2nd Law of Thermodynamics
Introduction to the Second Law of Thermodynamics
- This lecture discusses the second law of thermodynamics, focusing on how universal processes work.
- The driving force behind physical and chemical processes involves a combination of enthalpy and entropy.
Enthalpy vs. Entropy
- In exothermic processes, energy (enthalpy) decreases, which is generally favorable.
- However, many spontaneous processes are endothermic, indicating that enthalpy change alone doesn't fully explain spontaneity.
- Entropy plays a crucial role in determining spontaneity.
The Limitation of Entropy
- Although increasing entropy is generally favorable, some spontaneous processes involve a decrease in entropy (e.g., crystallization, freezing).
- These examples appear to contradict the idea that entropy must always increase for a spontaneous process.
The Second Law of Thermodynamics: Entropy of the Universe
- The second law states that for a spontaneous change, the entropy of the universe must increase, not just the system.
- The universe comprises both the system and the surroundings.
- If the entropy of the system decreases, it must be accompanied by a larger increase in the entropy of the surroundings, ensuring that: \Delta S_{universe} > 0
Spontaneity and Equilibrium
- \Delta S_{universe} > 0 : Spontaneous change in the forward direction.
- \Delta S_{universe} < 0 : Non-spontaneous change in the forward direction; spontaneous in reverse.
- ΔSuniverse=0: System is at equilibrium.
The Challenge of Measuring the Surroundings
- Direct measurement of the entropy change of the surroundings is impossible, as the surroundings encompass the entire universe.
- A more useful form of the second law is needed, relating ΔSsurroundings to a measurable property of the system.
Relating Surroundings to the System
- Exothermic processes release heat to the surroundings, increasing its entropy.
- Endothermic processes absorb heat from the surroundings, decreasing its entropy.
- At constant pressure, the heat exchanged (Q) is equal to the change in enthalpy ($\Delta H$).
- ΔS<em>surroundings is proportional to −ΔH</em>system.
Temperature Dependence
- The impact on ΔSsurroundings is greater when the surroundings are initially at a lower temperature.
- ΔSsurroundings is inversely proportional to temperature (T).
- Analogy: Giving \$1,000 to someone with little money has a greater impact than giving it to a billionaire.
- ΔSsurroundings∝T1
Combining Proportions
- Combining the relationships:
ΔS<em>surroundings=−TΔH</em>system
- Substituting ΔS<em>surroundings into the equation for ΔS</em>universe
\Delta S{universe} = \Delta S{system} - \frac{\Delta H_{system}}{T} > 0 - This equation involves measurements only on the system.
Gibbs Free Energy
- Multiplying the previous equation by -T (and reversing the inequality):
-T\Delta S{universe} = -T\Delta S{system} + \Delta H_{system} < 0 - Defining Gibbs Free Energy (G):
G=H−TS - At constant temperature:
ΔG=ΔH−TΔS
Gibbs Free Energy and Spontaneity
- \Delta G < 0 : Spontaneous change.
- The lowering of free energy ($\Delta G$) is the true driving force for processes in the universe.
- Free energy accounts for both enthalpic and entropic contributions.
- ΔG represents the maximum work obtainable from a process.
- Delta G = -T * Delta S universe
Delta G and Equilibrium
- \Delta G < 0 : Spontaneous forward reaction.
- \Delta G > 0 : Non-spontaneous forward reaction (spontaneous reverse reaction).
- ΔG=0: Equilibrium.
Standard Free Energy of Reaction
- Standard free energy change for a reaction:
ΔG∘=∑nΔG<em>f∘(products)−∑mΔG</em>f∘(reactants)
- n and m are the stoichiometric coefficients.
- Standard conditions: gases at 1 atm, solutions at 1 M, pure solids and liquids, and a standard temperature of 25°C.
- The free energy of formation ($\Delta G_f^\circ$) of an element in its standard state is zero.
- For compounds, ΔGf∘ is the free energy change when one mole of the compound is synthesized from its elements in their standard states.
Interpreting the Magnitude of Delta G
- If |\Delta G| < 10 \text{ kJ} , significant amounts of both reactants and products are present at equilibrium.
- Large negative ΔG: Essentially a one-way, spontaneous forward reaction.
- Large positive ΔG: Essentially no forward reaction (non-spontaneous).
- This will be related to the equilibrium constant K in the next class.
Temperature Dependence of Spontaneity
- ΔG=ΔH−TΔS
Favorable vs. Unfavorable Conditions:
- Enthalpy: Exothermic ($\Delta H < 0$) is favorable; endothermic ($\Delta H > 0$) is unfavorable.
- Entropy: Increase in entropy ($\Delta S > 0$) is favorable; decrease ($\Delta S < 0$) is unfavorable.
Qualitative Analysis:
- if the signs of delta H and delta S are opposite we don't need to calculate anything to figure out delta G
- If \Delta H > 0 and \Delta S < 0 , ΔG is always positive (non-spontaneous at all temperatures).
- If ΔH<0 and ΔS>0, ΔG is always negative (spontaneous at all temperatures).
- If ΔH and ΔS have the same sign:
- \Delta H > 0 (unfavorable) and \Delta S > 0 (favorable): High temperatures favor spontaneity.
- \Delta H < 0 (favorable) and \Delta S < 0 (unfavorable): Low temperatures favor spontaneity.
- In freshman chemistry there are assumption that delta H and delta S are constant over a temp range
- Partial differential equations are used in P-Chem
- The calculation of the temperature required for spontaneity it's a good estimate, but it not an exact calculation
Entropy Changes During Physical Changes
- Entropy increases with temperature for solids, liquids, and gases.
- Phase transitions (melting, boiling) involve significant increases in entropy.
- At the melting point, the temperature remains constant while the solid melts to become a liquid
- Gases > liquids > solids in terms of entropy due to increased molecular motion.
Calculating Entropy Changes During Phase Transitions
- Phase transitions occur at equilibrium, where ΔG=0.
- Therefore, ΔG=ΔH−TΔS=0
- ΔS<em>phasechange=TΔH</em>phasechange
Example Calculation
- For the fusion of water at 0°C:
- ΔHfusion=6.02 kJ/mol
- \Delta S_{fusion} = \frac{6.02 \times 10^3 \text{ J/mol}}{273 \text{ K}} = 22.1 \text{ J/(K \cdot mol)}
- As expected, the entropy increases as ice melts to form liquid water.