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Energy and Chemical Reactions: Thermochemistry
orThermodynamics
Chapter Five
Chemistry 221 Professor Michael Russell
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Energy & Chemistry
Burning peanuts supplies sufficient energy to boil a cup of water
Burning sugar (sugar reacts with KClO3, a strong oxidizing agent)
These reactions are PRODUCT FAVORED They proceed almost completely from
reactants to products, perhaps with some outside assistance.
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Energy and ChemistryENERGY is the capacity to do
work or transfer heat. HEAT is the form of energy that
flows between 2 samples because of their difference in temperature.
Other forms of energy - • light – next chapter• electrical - CH 223• kinetic and potential
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Potential energy - energy a motionless body has by virtue of its position
In chemistry, positive and negative particles (ions) attract one another.
As the particles attract to make a bond, they have a lower potential energy
Potential Energy
NaCl - composed of Na+ and Cl- ions.
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Kinetic Energy
Three forms of kinetic energy:
Translational - from physics, KE = 1/2 mv2 = 0.5(mass)(velocity)2
Vibrational Rotational
translate
rotate
vibrate
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Internal Energy (E)PE + KE = Internal
Energy (E or U) The higher the T
the higher the internal energy
So, use changes in T (∆T) to monitor changes in E (∆E).
Page III-5-1 / Chapter Five Lecture Notes
Page III-5-1 / Chapter Five Lecture Notes
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Thermodynamics
Thermodynamics is the science of heat (energy) transfer.
Heat energy is associated with molecular motions (Kinetic Molecular Theory)
Heat transfers until thermal equilibrium is established.MAR
Directionality of Heat TransferHeat always transfers from the hot
object to the cooler object. EXOthermic: heat transfers from SYSTEM to SURROUNDINGS.
T(system) goes down T(surr) goes up - this is what we usually measure
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Directionality of Heat TransferHeat always transfers from the hot
object to the cooler object. ENDOthermic: heat transfers from SURROUNDINGS to the SYSTEM.
T(system) goes up T(surr) goes down - this is what we usually measure
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Energy & ChemistryAll of thermodynamics depends on
the law of CONSERVATION OF ENERGY.
• The total energy is unchanged in a chemical reaction.
• If PE of products is less than reactants, the difference must be released as KE.
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UNITS OF ENERGY1 calorie = heat required to
raise temp. of 1.00 g of H2O by 1.0 oC.
1000 cal = 1 kilocalorie = 1 kcal
1 kcal = 1 Calorie (a food "calorie")
But we use the unit called the JOULE
1 cal = 4.184 joules James Joule 1818-1889
Memorize 4.184! MAR
Specific Heat Capacity
Thermochemistry is the science of heat (energy) flow. A difference in temperature leads to energy transfer.
The heat, q, "lost" or "gained" is related to a) sample massb) change in T andc) specific heat capacity
Page III-5-2 / Chapter Five Lecture Notes
Page III-5-2 / Chapter Five Lecture Notes
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Specific Heat Capacity:
Substance Spec. Heat (J/g•K) H2O(l) 4.184
Ethylene glycol(l) 2.39 Al(s) 0.902 glass(s) 0.84
Aluminum
Water
The heat required to raise an object's temperature by 1 ˚C.
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q = mC TImportant!
q = heat "lost" or "gained" m = sample massC = specific heat capacity
T = change in temperatureT = final T - initial T
q is positive when heat flows in (cold surroundings) - endothermic
q is negative when heat flows out (hot surroundings) - exothermic
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Specific Heat CapacityIf 25.0 g of Al cool from
310. oC to 37 oC, how many joules of heat energy are lost by the Al?
q = mC∆T CAl = 0.902 J g-1 K-1 MAR
Specific Heat CapacityIf 25.0 g of Al cool from 310. oC to 37 oC, how
many joules of heat energy are lost by the Al? CAl = 0.902 J g-1 K-1
heat gain/lost = q = (mass)(sp. ht.)(∆T)
Notice that the negative sign on q signals heat "lost by" or transferred OUT of Al.
where ∆T = Tfinal - Tinitial
q = (25.0 g)(0.902 J/g•˚C)(37 - 310.)˚C q = - 6160 J
Notice also that ∆T can be either K or ˚C - the difference in temperatures is the same!
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Specific Heat CapacityA piece of iron (88.5 g) at 77.8 oC is placed in 244 g
of water at 18.8 oC. What is the final temperature of the mixture?
By the law of conservation of energy:
qhot + qcold = 0, or
mFeCFe∆TFe + mwaterCwater∆Twater = 0
CFe = 0.449 J g-1 K-1
Cwater = 4.184 J g-1 K-1 Memorize
Final Temperature (warm) same for Fe & H2OMAR
Specific Heat Capacity
qhot + qcold = 0
mFeCFe∆TFe + mwaterCwater∆Twater = 0
88.5 * 0.449 * (Tf - 77.8) + 244 * 4.184 * (Tf - 18.8) = 0
39.7Tf - 3090 + 1020Tf - 19200 = 0
1060Tf = 22300
Tf = 21.0 oC
Efficient method to determine approximate final temperature of mixture
Fe (88.5 g, 0.449 J/g•K, 77.8 oC) and water (244 g, 4.184 J/g•K, 18.8 oC); final temperature?
Page III-5-3 / Chapter Five Lecture Notes
Page III-5-3 / Chapter Five Lecture Notes
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Heat TransferNo Change in State
q transferred = (mass)(sp. ht.)(∆T)
Heat Transfer with Change of State
As matter absorbs heat, its temperature rises until it undergoes a phase change (change of state)
Changes of state involve energy (at constant T) Ice + 333 J/g (heat of fusion) -----> Liquid water
q = (heat of "something")("mass")
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Heat of fusion of ice = 333 J/gSpecific heat of water = 4.184 J/g•K
Heat of vaporization = 2260 J/g
What quantity of heat is required to melt 500. g of ice at 0.0 oC and heat the water to steam at 100.0 oC?
+333 J/g
Heat & Changes of State
solid (ice) liquid (0 – 100 °C) gas (steam)
+2260 J/g
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What quantity of heat is required to melt 500. g of ice at 0.0 oC and heat the water to steam at 100.0 oC?
1. To melt ice q = (500. g)(333 J/g) = 1.67 x 105 J2. To raise water from 0.0 oC to 100.0 oC q = (500. g)(4.184 J/g•K)(100. - 0.)K = 2.09 x 105 J3. To evaporate water at 100. oC q = (500. g)(2260 J/g) = 1.13 x 106 J4. Total heat energy = 1.51 x 106 J = 1510 kJ
Heat & Changes of State
Heat Transfer covered more in Chapter 12 of CH 222
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CHEMICAL REACTIVITYWhat drives chemical
reactions? How do they occur, and how fast?
The first question is answered by
THERMODYNAMICS, and the second question is answered by KINETICS.
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CHEMICAL REACTIVITYTHERMODYNAMICS dictates if the reaction will
occur or not.
Sand will not decompose into silicon and oxygen
Paper will combine with oxygen to burn
Page III-5-4 / Chapter Five Lecture Notes
Page III-5-4 / Chapter Five Lecture Notes
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CHEMICAL REACTIVITYKINETICS dictates how fast the reaction will
occur.Example: diamond into graphite is
thermodynamically favored, but the kinetics of the reaction is too slow to be of useful
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CHEMICAL REACTIVITYWe have already seen a number of
"driving forces" for reactions that are PRODUCT-FAVORED.
• formation of a precipitate• gas formation• H2O formation (acid-base reaction)• electron transfer in a battery
In general, reactions that transfer energy to their
surroundings are product-favored.
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FIRST LAW OF THERMODYNAMICS
∆E = q + w
heat energy transferred
energy change
work done by the system
Energy is conserved! Chemists focus on q more than w
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ENTHALPYMost chemical reactions occur at constant P, so
∆E = q + w and ∆E = ∆H + w (P const)
w is usually small, so ∆H ≈ ∆E
Heat transferred at constant P = qp
qp = ∆H where H = enthalpy
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If Hfinal < Hinitial then ∆H is negativeProcess is EXOTHERMIC
∆H is negative
If Hfinal > Hinitial then ∆H is positiveProcess is ENDOTHERMIC
∆H is positive
ENTHALPY∆H = Hfinal - Hinitial
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Consider the formation of waterH2(g) + 1/2 O2(g) --> H2O(g) + 241.8 kJ
Exothermic reaction - heat is a "product" and ∆H = – 241.8 kJ
USING ENTHALPY
Page III-5-5 / Chapter Five Lecture Notes
Page III-5-5 / Chapter Five Lecture Notes
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Making liquid H2O from H2 + O2 involves two exothermic steps.
USING ENTHALPY
H2 + O2 gas
Liquid H2OH2O vapor
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Making H2O from H2 involves two steps.H2(g) + 1/2 O2(g) ---> H2O(g) + 242 kJH2O(g) ---> H2O(liq) + 44 kJ ----------------------------------------------
H2(g) + 1/2 O2(g) --> H2O(liq) + 286 kJExample of HESS'S LAW-If a rxn. is the sum of 2 or more others, the net ∆H is the sum of the ∆H's of the other rxns.
USING ENTHALPY
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Hess's Law & Energy Level Diagrams
Forming H2O can occur in a single step or in a two steps. ∆Htotal is the same no matter which path is followed.
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Hess's Law & Energy Level Diagrams
Forming CO2 can occur in a single step or in a two steps. ∆Htotal is the same no matter which path is followed.
∆H is a STATE FUNCTION - depends only on the state of the system and not how it got there.
Other state functions: V, T, P, and energy
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Standard Enthalpy ValuesMost ∆H values are labeled ∆Ho Measured under standard conditions
P = 1 bar (approx. 1 atm) Concentration = 1 mol/LT = usually 25 oC
with all species in standard statesi.e., C = graphite and O2 = gas
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Enthalpy Values
H2(g) + 1/2 O2(g) --> H2O(g)∆H˚ = -242 kJ
2 H2(g) + O2(g) --> 2 H2O(g)
∆H˚ = -484 kJ H2O(g) ---> H2(g) + 1/2 O2(g)
∆H˚ = +242 kJ H2(g) + 1/2 O2(g) --> H2O(liquid)
∆H˚ = -286 kJ
Depend on how the reaction is written and on phases of reactants and products
Page III-5-6 / Chapter Five Lecture Notes
Page III-5-6 / Chapter Five Lecture Notes
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Standard Enthalpy ValuesNIST (Nat'l Institute for Standards and
Technology) gives values of ∆Hf
o = standard molar enthalpy of formation
- the enthalpy change when 1 mol of compound is formed from elements under standard conditions.
These values are available in your text
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∆Hfo, standard molar
enthalpy of formation
H2(g) + 1/2 O2(g) --> H2O(g)
∆Hfo (H2O, g)= -241.8 kJ/mol
By definition,
∆Hfo = 0 for elements in their standard states.
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Using Standard Enthalpy Values
Use ∆H˚ values to calculate the enthalpy change for:
H2O(g) + C(graphite) --> H2(g) + CO(g)
(product is called "water gas")
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Using Standard Enthalpy Values
Find enthalpy change for this reaction:
H2O(g) + C(graphite) --> H2(g) + CO(g)
From reference books we find:
H2(g) + 1/2 O2(g) --> H2O(g)
∆Hf˚ of H2O vapor = - 242 kJ/mol
C(s) + 1/2 O2(g) --> CO(g)
∆Hf˚ of CO = - 111 kJ/mol
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Using Standard Enthalpy Values
H2O(g) --> H2(g) + 1/2 O2(g) ∆Ho = +242 kJ
C(s) + 1/2 O2(g) --> CO(g) ∆Ho = -111 kJ
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To convert 1 mol of water to 1 mol each of H2 and CO requires 131 kJ of energy. The "water gas" reaction is ENDOthermic.
H2O(g) + C(graphite) --> H2(g) + CO(g) ∆Honet = +131 kJ
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Using Standard Enthalpy ValuesFind ∆Ho
rxn for CaCO3(s) --> CaO(s) + CO2(g)
using Hess's Law and:
Ca(s) + 3/2 O2(g) + C(s) --> CaCO3(s)
∆Hof = -1206.2 kJ as well as
Ca(s) + 3/2 O2(g) + C(s) --> CaO(s) + CO2(g)
∆Horxn = -1028.6 kJ
CaCO3
CaO
Page III-5-7 / Chapter Five Lecture Notes
Page III-5-7 / Chapter Five Lecture Notes
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Using Standard Enthalpy Values
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Using Standard Enthalpy ValuesFind ∆Ho
rxn for CaCO3(s) --> CaO(s) + CO2(g)
CaCO3(s) --> Ca(s) + 3/2 O2(g) + C(s)
∆Ho = -(-1206.2 kJ) = +1206.2 kJ
Ca(s) + 3/2 O2(g) + C(s) --> CaO(s) + CO2(g)
∆Horxn = -1028.6 kJ
----------------------------------------------------------- CaCO3(s) --> CaO(s) + CO2(g), and
∆Horxn = +1206.2 kJ + (-1028.6 kJ) = +177.6 kJ
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Using Standard Enthalpy Values
In general, when ALL enthalpies of formation are known,
Calculate ∆H of reaction?
∆Horxn =
Σ ∆Hfo (products)
- Σ ∆Hfo (reactants)
Remember that ∆ = final – initial
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Using Standard Enthalpy Values
Answer: ∆Ho
rxn = {∆Hfo
(CaO) + ∆Hfo
(CO2)} - {∆Hfo
(CaCO3)} ∆Ho
rxn = {-635.1 + -393.5} - {-1206.2}
∆Horxn = +177.6 kJ
Same answer as before with Hess's Law, but simpler
Example: Find ∆Horxn for
CaCO3(s) --> CaO(s) + CO2(g) using:
∆Horxn = Σ ∆Hf
o (prod) - Σ ∆Hf
o (react)
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Using Standard Enthalpy ValuesCalculate the heat of combustion of
methanol, i.e., ∆Horxn for
CH3OH(g) + 3/2 O2(g) --> CO2(g) + 2 H2O(g)
∆Horxn = Σ ∆Hf
o (prod) - Σ ∆Hf
o (react)
As before, look up ∆Hfo values for reactants
and products in your text Elements in standard states have ∆Hf
o = 0
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Using Standard Enthalpy Values
∆Horxn = {∆Hf
o (CO2) + 2 ∆Hf
o (H2O)}
- {3/2 ∆Hfo
(O2) + ∆Hfo
(CH3OH)} = {(-393.5 kJ) + 2 (-241.8 kJ)} - {0 + (-201.5 kJ)} ∆Ho
rxn = -675.6 kJ per mol of methanol
CH3OH(g) + 3/2 O2(g) --> CO2(g) + 2 H2O(g) ∆Ho
rxn = Σ ∆Hfo (prod) - Σ ∆Hf
o (react)
Page III-5-8 / Chapter Five Lecture Notes
Page III-5-8 / Chapter Five Lecture Notes
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Measuring Heats of ReactionCALORIMETRY
Constant Volume "Bomb" Calorimeter
• Burn combustible sample.
• Measure heat evolved in a reaction.
• Derive ∆E for reaction.
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Calorimetry
Some heat from reaction warms water qwater = (sp. ht.)(water mass)(∆T)
Some heat from reaction warms "bomb" qbomb = (heat capacity, J/K)(∆T)
Total heat evolved = qtotal = qwater + qbomb
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Calculate heat of combustion of octane: C8H18 + 25/2 O2 -->
8 CO2 + 9 H2O
• Burn 1.00 g of octane • Temp rises from 25.00 to 33.20 oC • Calorimeter contains 1200. g water • Heat capacity of bomb = 837 J/K
Measuring Heats of ReactionCALORIMETRY
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Step 1 Calc. heat transferred from reaction to water.
q = (4.184 J/g•K)(1200. g)(8.20 K) = 41,200 JStep 2 Calc. heat transferred from
reaction to bomb.q = (bomb heat capacity)(∆T) = (837 J/K)(8.20 K) = 6860 JStep 3 Total heat evolved 41,200 J + 6860 J = 48,100 JHeat of combustion of 1.00 g of octane =
- 48.1 kJ (-5.48*103 kJ/mol)
Measuring Heats of ReactionCALORIMETRY
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End of Chapter Five
See also: • Chapter Five Study Guide • Chapter Five Concept Guide
Page III-5-9 / Chapter Five Lecture Notes
Page III-5-9 / Chapter Five Lecture Notes