thermodynamics (that’s hot!!! or…. not!) the nature of energy kinetic energy potential energy...

49
Thermodynamics (That’s Hot!!! Or…. Not!)

Upload: albert-fields

Post on 26-Dec-2015

240 views

Category:

Documents


23 download

TRANSCRIPT

Page 1: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Thermodynamics(That’s Hot!!! Or…. Not!)

Page 2: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

The Nature of Energy

• Kinetic Energy

• Potential Energy

• Physics and Chemistry Agree

– Sometimes

Page 3: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

First Law of Thermodynamics

• Energy in the universe is constant

• You’ve heard this stated another way

• Law of conservation of energy

– Energy can be neither created nor destroyed

– It is transferred.

Page 4: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

What is Energy?

When you think of energy, what comes to mind?

Page 5: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

“Forms” of EnergyWe associate energy with “enthalpy”

• The “force” that holds things together

• Whenever there is a “change”, we can describe it as a change in Energy (enthalpy)

• How much of an energy change is there?

• How do we measure the change?

Atoms →moleculesmolecules→ cellscells → plants / animals Plants / animals→ ecosystems

SolidLiquidGasPlasma

Page 6: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Foreshadowing Energy

• Entropy and Free energy will be discussed in the next chapter

• Enthalpy is what we are studying now

– Describe what bonds atoms and molecules to each other

– The production of heat (or absorbing)

Page 7: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Measuring EnergyTemperature, Heat and Work

Temperature - random motion of particles

average kinetic energy

Heat - transfer of energy

due to a temperature difference– Heat is not contained by an object

– If your hand is the same temperature as the radiator, would it feel hot?

– It is the temperature difference that feels hot

– The fire has a lot of heat.

Work is force acting over a distance.

Page 8: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

When Energy Transfers Occur, Does the Pathway Matter?

Or Is It a State Function?

• Energy of a “system” is independent of where the energy came from or how it got there

• Energy of a system depends on what is in the system and their temperatures.

–Energy is a STATE FUNCTION

Page 9: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Internal Energy of a System

• Sum of the potential and kinetic energies

• A change in energy is done by work (motion) or heat

• E = q + w

q = heat

w = work

Page 10: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

WorkUsually in an open container the only work done is by a gas pushing on the surroundings (or by the surroundings pushing on the gas).

Work = Force x distance = Pressure x area x height= Pressure x VolumePressure and Volumes are State Functions

Page 11: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

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

Page 12: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

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 (H) of the system.

• Enthalpy is the internal energy plus the product of pressure and volume:

H = E + PVSince E, P, and V are State functions, then Enthalpy is a state function as well!

Page 13: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

State Functions

• However, q and w are not state functions.

• Whether this battery is shorted out or is discharged by running the fan, its E is the same.

– But q and w are different in the two cases.

Page 14: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Heat and Work

• More proof that heat and work are not state functions

• Ex. 2: Imagine two magic boxes

• Each has 1g sugar or 1g of magnesium.

There is a different amount of work (gases expanding against the atmosphere), light and heat produced for each gram of material burned.

Page 15: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Enthalpy

• When the system changes at constant pressure, the change in enthalpy, H, is

H = (E + PV)

• This can be written

H = E + PV

Page 16: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Enthalpy• Since E = q + w and 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 is the heat gained or lost.

Page 17: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Endothermicity and Exothermicity

• A process is endothermic when H is positive.

Page 18: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Endothermicity and Exothermicity

• A process is endothermic when H is positive.

• A process is exothermic when H is negative.

Page 19: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Signs and Thermodynamics

• Energy Change

E < 0, or negative

• system loses energy

E > 0, or positive

• system gains energy

Page 20: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Sign Conventions in Thermodynamics• Heat

q > 0

• Increase in temp

q < 0

• Decrease in temp

Page 21: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Sign Conventions in Thermodynamics

• Work is more complicated

W = - PV• P = Pressure on the system

• V = Change in volume

• If a piston increases in size, it must move against the universe. So energy has left the system and gone into the universe. This is exothermic so E would be negative. Since the change in volume is positive, the sign is -PV. (Pg 247 in Book)

Page 22: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Sign Conventions• So any work done by the system on the universe will be

exothermic meaning w = -

• If work is done on the system by the universe, then it is endothermic meaning w = + .

• Pressure is measured in N/m2 which = 1Pa

• If you have 1kPa of Pressure and Volume is in L, then PV = J

• 1L•kPa = 1J

• 101.3kPa = 1 atm

• 1L•atm = 101.3 J

(in case you were wondering)

Page 23: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Sample Problem

• A balloon is heated with 1.3 x 108 J and expands from 4.00 x 106 L to 4.5 x 106 L. Assuming constant outside pressure of 1.0 atm, calculate the change in energy

• E = q + w

• q = +1.3 x 108 J

• W = -P V = -1.0 atm x (4.50 x 106 L - 4.00 x 106 L)

- 0.50 x 106 L atm x (101.3 J / L ATM ) = -5.1 x 107 J

• E = +1.3 x 108 J - 5.1 x 107J = 8.0 x 107 J

Page 24: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

H= qp

• E = Eprod - Ereact

• CH4 + 2O2 CO2 + 2 H2O + energy

qp = H = -890 Kj/mol

notice negative value (energy left system)

• Stoichiometry type problems

• Energy is a reactant or product

Page 25: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Chemical Energy

• CH4 + O2 CO2 + 2 H2O + energy

• We must define “THE SYSTEM”

• The container with the methane and oxygen is a system

• The rest of the Universe is not the system.

• Heat flows out of the system – exothermic

CH4 + O2 CO2 + 2 H2O

energy

Page 26: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Chemical Energy

• CH4 + 2O2 CO2 + 2 H2O + energy

• Chemical (potential) energy

– is converted to thermal (random kinetic energy)

• CH4 + 2O2 has more potential energy

• CO2 + 2 H2O has less potential energy

• The difference is the energy released

CH4 + O2

CO2 + 2 H2OE

Page 27: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Chemical Energy

• N2O2 + energy 2 NO

• N2O2 has less potential energy than

• 2 NO

• The difference is the energy absorbed from universe

• This is endothermic

N2O2

2 NO

E

Page 28: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Enthalpy Problems

• CH4 + 2O2 CO2 + 2 H2O + energy

qp = H = -890 Kj/mol

• A 5.8g sample of methane is burned in oxygen at a constant pressure. How much heat is given off? What is the enthalpy change?

• 5.8g x 1 mol x -890. kJ = -322 kJ 16.0g mol

• E = Eprod - Ereact = q = -322kJ

• q = 322 kJ

Page 29: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Ways to determine Enthalpies of Reactions• Calorimetry – determine through

experimentation and calculating heat flow.

• Hess’ Law – Calculate enthalpies of a series of reactions that when added together give the desired reaction

• Heats of Formations – Use determined energies of compounds to determine the overall enthalpy change.

• Bond Energies – Bonds broken – bonds formed (later)

Page 30: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Calorimetry

Since we cannot know the exact enthalpy of the reactants and products, we measure H through calorimetry, the measurement of heat flow.

Page 31: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Heat Capacity and Specific HeatThe amount of energy required to raise the temperature of a substance by 1 K (1C) is its heat capacity.

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.

• Molar Heat Capacity is the amount of energy required to raise the temperature of 1 mole of a substance 1K.

• Remember a change of 1K and 1oC are the same!

Page 32: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Heat Capacity and Specific Heat

Specific heat (Cp), then, is used mathematically by the following equation:

turein tempera changeheat x specific x mass ferredheat trans

TmCq P

Page 33: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Calorimetry– Why does a piece of metal feel cold to your

hand?

– Why does the sand heat up faster than the water at the beach?

– Why does the center of the United States have more temperature extremes than the coasts?

– Why do ceramic tiles prevent a spacecraft from burning up upon reentry into the atmosphere?

Page 34: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Calorimetry

• Constant Pressure Calorimetry (open)

q = H

q = mCp T.

• Constant Volume Calorimetry (Bomb)

q = E (need to know heat capacity of calorimeter)

qrxn = Ccal ΔT

Page 35: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Hess’ Law or State Functions

NO2(g) 1NO(g) + 1/2O2(g) H = 56 kJ/mol

Double the reaction = double the enthalphy

2NO2(g) 2NO(g) + O2(g) H = 112 kJ/mol

The reverse of the reaction, “negative”

2NO(g) + O2(g) 2NO2(g) H =- 112 kJ/mol

Page 36: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Hess’ Law

N2(g) + 2O2(g) 2NO2(g) H = 68 kJ/mol

Can be determined by:N2(g) + O2(g) 2NO(g) H = 180 kJ/mol

2NO(g) + O2(g) 2NO2(g) H =- 112 kJ/mol

N2(g) + 2O2(g) 2NO2(g) H = 68 kJ/mol

Page 37: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Hess’s Law

• Works because Enthalpy is a state function

– The pathway is not important

– How we get there is not important

– You can use a series of known equations to “add up” to equal the equation you desire.

• Arrange the steps to equal the overall equation

– Add up the enthalpies

Page 38: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

2B(s) + 3H2(g) B2H6

kJ

2B(s) + 3/2 O2(g) B2O3(S) -1273

B2O3(s) + 3H2O(g) B2H6(g) + 3O2 +2035

3H2(g) + 3/2O2(g) 3H2O(l) -858

3H2O(l) 3H2O(g) 132

Pg 258

2B(s) + H2(g) B2H6 +36

Page 39: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

2B(s) + 3H2(g) B2H6

kJ

2B(s) + 3/2 O2(g) B2O3(S) -1273

B2H6(g) + 3O2 B2O3(s) + 3H2O(g) -2035

H2(g) + 1/2O2(g) H2O(l) -286

H2O(l) H2O(g) 44

OK

Backwards

Opposite sign

Not enough

X 3Not enough

X 3

Page 40: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

kJ

2B(s) + 3/2 O2(g) B2O3(S) -1273

B2O3(s) + 3H2O(g) B2H6(g) + 3O2 +2035

3H2(g) + 3/2O2(g) 3H2O(l) -858

3H2O(l) 3H2O(g) 132

2B(s) + 3H2(g) B2H6

+36

Page 41: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Hess’s Law

Calculate ΔH for the reaction

2 C(s) + H2(g) C2H2(g)

given the following chemical equations and their respective enthalpy changes:

C2H2(g) + 5/2 O2(g) 2 CO2(g) + H2O(l) ΔH = -1299.6 kJ

C(s) + O2(g) CO2(g) ΔH = -393.5 kJ

H2(g) + ½ O2(g) H2O(l) ΔH = -285.8 kJ

Page 42: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Enthalpies of FormationAn enthalpy of formation, Hf, is defined as the enthalpy change for the reaction in which one mole of a compound is made from its constituent elements in their elemental forms.

Standard enthalpies of formation, Hf°, are measured under standard conditions (25 °C and 1.00 atm pressure).

See Appendix of textbook for tables of Hf°.

Page 43: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Calculation of H

• Imagine this as occurring

in three steps:

C3H8 (g) + 5 O2 (g) 3 CO2 (g) + 4 H2O (l)

C3H8 (g) 3 C (graphite) + 4 H2 (g)

3 C (graphite) + 3 O2 (g) 3 CO2 (g)

4 H2 (g) + 2 O2 (g) 4 H2O (l)

C3H8 (g) + 5 O2 (g) 3 CO2 (g) + 4 H2O (l)

Page 44: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Calculation of HWe can use Hess’s law in this way:

H = nHf°products – mHf° reactants

where n and m are the stoichiometric coefficients.

Take the sum of the products’ heats of formation and subtract the sum of the reactants’ heats of formation.

The Standard Heat of Formation of any element in it’s standard state is 0!

Page 45: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Practice

• For which of the following reactions at 25 ºC would the enthalpy change represent a standard enthalpy of formation?

(A) 2 Na(s) + ½ O2(g) Na2O (s)

(B) 2 K(l) + Cl2(g) 2 KCl(s)

(C) C6H12O6(s) 6 C(diamond) + 6 H2(g) + 3O2(g)

Page 46: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Practice

• Calculate the standard enthalpy change for the combustion of 1 mol of benzene, C6H6(l), to form CO2(g) and H2O(l).

• ΔHfº: CO2(g) = -393.5 kJ/mol

H2O (l) = -285.8 kJ/mol

C6H6(l) = 49.0 kJ/mol

O2 (g) = 0 kJ/mol

Page 47: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Practice

• Calculate the standard enthalpy change for the combustion of 1 mol of benzene, C6H6(l), to form CO2(g) and H2O(l).

• ΔHfº: CO2(g) = -393.5 kJ/mol

H2O (l) = -285.8 kJ/mol

C6H6(l) = 49.0 kJ/mol

O2 (g) = 0 kJ/mol

• -3267 kJ/mol

Page 48: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Practice

• The standard enthalpy change for the reaction

CaCO3(s) CaO(s) + CO2(g)

is 178.1 kJ. From the values for the standard enthalpies of formation of CaO(s) (-635.5 kJ) and CO2(g) (-393.5 kJ), calculate the standard enthalpy of formation of CaCO3(s).

Page 49: Thermodynamics (That’s Hot!!! Or…. Not!) The Nature of Energy Kinetic Energy Potential Energy Physics and Chemistry Agree –Sometimes

Practice

• The standard enthalpy change for the reaction

CaCO3(s) CaO(s) + CO2(g)

is 178.1 kJ. From the values for the standard enthalpies of formation of CaO(s) (-635.5 kJ) and CO2(g) (-393.5 kJ), calculate the standard enthalpy of formation of CaCO3(s).

• -1207.1 kJ/mol