Entropy, Free Energy, and Nuclear Chemistry Notes
Thermodynamics Review
- Thermodynamics: Study of heat and motion.
- Thermochemistry: Subset of thermodynamics (studied in Chpt 5).
Definitions
- System: Part of the universe under study.
- Surroundings: Rest of the universe (not under study).
- Exothermic Reaction: Transfers thermal energy from the system to the surroundings.
- Endothermic Reaction: Transfers thermal energy from the surroundings to the system.
- First Law of Thermodynamics: Law of conservation of energy.
- Enthalpy Change: Thermal energy transferred at constant pressure.
- State Function: Quantity whose value is determined only by the initial and final state of a system.
Spontaneous Processes
- Many naturally occurring processes tend to be exothermic, but enthalpy is only part of the story.
- Examples of Spontaneous Processes:
- Water flows downhill.
- Ice melts on a warm day.
- Eating an apple and excreting CO<em>2 and H</em>2O. Ingesting CO<em>2 and H</em>2O does not spontaneously produce an apple.
- Zinc metal dissolving in a strong acid solution: Zn(s)+2H<em>3O+(aq)→Zn2+(aq)+H</em>2(g)+2H2O(l)
Entropy and Spontaneity
- Two factors are important: Enthalpy and Entropy.
- Entropy (S): Measure of disorder (more disorder, more entropy).
- AS=S<em>2−S</em>1
- Balls naturally roll down hills, not up. Negative ΔH favors spontaneity.
- Rooms naturally get messy, more disordered. Positive ΔS favors spontaneity.
Generalizations About Entropy Changes
- As the temperature of a system increases, entropy increases (ΔS is positive).
- As the volume in which gas particles can move increases, entropy increases (ΔS is positive).
- As the number of gas particles in the system increases, entropy increases (ΔS is positive).
- As the size and complexity of the molecules increase, entropy increases.
- Examples:
- 2C<em>2H</em>4(g)→C<em>4H</em>8(g): ΔS is negative because there are fewer molecules (less disorder).
- C<em>4H</em>8(g;298K;1atm)→C<em>4H</em>8(g;298K;0.5atm): ΔS is positive because volume increased.
- C<em>4H</em>8(g;298K;1atm)→C<em>4H</em>8(g;398K;1atm): ΔS is positive because temperature increased.
- Ranking entropy: H2O(s) < H2O(l) < H_2O(g)
Spontaneity and ΔH and ΔS
- 2C(graphite)+O2(g)→2CO(g)
- ΔH is negative (favors).
- ΔS is positive (favors).
- N<em>2(g)+2O</em>2(g)→2NO2(g)
- ΔH is positive (disfavors).
- ΔS is negative (disfavors).
Second Law of Thermodynamics
- In a spontaneous process, the entropy of the universe increases (\Delta S_{univ} > 0).
- ΔS<em>univ=ΔS</em>sys+ΔSsurr
- ΔS<em>surr relates to the heat change of the system (ΔH</em>sys) and temperature.
- ΔS<em>surr=−TΔH</em>sys
- The 2nd Law: \Delta S{univ} = \Delta S{sys} - \frac{\Delta H_{sys}}{T} > 0
- T \cdot (\Delta S{sys} - \frac{\Delta H{sys}}{T}) > 0
- \Delta H{sys} - T\Delta S{sys} < 0
Gibb's Free Energy
- AG=AH−TAS
- If ΔG is negative, the reaction is spontaneous.
- If ΔG is positive, the reaction is non-spontaneous.
- If ΔG is zero, the reaction is at equilibrium.
- ΔG<em>sys=ΔH</em>sys−TΔSsys
Calculating ΔH, ΔS, and ΔG
ΔH<em>rxn∘=ΣnΔH</em>f∘(products)−ΣnΔHf∘(reactants)
- Standard state (1 atm and 1 M soln)
- Formation reaction
- n is the number of moles in the balanced reaction
Consider the reaction: 2Al(s)+Fe<em>2O</em>3(s)→Al<em>2O</em>3(s)+2Fe(s)
ΔSrxn∘=ΣnS∘(products)−ΣnS∘(reactants)
- Note: S∘ is used, not ΔS∘. The zero of entropy has been assigned (no zero of enthalpy has been assigned, so only changes can be measured).
3rd Law of Thermodynamics: The entropy of a perfect crystal is zero at 0 K.
For the previous reaction:
- ΔS∘=(1mol)(51.0J/mol⋅K)+(2mol)(27.2J/mol⋅K)−(2mol)(28.33J/mol⋅K)−(1mol)(90.0J/mol⋅K)=−41.2J/K
Using ΔG=ΔH∘−TΔS∘, at 25°C:
- ΔG∘=−848.0kJ−298K(−0.0412kJ/K)=−835.7kJ
Another way to calculate ΔG∘ is:
- ΔG<em>rxn∘=ΣnΔG</em>f∘(products)−ΣnΔGf∘(reactants)
Examples:
- a) ΔG∘=−,ΔH∘=+,ΔS∘=?
- (−)=(+)−(?)
- ΔS∘ = positive
- b) ΔG∘=+,ΔH∘=+,ΔS∘=?
- (+)=(+)−(?)
- ΔS∘ = negative or undetermined
- c) ΔS∘=+,ΔH∘=−,ΔG∘=?
- (?)=(−)−(+)
- ΔG∘ = negative
- d) ΔS∘=−,ΔH∘=−,ΔG∘=?
- (?)=(−)−(−)
- ΔG∘ = positive or negative
Cyanopyridine Example:
- C<em>4H</em>6(g)+C<em>2N</em>2(g)→C<em>6H</em>4N<em>2+H</em>2(g)
- Values provided in table in the original document.
- ΔH=257.92kJ−111.27kJ−296.52kJ=−149.87kJ
- ΔS=320.69J/K+129.83J/K−276.3J/K−239.78J/K=−65.57J/K
- ΔG=ΔH−TΔS=(−149.87kJ)−(298K)(−0.06557kJ/K)=−130.33kJ
- Conclusion: Yes, the reaction is worthwhile to attempt in the lab because it is spontaneous (negative ΔG).
- Methanol Example:
- Calculate ΔG∘ for the reaction:
- 2CH<em>3OH(g)+3O</em>2(g)→2CO<em>2(g)+4H</em>2O(g)
- ΔG∘=(2mol)(−394kJ/mol)+(4mol)(−229kJ/mol)−(2mol)(−163kJ/mol)=−1378kJ
Temperature and Spontaneity Example:
- ΔH∘=72.4kJ/mol and ΔS∘=142J/mol⋅K
- T=ΔS∘ΔH∘=0.142kJ/mol⋅K72.4kJ/mol=510K
Oxidation Numbers
- Each atom in a pure element has an oxidation number of zero.
- For monatomic ions, the oxidation number is equal to the charge of the ion.
- The following elements always have the same oxidation number in compounds:
- F is -1
- H is +1, except when with a metal
- O is -2, except when in a peroxide ion (O22−
- The sum of the oxidation numbers in a molecule or ion must add up to the charge of the molecule or ion.
Examples For Oxidation States
- O2: 0
- HNO3: +1 +5 -2
- CO: +2 -2
- CO2: +4 -2
- SO42−: +6 -2
- S8: 0
- Fe<em>2S</em>3: +3 -2
- Cr<em>2O</em>72−: +6 -2
Oxidation-Reduction (Redox)
- Oxidation: Loss of electrons
- Reduction: Gain of electrons
- LEO the lion says GER (Loss of Electrons is Oxidation, Gain of Electrons is Reduction)
- In a reaction, if one thing is oxidized, another thing must be reduced.
Redox Example
- Cu2+(aq)+Zn(s)→Cu(s)+Zn2+(aq)
- What is being oxidized? Zn
- What is being reduced? Cu
- Oxidizing Agent: Helps the other thing get oxidized (oxidizing agent is reduced).
- Reducing Agent: Helps the other thing get reduced (reducing agent is oxidized).
- Cl<em>2+H</em>2S→S8+HCl
- Oxidized: H2S
- Reduced: Cl2
- Oxidizing agent: Cl2
- Reducing agent: H2S
Voltaic Cells
Voltaic (or Galvanic) Cell generates electricity spontaneously.
Electrons are produced in one ½-cell (oxidation ½-cell).
Electrons are gained in the other ½-cell (reduction ½-cell).
Anode: Electrode where oxidation is occurring.
Cathode: Electrode where reduction is occurring.
Electrons flow from negative electrode (anode) to positive electrode (cathode).
Negative ions in the salt bridge go in the opposite direction of the electrons.
Voltage of the cell results from the two ½-cell reactions. E<em>cell=E</em>ox+Ered
Reverse a ½-reaction Change the sign of the potential.
Multiply a ½-reaction by a number DO NOT multiply the potential by a number.
Add two ½-reactions Add their potentials: E∘<em>cell=E∘</em>red+Eox∘
A positive cell voltage means the reaction is spontaneous in the direction written.
Voltaic Potential Examples
- A voltaic cell has a Mg electrode in 1 M Mg(NO<em>3)</em>2(aq) and a Ag electrode in 1 M AgNO3(aq).
- Mg2+(aq)+2e−→Mg(s)E∘=−2.37V (anode)
- Ag+(aq)+e−→Ag(s)E∘=+0.80V (cathode)
- E∘<em>cell=E∘</em>cathode−Eanode∘=0.80V−(−2.37V)=+3.17V
- A voltaic cell has a Cu electrode in 1 M CuSO<em>4(aq) and a Fe electrode in 1 M FeSO</em>4(aq).
- Cu2++2e−→Cu(s)E∘=+0.337V (cathode)
- Fe2++2e−→Fe(s)E∘=−0.44V (anode)
- Ecell∘=(0.337V)−(−0.44V)=0.777V
- Will the following reaction happen spontaneously? 2Al(s)+3Sn4+(aq)→2Al3+(aq)+3Sn2+(aq)
- Al3++3e−→Al(s)E∘=−1.66V (anode)
- Sn4++2e−→Sn2+(aq)E∘=+0.15V (cathode)
- Ecell∘=0.15−(−1.66)=+1.81V
Thermodynamics and Equilibrium
The equation E∘=nFRTlnK relates the standard state cell potential for a chemical reaction to the equilibrium constant.
R=8.314J/mol⋅K, F=96485C/mol
Using ΔG=−RTlnK and E∘=nFRTlnK
- ΔG=−nFE∘
Relating E∘ to K:
- E=E∘−nFRTlnQ
- Nernst Equation: E=E∘−n0.0257VlnQ at 25°C
- At equilibrium: Q = K and E = 0
- E∘=n0.0257VlnK
The redox reaction Co(s)+2H+→Co2+(aq)+H2(g). E° has a potential of 0.277 V.
- What is ΔG∘ for this reaction?
- ΔG∘=−nFE∘=−(2)(96485C/mol)(0.277V)=−53.5kJ/mol
- What is K for this reaction?
- E∘=n0.0257lnK
- lnK = 21.56
- K = 2.1 x 10^9
Nuclear Chemistry
- Radioactive decay: The disintegration of an unstable atomic nucleus by spontaneous emission of radiation.
- Radioisotopes: Nuclei that undergo radioactive decay.
Differences Between Chemical and Nuclear Reactions:
| Chemical Reactions | Nuclear Reactions |
|---|
| Atoms usually change their identity. | Atoms retain their identity. |
| Reactions involve only electrons. | Reactions involve mainly protons and neutrons. |
| Reaction rates can be sped up by raising the temperature. | Reaction rates are unaffected by changes in temperature. |
| Energy absorbed or given off is comparatively small. | Reactions sometimes involve enormous changes in energy. |
| Mass is conserved. | Huge changes in energy are accompanied by measurable changes in mass. |
Types of Radiation and Decay
| Radiation | Mass | Charge | Identity | Penetrating Power |
|---|
| alpha ($\alpha$) | 4 | 2+ | He$^{2+}$ | Paper can stop $\alpha$ rays. |
| beta ($\beta$) | 0.00055 | 1- | e$^-$ | Aluminum can stop $\beta$ particles. |
| gamma ($\gamma$) | 0 | 0 | High-energy photon | Lead is needed to stop $\gamma$ rays. |
- The more mass the particle has, the less penetrating it is.
- The faster the particle is, the more penetrating it is.
Nuclear Equations and Symbols
- Elements may change in nuclear reactions.
- The sum of mass numbers of reactants must equal the sum of mass numbers of products.
- The sum of atomic numbers of reactants must equal the sum of atomic numbers of products.
Nuclear Symbols
| Particles | Symbols |
|---|
| Proton | 1<em>1p or 1</em>1H |
| Neutron | 01n |
| Electron | 0ˆ<em>−1e or 0ˆ</em>−1β |
| Positron | 0ˆ<em>+1e or 0ˆ</em>+1β |
| Alpha particle | 4ˆ2He or α |
| Beta particle | β or 0ˆ−1β |
| Gamma ray | γ |
Types of Decay
- Alpha Decay (also called alpha emission): Nucleus loses an alpha particle (4ˆ2He).
- Example: 222ˆ<em>86Rn→218ˆ</em>84Po+4ˆ2He
- Beta Decay (also called beta emission): Nucleus loses a beta particle (0ˆ−1e).
- Example: 3ˆ<em>1H→3ˆ</em>2He+0ˆ−1e
- Gamma Radiation: A photon of high-energy gamma ray (γ) is emitted (typically occurs after another radioactive decay).
- Positron Emission: A positron (0ˆ+1e) is emitted (equal mass but opposite charge of an electron).
- Example: 18ˆ<em>9F→18ˆ</em>8O+0ˆ+1e
- Electron Capture: Nucleus absorbs an electron (0ˆ−1e) and then releases an X-ray.
- Example: 125ˆ<em>53I+0ˆ</em>−1e→125ˆ52Te
Radioactive Decay Series
- Parent: Unstable in a radioactive decay step.
- Daughter: Stable in a radioactive decay step.
Energy from Nucleus
- E=mc2
- For nuclear reactions, mass changes may be measurable.
- For chemical reactions, mass changes are not measurable.
Half-Life
Half-life: Time required for one-half of the sample to undergo radioactive decay.
Radioactive decay is a first-order process.
ln[A]=−kt+ln[A]0 or with activity (defined as disintegrations/time).
t1/2=k0.693
Examples
- You obtain a new sample of cobalt-60, half-life 5.25 years, with a mass of 400 mg. How much cobalt-60 remains after 19.5 years?
- k=5.25years0.693=0.132
- ln[A]=−(0.132)(19.5)+ln[400]
- ln[A]=−2.574+5.991
- ln[A]=3.417
- A=e3.417=30.48mg
- A sample of radon-222 has an initial activity of 7.0×104 disintegrations per second (dps). After 6.6 days, its activity is 2.1×104 dps. What is the half-life of radon-222?
- ln[2.1×104]=−k(6.6days)+ln[7.0×104]
- 11.16=−6.6k+11.16
- k=0.183
- t1/2=0.1830.693=3.8days
- You obtain a 20.0 mg sample of mercury-190 which has a half-life of 20 minutes. How long will it take for 15.0 mg of your sample to decay?
- k=20min0.693=0.0347min−1
- ln[15]=−0.0347min−1t+ln[20]
- t=8.29min
Radioisotopic Dating
- Use certain isotopes to estimate the age of various items.
- 235U [half-life = 4.5 billion years] - Determines age of rock.
- 3H [half-life 12.3 years] - Used to date aged.
- Carbon-14 Dating [Half-life of 5730 years] - Used to date things that were living things.
Nuclear Fission
- Fission: When a large nucleus breaks into smaller nuclei.
- Happens through a nuclear chain reaction.
- Only certain isotopes undergo nuclear chain reactions.
- Disasters:
- Three-mile Island, Pennsylvania, 1979
- Chernobyl, former Soviet Union, 1986
- Fukushima-Daiichi, Japan, 2011
Nuclear Fusion
- Reaction takes smaller nuclei and builds larger ones.
- Releases tremendous amounts of energy.
- 1 g of H would release same as 20 tons of coal.