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Chemistry Chapter-5-PowerPoint-Lecture-PDF.pdf
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Oct 08, 2025
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About This Presentation
Chemistry
Size:
2.72 MB
Language:
en
Added:
Oct 08, 2025
Slides:
54 pages
Slide Content
Slide 1
Chapter 5
Thermochemistry
John D. Bookstaver
St. Charles Community College
Cottleville, MO
Lecture Presentation
© 2012Pearson Education, Inc.
Slide 2
Thermochemistry
© 2012 Pearson Education, Inc.
Energy
•Energyis the ability to do work or
transfer heat.
–Energy used to cause an object that has
mass to move is called work.
–Energy used to cause the temperature of
an object to rise is called heat.
Slide 3
Thermochemistry
© 2012 Pearson Education, Inc.
Kinetic Energy
Kinetic energyis energy an object
possesses by virtue of its motion:
1
2
E
k= mv
2
Slide 4
Thermochemistry
© 2012 Pearson Education, Inc.
Potential Energy
•Potential energyis
energy an object
possesses by virtue of
its position or chemical
composition.
•The most important
form of potential energy
in molecules is
electrostatic potential
energy, E
el:
KQ
1Q
2
d
E
el=
Slide 5
Thermochemistry
© 2012 Pearson Education, Inc.
Units of Energy
•The SI unit of energy is the joule (J):
•An older, non-SI unit is still in
widespread use: the calorie (cal):
1 cal = 4.184 J
1 J =1
kg m
2
s
2
Slide 6
Thermochemistry
© 2012 Pearson Education, Inc.
Definitions: System and Surroundings
•The systemincludes the
molecules we want to
study (here, the hydrogen
and oxygen molecules).
•The surroundingsare
everything else (here, the
cylinder and piston).
Slide 7
Thermochemistry
© 2012 Pearson Education, Inc.
Definitions: Work
•Energy used to
move an object over
some distance is
work:
•w= Fd
where wis work, F
is the force, and dis
the distance over
which the force is
exerted.
Slide 8
Thermochemistry
© 2012 Pearson Education, Inc.
Heat
•Energy can also be
transferred as heat.
•Heat flows from
warmer objects to
cooler objects.
Slide 9
Thermochemistry
© 2012 Pearson Education, Inc.
Conversion of Energy
•Energy can be converted from one type to
another.
•For example, the cyclist in Figure 5.2 has
potential energy as she sits on top of the hill.
Slide 10
Thermochemistry
© 2012 Pearson Education, Inc.
Conversion of Energy
•As she coasts down the hill, her potential
energy is converted to kinetic energy.
•At the bottom, all the potential energy she
had at the top of the hill is now kinetic energy.
Slide 11
Thermochemistry
© 2012 Pearson Education, Inc.
First Law of Thermodynamics
•Energy is neither created nor destroyed.
•In other words, the total energy of the universe is
a constant; if the system loses energy, it must be
gained by the surroundings, and vice versa.
Slide 12
Thermochemistry
© 2012 Pearson Education, Inc.
Internal Energy
The internal energyof a system is the sum of all
kinetic and potential energies of all components
of the system; we call it E.
Slide 13
Thermochemistry
© 2012 Pearson Education, Inc.
Internal Energy
By definition, the change in internal energy, E,
is the final energy of the system minus the initial
energy of the system:
E= E
final−E
initial
Slide 14
Thermochemistry
© 2012 Pearson Education, Inc.
Changes in Internal Energy
•If E> 0, E
final> E
initial
–Therefore, the system absorbedenergy
from the surroundings.
–This energy change is called endergonic.
Slide 15
Thermochemistry
© 2012 Pearson Education, Inc.
Changes in Internal Energy
•If E< 0, E
final< E
initial
–Therefore, the system releasedenergy to
the surroundings.
–This energy change is called exergonic.
Slide 16
Thermochemistry
© 2012 Pearson Education, Inc.
Changes in Internal Energy
•When energy is
exchanged between
the system and the
surroundings, it is
exchanged as either
heat (q) or work (w).
•That is, E= q+ w.
Slide 17
Thermochemistry
© 2012 Pearson Education, Inc.
E, q, w, and Their Signs
Slide 18
Thermochemistry
© 2012 Pearson Education, Inc.
Exchange of Heat between System and
Surroundings
•When heat is absorbed by the system from the
surroundings, the process is endothermic.
Slide 19
Thermochemistry
© 2012 Pearson Education, Inc.
Exchange of Heat between System and
Surroundings
•When heat is absorbed by the system from the
surroundings, the process is endothermic.
•When heat is released by the system into the
surroundings, the process is exothermic.
Slide 20
Thermochemistry
© 2012 Pearson Education, Inc.
State Functions
Usually we have no way of knowing the
internal energy of a system; finding that value
is simply too complex a problem.
Slide 21
Thermochemistry
© 2012 Pearson Education, Inc.
State Functions
•However, we do know that the internal energy
of a system is independent of the path by
which the system achieved that state.
–In the system depicted in Figure 5.9, the water
could have reached room temperature from either
direction.
Slide 22
Thermochemistry
© 2012 Pearson Education, Inc.
State Functions
•Therefore, internal energy is a state function.
•It depends only on the present state of the
system, not on the path by which the system
arrived at that state.
•And so, Edepends only on E
initialand E
final.
Slide 23
Thermochemistry
© 2012 Pearson Education, Inc.
State Functions
•However,qand ware
notstate functions.
•Whether the battery is
shorted out or is
discharged by running
the fan, its Eis the
same.
–But qand ware different
in the two cases.
Slide 24
Thermochemistry
© 2012 Pearson Education, Inc.
Work
Usually in an open
container the only work
done is by a gas
pushing on the
surroundings (or by
the surroundings
pushing on the gas).
Slide 25
Thermochemistry
© 2012 Pearson Education, Inc.
Work
We can measure the work done by the gas if
the reaction is done in a vessel that has been
fitted with a piston:
w= −PV
Slide 26
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpy
•If a process takes place at constant
pressure (as the majority of processes we
study do) and the only work done is this
pressure–volume work, we can account
for heat flow during the process by
measuring the enthalpy of the system.
•Enthalpyis the internal energy plus the
product of pressure and volume:
H= E+ PV
Slide 27
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpy
•When the system changes at constant
pressure, the change in enthalpy, H, is
H= (E+ PV)
•This can be written
H= E+ PV
Slide 28
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpy
•Since E= q+ wand w= −PV, we
can substitute these into the enthalpy
expression:
H= E+ PV
H= (q + w) −w
H= q
•So, at constant pressure, the change in
enthalpy isthe heat gained or lost.
Slide 29
Thermochemistry
© 2012 Pearson Education, Inc.
Endothermicity and Exothermicity
•A process is
endothermic
when His
positive.
Slide 30
Thermochemistry
© 2012 Pearson Education, Inc.
Endothermicity and Exothermicity
•A process is
endothermic
when His
positive.
•A process is
exothermic when
His negative.
Slide 31
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpy of Reaction
The changein
enthalpy, H, is the
enthalpy of the
products minus the
enthalpy of the
reactants:
H= H
products−H
reactants
Slide 32
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpy of Reaction
This quantity, H, is called the enthalpy of
reaction, or the heat ofreaction.
Slide 33
Thermochemistry
© 2012 Pearson Education, Inc.
The Truth about Enthalpy
1.Enthalpy is an extensive property.
2.Hfor a reaction in the forward
direction is equal in size, but opposite
in sign, to Hfor the reverse reaction.
3.Hfor a reaction depends on the state
of the products and the state of the
reactants.
Slide 34
Thermochemistry
© 2012 Pearson Education, Inc.
Calorimetry
Since we cannot
know the exact
enthalpy of the
reactants and
products, we
measure Hthrough
calorimetry, the
measurement of
heat flow.
Slide 35
Thermochemistry
© 2012 Pearson Education, Inc.
Heat Capacity and Specific Heat
The amount of energy required to raise the
temperature of a substance by 1 K (1C) isits
heat capacity.
Slide 36
Thermochemistry
© 2012 Pearson Education, Inc.
Heat Capacity and Specific Heat
We define specific
heat capacity(or
simply specific heat)
as the amount of
energy required to
raise the temperature
of 1 g of a substance
by 1 K (or 1 C).
Slide 37
Thermochemistry
© 2012 Pearson Education, Inc.
Heat Capacity and Specific Heat
Specific heat, then, is
Specific heat=
heat transferred
mass temperature change
s=
q
mT
Slide 38
Thermochemistry
© 2012 Pearson Education, Inc.
Constant Pressure Calorimetry
By carrying out a
reaction in aqueous
solution in a simple
calorimeter such as this
one, one can indirectly
measure the heat
change for the system
by measuring the heat
change for the water in
the calorimeter.
Slide 39
Thermochemistry
© 2012 Pearson Education, Inc.
Constant Pressure Calorimetry
Because the specific
heat for water is well
known (4.184 J/g-K), we
can measure Hfor the
reaction with this
equation:
q= msT
Slide 40
Thermochemistry
© 2012 Pearson Education, Inc.
Bomb Calorimetry
•Reactions can be
carried out in a sealed
“bomb” such as this
one.
•The heat absorbed
(or released) by the
water is a very good
approximation of the
enthalpy change for
the reaction.
Slide 41
Thermochemistry
© 2012 Pearson Education, Inc.
Bomb Calorimetry
•Because the volume
in the bomb
calorimeter is
constant, what is
measured is really the
change in internal
energy, E, not H.
•For most reactions,
the difference is very
small.
Slide 42
Thermochemistry
© 2012 Pearson Education, Inc.
Hess’s Law
His well known for many reactions,
and it is inconvenient to measure H
for every reaction in which we are
interested.
•However, we can estimate Husing
published Hvalues and the
properties of enthalpy.
Slide 43
Thermochemistry
© 2012 Pearson Education, Inc.
Hess’s Law
Hess’s law states that
“[i]f a reaction is
carried out in a series
of steps, Hfor the
overall reaction will be
equal to the sum of
the enthalpy changes
for the individual
steps.”
Slide 44
Thermochemistry
© 2012 Pearson Education, Inc.
Hess’s Law
Because His a state
function, the total
enthalpy change
depends only on the
initial state of the
reactants and the final
state of the products.
Slide 45
Thermochemistry
© 2012 Pearson Education, Inc.
Enthalpies of Formation
An enthalpy of formation, H
f, is defined
as the enthalpy change for the reaction
in which a compound is made from its
constituent elements in their elemental
forms.
Slide 46
Thermochemistry
© 2012 Pearson Education, Inc.
Standard Enthalpies of Formation
Standard enthalpies of formation, H
f°,are
measured under standard conditions (25 °C
and 1.00 atm pressure).
Slide 47
Thermochemistry
© 2012 Pearson Education, Inc.
Calculation of H
•Imagine this as occurring
in three steps:
C
3H
8(g) + 5O
2(g)3CO
2(g) + 4H
2O(l)
C
3H
8(g)3C
(graphite)+ 4H
2(g)
Slide 48
Thermochemistry
© 2012 Pearson Education, Inc.
Calculation of H
•Imagine this as occurring
in three steps:
C
3H
8(g)3C
(graphite)+ 4H
2(g)
3C
(graphite)+ 3O
2(g) 3CO
2(g)
C
3H
8(g) + 5O
2(g)3CO
2(g) + 4H
2O(l)
Slide 49
Thermochemistry
© 2012 Pearson Education, Inc.
Calculation of H
•Imagine this as occurring
in three steps:
C
3H
8(g)3C
(graphite)+ 4H
2(g)
3C
(graphite)+ 3O
2(g) 3CO
2(g)
4H
2(g) + 2O
2(g) 4H
2O(l)
C
3H
8(g) + 5O
2(g)3CO
2(g) + 4H
2O(l)
Slide 50
Thermochemistry
© 2012 Pearson Education, Inc.
C
3H
8(g)3C
(graphite)+ 4H
2(g)
3C
(graphite)+ 3O
2(g) 3CO
2(g)
4H
2(g) + 2O
2(g) 4H
2O(l)
C
3H
8(g) + 5O
2(g) 3CO
2(g)+ 4H
2O(l)
Calculation of H
•The sum of these
equations is
C
3H
8(g) + 5O
2(g)3CO
2(g) + 4H
2O(l)
Slide 51
Thermochemistry
© 2012 Pearson Education, Inc.
Calculation of H
We can use Hess’s law in this way:
H= nH
f,products–mH
f°
,reactants
where nand mare the stoichiometric
coefficients.
Slide 52
Thermochemistry
© 2012 Pearson Education, Inc.
H= [3(−393.5 kJ) + 4(−285.8 kJ)] –[1(−103.85 kJ) + 5(0 kJ)]
= [(−1180.5 kJ) + (−1143.2 kJ)] –[(−103.85 kJ) + (0 kJ)]
= (−2323.7 kJ) –(−103.85 kJ) = −2219.9 kJ
Calculation of H
C
3H
8(g) + 5O
2(g)3CO
2(g) + 4H
2O(l)
Slide 53
Thermochemistry
© 2012 Pearson Education, Inc.
Energy in Foods
Most of the fuel in the food we eat comes
from carbohydrates and fats.
Slide 54
Thermochemistry
© 2012 Pearson Education, Inc.
Energy in Fuels
The vast
majority of the
energy
consumed in
this country
comes from
fossil fuels.
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