PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

79
PPT 107 PHYSICAL CHEMISTRY Semester 2 Academic session 2012/2013 1

Transcript of PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

Page 1: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

1

PPT 107 PHYSICAL CHEMISTRY Semester 2

Academic session 2012/2013

Page 2: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

2

CHAPTER 2FIRST LAW OF THERMODYNAMICS

Page 3: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

3

THERMODYNAMIC SYSTEM

Characterized by the 4 laws of thermodynamics

Page 4: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

4

Page 5: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

5

CHAPTER 2

First law of thermodynamics

Page 6: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

6

Key Concepts

• Work• Pressure-Volume Work (P-V Work)• Heat• First Law of Thermodynamics• Enthalpy• Perfect Gas• Molecular Nature of Internal Energy

Page 7: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

7

Units• The General Conference on Weights and Measures recommended a single system of units

for use in science. This system is called the International System of Units , abbreviated SI.

• The SI uses meters (m) for length, kilograms (kg) for mass, and seconds (s) for time. A force

that produces an acceleration of one meter per square second when applied to a one-kg mass

is defined as one newton(N):

• SI units for some quantities: pressures would always be given in [newtons / square meter]:

(pascals), cubic meters for volume, kg/cubic m for density, kelvins for temperature, moles

for amount of substance, and kg/mol for molar mass.

• However, it seems clear that many scientists will continue to use such units as atmospheres

and torrs for many years to come. The current scientific literature increasingly uses SI units,

but since many non-SI units continue to be used, it is helpful to be familiar with both SI

units and non-SI units.

Page 8: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

8

WORK

Work is done when and object, e.g. a system's wall, moves against an opposing force. This is equivalent to an ordered motion done by the system on the surroundings or vice versa.

Work (w) is defined as the force (F) that produces the movement of an object through a distance (d):

Work = force ×distancew = F x d

Work also has units of J, kJ, cal, kcal, Cal, etc.

Page 9: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

9

Suppose a force F acts on a body while the body undergoes an

infinitesimal displacement dx in the x direction. The infinitesimal

amount of work dw done on the body by the force F is defined as:

the units of work are those of force times length. The SI unit of work

is the joule (J).

Power P is defined as the rate at which work is done. If an agent

does work dw in time dt, then P = dw/dt. The SI unit of power is the

watt (W): 1 W=1 J/s

Page 10: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

10

Page 11: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

11

P-V workWork in thermodynamics is defined as in classical mechanics. When part

of the surroundings exerts a macroscopically measurable force F on

matter in the system while this matter moves a distance dx at the point of

application of F, then the surroundings has done work [dw=Fx dx] on the

system, where Fx is the component of F in the direction of the

displacement. F may be a mechanical, electrical, or magnetic force and

may act on and displace the entire system or only a part of the system.

When Fx and the displacement dx are in the same direction, positive work

is done on the system: dw>0. When Fx and dx are in opposite directions,

dw is negative.

Page 12: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

12

Page 13: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

13

Pressure-volume (P-V) work

Initial state

Final state

Changing the

volume by 2 ways

Final state

By holding the pressure constant and increasing the volume by heating

the gas using Charle’s law

By removing weights and decreasing the

pressure and allowing the volume to adjust according to Boyle's

law with no heat addition

OR

The work done in a volume change is called P-V work

Page 14: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

14

[dw=Fx dx]

F = PA

dw = PA dx

dwrev = -P dV closed system,

reversible process

where 1 and 2 are the initial and final states of the system, respectively

Page 15: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

15

The example of PV work – in the cylinder of an automobile engine• The combustion of the gasoline causes gases within the cylinder to expand, pushing the

piston outward and ultimately moving the wheel of the car. The relationship between a volume change (ΔV) and work (w):

W= -P ΔVWhere P is external pressure

The units of PV work are L·atm; 1 L·atm = 101.3 J.

• If the gas expands, ΔV is positive, and the work term will have a negative sign (work energy is leaving the system).

• If the gas contracts, ΔV is negative, and the work term will have a positive sign (work energy is entering the system).

• If there is no change in volume, ΔV = 0, and there is no work done. (This occurs in reactions in which there is no change in the number of moles of gas.)

Pressure-volume work

Page 16: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

16

Work done by gas

if ΔV < 0, then W > 0.; increases in volume means work done BY the system on the environment.

if ΔV > 0, then W < 0.; decreases in volume means work done by the environment ON the system.

The units of PV work are L·atm; 1 L·atm = 101.3 J.

Page 17: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

17

Work and heat are not state functions

On a graph of pressure versus volume, the work is the area under the curve that describes how the state is changed from State 1 to State 2.

A curved black line from State 1 to State 2 represents a change brought about by removing weights and decreasing the pressure and allowing the volume to adjust according to either Boyle’s law (the line is curved and the amount of work done on the gas is shown by the red shaded area below this curve)

or Charle’s law (the resulting change in state proceeds from State 1 to an intermediate State "a" on the graph by heating. State "a" is at the same pressure as State 1, but at a different volume. If we then remove the weights, holding a constant volume, we proceed on to State 2. The work done in this process is shown by the yellow shaded area).

Page 18: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

18

Notice that not only does the work done by the gas depend on the process, but also the heat transferred to the gas. In the first process, the curved line from State 1 to State2, no heat was transferred to the gas; the process was adiabatic. But in the second process, the straight line from State 1 to State "a" and then to State 2, heat was transferred to the gas during the constant pressure process.

The work done by a gas not only depends on the initial and final states of the gas but also on the process used to change the state. Different processes can produce the same state, but produce different amounts of work.

The heat transferred to a gas not only depends on the initial and final states of the gas but also on the process used to change the state.

Using either process we change the state of the gas from State 1 to State 2. But the work for the constant pressure process is greater than the work for the curved line process.

Page 19: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

19

What are Reversible and Irreversible Processes?

There are two main types of thermodynamic processes: the reversible and irreversible. The reversible process is the ideal process which never occurs, while the irreversible process is the natural process that is commonly found in the nature. Therefore:• The reversible process is an idealization.• All real processes on Earth are irreversible.

A reversible process is one that can be

halted at any stage and reversed. In a reversible process,

the system is at equilibrium at every stage of the process.

REVERSIBLE IRREVERSIBLE

An irreversible process is one where it cannot be halted at

any stage and reversed and the

system is not always at equilibrium at

every stage of the process.

P-V Work

Page 20: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

20

What is a Reversible Process?The process in which the system

and surroundings can be restored to the initial state from the final state without producing any changes in the thermodynamics properties of the universe is called a reversible process. In the figure below, let us suppose that the system has undergone a change from state A to state B. If the system can be restored from state B to state A, and there is no change in the universe, then the process is said to be a reversible process. The reversible process can be reversed completely and there is no trace left to show that the system had undergone thermodynamic change.

Page 21: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

21

For the system to undergo reversible change, it should occur infinitely slowly due to infinitesimal gradient. During reversible process, all the changes in state that occur in the system are in thermodynamic equilibrium with each other. Thus there are two important conditions for the reversible process to occur. Firstly, the process should occur in infinitesimally small time and secondly all of the initial and final state of the system should be in equilibrium with each other. If during the reversible process the heat content of the system remains constant, i.e. it is adiabatic process, then the process is also isentropic process, i.e. the entropy of the system remains constant. The phenomenon of undergoing reversible change is also called reversibility. In actual practice the reversible process never occurs, thus it is an ideal or hypothetical process.

Page 22: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

22

What is an Irreversible Process?The irreversible process is also called the natural process because all the processes occurring in nature are irreversible processes. The natural process occurs due to the finite gradient between the two states of the system. For instance, heat flow between two bodies occurs due to the temperature gradient between the two bodies; this is in fact the natural flow of heat. Similarly, water flows from high level to low level, current moves from high potential to low potential, etc.

Here are some important points about the irreversible process:1. In the irreversible process the initial state of the system and surroundings

cannot be restored from the final state.2. During the irreversible process the various states of the system on the path

of change from initial state to final state are not in equilibrium with each other.

3. During the irreversible process the entropy of the system increases decisively and it cannot be reduced back to its initial value.

4. The phenomenon of a system undergoing irreversible process is called as irreversibility.

Page 23: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

23

Calculation of PV work for reversible processes

The integral (2.28) is called a line integral. The value of the line integral (2.28) is defined as the sum of the infinitesimal quantities P(T, V)dV for the particular process used to go from state 1 to state 2. This sum equals the area under the curve that plots P versus V. Figure 2.3 shows three of the many possible ways in which we might carry out a reversible volume change starting at the same initial state (state 1 with pressure P1 and volume V1) and ending at the same final state (state 2).

Page 24: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

24

In process (a), we first hold the volume constant at V1 and

reduce the pressure from P1 to P2 by cooling the gas. We then

hold the pressure constant at P2 and heat the gas to expand it

from V1 to V2.

Page 25: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

25

In process (b), we first hold P constant at P1 and heat the gas until its

volume reaches V2. Then we hold V constant at V2 and cool the gas

until its pressure drops to P2.

Page 26: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

26

In process (c), the independent variables V and T vary in an

irregular way, as does the dependent variable P.

Page 27: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

27

Page 28: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

28

Example for P-V WORKInflating balloon requires the inflator to do pressure-work on the surroundings. If balloons is inflated from a volume of 0.100L to 1.85L against an external pressure of 1.00 atm, how much work is done (in joules)?

Answer:ΔV = V1 -V2 = 1.85L -0.100L = 1.75L

W= -P ΔV = -1.00 atm x 1.75L = -1.75L.atm

Convert to Joule:-1.75L.atm x 101.3 J= -177 J 1L.atm

The work is negative because it is being done by the system as its volume increases due to the expansion of the gas into the much bigger volume.

Page 29: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

29

Study Example 2.2 page 44Find the work for processes (a) and (b) of Fig. 2.3 if P1 3.00 atm, V1 500 cm3, P2 1.00 atm, and V2 2000 cm3.

Figure 2.3The work w done on the system in a reversible process (the heavy lines) equals minus the shaded area under the P-versus-V

curve. The work depends on the process used to go from state 1 to state 2.

Use this equation:

Simple as the previous example.Processes (a) and (b) are expansions. Hence the system does positive work on its surroundings, and the work w done on the system is negative in these processes.

Answer: = - 152 J and = -456 J

Page 30: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

30

Page 31: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

31

Page 32: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

32

Page 33: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

33

HEAT

Heat is a exchange of thermal energy between a system and its surroundings caused by temperature difference.

Notice the distinction between heat and temperature. Temperature is a measure of the thermal energy of a sample matter. Heat is transfer of the thermal energy.

Heat may be defined as energy in transit from a high temperature object to a lower temperature object.

Anytime two substances with different temperatures come in contact with each other, there is an energy transfer. One substance loses heat energy and the other substance gains heat energy.

Heat energy flows from a hotter substance to a colder substance.

Page 34: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

34

Let bodies 1 and 2 have masses m1 and m2 and initial temperatures T1 and T2, with T2 > T1 ; let Tf be the final equilibrium temperature. Provided the two bodies are isolated from the rest of the universe and no phase change or chemical reaction occurs, one experimentally observes the following equation to be satisfied for all values of T1 and T2:

where c1 and c2 are constants (evaluated experimentally) that depend on the composition of bodies 1 and 2. We call c1 the specific heat capacity (or specific heat) of body 1. We define q, the amount of heat that flowed from body 2 to body 1, as equal to m2 c2 (T2-Tf).

Page 35: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

35

The unit of heat commonly used in the nineteenth and early

twentieth centuries was the calorie (cal), defined as the quantity of

heat needed to raise one gram of water from 14.5°C to 15.5°C at 1

atm pressure. (This definition is no longer used, as we shall see in

Sec. 2.4.) By definition, 1.00 cal/(g °C) at 15°C and 1 atm. Once

the specific heat capacity of water has been defined, the specific

heat capacity c2 of any other substance can be found from the

above relation by using water as substance 1. When specific heats

are known, the heat q transferred in a process can then be

calculated from above relation.

Page 36: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

36

The specific heat capacities of substances are functions of temperature and pressure. When an infinitesimal amount of heat dqp flows at constant pressure P into a body of mass m and specific heat capacity at constant pressure cp, the body’s temperature is raised by dT and

where cp is a function of T and P. Summing up the infinitesimal flows of heat, we get the total heat that flowed as a definite integral:

The pressure dependence of cp was omitted because P is held fixed for the process. The quantity mcp is the heat capacity at constant pressure Cp of the body: Cp ≡ mcp.

Page 37: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

37

Equation to be more accurately written as:

If the dependence of cp2 and cp1 on T is negligible the above eq can be reduces to original eq.

The heat can be transferred reversibly or irreversibly. A reversible transfer of heat requires that the temperature difference between the two bodies be infinitesimal. When there is a finite temperature difference between the bodies, the heat flow is irreversible.

Page 38: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

38

For example, if the ice cube in the diagram is placed in the container of water, there is an energy transfer. The hotter substance loses heat energy and the colder substance gains heat energy.

The water and its container lose heat energy and become cooler.

The ice cube gains heat energy and becomes warmer (this causes the ice cube to melt).

According to the law of energy conservation the total heat energy lost by the water and its container is equal to the total heat energy gained by the ice.

Heat can be transferred reversibly or irreversibly. A reversible transfer of heat requires that the temperature difference between the two bodies be infinitesimal. When there is a finite temperature difference between the bodies, the heat flow is irreversible.

Page 39: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

39

Page 40: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

40

Heat capacitywhen system absorbs heat (q) its temperature changes by ΔT:

Experimental measurements demonstrate that the heat absorbed by a system and its corresponding temperature change are directly proportional: qαΔT. The constant of proportionality between q and ΔT is called the heat capacity.

Heat capacity (C) is the amount of heat (q) a substance must absorb to raise its temperature(ΔT) by 1 °C.-Heat capacity has units of J/°C (or J/K), and is an extensive property, depending on the sample size.

Page 41: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

41

Specific Heat Capacity

The specific heat (c, or specific heat capacity, Cs) of an object, is the quantity of heat required to change the temperature of 1 gram of a substance by 1°C (or K):

Specific heat has units of J/g°C, and is an intensive property, which is independent of the sample size.

Page 42: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

42

Example

Calculate the amount of heat needed to increase the temperature of 250g of water from 20oC to 56oC.

Answer:q = m x Cg x (Tf - Ti) m = 250g Cg = 4.18 J oC-1 g-1 (from table) Tf = 56oC Ti = 20oC

q = 250 x 4.18 x (56 - 20) q = 250 x 4.18 x 36 q = 37 620 J = 38 kJ

Page 43: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

43

What is the difference between heat capacity and specific heat?

Heat capacity is the amount of heat required to raise the temperature of any quantity of substance by 1 degree centigrade.

Specific heat is the amount of heat required to raise the temperature of 1kg (MASS) of substance by 1 degree substance.

The unit for specific heat is J/(g*K). The unit for heat capacity is J/K.

Difference between specific heat capacity and heat capacity is identical to difference between concentration and amount of substance - one is intensive, other extensive property.

Page 44: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

44

Is the law of conservation of Energy.

Page 45: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

45

1st Law = Conservation of Energy

The first law of thermodynamics is simply an expression of the conservation of energy principle.

The principle of the conservation of energy states that energy can neither be created nor destroyed. But it can change from one type of energy to another (for example kinetic to potential) but the total amount remains fixed (The total energy of a closed system remains constant.)

Page 46: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

46

(the change in the internal energy of a closed system is equal to the amount of heat supplied to the system, minus the amount of work performed by the

system on its surroundings)

The standard unit for all these quantities would be the joule.

In thermodynamics, energy is classified into three different types: 1. work (W) 2. heat (Q) 3. internal energy (ΔU)

This allows us to write a simple form for conservation of energy (or the first law of thermodynamics) as

Page 47: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

47

ENERGY• Energy is defined as the ability or capacity to do work on some form of matter

(the amount of work one system is doing on another). There are several forms of energy:

• Potential energy is the energy that a body possesses as a consequence of its position in a gravitational field (e.g., water behind a dam).

•Kinetic energy is the energy that a body possesses as a consequence of its motion (e.g., wind blowing across a wind generator). It is dependent upon an object's mass and velocity (e.g., moving water versus moving air).

• Internal energy is the total energy (potential and kinetic) stored in molecules. It is the energy associated with the random, disordered motion of molecules; it refers to the invisible microscopic energy on the atomic and molecular scale.

The First Law of Thermodynamics states that energy lost during one process must equal the energy gained during another, i.e., all energy is conserved.

Page 48: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

48

Unit of Energy

• Energy is measured in Joules (J) or Calories (cal).1 J = 1 kg m2s-2

• A calorie (cal) is the amount of energy needed to raise the temperature of 1 g of water by 1°C.

1 cal = 4.184 J

Page 49: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

49

INTERNAL ENERGY

The total (internal) energy in a system includes potential and kinetic energy.

It involves energy on the microscopic scale.

• translational kinetic energy• vibrational and rotational kinetic energy

Binding energies – atomic bonds(potential energy from intermolecular forces)

The internal energy, U of a system is the sum of the kinetic and potential energies of all the particles that compose the system or the total energy of a system (the energy associated with the random, disordered motion of molecules).

Page 50: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

50

• There are two ways to change the internal energy: with work and heat.

• Internal energy of an object can be changed by the following methods:

1. It increases if energy is added to the system.• i.e. by heating or by doing work on the system.

2. It decreases if energy is removed from the system or work is done by the system.• i.e. Thus heat and work changes the internal energy of an object.

Page 51: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

51

Reaction between carbon and oxygen to form carbon dioxideC(s) + O2(g) CO2(g)

Example

if the reactants have a higher internal energy than a products, ΔUsys is negative and energy flows out of the system into the surroundings.

if the reactants have a lower internal energy than a products, ΔUsys is positive and energy flows into the system from the surroundings.

Page 52: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

52

Internal energy is the state function, which means that its value depends only the state of the system, not the how the system arrive at the state.

Example:Altitude is a state function. The change in altitude during climbing depends only on the difference between the final and initial altitudes.

Page 53: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

53

Why energy is a state function but heat and work are not?

State Function is a thermodynamic parameter whose value does not depend on the thermodynamic process...It depends only on the initial and final states.

State functions are characterized by the idea that no matter what path you take to get from point A to point B, the difference between B and A remains the same. An example of how this works can be illustrated using gravitational potential energy. Say you lift a box 5 meters vertically straight up into the air from the surface of the ground (which we shall set to a height of 0 m). You increase its energy by an amount mg h where h = 5m. Now say that you lift a box from the ground level up 1 meter above the ground, walk to the right 5 meters, lift the box 1 more meter, walk to the left 2 meters, raise the box 7 meters, walk to the left 1 more meter, and lower the box 4 meters. How much did the gravitational potential energy change? The same amount as before, mg h where h = 5m, because the box is still only 5 meters above where it started in either case and the potential energy depends only on the final height minus the initial height (it depends only on the final and initial position).

In contrast, you expended a lot more energy (more work) moving the box around than you did just standing in place and lifting it straight up. So the work you did is NOT a state function. This function depends on the path. When you lifted the box straight up you did less work than your body did lugging the box around left and right while lifting it up and down. So the potential energy is a state function, but the work you did is a path function.

Now in thermodynamics you usually apply these ideas to the 1st law or conservation of energy:

U = Q + W

In this example, Q and W are path functions...the exact amount of work you do or the heat transferred to the system depend on how you add the heat or do the work (these individual values will vary depending on whether or not you did these things in either a direct or roundabout way). However, if you add these two path functions together the overall result, U, is a state function. It only depends on U (final) – U (initial) , regardless of whether or not you did direct or roundabout Q's and W's.

Page 54: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

54

ProblemsProblem 1: A gas expands against a constant pressure of 1 atm from a volume of 10 L to 20 L. During this process, the system absorbs 600 J of heat from the surroundings. Calculate the internal energy of the system.

Answer:ΔU = q + w= 600 J + (-PΔV) = -413 J = 600 J + {- 101.3 Pa (20-10) L}= 600 J + (-1013 J) = - 413 J

Problem 2 :q amount of heat is transferred to the system from the surroundings and w amount of work is done by the system. Write the expression for the internal energy.

Answer:ΔU = q – w

Page 55: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

55

Study Example 2.3 pg. 50Calculate U when 1.00 mol of H2O goes from 25.0°C and 1.00 atm to 30.0°C and 1.00

atm. Densities of water are 0.9970 g/cm3 at 0°C and 0.9956 g/cm3 at 100°C.

Refer to sildes ‘Specific Heat Capacity’, ‘P-V Work’, and the First Law equation to solve !

Answer: ΔU = q + w = 90 cal.

Page 56: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

56

Page 57: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

57

Now, you’ve learn about heat & work, so what is the difference between HEAT &

WORK?

Heat is an energy transfer between system and surroundings due to a temperature difference.

Work is an energy transfer between system and surroundings due to a macroscopic force acting

through a distance.

Page 58: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

58

Heat and work, both, are energy. The difference is just the amount of ordered motion during the energy transfer.

Page 59: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

59

Work and HeatEnergy transfer between system and surrounding occurs either in the form of work or heat.

Work (W) → refers to mechanical work Heat (Q) → refers to energy transferred from a hot to a cold object.

W = Fd

A system can exchange energy with its surroundings through heat and work:

Page 60: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

60

Summary

According to the first law thermodynamic, the change in the internal energy of the system(ΔU) must be the sum of the heat transferred (q) and the work done (w):

Sign of conventions for q, w, and ΔU

Page 61: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

61

Enthalpy vs. EnergyEnthalpy (H) is the heat flow in or out of a system at constant pressure (i.e., carried out in open containers at or near atmospheric pressure):

where U = energy, P = pressure, and V = volume.

Enthalpy depends on the amount of substance present.

H = ΔU +PΔV 

ΔU = qv const. V , closed syst., P-V work only

ΔH = const. P, closed syst., P-V work only

For constant-volume process:

For constant-pressure process:

Page 62: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

62

What is the relationship between the change in energy and enthalpy?

Energy transfer occurs as heat when little or no work gets done. This is the case in three scenarios:

1. Reactions that do not involve gases (done at constant pressure with little or no volume change).

2. Reactions in which the number of moles of gas does not change (when Δn = 0 then ΔV = 0).

3. Reaction in which the volume (i.e., moles) changes but the work is negligible compared to the heat.

Page 63: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

63

Heat capacity at constant pressure (or isobaric heat – constant P

An isobaric process is a constant-pressure process. In general, none of the three quantities ΔU, Q and dW is zero in an isobaric process

For closed syst. in equilib., P-V work only

ΔH =

Page 64: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

64

Heat capacity at constant volume (or isochoric heat capacity)-constant V

V f = V i : vertical line on p V diagram

An isochoric process is a constant-volume process. When the volume of a thermodynamic system is constant, it does zero work on the surroundings. Then W = 0, and

In an isochoric process, all the energy added as heat remains in the system as an increase in internal energy. Heating a gas in a closed constant-volume container is an example of an isochoric process. (Note that there are types of work that do not involve a volume change. For example, we can do work on a fluid by stirring it. In some cases, “isochoric” is used to mean that no work is done).

For closed syst. in equilib., P-V work only w is zero

Page 65: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

65

What is Joule Thompson's experiment?

It is an experiment in which the Joule-Thomson coefficient is measured. Basically, you are expanding a gas under adiabatic conditions to ensure constant enthalpy and you will notice that there will be a temperature change (most likely cooling).

We look at the Joule Expansion to learn how to relate derivatives, such as du/dV under constant temperature and du/dT under constant volume. The Joule Expansion can be used to find these quantities.

Page 66: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

66

Joule coefficientInitially, chamber A is filled with a gas, and

chamber B is evacuated. The valve between the chambers

is then opened. After equilibrium is reached, the

temperature change in the system is measured by the

thermometer.

Because the system is surrounded by adiabatic walls, q = 0, no heat flows into or out

of the system. Finite unbalanced forces act within the system, and as the gas rushes

into B, there is turbulence and lack of pressure equilibrium. Therefore dw = -PdV

does not apply. The only motion that occurs is within the system itself. Therefore the

gas does no work on its surroundings, and vice versa. Hence w=0 for expansion into a

vacuum. Since ∆U=q+w for a closed system, we have ∆U = 0+0 = 0.

The experiment measures the temperature change with change in volume at constant

internal energy,

Page 67: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

67

Joule–Thomson experimentinvolves the slow throttling of a gas through a rigid, porous plug

P2 < P1

The partition B is porous but not greatly so. This allows the gas to be slowly

forced from one chamber to the other.

w = wL + wR

Page 68: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

68

w=wL+wR

P1V1 - P2V2

Measurement of the temperature change ∆T=T2 - T1 in the

Joule–Thomson experiment gives ∆T/ ∆P at constant H

Page 69: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

69

Perfect gas and the first law

Perfect gas obeys both the following equations:

For a closed system in equilibrium, the internal energy (and any other state function)can be expressed as a function of temperature and volume. However eqn. above states that for a perfect gas U is independent of volume. Therefore U of a perfect gas depends only on temperature. So:

We now apply the first law to a perfect gas:

Page 70: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

70

Page 71: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

71

Page 72: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

72

Page 73: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

73

An isothermal process is one that occurs at constant temperature. The gas-piston container in our example could expand isothermally if it were kept immersed in a large hot-water bath while the gas expanded. Since the temperature doesn't change during an isothermal process, there is no change in internal energy. The first law then tells you that the work done by the gas is just equal to the heat that flows into the system from the bath.

An adiabatic process is one that occurs without the exchange of heat with the surroundings. If the gas-piston system were insulated so that heat could not get in or out, any expansion or compression would occur adiabatically. Since Q = 0 for an adiabatic process, the first law tells you that the change in internal energy is just equal to the work done on the system.

Both are reversible/irreversible processes?

Isothermal process in a perfect gas Adiabatic process in a perfect gas

dq = 0 and q = 0

Page 74: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

74

When a gas expands adiabatically, the work done in the expansion comes at the expense of the internal energy of the gas, causing the temperature of the gas to drop.

The figure below shows P-V diagrams for these two processes.

The figure compares two processes that begin with the same state and involve expansion to the same final volume. For the isothermal process, the product of P·V remains constant since T remains constant. Since the temperature must decrease for the adiabatic process, it follows that the final pressure must be less for this process. Thus the adiabatic lies below the isotherm.

Page 75: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

75

Page 76: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

76

THE MOLECULAR NATURE OF INTERNAL ENERGY

The molecular description of internal energy is outside the scope of thermodynamics, but a qualitative understanding of molecular energies is helpful.

Consider first a gas. The molecules are moving through space. A molecule has atranslational kinetic energy mv2, where m and v are the mass and speed of the molecule. A translation is a motion in which every point of the body moves the same distance in the same direction.

If each gas molecule has more than one atom, then the molecules undergo rotational and vibrational motions in addition to translation. A rotation is a motion in which the spatial orientation of the body changes, but the distances between all points in the body remain fixed and the center of mass of the body does not move (so that there is no translational motion).

Besides translational and rotational energies, the atoms in a molecule have vibrational energy. In a molecular vibration, the atoms oscillate about their equilibrium positions in the molecule. A molecule has various characteristic ways of vibrating, each way being called a vibrational normal mode.

Page 77: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

77

Figure 2.14 shows translational, rotational, and vibrational motions in CO2.

Page 78: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

78

The limitations of the first law of Thermodynamics.

1. No restriction on the direction of the flow of heat: the first law establishes definite relationship between the heat absorbed and the work performed by a system. The first law does not indicate whether heat can flow from a cold end to a hot end or not. For example: we cannot extract heat from the ice by cooling it to a low temperature. Some external work has to be done.

2. Does not specify the feasibility of the reaction: first law does not specify that process is feasible or not for example: when a rod is heated at one end then equilibrium has to be obtained which is possible only by some expenditure of energy.

3. Practically it is not possible to convert the heat energy into an equivalent amount of work.

• To overcome this limitations, another law is needed which is known as second law of thermodynamics. The second law of thermodynamics helps us to predict whether the reaction is feasible or not and also tell the direction of the flow of heat. It also tells that energy cannot be completely converted into equivalent work.

Page 79: PPT 107 PHYSICAL CHEMISTRY Semester 2 Semester 2 Academic session 2012/2013 1.

79….END OF CHAPTER 2….