Chemistry (Thermodynamics) Flashcards
Heat and temperature
Heat: Total energy applied.
Temperature: Average kinetic energy
Temperature ∝ Kinetic ∝ Velocity
Heat in joules and temp in Kelvins.
Liquid to gas
q= m (ΔH vaporation)
Solid to liquid
q= m(Δ fusion)
Heat capacity
calculating (q) of gas, solid, liquid heating up
Phase change: Q = m•ΔH(vap/fus)
Temp. Based: Q= m•C (specific heat)•ΔT
Calorimetry
Calorimeter measures heat exchange
1) heat lost is heat gained by another
a. -q lost = q gain
2) Adiabatic: no heat gained or lost.
3) Coffee cup calorimeter: constant pressure (gas can escape).
4) Calorie: amount of energy needed to increase 1g of water by 1°C
5) bomb calorimeter: constant volume
Q rxn= Q water (reaction will produce heat and be absorbed by water)
How to measure heat of water
Q rxn = m•Cp•ΔT water
STP and Standard conditions
STP: 0°C, 1atm. Used for ideal gas law
Standard Conditions: 25°C, 1atm. Used for G °, S °, H °, and E °
Enthalpy
Change in energy in a system
- Reactant molecules: bonds broken (energy in (+))
- Product molecules: bonds formed (energy out (-))
- equation: ΔH= Σin - Σout/ Σbonds broken - Σbonds formed.
Calculating ΔH: Bond Dissociation
Ereactants - Eproducts
2H2 + O2 —> 2H2O H-H: 435 KJ/mol O-H: 460 KJ/mol O-O: 500 KJ/mol 2(435) + (500) - 4(460)
Calculating ΔH: Heat of formation
ΔH= ΣHf products- ΣHf reactants
- zero for elements in standard state.
- Hf must be given
- fractions can be used.
Hess’ Law
Combine couple of reactions to form something new and individual enthalpies will add up.
Entropy
Number of things and space they occupy
Entropy: S= K (Boltzmann’s constant)•ln Ω
Loss of gas’s impacts entropy
Changes in entropy
ΔS= Σproducts - Σ reactants.
ΔS= ΔQ/T
Laws of thermodynamics
0th: ΔT means energy will flow
1st: energy always conserved (E= Q +W)
2nd: Entropy always increasing
3rd: Entropy of a solid at 0 Kelvins is zero!
Gibbs Free Energy
ΔG rxn= Gprod - G react
Gibbs free energy used to determine reaction spontaneity.
- ΔG>0 non spontaneous (+), ΔG<0 spontaneous (-), ΔG=0 equilibrium
Equilibrium using G
ΔG = ΔG° + RT ln Q
@equilibrium ΔG= 0 and Q= keq
∴ ΔG° = -RT ln (Keq)