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Lecture on Chapter 17: Energy in Thermal Processes: The First Law
of Thermodynamics
One of the great conceptual breakthroughs of thermodynamics in the mid 19th-century
was the realization that energy could leave or enter a system in 2 ways: mechanical
work and heat. Before that, people didn't realize the connection between
thermal and mechanical energy.
Heat and Internal Energy
We begin with some definitions:
- Internal energy Eint is the energy associated
with the kinetic and potential energy of the atoms and molecules of a system viewed
from a reference frame at rest with respect to the system. The kinetic and potential
energy come from the translational, rotational, and vibrational motion of the atoms
and molecules as well as from the intermolecular potential energy. For an ideal gas
the internal energy is simply the kinetic energy of the particles.
- Heat is the energy transferred between a system and its environment because
of the temperature difference between them. The amount of energy transferred is
often denoted by Q. As a result of this energy transfer, the energy of the
system changes.
The unit of heat is the calorie which is defined as the heat necessary to
raise the temperature of 1 g of water from 14.5o to 15.5oC. The temperature
is given because the amount of heat needed to raise the temperature of water by
1oC is slightly temperature dependent. Note that 1 Calorie = 1000 calories.
Calories with a capital ``C'' is used with regard to food. Now that we know that
heat, like work, is a measure of the energy transferred to a system, we can express
calories in terms of Joules:
We will typically measure heat in Joules.
Specific Heat
The amount of heat needed to raise the temperature of an object by 1oC, say,
depends on the size of an object and what material it is made of. For example,
it takes a lot more heat to bring a big pot of water to a boil than a cup of
water. So the amount of heat Q needed to increase the temperature of
an object of mass m by a certain amount is proportional to
and to m:
where the constant of proportionality c is called the specific heat.
We can rewrite this equation as follows to give the definition of c:
Notice that the specific heat is the amount of heat per unit mass that is needed
to raise the temperature of a substance by an amount . We can
also define a molar specific heat as the amount of heat per mole that is needed
to raise the temperature of a substance by :
where n is the number of moles. The specific heat c varies from material to
material. For example it takes a lot more heat to raise the temperature of a gram
of water than a gram of copper by 1oC. So the specific heat of water is
much higher than the specific heat of copper.
A related term you should be familiar with is heat capacity.
The heat capacity of an object is mc or nC. Heat capacity is
proportional to the mass of an object.
Qualitatively one can think of the heat capacity as a measure of the
ability of the system to store energy. The more energy it can hold, the
higher its heat capacity. In places of the country where it's cold in the
winter, there is often a radiator in each room which has hot water circulating
through it to heat the room. The radiator is usually made of metal
and it's big and heavy so that it can hold lots of energy. It has a large
heat capacity. If the radiator is small and doesn't have much mass,
then it has a small heat capacity; it doesn't hold much energy and the
room is cold.
If we add a little bit of heat dQ to the system, we change its temperature
by a tiny amount dT. So we can write the specific heat as a derivative:
Note that Q is positive if heat flows into the system and negative if heat flows out.
Calorimetry
Calorimeters are instruments used to measure the specific heat of objects.
To measure the specific heat cx of an object of mass mx, we heat
it to a temperature Tx, then put it in a vessel containing some substance
like water of a known mass mw at temperature
Tw. After equilibrium is reached, we measure the temperature T of the
combination. Conservation of energy requires that the heat Qhot leaving the
hot object equals the heat entering the water:
Since heat is leaving the hot object, Qhot<0, which means
-Qhot>0.
Eq. (7) can be rewritten as
mwcw(T-Tw)=-mxcx(T-Tx)
|
(8) |
where cw is the specific heat of water. Solving for cx gives the
specific heat of the object:
By substituting in the known values on the right hand side, we can calculate the specific
heat of the object.
Latent Heat
One of the more interesting things that happens when we heat (or cool) substances is
that they change their phase. For example, ice melts or water turns into steam.
These phase changes are called phase transitions and are an active area of research.
In so-called first order phase transitions, such as crystal-to-liquid, latent heat
is required to break the bonds between molecules and effect the phase change.
For example, if you heat a crystal at a constant rate, the temperature of the
crystal will rise at a constant rate until the melting temperature is reached.
At that point the temperature stays constant and the heat is used to break the
bonds between the molecules so that the molecules can flow and be in the liquid
state. The amount of heat Q needed to melt the solid is proportional to
the mass m of the crystal:
where the constant of proportionality L is called the latent heat. When heat flows into
the crystal, we use the plus sign. When heat flows out of the liquid as it freezes
into a crystal, we use the minus sign. The heat of fusion Lf is the term used
to describe the latent heat during melting or freezing. The heat of vaporization
Lv is the latent heat associated with boiling or condensing, i.e., the liquid
to vapor transition. The value of the latent heat depends on the substance.
Example: This is problem 17.15. If 90.0 g of molten lead (Pb) at
327.3oC is poured into a 300 g casting form made of iron (Fe) and
initially at 20.0oC, what is the final temperature of the system? (Assume
no energy loss to the environment occurs.)
The heat leaving the molten lead goes into the iron (
QFe=-QPb).
As the lead cools, it solidifies, so we need to add the heat of fusion
to eq. (8) which we can rewrite as
Solve for the final temperature T:
Then plug in the numbers:
mPb=0.090 kg,
TPb=327.3oC=600.45 K,
mFe=0.300 kg,
TFe=20oC=293.15 K,
cFe=448 J/kgoC,
cPb=128 J/kgoC, and
J/kg. The specific
heats come from Table 17.1 in your book, and Lf comes from
Table 17.2 in your book. The final answer is T=59.4oC.
Work
The macroscopic state of a system in equilibrium is specified by macroscopic
variables such as pressure, volume, temperature, and internal energy. The state
of a system does not depend on its history. There are numerous ways that it
could have gotten to that state. To go from one state to another, we can transfer
energy to the system through heat or work. Your book calls heat and work transfer
variables. We've already discussed heat. Now let's discuss work.
Consider gas in a cylinder with a piston pushing down on the gas. Hold the
piston fixed for a moment. Suppose the volume of the gas is V and that the
gas exerts a pressure P on the piston and the walls of the cylinder. Let the
area of the face of the piston be A. Now suppose we compress the gas
quasi-statically by moving the piston so slowly that the gas remains
in equilibrium at all times. If we apply a force on the piston and
move the piston a distance
, then the work done on the gas is
where the direction is downward and we used P=F/A or F=PA.
Note that
Adz=-dV. The minus sign is because the volume shrinks and so dV<0 while
Adz>0. So the work done on the gas is
If the gas is compressed, the system gains energy and dW>0. dV<0 so -dV>0.
The total work done on the gas as the volume changes from Vi to Vf is
given by integrating:
If we draw the path to go from the initial (Vi, Pi) to the final
(Vf,Pf) on a PV diagram, the negative of the area under the curve
corresponds to the work done on the gas, provided the system moves along
the curve quasi-statically. The amount of work done on the gas will
depend on the path taken between the initial and final points
because the area under the curve will depend on the curve in the PV plane.
Similarly the heat transferred to a system can depend on the process
taken between fixed initial and final states of the system. Before we
give an example of this, let's discuss the first law of thermodynamics.
First Law of Thermodynamics
We've seen that the 2 ways to transfer energy to a system is by
work and by heat. So the total change in internal energy
is
This is the first law of thermodynamics. It is just a statement of the
conservation of energy.
Remember that the sign convention is such that Q is positive if heat
flows into the system and negative if heat flows out. The work W done
on a system is positive if the internal energy of the system increases.
W is negative if work is done by the system which lowers the internal
energy of the system. For an infinitesimal change in energy dEintdue to a tiny amount of heat dQ and due to a tiny
amount of work dW being done on the system, the first law of
thermodynamics becomes:
Applications of the First Law of Thermodynamics
There are a various types of processes that a system can be subjected
to. Let's list them:
- In an adiabatic process no heat enters or leaves the system.
So Q=0. One way to do this is to put the system in a container whose
walls are perfect thermal insulators so that no heat can enter or leave.
In the real world, there are no perfect insulators but we can imagine
such a system to make our calculations easier. Another way to get an adiabatic
process is to perform the process very rapidly because heat exchange
takes place slowly. Since Q=0 in an adiabatic process, the first law
becomes
So if a gas expands adiabatically, W is negative and the internal energy is
lowered. If the gas is compressed adiabatically, W>0 and the internal energy is
increased.
- Free expansion is a special type of adiabatic process with
both Q=0 and W=0. From the first law, this makes
.
So there is no change in internal energy when free expansion occurs.
For an example of free expansion consider a box with perfectly insulating
walls and a partition in the middle. On
one side of the partition is an ideal gas and on the other side of the
partition is vacuum. Now remove the partition. The gas expands to fill
the whole box. This is free expansion because no heat is transferred and
no work is done. The expanding gas doesn't exert any force on anything.
Recall that the internal energy of an ideal gas is given by 3RT/2.
Eint depends only on the temperature T. Since the internal energy
doesn't change in free expansion, the temperature of an ideal gas doesn't
change in free expansion.
- In an isobaric process the pressure is kept constant
(P = constant).
An example is an ideal gas in a cylinder with a piston that is free to
move. The constant pressure is provided by the weight of the piston
and the atmospheric pressure on the piston.
- In an isovolumetric process the volume is kept constant
(V = constant). As an example, imagine clamping the piston so that it
cannot move. In this case no work is done (W=0). So the first law
gives
So if you heat a gas in a fixed volume, all the heat goes into increasing
the temperature and pressure. For example if you throw an aerosol can
into the fire, the pressure and temperature of the gas in the can increase
until the can explodes. (Of course, the gas does work in tearing apart the
can.)
- In an isothermal process the temperature is held constant, though the
pressure and volume may vary. For an ideal gas the internal energy
Eint=3RT/2is solely a function of the temperature. So if T is a constant, Eint is a
constant and the change in the internal energy is zero (
).
The first law of thermodynamics implies that
So any work done on the ideal gas leaves as heat. We can calculate the
work done on an ideal gas as it moves along an isotherm (T = constant)
from an initial pressure Pi and volume Vi to a final pressure Pfand volume Vf. We can use the ideal gas law PV=nRT or P=nRT/V.
Notice that if the gas is compressed, then Vf is smaller than Vi and
the ratio
Vf/Vi <1 which implies that
,
so positive
work is done on the gas (W>0). Since Q=-W, we know how much heat
leaves the system and we can write
Well, that's the laundry list of processes. We can arrange these processes to form
a cycle so that the system returns to the same state at the end of each cycle.
So the internal energy is the same since it just depends on the state of the system,
not on what has happened to it. This means that
and hence
that Q=-W after each cycle. So the net heat that enters the system goes into
work. This is how a heat engine works; heat gets converted into work.
Let's look a bit closer at the first law of thermodynamics.
The change in internal energy
depends solely on
the initial and final states, not on the path between them. However,
the heat Q and work W do depend on the path (though the sum does not).
For example a gas can go from an initial state with (Vi, Pi) to a
final state (Vf,Pf) in either of 2 ways. The first way is isothermal.
The gas expands slowly by pushing a piston. So the gas does work. It
stays at the same temperature Ti by absorbing
heat from an energy reservoir or heat bath. A heat bath or energy
reservoir is considered to be a source of internal energy that is so
large that a finite transfer of energy from the reservoir does not
change the reservoir's temperature. The second way is by free expansion.
The gas is thermally isolated with perfectly insulating walls.
A partition or membrane holds the gas at its initial volume and pressure.
Then the partition is removed and the gas undergoes free expansion to the
final pressure and volume (Vf,Pf). No work is done (W=0) and no
heat is transferred (Q=0), but the initial and final states are the same as
that of the isothermal process. In comparing the 2 processes, we see
that Q and W differ but
is the same because the
initial and final states are the same.
Constant volume and constant pressure molar specific heats
This difference in path or process implies that the amount of heat Q
needed to produce a given temperature change will be different if
we hold the volume fixed or if we hold the pressure fixed. This will produce
2 different values for the molar specific heat:
where CV is the molar specific heat at constant volume and CP is the
molar specific heat at constant pressure. n is the number of moles of
the substance. If we add an infinitesimal amount of heat dQ, then
where n is the number of moles.
Let us calculate CV for an ideal gas. The volume is held fixed so no
work is done. The first law of thermodynamics implies that
The heat dQ added to the system raises the temperature of the system by an
amount dT.
where we used the equipartition theorem.
So using eq. (26), we obtain
Notice that CV=3R/2 means that the specific heat for an ideal gas is
a constant independent of temperature. This value of CV agrees well
with measurements of the constant volume molar specific heats of
monatomic gases.
For a monatomic ideal gas the equipartition theorem gives
Eint=3nRT/2.
The internal energy depends solely on the temperature.
If we change the temperature by an amount , then
the change in the internal energy
We can express this in terms of CV=3R/2:
Equations (32) and (31) are true for any process
in which the temperature of an ideal gas changes by , not
just for processes where the volume is held fixed. These are
very useful equations for an ideal gas. If you get stuck on an ideal
gas problem, try using these equations.
Now let's derive an equation for CP. When we add heat Q,
eq. (24) tells us
. When the pressure P is held
constant, the volume can change and work can be done on the gas.
The ideal gas law (PV=nRT) implies that
, so
. Now let's plug this into the first law of thermodynamics:
Using eq. (32) yields
Cancelling out , we obtain
or
Thus,
This agrees with measurements on monatomic gases.
The ratio of the molar specific heats is a dimensionless quantity :
For a monatomic gas,
This agrees well with experimentally measured values of for
monatomic gases.
Specific heat of Diatomic Gases
So far we have been discussing ideal monatomic gases. What about diatomic
gases in which each molecule has 2 atoms. Recall that when we talked
about the equipartition theorem, we said that each degree of freedom
contributes kBT/2 to the average internal energy Eint. The
translational kinetic energy has 3 degrees of freedom which contributes
3kBT/2. If we include the 2 rotational degrees of freedom about the
2 axes perpendicular to the line along which the diatomic molecule lies,
we get an additional contribution of
. So translations
and rotations yield
Eint=5NkBT/2=5nRT/2. This implies that
and
If we imagine that the 2 atoms in a molecule are connected by a spring so
that there is a vibrational degree of freedom, then the kinetic energy
associated with vibration contributes kBT/2 and the potential energy
contributes kBT/2 to Eint. Adding the translational, rotational,
and vibrational degrees of freedom yields
Eint=7RT/2,
CV=7R/2 and CP=9R/2.
Adiabatic Processes for an Ideal Gas
In an adiabatic process no energy is transferred by heat so Q=0.
So
dEint=dW. An example of an adiabatic process is one in
which a gas expands or is compressed very rapidly before there
is time to transfer heat. Another example is an expanding
gas in a perfectly insulating container.
Let us consider adiabatic processes for an ideal
gas. Suppose we put the ideal gas in a container with perfectly
insulating walls and allow the gas to expand.
If one uses
dEint=dW, together with the ideal
gas law, eq. (37) and eq. (32), then one
can show that (see page 604 of Serway and Jewett):
where
. Contrast this with a process in which the
temperature is held constant. In that case the ideal gas law implies that
PV = constant. Eq. (43) implies that in terms
of initial and final states
for an adiabatic process.
Using the ideal gas law we can also write
Thermal Conductivity
When heat goes through an object, that's thermal conduction. For example
when you cook soup, you put the soup in a metal pot and put the pot on
the stove. The heat from the burner is conducted through the pot into the
soup. Most pots are made of metal rather than glass because metal conducts
heat better. We say that metal has a higher thermal conductivity
than glass. Thermal conductivity is a measure of how well a substance
conducts heat. You can think of this as energy flowing through a
substance. Microscopically energy transfer occurs when hot energetic
molecules with lots of kinetic energy collide with less energetic
cold molecules and transfer some of their energy to the molecules
with less energy. It's like standing in a crowd. If the people on one
side of you start pushing and shoving, you get pushed and shoved
into people on the other side of you.
To represent thermal conduction mathematically, we talk about the rate
of energy transfer dQ/dt, i.e., the amount of heat that flows per
unit of time. This has the units of energy per unit time or
power . Heat flows from the hot side to the cold side.
The greater the temperature difference, the faster the
energy transfer, and the greater the heat flow dQ/dt. So
dQ/dt will be proportional to the temperature
gradient, i.e., to dT/dx. This is the slope of how the
temperature changes with distance. The steeper the slope,
the faster the rate of the energy transfer.
=2.5 true in
tempgradient.eps
The heat flow is also
proportional to the area A through which the heat is flowing
because there are more ``channels'' to conduct the heat. This
is why traffic moves faster when there are more lanes open
on the freeway. Traffic crawls if there is only one lane open
on the 405. So we can write
The constant of proportionality is called the thermal conductivity
and is denoted by .
Note that the book's sign convention
has Q>0 when heat flows into the cold body and Q<0 when
heat flows out of a hot body. If you don't want to worry
about the sign, just write
Note that objects feel colder when their thermal conductivity
is higher. Remember the example of going to your car late
at night? The metal exterior feels colder than the seat.
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Clare Yu
2002-01-17