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Ideal Gas Law
Relationship between P, V, n, T for an ideal gas
R = gas constant
Equation forms:
PV = nRT
PVm = RT (molar volume form)
Vm = V/n
To use the Ideal Gas Law:
Rearrange PV = nRT
Convert units
Sub values
Kinetic Model Assumptions
What assumptions define a perfect (ideal) gas?
Molecules in random motion
Point particles (no volume)
Move in straight lines between collisions
No interactions except elastic collisions
Pressure from Molecular Collisions
What causes gas pressure?
Pressure = force from molecular impacts on container walls
Derived from momentum change during collisions
Leads to relation:
PV = 1/3 Nmv2
Translational Kinetic Energy
What is the avg translational kinetic energy of an ideal gas?
Per mole: Etrans = 3/2 RT
Per molecule: 3/2 kBT
Shows U depends only on T for ideal gases
U = E
Equipartition Principle
What does equipartition say about energy contributions?
Each translational or rotational degree of freedom → RT/2
Each vibrational degree → RT
Explains why diatomic gases have:
High T: U = 7/2 RT
Room T: U = 5/2 RT (vibration not excited)
Internal Energy U of Different Molecules
What is U for different ideal gases?
Monatomic: U = 3/2 nRT
Linear molecules: U = 5/2 nRT
Nonlinear molecules: U = 3 nRT
Only valid when vibrational modes not excited
Key insights of U:
U = U(T) only
Independent of volume or pressure
Breaks down real gases due to interactions
Van der Waals Equation
Van der Waals introduces:
Repulsion (finite size): replace V → (V - nb)
Attraction: replace P → (P + an2/V2)
Full equation:
(P + an2/V2) (V - nb) = nRT
Compressibility Factor Z
What is compressibility factor z?
z = PV/nRT
z = 1: ideal gas
z ≠ 1: real gas deviations
used to quantify non-ideality
Virial Equation:
Expansion: z = PV/RT = 1 + B2P/RT + B3P2/RT + …
Describes intermolecular forces
What Thermodynamics studies
Transformation of energy in chemical systems
Predicts direction of reactions + equilibrium
Determines driving forces (ΔG, ΔS, ΔH)
0th, 1st, 2nd, 3rd Laws
The four laws of thermodynamics:
Zeroth: Defines temperature via thermal equilibrium
First: Energy conservation → ΔU = q + w
Second: Direction of spontaneous change → ΔSuniv >= 0
Third: Defines absolute entropy (S → 0 at 0K for perfect crystal)
System / Surroundings / Universe
System = Part of universe being studied
Surroundings = Everything else
Universe = system + surroundings
Types of systems:
Open: exchanges matter + energy
Closed: exchanges energy only
Isolated: exchanges neither
State Functions
What is a State function?
Depends only on current state, not path
Examples:
P, V, T, U, H, G, S
q and w are NOT state functions
Zeroth Law
If A is in thermal equilibrium with B, and B with C, then A is with C
First Law
ΔU = q + w
q > 0: heat into system
w > 0: work done ON system
Sign conventions:
w > 0: surroundings compress system
w < 0: system expands (does work ON surroundings)
Heat vs Work
Heat q: energy transfer due to temperature differences
Work w: energy transfer due to force acting through distance
Reversible vs Irreversible Processes
Reversible: System always in equilibrium; max work
ΔSuniv = 0
Irreversible: Real processes; spontaneous; not at equilibrium
ΔSuniv > 0
Types of processes
Isothermal: T constant
Isobaric: P constant
Isochoric: V constant
Adiabatic: q = 0
Exothermic: release heat into surroundings (q < 0)
Endothermic: absorb heat from surroundings (q > 0)
Expansion Work
w = -Pext ΔV
Expansion (ΔV > 0): w < 0
Compression (ΔV < 0): w > 0
Pext = constant
Free Expansion:
Expansion into vacuum → Pext = 0
w = 0, q = 0, so ΔU = 0
Reversible Isothermal Expansion/Compression of an ideal gas:
Pgas = nRT/V
Reversible: Pext = Pgas
w = -nRT ln(Vf / Vi)
If isothermal, ΔU = 0, so q = -w
Enthalpy Definition
H = U + PV
State Function
At constant V:
ΔU = qv
At constant P:
ΔH = qp
Determines which heat capacity to use (CV or CP)
ΔH: tracks heat at constant pressure → calorimetry
Heat Capacity
C = dq/dT
q = C ΔT
CV = heat capacity at constant volume
CP = heat capacity at constant pressure
CP > CV
Specific vs Molar Heat Capacity
Specific (Cs) = per gram
Molar (Cm) = per mole
CP, m = CP / n
Constant Volume Process
V = constant → no PV work
w = 0
ΔU = qV
Heat at constant volume directly changes internal energy
Heat Capacity:
CV = n CV, m
ΔU = n CV, m ΔT
Relationship between CP and CV
CP, m = CV, m + R
Monatomic ideal gas:
CV, m = 3/2 R, CP, m = 5/2 R
Reaction Enthalpy (delta Hrxn)
ΔrH = sum[vi Hm,i (products)] - sum[vj Hm,j (reactants)]
Standard Reaction Enthalpy:
Same formula as ΔrH but using standard molar enthalpies
Kirchhoff’s Law
ΔrH0(T) = ΔrH0(T0) + \intT_T0 [sum v Cpm(prod) - sum v Cpm(react)] dT
Why the 2nd Law?
2nd Law introduces entropy S, criterion for spontaneity
Spontaneous vs Nonspontaneous Processes
Spontaneous:
Occurs in 1 direction only (irreversible)
Always involves loss of work ( w → q)
can be slow
Nonspontaneous:
Occurs only with external intervention (work input)
First law may show ΔU = 0, but spontaneity still requires entropy
Entropy S
Measure of disorder, randomness
High S → high disorder
Perfect crystal at 0K has S = 0 (third law)
Definition of entropy change:
ΔS = \intstate 2_state1 [d qrev / T]
dS = dqrev / T
Only reversible heat matters
If the process is irreversible, construct a reversible path
2nd Law Statements:
Reversible: ΔSuniv = 0
Irreversible (spontaneous): ΔSuniv > 0
Suniv = system + surroundings
Cases of Entropy
Isolated System:
No heat or matter exchange
Entropy must increase for any spontaneous change
ΔSsys > 0
Isothermal Expansion:
ΔS = nR ln(V2 / V1) = nR ln(P1 / P2)
P1V1 = P2V2 = nRT
works for reversible and irreversible expansions
Constant V (Isochoric) or Constant P (Isobaric):
dS = CV or P dT / T
If C is constant:
ΔS = CV or P ln(T2 / T1)
Applies to any Isochoric/Isobaric processes
Adiabatic Process:
Reversible adiabatic:
qrev = 0 → ΔS = 0
Irreversible adiabatic:
ΔSuniv > 0 → Ssys > 0
Phase Changes:
for reversible phase transitions:
ΔS = ΔH / T
Standard Entropy of Reaction
deltar Sdeg = sum[viSdeg(prod)] - sum[vjSdeg(react)]
Temp Dependence of reaction entropy:
ΔrS0(T) = ΔS0(T) + \intT_T0 [sum(prod) - sum(react)] dT / T
Gibbs Free Energy
Because spontaneity requires evaluating ΔSsys + ΔSsurr → inconvenient
Gibbs shows at constant T and P, S can be determined using:
G = H - TS
A state function with units of J
Molar Gibbs energy: Gm = G / n
At constant T:
ΔG = ΔH - TΔS
Spontaneity Criterion (Constant T and P):
ΔG < 0 → spontaneous (ΔSuniv > 0)
ΔG = 0 → equilibrium (ΔSuniv = 0)
ΔG > 0 → nonspontaneous
Standard Gibbs Energy of Reaction:
ΔrGdeg = sum[v ΔrG∘(prod)] - sum[v ΔrG∘(react)]
Gibbs vs 2nd Law
When can we replace the 2nd law with ΔG?
Only when T and P are constant
ΔSuniv > 0 ←> ΔG < 0
Chemical Potential Definition
μi = (dG / dni)P, T, n
Partial molar Gibbs energy → measures how much G changes when adding species i
3rd Law of Thermodynamics
A perfect crystal at 0K has 0 entropy:
S(0) = 0
Defines the absolute entropy scale
Boltzmann Entropy:
Statistical definition of entropy
S = k ln(W)
W = # of microstates
Perfect crystal: W = 1 → S = 0
Phase Diagram
What does a P vs T phase diagram show?
Shows which phase (solid, liquid, gas) is most stable at each (P, T)
Phase boundaries = equilibrium between two phases
Triple point = all 3 phases coexist
Critical point = end of liquid-gas boundary (supercritical fluid)
What do these three phase boundaries represent?
Fusion curve: equilibrium ⇌ liquid
Vaporization curve: liquid ⇌ gas
Sublimation curve: solid ⇌ gas
Each point on a boundary = unique (P, T) where two phases coexist
Vapor Pressure:
Pressure of vapor in equilibrium with its liquid
function of T onle: Pvap(T)
Triple Point:
Unique (P, T) where s, l, g coexist
Degrees of freedom F = 0 → neither P nor T can vary
Critical Point:
Liquid-gas boundary ends
Above Tc: no liquids exists regardless of pressure
supercritical fluid forms → gas-like expansion, liquid-like density
The Gibbs Phase Rule
F = C - P + 2
For one-component (C = 1) systems: F = 3 - P
P = 1 → F = 2 (T and P vary freely)
P = 2 → F = 1 (boundary line)
P = 3 → F = 0 (triple point)
What condition defines phase equilibrium?
μA = μB
GA = GB
ΔG = 0 along phase boundaries
Clausius-Clapeyron Equation (general)
dp/dT = ΔS/ΔV = ΔH / TΔV
Vaporization form
ln(P2 / P1) = - ΔHvap / R (1/T2 - 1/T1)
Standard State
What is activity “a” and why do we use it?
Activity a corrects for non-ideal behavior so that
G - G0 = RT ln(a)
remains valid for all systems
standard state: a = 1
solids: a = 1
liquids: a = 1
ideal gas: a = P/P0
solute: a = y(c/c0)
solvent: a = yx
Reaction Gibbs Energy and Q
How is ΔG related to Q?
ΔG = ΔG0 + RT ln(Q)
Forward spontaneous if ΔG < 0
Reverse spontaneous if ΔG > 0
At equilibrium:
ΔG = 0, so:
ΔG0 = -RT ln(K)
Q = K
So can say:
ΔG = RT ln(Q / K)
What does magnitude of K tell us?
K > 1: products favored
K < 1: reactants favored
K = 1: neither favored
Even if ΔG0 > 0, K > 0 always (some forward reaction must occur)
Q vs K:
Q < K: forward spontaneous
Q > K: reverse spontaneous
Q = K: equilibrium
Van’t Hoff Equation
How does K change with temperature?
ln(K2 / K1) = - ΔH0 / R (1/T2 - 1/T1)
Assumes ΔH0 and ΔS0 are constant with T
Free Energy and Work
What is the physical meaning of ΔG?
At constant T and P:
-ΔG = Wmax
real processes are irreversible → actual work < max work
Temperature and Spontaneity
ΔH < 0, ΔS > 0 → spontaneous at all T
ΔH < 0, ΔS < 0 → spontaneous at low T
ΔH > 0, ΔS > 0 → spontaneous at high T
ΔH > 0, ΔS < 0 → never spontaneous
Electrochemistry, Cell Reaction Construction
How do you construct a full redox reaction from half-reactions?
Write both half-reactions as reductions
Cell reaction = (rhs) - (lhs)
Electrons must cancel → defines n
Ex:
Cu2+ + 2e- → Cu
Zn2+ + 2e- → Zn
Total: Cu2+ + Zn → Cu + Zn2+
Nernst Equation
E = E0 - RT/nF ln(Q)
at equilibrium: E = 0 → Q = K
Boiling Point Elevation
Why does adding solute raise the boiling point>
Solute lowers solvent vapor pressure → requires higher T to reach Pvap = Pext
Boiling point elevation:
ΔTb = KbbB
Kb = solvent-dependent
bB = molality
Depends only on # of solute particles, not identity
Freezing Point Depression
Why does adding solute lower the freezing point?
Solute disrupts crystal formation → requires lower T for solid to form
ΔTf = -KfbB
bB = n / m = mB / MB / msolvent
Depends only on # of solute particles
Osmosis
Flow of pure solvent → more concentrated solution through a membrane
Osmotic Pressure:
Π = cBRT
cB = n/V
Donnan Membrane Equilibrium
Donnan Potential:
E = -RT/ziF ln( [ion]2 / [ion]1)
zi: charge of ion
Why quantum mechanics?
Could not explain:
Blackbody radiation
Photoelectric effect
Line spectra
Planck’s Quantization
Energy is emitted/absorbed in discrete packets (photons)
E = hv = hc/λ
v = freq
Particle in a Box
Wavefunctions: chi(x) = sqrt(2/L) sin(n pi x / L)
Energies: En = n2h2/8mL2
Energy spacing increases with n
ΔE = hv gives absorption wavelength
Absorption vs Emission
hv = E2 - E1
Absorption: E1 → E2
Emission: E2 → E1
Beer-Lambert Law
A = εcl
A: absorbance
ε: molar extinction coefficient
c: concentration
l: path length
Transmittance Relation
A = -log10(T) = log10(I0 / I)
I: intensity
T = I / I0
Conjugation and λmax
More conjugation → smaller ΔE → longer lambda (red-shift)
Molecular Orbitals
Electronic transitions occur between MO’s
Linear combi of atomic orbitals → bonding (sigma, pi) + antibonding (sigma\, pi\) orbitals
Nonbonding (n) orbitals from lone pairs also participate
Rules MO electrons must follow:
Max 2 electrons per MO
Opposite spins (Pauli exclusion principle)
Fill lowest energy first (Aufbau)
Term Symbols and Spin multiplicity
Multiplicity = 2S + 1
S = total electron spin
Singlet (S=0), Triplet (S=1)
Frank-Condon Principle
Electronic transitions occur faster than nuclei can move
Geometry fixed during excitation (vertical transition)
Intensity depends on vibration wavefunction overlap
When is an electronic transition intense?
When initial and final vibrational wavefunctions have large overlaps → high probability density
Fluorescence
Absorption: S0 → S1 (vertical FC transition)
Vibrational relaxation (nonradiative)
Fluorescence: S1(v=0) → S0(v>0)
Relaxation to S0(v=0)
Stokes Shift
Fluorescence occurs at longer lambda (lower energy) than absorption due to vibrational relaxation before emission
IR Spectroscopy
What does IR spectroscopy probe?
vibrational transitions within the same electronic state
What is the IR unit wavenumber?
ν~ = 1/lambda (cm-1)
higher v~ → higher energy
Harmonic Oscillator Model
Bond modeled as spring:
F = -kx
energy levels equally spaced
selection rule: Δv = +-1
IR Activity Rule
When is a vibration IR active?
Dipole moment must change during vibration
Dipole moment: size of an electric dipole
Homonuclear diatomics → IR inactive
Heteronuclear → IR active
Morse Oscillator
Real bonds are anharmonic → allows:
Overtones (Δv = +-2, +-3, …)
Hot bands
Bond Dissociation
Number of Vibrational Modes
How many fundamental vibrational modes?
Linear: F = 3N - 5
Nonlinear: F = 3N - 6
Which nuclei are NMR-active?
Odd mass, odd atomic #, or both → nuclear spin I ≠ 0 → magnetic moment
13C and 1H
Spin states for C and H:
I = ½ → 2I + 1 = 2 states
mi = +1/2 (alpha, low E)
mi = -1/2 (beta, high E)
Energy Gap in NMR
Expression for ΔE between alpha and beta states?
ΔE = hv = yhB0
B0 increase → ΔE increase → v increase
Larmor Frequency
v = yB0/(2pi)
Precession freq of nuclear magnetic moment around B0
Resonance Condition
When does NMR absorption occur?
When RF photon matches ΔE:
hv = yhB0
spin flip alpha → beta
Chemical Shift (dirac)
dirac = v - vref / vref * 10^6 ppm
How do shielding effects change dirac?
Shielding: omega B < 0 → Bloc < B0 → dirac decreases (upfield)
Deshielding: omega B > 0 → Bloc > B0 → dirac increases (downfield)
What controls chemical shift?
Local electron density → shielding
electronegativity, hybridization, etc
1H NMR (chemical shift vs intensity)
1H NMR provides:
Location (chemical shift dirac)
Area (integration → # of H)
Fine structure (J-coupling → neighbors)
J-coupling Basics
What causes spin-spin splitting
Through bond coupling (1-5 bonds)
Neighboring spins (alpha/beta) shift resonance → multiplets
J (Hz) = constant, independent of B0
n+1 Rule
Splitting pattern for n neighboring nonequivalent protons?
Multiplicity = n + 1
Intensitiies follow Pascal’s triangle
AX Systems
Splitting pattern for an AX system:
A split by X → doublet
X split by A → doublet
2 doublets, same J
AX2 Systems
A split by 2 equivalent X → triplet (1:2:1)
X split by A → doublet
A3X2 Systems
CH2 has 3 neighbors → quartet (1:3:3:1)
CH3 has 2 neighbors → triplet (1:2:1)
OH usually a singlet (rapid exchange)