Thursday, February 13
5.2.3: Distinguish quantities that are state functions from those that are not.
5.4.1: Interpret the enthalpy of reaction, ΔH, using the enthalpies of the products and reactants.
5.4.2: Determine how ΔH changes when the equation for a balanced reaction is multiplied by the same number, or when the reaction is reversed.
5.5.1: Interpret heat capacity and specific heat as measures of the heat needed to change the temperature of a substance.
5.5.2: Use the relationships among Cs, q, m, and ΔT to calculate one of the values given the other three.
5.5.3: Describe how a constant-pressure calorimeter works and analyze the results of constant-pressure calorimetry to determine heats of reactions.
State Function:
Only the values of the initial and final states matter.
The steps between or the path followed does not change the value of the function.
Path Function:
The path between initial and final states changes the value of the function.
Example: Change in elevation is a state function, while distance walked is a path function.
Thermal Energy Released:
When 4.50 g of methane gas is burned in a constant-pressure system.
ΔH_rxn = −890 kJ/mol CH4(g) + 2 O2(g) → CO2(g) + 2 H2O(l)
For 4.50 g CH4:
Molar mass of CH4 ≈ 16 g/mol
Energy released:
ΔH = -890 kJ/mol × (4.50 g / 16 g/mol) = -250 kJ
Hydrogen Peroxide Reaction:
2.50 g of aluminum reacts at constant pressure:
2 Al(s) + Fe2O3(s) → 2 Fe(s) + Al2O3(s)
ΔH = −851.5 kJ
Calorimetry: Measurement of heat flow to determine ΔH.
Calorimeter: Instrument to measure heat flow.
Formula: SH = q
Heat Capacity: Energy required to raise temperature of a substance by 1 K (1°C).
Specific Heat (Cs): Heat capacity for 1 gram of substance.
Molar Heat Capacity: Heat capacity for 1 mole of substance.
Data Table:
Specific heats for common substances at 298 K:
N2(g): 1.04 J/g·K
H2O(l): 4.18 J/g·K
Al(g): 0.90 J/g·K
Fe(s): 0.45 J/g·K
CH4(g): 2.20 J/g·K
CaCO3(s): 0.82 J/g·K
Reactions in aqueous solution allow measuring heat change for water in the calorimeter.
Specific Heat of Water: 4.184 J/g·K (used for dilute solutions).
Heat Change Calculation:
q = m × Cs × ΔT
This formula is essential for determining ΔH.
Heating Water:
Calculate heat needed to warm 250 g of water from 22°C to 97°C:
q = (250 g) × (4.184 J/g·K) × (97°C - 22°C)
q = 78 kJ
Molar Heat Capacity of Water:
Use specific heat value in calculations.
Rocks for Heat Storage:
Calculate heat absorbed by 50.0 kg of rocks with specific heat of 0.82 J/g·K and a temperature increase of 12.0°C.
HCl and NaOH Reaction:
Mixing amounts of HCl and NaOH increases temperature from 21.0 to 27.5°C.
Calculate ΔH per mole of HCl:
Total volume = 0.10 L, density = 1.0 g/mL, specific heat = 4.18 J/g·K.
HCl and AgNO3 Reaction:
Mixing amounts increases temperature from 22.30 to 23.11°C.
Reactions in a sealed bomb calorimeter yield heat absorbed or released as an approximation of the enthalpy change for the reaction.
Formula: q_rxn,cal = −C × ΔT.
Bomb calorimeter’s constant volume measures change in internal energy, ΔE, not ΔH.
Difference is typically small for most reactions, allowing for equating ΔE with ΔH.