Thermochemistry - Washington University in St. · PDF fileChapter 4 Thermochemistry 4.1 Energy...
Transcript of Thermochemistry - Washington University in St. · PDF fileChapter 4 Thermochemistry 4.1 Energy...
Chapter 4
Thermochemistry
4.1 Energy Storage and Refer-
ence
Thermochemistry is the study of the energy released
when the atomic-level “associations” are changed. A
chemical reaction (rxn) is one where these associations
change.
We are free to choose our energy reference, or zero
of energy, as we please. We could choose the reference to
be separated atoms. However, as you will see, a smarter
choice for our standard state is the most stable elemental
form at a convenient T and P. Once the zero is cho-
sen, our job is: to follow the energy. That means, if the
atom-atom associations change to a more energetically
favorable arrangement, there must be an exactly com-
pensating release of energy which we can measure with
the aid of calorimeters.
4.2 Chemical Rxns
Consider the formation of a molecule of 2 in the gas
phase. (By in the gas phase we mean that there are no
interactions between 2 units. (This is an idealization
achieved only at low .)
() +2()→ 2()
1. We take the most stable elemental form at 1 bar and
the specified temperature (usually 298.15 K) as the
REFERENCE state for the energy state function
. That is, the = ≡ 02. The combustion of diamond (to 2) yields almost
2 kJ/mole more energy than does graphite at STP.
This means that at modest pressures diamond has
a higher enthalpy than graphite, i.e. diamond is
“metastable” wrt graphite at STP. However, the
barrier is so large that diamonds will easily out-
last human-kind and therefore we can consider dia-
monds a stationary state.
3. A reaction with a -ve ∆ ≡[(P)− (R)] meansthat the enthalpy is lower for the products, i.e. the
reaction is energetically “down-hill”. This type of
reaction is called exothermic, and as energy must
be conserved, some energy will come “out”. If your
holding the beaker (a diabatic vessel), your hand
will feel the energy released (from the molecular as-
sociations sector into molecular kinetic energy), as
the reaction proceeds.
4.3 Hess’s law
4.3.1 Overview
1. Hess’s law is no more than a reminder that enthalpy
is a state function.H = 0 =
P .
2. For a specified reaction,
+ → + ; ∆ =P
∆.
The stoichiometric coefficients being +ve for
products and -ve for reactants. This sign conven-
tion achieves the ∆ ≡ P− R Think about it thisway: The energy (heat) released and enthalpy are on
opposite sides of an equation that balances energy
as well atoms. Therefore energy balanced reaction
expressions would read
+ → + + or
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∆ + + → +
Energy Q ∆h Name
out +ve -ve exothermic
in -ve +ve endothermic
3. The value of ∆ only makes sense in the context
of a reaction with specified coefficients. (The sub-
script is telling you, the reader, to look for the
balanced equation that the writer is referring to.) In
other words, if an alternate reaction0 is specified as
2+ 2 → 2 + 2 then
∆0 = 2∆
Definition 1 The subscript refers to “one unit
of the reaction” with the stoichiometric coefficients
as written. This means, any quantity such as
∆ has an implied reaction with specified coef-
ficients. The change (∆) refers to taking the sto-
ichiometric coefficient number of moles of R and
converting them into P.
4. Hess’s law is most often applied to get the standard
(P= 1 bar, T
= 298.15 K) enthalpy of reac-
tion, which would read, for a rxn statement with
specified stoichiometric coefficients ,
∆ =P
∆.
Definition 2 The standard enthalpic state ( =
= 0) is taken (for convenience) to be that of the
most stable elemental form at STP.
Definition 3 If the reaction produces a single mole
of product ( = 1) from the elements in their stan-
dard states then ∆=∆
5. Consider this example.
Note that there are 4 measurable enthalpies, 3
of which would be standard enthalpies (if P=1 bar,
T=298.15 K) of formation:
∆ [2] = −286 [
]∆ [] = −635 [
]
and ∆ [()2] = −985 [
]
Therefore, for the rxn 2 + →, we have∆ = ∆
[()2]−(∆ [2]+∆
[])
= −64 []
4.3.2 Bond Enthalpies (energies)
One can get enthalpies corresponding to average bond
energies. These bond enthalpies are extremely valuable
in building up (in a ticker-toy fashion) estimates of the
enthalpies of molecules1. These energies are useful for
systems with no delocalized bonding. Values for organ-
ics are far more accurate than those for inorganics. Using
tables like those given in the text on pg. 69 (also found
on the WWW) are the starting point. To help under-
stand what bond enthalpies are, what they are not and
how to use them, consider the following examples.
1. The enthalpy of 4 is 1664 kJ/mole less than that
of the separated atoms.
(a) Therefore, − ≡ 166344
= 416
(b) The energy required to dissociate one H from
4 is 427 .
∆ = +427 .
2. Review example 4.1 in the text, − = 4635
kJ/mole.
3. Do problem 4.30, pg 78. ....
4. Finally, consider the enthalpy of formation
22(), i.e.
2( ) + 2()→ 22() ;∆
Enthalpy diagram for 22 All values in
1The utility of bond enthalpies is that much (but certainly not
all) of chemistry is “local”.
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The value of∆ (22()) can be estimated from
the following data.
(a) The energy released to form 22 from
atomic elements. This energy is a sum of bond
enthalpies2.
2() + 2()→ 22();
−[− + 2−] =−[172 + 2(261)] = −695[
]
(b) The value of ∆ for 2,
2()→ 2() ;∆ = 2434[
]
(c) The energy required to take atoms of from
the reference state to the gas phase.
2()→ 2() ;∆ = 2 ∗ 2271[
]
(d) Adding the above (a+b+c) we estimate,
∆ (22()) = 25 []
a result that relies on estimates of the bond enthalpies.
Remark 1 Note this is inaccurate as it involves the
difference between large numbers with a resulting small
value. This is a situation always to be avoided if at all
possible. This points to WHY we choose the reference
states to be the stable forms at a convenient T and P
rather than say the separated atoms. Let me elaborate
on this point. Consider the molecules O2 and N2. The
enthalpies associated with these bonds are 494 and 942
kJ/mole, respectively. (The binding energy of N2, the
triple bond, is one of the strongest molecular bonds.) If
we chose our reference state to be the separated atoms,
the molecular enthalpies would be H=(O2) = -494
and H=(N2) = -942 kJ/mole below the separated
atoms. In general, the bonded forms are hundreds of
kJ (100 kJ/mole = 1.03 ev/unit), in association energy,
below the separated atoms. As we are almost always in-
terested in the enthalpy difference between bonded forms,
it is convenient to take our reference as a bonded form.
This largely avoids taking the difference between large
numbers.
Remark 2 An analogy: Say we are interested in the
gravitational potential energy of objects in this room. We
need a reference from which to measure the height of the
object. We could take this reference as the center of the
earth, the sidewalk outside, the floor level of the lab, or
the level of the bench top we are doing the experiment on.
If we choose the later we can carry the ruler in our hands
and it can be made cheaply with precision markings. If
we choose any of the others, we have to have a long (very
2Some of these values have large uncertainties. For example,
another source for the Se-Cl gives 243 rather than 261 kJ/mole.
long indeed for the first ones in the list) and these rulers
will be very hard (expensive) to make accurately and easy
to use.
Remark 3 We are free to choose the zero of energy
variables as we please! However we must always be sure
our zero is communicated to all potential users. This is
why we all agree to use the same “smart” choices of the
reference states.
4.4 ∆( )
To determine how the enthalpy for a reaction changes
with temperature ∆( ), all we need to appreciate
is that in changing the temperature all the enthalpies
(those of the reactants R and products P) change inaccordance with their heat capacities. The individual
enthalpies increase with T (C is a strictly positive quan-
tity) but ∆( ) can increase or decrease with T.
Consider my favorite reaction: + → +
∆(2) = ∆(1)+R 21[() + ()− ()− ()]
It is convenient (for me) to define,
[] = C ≡ (P)−(R)=PP −
PR
Then we just have
∆(2) = ∆(1) +R 21C( )
Note that if, as is generally the case, the individual
heat capacities are represented as polynomials, C( )can be represented as a polynomial, derived by just sum-
ming terms of like order, with + signs for products and
− for reactants. (Don’t forget the stoichiometric coef-ficients!)
Remark 4 You should now understand why heat ca-
pacities are fit to readily integrated standard functional
forms (such as polynomials.)
Exercise 4.4.1 In the figure above, two of four cases
are drawn. Draw the other two. For which cases can the
sign of the enthalpy change with increasing temperature?
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4.5 Experimental ∆ and ∆
Data from:
1. Calorimetry - The heat released by the reaction is
captured in calorimeter which is ideally adiabati-
cally separated from the remainder of the universe.
2. Spectroscopic studies
3. And most importantly, from other ∆ and
∆ values using Hess’s law. Here you have to
be confident of the values for the other “legs”. This
has been done for tabulated values by measuring all
legs and checking for consistency, (i.e. going in a
complete cycle and ending up with no change.)
4. QMical calc (isodesmic)
4.5.1 Calorimetry
Lets discuss the three most common types of calorimetry.
1. Constant-pressure calorimetry is the simplest
type and can be used if there are no gases or volatile
species involved. As (in the ideal experiment) no
heat is lost to the outside, the heat given up by the
reaction is captured by the calorimeter, ∆ =
However, the process that actually occurs (A)
is not the reaction enthalpy change at a fixed tem-
perature (as heating or cooling) can occur during
the reaction. Therefore to get the reaction enthalpy
∆, we need to break down the real process into
two steps.
.
(a) The actual process (A) is R(1)→ P(2) is thesum of:
(b) The desired step (B), the conversion of reac-
tants to productsR→ P at a constant (initial)temperature R(1)→ P(1)
(c) The heating of the products to the final
temperature (C): P(1)→ P(2) ∆ =R 21[(P) +] Clearly one needs a sep-
arate experiment to determine (P) +
(d) The desired ∆ = ∆− ∆
(e) However if really in an adiabatic enclosure
∆ = −∆
(f) ∴ the object of the experiment is really to get∆ so that the
Rin (c) can be done.
2. Bomb calorimetry (Constant V, ∆ = )
is used when there are volatile or gaseous species in
the reaction. As dV=0, ∆ = is the measured
quantity and ∆ must be calculated by adding the
change in PV energy.
Overview
While the process by which accurate values can be
obtained is quite involved, the basic process can be
analyzed with the aid of another triangle diagram,
this time referring the changes in the internal en-
ergies (rather than H) between various thermody-
namic states.
(a) The actual process (A) R(1)→ P(2) can bedecomposed into:
(b) A heating step (B),
∆ =R 21[(R) + ]
(again requires one or more separate experi-
ments) and
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(c) The desired internal energy change is (C). If
the calorimeter is really adiabatic,
∆ = ∆ −∆ = −∆
(d) Again the object of the experiment is really to
get ∆ so that theRin (b) can be done.
(e) Corrections must be applies for the energy in-
put from ignition and stirring. To get stan-
dard state values requires an additional set of
corrections3.
Step-by-step Bare-bones logic.
(a) Determine the heat capacity of the calorimeter
(C = all parts including the water in
inner bath, not a molar value.) Measure the
change in temperature ∆ when you dump
in a known amount of energy. This can be
done by i) passing a known current through a
known resistor ( = = 2 = 2)
or ii) using a reference reaction for which the
heat released (under constant volume condi-
tions) is already known.
C)=
∆
[ ])=−∆
∆
(b) run reaction and measure temperature increase
in the heat bath ⇒ ∆exp(c) Calculate exp = [
] ·∆exp[K]
(d) Calculate the ∆ = exp and the molar value
by dividing by the number of moles of product
∆ = ∆
(e) Calculate ∆ =∆ +∆( )
∆( ) =∼ 0 if only l s
˜∆( ) if g involved
This procedure illustrates the “first-pass” logic
but cannot give the standard reference values.
To get these, the previously mentioned (Wash-
burn) corrections must be made (see footnote)
for which you need to know the pressure of the
“bomb” and the EoS of the gases involved.
3. Differential Scanning Calorimetry (DSC) is
a simple and fast method of determining the en-
thalpies of condensed phase (s-s or s-l) exother-
mic phase transitions (PTs). The way to view this
process in as follows:
3Search WEB for “Washburn corrections”. These procedures
correct for: a) Compression of the condensed phase and gas phase
species to 1 atm pressure, b) Enthalpy of solution and of dilution
of the product gases in the aqueous phase (e.g. HCl, 1:600), c)
Vaporization of water because of the heat liberated by the reaction,
and d) energy changes associated with non-isothermal reactions.
(a) The experimental and reference sample are
each connected to heaters which try to keep
the temperatures of the two samples the same.
(That is, the temperatures of both samples
start at 298 K and heat at a rate of, say, 5
C/min.
(b) The power [] ( = · = 2) is mea-
sured for both samples. There will be a power
difference (∆ = −) due to the
fact that the samples will have different heat
capacities. (The sample with the larger heat
capacity will require more power to heat.) i)
If the heat capacities are different but constant
∆ will be a constant. ii) If the heat capac-
ity of the sample grows linearly while the heat
capacity of the reference is constant, ∆
will increase linearly. If they both increase lin-
early, ∆ will increase linearly with the dif-
ference in slopes of the heat capacities.
(c) Or iii) when a PT occurs in the sample (one
must not occur in the reference), much more
heat will have to be dumped into the sam-
ple than in the reference. The total heat re-
quired to execute the PT is the excess en-
ergy, which is calculated from the excess power
times the time = ∆ =R[∆] with
∆ = ∆ −∆
(d) As DSC is employed for condensed phases
∆ ≈ ∆
Fig. of DSC
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