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States of Matter - Factors
Almost all matter exists in three classical states: solid, liquid, gas.
The state depends on:
Temperature (thermal energy available).
Pressure (external force per unit area).
Intermolecular forces (IMFs) between atoms, ions, and/or molecules.
Solids - Definition
Condensed phase of matter that is ordered.
Solids - Particle Arrangement
Atoms/ions/molecules are closely packed, usually in a lattice.
Solids - Motion
Particles vibrate but are largely immobile.
Solids - Properties
Definite shape and volume.
Generally rigid and resistant to compression.
Wide variation in melting point, hardness, electrical conductivity, depending on bonding/IMFs.
Solids - Types
Ionic solids (e.g., NaCl) → high melting points, brittle, conduct electricity when molten.
Covalent network solids (e.g., diamond, SiO₂) → very hard, high melting point, poor conductors (except graphite).
Metallic solids → good conductors, malleable, variable hardness.
Molecular solids (e.g., ice, I₂) → lower melting points, soft, depend strongly on IMFs.
Liquids - Definition
Condensed phase of matter but disordered.
Special note: Liquids exist only within certain temperature-pressure ranges
Liquids - Particle Arrangement
Molecules are close enough for IMFs to hold them together, but not fixed in place.
Liquids - Properties
Definite volume, but no fixed shape (takes container shape).
Fluidity → particles can slide past each other.
Physical properties depend on IMFs:
Viscosity → resistance to flow.
Surface tension → energy required to increase surface area (important in capillary action).
Vapour pressure → tendency of molecules to escape into gas phase.
Gases - Definition
Uncondensed, disordered phase of matter.
Gases - Particle Arrangement
Atoms/molecules are far apart, in constant, random motion.
Gases - Properties
No fixed shape or volume; expand to fill any container.
Generate pressure via collisions with container walls.
IMFs are extremely weak/negligible due to large separations.
Gases - Variables
n = number of particles (mol).
V = volume (L or m³).
P = pressure (Pa, kPa, atm).
T = temperature (K, °C).
Boyle’s Law (P-V relationship)
P ∝ 1\V (at constant T, n)
Charles’ Law (V-T Relationship)
V ∝ T (at constant P, n)
Guy-Lussac’s Law (P-T Relationship)
P ∝ T (at constant V, n)
Avogadro’s Law (V-n Relationship)
V ∝ n (at constant P, T)
Ideal Gas Law - Formula
PV = nRT
Ideal Gas Law - Gas Constant (R)
R (Gas constant): depends on units:
8.314 J/mol K (SI units).
0.0821 atm/mol K (lab units).
Ideal Gas Law - Assumptions
Negligible intermolecular forces.
Negligible molecular volume.
Ideal Gas Law - Limitations
Assumptions fail at high pressures (molecules close together) and low temperatures (IMF significant)
Dalton’s Law of Partial Pressure
For an ideal mixture, identity of gas doesn’t matter, only the total number of particles (moles).
Dalton’s Law of Partial Pressures: Ptotal = PA + PB + ...
Where PA and PB are the partial pressures of gases A and B.
Mole Fraction (χ)
A way to express the composition of a mixture based on how many moles of each component it contains.
χA = nA/ntotal
nA = moles of gas A
ntotal = ∑ni = total moles of all gases
PA = χA ⋅ Ptotal
Plasma
A fourth state of matter, occurs at very high temperatures when atoms are ionized (e.g., stars, lightning).
Phase Changes
Transitions between states (melting, freezing, evaporation, condensation, sublimation, deposition) depend on IMFs and energy input/output.