature (K)
Gas Constant: L·atm·mol–1·K–1 or J·mol–1·K–1
Calculations: Solve for any variable if the other three are known.
Stoichiometry: Use the ideal gas law to relate moles of gas to volume in chemical reactions.
Density and Molar Mass: , where M is molar mass.
Application: Density of water vapor affects storm strength, such as hurricanes.
Partial Pressure and Dalton's Law
Partial Pressure: The pressure exerted by a single gas in a mixture.
Dalton's Law:
Mole Fraction:
Partial Pressure Formula:
Chapter 11 - Intermolecular Forces
Types of Intermolecular Forces
Intermolecular forces are attractions between molecules, affecting physical properties like boiling and melting points.
Dispersion Forces (London Forces):
Present in all molecules.
Strength increases with molecular size and mass.
Dipole-Dipole Interactions:
Occur in molecules with permanent dipoles (polar molecules).
Example: HCl, SO2
Hydrogen Bonding:
Occurs when H is bonded to N, O, or F.
Strongest among small molecules.
Example: Water (H2O), ammonia (NH3)
Ranking (Small Molecules):
Hydrogen bonding (strongest)
Dipole-dipole
Dispersion (weakest)
Vapor Pressure
Measurement: Vapor pressure is measured by sealing a liquid in a container and observing the equilibrium pressure of its vapor.
Relation to Intermolecular Forces: Stronger intermolecular forces result in lower vapor pressure.
Enthalpy of Vaporization ()
Definition: The energy required to convert one mole of liquid to vapor at constant pressure.
Formula: (units: kJ/mol)
Applications: Water's high is important for cooling (sweating), climate regulation, and steam engines.
Hydrogen Bonding in Living Systems
Role: Hydrogen bonds stabilize DNA structure, proteins, and influence water's properties in biological systems.
Definition of a Foam
Foam: A colloidal system where gas bubbles are dispersed in a liquid or solid.
Useful Constants
Avogadro's Number:
Gas Constant: L·atm·mol–1·K–1 or J·mol–1·K–1
Planck's Constant: J·s
Speed of Light: m·s–1