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Calorimetry
Measures heat of reaction
Heat from rxn that warms up water
q(water) = (water mass)(Cp)(DeltaT)
Heat from rxn warms “bomb”
q(bomb) = (heat capacity)(DeltaT)
-q(rxn) =
q(bomb) + q(water)
ΔH
Change in heat content of a system
q = ΔH
As long as pressure stays constant
ΔH =
Hfinal - Hinitial
-ΔH
Heat lost in rxn (exothermic)
+ΔH
Heat gained in rxn (endothermic)
State functions
Pathways from which you get from point a to point b don’t matter
Thermochemistry
Science of Energy Transfer as heat
Delta T
Measures Energy transfer
Thermodynamics depends on
Law of conservation of energy
Law of Conservation of Energy
The total energy of an isolated system remains constant but conserved over time.
Directionality of energy transfer
Energy transfer of heat is always from a hotter to a cooler object
1 Cal
4.184 Joules
ΔH
Enthalpy change
Enthalpy
The total heat content of a system under constant pressure
Ea
Activation energy
Heat Capacity
Amount of energy required to raise an object’s (size) temperature by 1 C
Specific heat capacity
Amount of energy required to raise a material’s (compound) temperature by 1 C
q
Heat lost or gained
Heat transfer equation
q = m*Cp*DeltaT
Heat (q) is related to:
Sample mass, Change in T, and Specific heat capacity (Cp)
0 C
Melting/ freezing point
100 C
Boiling/ condensation
ΔH fusion
335 J/ g
ΔH vapor
2330 J/ g
ΔH fusion is
Heat required to convert a solid at its melting point (0 C)
ΔH vapor
Heat required to convert a liquid at its boiling point (100 C)
Activated complex
Midway between reaction
Cp H20
4.184 J/ gC
Hess’s Law
If a reaction is the sum of other reactions, then the total enthalpy is the sum of the other enthalpies