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The Story of Spontaneity and Energy Dispersal. You never get what you want: 100% return on investment. Spontaneity. Spontaneous process are those that occur naturally. Hot body cools A gas expands to fill the available volume - PowerPoint PPT Presentation

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Page 1: The Story of Spontaneity and Energy Dispersal

The Story of Spontaneity and Energy DispersalYou never get what you want:

100% return on investment

Page 2: The Story of Spontaneity and Energy Dispersal

SpontaneitySpontaneous process are those that

occur naturally.Hot body coolsA gas expands to fill the available volume

A spontaneous direction of change is where the direction of change does not require work to bring it about.

Page 3: The Story of Spontaneity and Energy Dispersal

SpontaneityThe reverse of a spontaneous

process is a nonspontaneous processConfining a gas in a smaller volumeCooling an already cool object

Nonspontaneous processes require energy in order to realize them.

Page 4: The Story of Spontaneity and Energy Dispersal

SpontaneityNote:

Spontaneity is often interpreted as a natural tendency of a process to take place, but it does not necessarily mean that it can be realized in practice.

Some spontaneous processes have rates sooo slow that the tendency is never realized in practice, while some are painfully obvious.

Page 5: The Story of Spontaneity and Energy Dispersal

SpontaneityThe conversion of diamond to

graphite is spontaneous, but it is joyfully slow.

The expansion of gas into a vacuum is spontaneous and also instantaneous.

Page 6: The Story of Spontaneity and Energy Dispersal

2ND LAW OF THERMODYNAMICS

Page 7: The Story of Spontaneity and Energy Dispersal

The 2nd Law of Thermodynamics“No process is possible in which the

sole result is the absorption of heat from a reservoir and its complete conversion into work”

Statement formulated by Lord Kelvin

Page 8: The Story of Spontaneity and Energy Dispersal

The 2nd Law of ThermodynamicsThe 2nd Law of Thermodynamics

recognizes the two classes of processes, the spontaneous and nonspontaneous processes.

Page 9: The Story of Spontaneity and Energy Dispersal
Page 10: The Story of Spontaneity and Energy Dispersal

HotReservoir

Heat Engine Work

HeatColdReservoir

Page 11: The Story of Spontaneity and Energy Dispersal
Page 12: The Story of Spontaneity and Energy Dispersal

What determines the direction of spontaneous change?The total internal energy of a system

does NOT determine whether a process is spontaneous or not.

Per the First Law, energy is conserved in any process involving an isolated system.

Page 13: The Story of Spontaneity and Energy Dispersal

What determines the direction of spontaneous change?Instead, it is important to note that

the direction of change is related to the distribution of energy.

Spontaneous changes are always accompanied by a dispersal of energy.

Page 14: The Story of Spontaneity and Energy Dispersal

Energy DispersalSuperheroes with

energy blasts and similar powers as well as the Super Saiyans are impossible characters.

They seem to violate the Second Law of Thermodynamics!

Page 15: The Story of Spontaneity and Energy Dispersal

Power

Kamehame wave

Page 16: The Story of Spontaneity and Energy Dispersal

Energy DispersalA ball on a warm

floor can never be observed to spontaneously bounce as a result of the energy from the warm floor

Page 17: The Story of Spontaneity and Energy Dispersal

Energy DispersalIn order for this to

happen, the thermal energy represented by the random motion and vibrations of the floor atoms would have to be spontaneously diverted to accumulate into the ball.

Page 18: The Story of Spontaneity and Energy Dispersal

Energy Dispersal It will also require the

random thermal motion to be redirected to move in a single direction in order for the ball to jump upwards.

This redirection or localization of random, disorderly thermal motion into a concerted, ordered motion is so unlikely as to be virtually impossible.

Page 19: The Story of Spontaneity and Energy Dispersal

Energy Dispersal and SpontaneitySpontaneous change can now be

interpreted as the direction of change that leads to the dispersal of the total energy of an isolated system!

Page 20: The Story of Spontaneity and Energy Dispersal

EntropyA state function, denoted by S.

While the First Law can be associated with U, the Second Law may be expressed in terms of the S

Page 21: The Story of Spontaneity and Energy Dispersal

Entropy and the Second LawThe Second Law can be expressed in

terms of the entropy:

The entropy of an isolated system increases over the course of a spontaneous change: ΔStot > 0

Where Stot is the total entropy of the system and its surroundings.

Page 22: The Story of Spontaneity and Energy Dispersal

EntropyA simple definition of entropy is that

it is a measure of the energy dispersed in a process.

For the thermodynamic definition, it is based on the expression:

Page 23: The Story of Spontaneity and Energy Dispersal

EntropyFor a measurable change between two

states,

In order to calculate the difference in entropy between two states, we find a reversible pathway between them and integrate the energy supplied as heat at each stage, divided by the temperature.

Page 24: The Story of Spontaneity and Energy Dispersal

Example

Page 25: The Story of Spontaneity and Energy Dispersal

Change in entropy of the surroundings: ΔSsur If we consider a transfer of heat dqsur to the surroundings,

which can be assumed to be a reservoir of constant volume.

The energy transferred can be identified with the change in internal energy dUsur is independent of how change brought about (U is state

functionCan assume process is reversible, dUsur= dUsur,rev

Since dUsur = dqsur and dUsur= dUsur,rev, dqsur must equal dqsur,rev

That is, regardless of how the change is brought about in the system, reversibly or irreversibly, we can calculate the change of entropy of the surroundings by dividing the heat transferred by the temperature at which the transfer takes place.

Page 26: The Story of Spontaneity and Energy Dispersal

Change in entropy of the surroundings: ΔSsur

For adiabatic change, qsur = 0, so DSsur = 0

Page 27: The Story of Spontaneity and Energy Dispersal

Entropy: A molecular look Boltzmann formula:

Entropy is a reflection of the microstates, the ways in which the molecules of a system can be arranged while keeping the total energy constant.

Page 28: The Story of Spontaneity and Energy Dispersal

Entropy as a State Function To prove entropy is a state function we must show that ∫dS

is path independent Sufficient to show that the integral around a cycle is zero or

Sadi Carnot (1824) devised cycle to represent idealized engine

dSdqT 0

HotReservoir

ColdReservoir

Engine-w2

-w1w3

w4

qh

qc

Th

Tc

Step 1: Isothermal reversible expansion @ Th

Step 2:Adiabatic expansion Th to Tc

Step 3:Isothermal reversible compression @ Tc (sign of q negative)Step 4: Adiabatic compression Tc to Th

Page 29: The Story of Spontaneity and Energy Dispersal

Carnot CycleStep 1: ΔU=0

Step 2: ΔU=w

Step 3: ΔU=0

Step 4: ΔU=-w

Page 30: The Story of Spontaneity and Energy Dispersal

Carnot Cycle - Thermodynamic Temperature Scale

The efficiency of a heat engine is the ratio of the work performed to the heat of the hot reservoir

e=|w|/qh The greater the work the greater

the efficiency Work is the difference between

the heat supplied to the engine and the heat returned to the cold reservoir

w = qh -(-qc) = qh + qc

Therefore, e = |w|/qh = ( qh + qc)/qh = 1 + (qc/qh )

HotReservoir

HeatEngine Work

HeatColdReservoir

qh

-qc

w

Page 31: The Story of Spontaneity and Energy Dispersal

Efficiency of Heat EnginesEfficiency is the ratio of the work done by

an engine in comparison to the energy invested in the form of heat for all reversible engines

All reversible engines have the same efficiency irrespective of their construction.

Page 32: The Story of Spontaneity and Energy Dispersal

Carnot Cycle - Thermodynamic Temperature Scale

HotReservoir

HeatEngine Work

HeatColdReservoir

qh

-qc

w William Thomson (Lord Kelvin) defined

a substance-independent temperature scale based on the heat transferred between two Carnot cycles sharing an isotherm

He defined a temperature scale such that qc/-qh = Tc/Th

e = 1 - (Tc/Th ) Zero point on the scale is that

temperature where e = 1 Or as Tc approaches 0 e approaches

1 Efficiency can be used as a measure

of temperature regardless of the working fluid

Applies directly to the power required to maintain a low temperature in refrigerators

Efficiency is maximized

Greater temperature difference between reservoirs

The lower Tc, the greater the efficiency

Page 33: The Story of Spontaneity and Energy Dispersal

Refrigeration

Page 34: The Story of Spontaneity and Energy Dispersal

Coefficient of performance (COP or β or c)

COP describes the qc in this case as the minimum energy to be supplied to a refrigeration-like system in order to generate the required entropy to make the system work.

Page 35: The Story of Spontaneity and Energy Dispersal

Entropy changes: ExpansionEntropy changes in a system are

independent of the path taken by the process

Total change in entropy however depend on the path:Reversible process: ΔStot = 0 Irreversible process: ΔStot > 0

Page 36: The Story of Spontaneity and Energy Dispersal

Isothermal Isochoric Isobaric Adiabatic

ΔU 0 nCvΔT q+w w

q nRT ln or -wirrev

nCvΔT nCpΔT or –wirrev 0

wrev -nRT ln 0 -nRT ln

wirrev -pextΔV 0 -pextΔV =-nCvΔT=-pextΔV

ΔH 0 (for ideal gas) ΔU=ΔU + pΔV

=nCpΔT

ΔS = = 0

Page 37: The Story of Spontaneity and Energy Dispersal

Entropy changes: Phase Transitions

Trouton’s rule: An empirical observation about a wide range of liquids providing approximately the same standard entropy of vaporization, around 85 J/mol K.

Page 38: The Story of Spontaneity and Energy Dispersal

General equations for entropy during a heating process S as a function of T and V, at

constant P

S as a function of T and P, at constant V

Page 39: The Story of Spontaneity and Energy Dispersal

Measurement of Entropy (or molar entropy)

Page 40: The Story of Spontaneity and Energy Dispersal

Measurement of Entropy (or molar entropy)The terms in the previous equation

can be calculated or determined experimentally

The difficult part is assessing heat capacities near T = 0.

Such heat capacities can be evaluated via the Debye extrapolation

Page 41: The Story of Spontaneity and Energy Dispersal
Page 42: The Story of Spontaneity and Energy Dispersal

Measurement of Entropy (or molar entropy)In the Debye extrapolation, the

expression below is assumed to be valid down to T=0.

Page 43: The Story of Spontaneity and Energy Dispersal

Third Law of ThermodynamicsAt T = 0, all energy of thermal motion has been

quenched, and in a perfect crystal all the atoms or ions are in a regular, uniform array.

The localization of matter and the absence of thermal motion suggest that such materials also have zero entropy.

This conclusion is consistent with the molecular interpretation of entropy, because S = 0 if there is only one way of arranging the molecules and only one microstate is accessible (the ground state).

Page 44: The Story of Spontaneity and Energy Dispersal

Third Law of Thermodynamics

The entropy of all perfect crystalline substances is zero at T = 0.

Page 45: The Story of Spontaneity and Energy Dispersal

Nernst heat theoremThe entropy change accompanying

any physical or chemical transformation approaches zero as the temperature approaches zero: ΔS 0 as T 0 provided all the substances involved are perfectly crystalline.

Page 46: The Story of Spontaneity and Energy Dispersal

Third-Law entropiesThese are entropies reported on the

basis that S(0) = 0.

Page 47: The Story of Spontaneity and Energy Dispersal
Page 48: The Story of Spontaneity and Energy Dispersal

Exercises

Page 49: The Story of Spontaneity and Energy Dispersal

HELMHOLTZ AND GIBBS ENERGIES

Page 50: The Story of Spontaneity and Energy Dispersal

Clausius inequality

The Clausius inequality implies that dS 0.

“In an isolated system, the entropy cannot decrease when a spontaneous change takes place.”

Page 51: The Story of Spontaneity and Energy Dispersal

Criteria for spontaneity

In a system in thermal equilibrium with its surroundings at a temperature T, there is a transfer of energy as heat when a change in the system occurs and the Clausius inequality will read as above:

Page 52: The Story of Spontaneity and Energy Dispersal

Criteria for spontaneityWhen energy is transferred as heat at constant volume:

*dq = dU At either constant U or constant S:

Which leads to

Page 53: The Story of Spontaneity and Energy Dispersal

Criteria for spontaneityWhen energy is transferred as heat at

constant pressure, the work done is only expansion work and we can obtain

At either constant H or constant S:

Which leads to

Page 54: The Story of Spontaneity and Energy Dispersal

Criteria for spontaneityWe can introduce new

thermodynamic quantities in order to more simply expressand

Page 55: The Story of Spontaneity and Energy Dispersal

Helmholtz and Gibbs energyHelmholtz energy,

A:A = U - TS

dA = dU – TdS

dAT,V ≤ 0

Gibbs energy, G:G = H - TS

dG = dH – TdS

dGT,p ≤ 0

Page 56: The Story of Spontaneity and Energy Dispersal

Helmholtz energyA change in a system at constant

temperature and volume is spontaneous if it corresponds to a decrease in the Helmholtz energy.

Aside from an indicator of spontaneity, the change in the Helmholtz function is equal to the maximum work accompanying a process.

Page 57: The Story of Spontaneity and Energy Dispersal

Helmholtz energy

Page 58: The Story of Spontaneity and Energy Dispersal
Page 59: The Story of Spontaneity and Energy Dispersal
Page 60: The Story of Spontaneity and Energy Dispersal

, useful

Page 61: The Story of Spontaneity and Energy Dispersal
Page 62: The Story of Spontaneity and Energy Dispersal

Variation of the Gibbs free energy with temperature

Page 63: The Story of Spontaneity and Energy Dispersal

Variation of the Gibbs free energy with pressure

Page 64: The Story of Spontaneity and Energy Dispersal

Variation of the Gibbs free energy with pressure

Page 65: The Story of Spontaneity and Energy Dispersal

Homework1. When 1.000 mol C6H12O6 (glucose) is oxidized to carbon

dioxide and water at 25°C according to the equation C6H12O6(s) + 6 O2(g) 6 CO2(g) + 6 H2O(l), calorimetric measurements give ΔrHθ= -2808 kJ mol-1 and ΔrSθ = +182.4 J K-1 mol-1 at 25°C. How much of this energy change can be extracted as (a) heat at constant pressure, (b) work?

2. How much energy is available for sustaining muscular and nervous activity from the combustion of 1.00 mol of glucose molecules under standard conditions at 37°C (blood temperature)? The standard entropy of reaction is +182.4 J K-1 mol-1.

3. Calculate the standard reaction Gibbs energies of the following reactions given the Gibbs energies of formation of their components

a) Zn(s) + Cu2+(aq) Zn2+(aq) + Cu(s)b) C12H22O11(s) + 12 O2(g) 12 CO2(s) + 11 H2O(l)

Page 66: The Story of Spontaneity and Energy Dispersal
Page 67: The Story of Spontaneity and Energy Dispersal
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One for the roadLife requires the assembly of a large

number of simple molecules into more complex but very ordered macromolecules. Does life violate the Second Law of Thermodynamics? Why or why not?