12.2 - Total Entropy
- 1Calculating entropy changes for reactions
- 2Calculating total entropy change
- 3Thermodynamic and kinetic stability
- 4The role of temperature in entropy changes
- 5The freezing of water as an example of entropy changes
Calculating entropy changes for reactions
During a reaction, the entropy change of the system (ΔSsystem) can be calculated using the formula:
ΔSsystem = Sproducts Sreactants
Where:
- Sproducts is the sum of the standard entropies of all products.
- Sreactants is the sum of the standard entropies of all reactants.
Standard entropy (S⦵) is the entropy of 1 mole of a substance under standard conditions (100 kPa pressure and 298 K temperature). Its units are J K-1 mol-1.
The steps for calculating ΔSsystem are:
- Find the sum of standard entropies for the products (ΣS⦵(products)).
- Find the sum of standard entropies for the reactants (ΣS⦵(reactants)).
- Subtract the sum of reactant entropies from the sum of product entropies.
If the balanced equation has coefficients other than 1, multiply the standard entropy of each substance by its coefficient.
Worked example 1 - Calculating entropy change for a reaction
Calculate the entropy change for the reaction where hydrogen chloride reacts with ammonia to produce ammonium chloride at standard conditions:
HCl(g) + NH3(g) ➔ NH4Cl(s)
Given:
- S⦵[HCl(g)] = 186.9 J K-1 mol-1
- S⦵[NH3(g)] = 192.8 J K-1 mol-1
- S⦵[NH4Cl(s)] = 94.6 J K-1 mol-1
Step 1: Calculate the entropy of the products
Sproducts = S⦵[NH4Cl] = 94.6 J K-1 mol-1
Step 2: Calculate the entropy of the reactants
Sreactants = S⦵[HCl] + S⦵[NH3]
= 186.9 + 192.8 = 379.7 J K-1 mol-1
Step 3: Equation
ΔSsystem = Sproducts Sreactants
Step 4: Substitution and correct evaluation
ΔSsystem = 94.6 379.7 = 285.1 J K-1 mol-1
The negative ΔSsystem indicates a decrease in entropy, reflecting the increased order as two gases form a solid.
Total entropy change
To determine if a reaction is feasible, we need to consider the total entropy change of both the system and its surroundings:
ΔS⦵total = ΔS⦵system + ΔS⦵surroundings
The entropy change of the surroundings can be calculated using the following equation:
ΔS⦵surroundings =
Where:
- ΔH⦵ = standard enthalpy change of the reaction (J mol-1).
- T is the temperature (K).
ΔS_total_ will be positive, indicating a spontaneous process, when:
- Both ΔS_system_ and ΔS_surroundings_ are positive.
- ΔS_surroundings_ is positive and larger in magnitude than a negative ΔS_system_.
- ΔS_system_ is positive and larger in magnitude than a negative ΔS_surroundings_.
Worked example 2 - Calculating total entropy change
Calculate the total entropy change, in J K-1 mol-1, for the reaction of ammonia with hydrogen chloride:
NH3(g) + HCl(g) ➔ NH4Cl(s)
Given:
- ΔH⦵ = 315 kJ mol-1 (at 298 K)
- ΔS⦵system = 285.1 J K-1 mol-1 (calculated in worked example 1)
Step 1: Conversion of kJ mol-1 into J mol-1
To convert from kJ mol-1 into J mol-1, multiply by 1,000
315 kJ mol-1 = 315,000 J mol-1
Step 2: Calculate ΔS⦵surroundings
ΔS⦵surroundings = = +1,057 J K-1 mol-1
Step 3: Calculate ΔS⦵total
ΔS⦵total = ΔS⦵system + ΔS⦵surroundings = 285.1 + 1,057 = +772 J K-1 mol-1
The positive total entropy change suggests that this reaction is likely to be feasible under standard conditions.
Worked example 3 - Calculating total entropy change
Calculate the total entropy change, in J K-1 mol-1, for the dissolution of ammonium nitrate crystals in water under standard conditions:
NH_4_NO_3(s)_ ➔ NH_4_^+^(aq)** + NO_3_^-^(aq)**
Given:
- ΔH = +25.70 kJ mol^-1^ (at 298 K)
- S⦵[NH_4_NO_3_] = 151.1 J K^-1^ mol^-1^
- S⦵[NH_4_^+^(aq)] = 113.4 J K^-1^ mol^-1^
- S⦵[NO_3_^-^(aq)] = 146.4 J K^-1^ mol^-1^
Step 1: Conversion of kJ mol-1 into J mol-1
To convert from kJ mol^-1^ into J mol^-1^, multiply by 1,000
25.70 kJ mol-1 = 25,700 J mol-1
Step 2: Calculate ΔS⦵surroundings
ΔS⦵surroundings = 86.24 J K-1 mol-1
Step 3: Calculate ΔS⦵system
ΔS⦵system = ΔS⦵products ΔS⦵reactants = 113.4 + 146.4 151.1 = +108.7 J K-1 mol-1
Step 4: Calculate ΔS⦵total
ΔS⦵total = ΔS⦵system + ΔS⦵surroundings = 108.7 86.24 = +22.5 J K-1 mol-1
Worked example 4 - Calculating total entropy change
Calculate the total entropy change, in J K-1 mol-1, for the reaction between barium hydroxide and ammonium chloride:
Ba(OH)2**•8H_2_O_(s)_ + 2NH_4_Cl_(s)_ ➔ BaCl_2(s)_ + 10H_2_O_(l)_ + 2NH_3(g)_
Given:
- ΔH = +164.0 kJ mol^-1^ (at 298 K)
- S⦵[Ba(OH)2**•8H_2_O] = 427.0 J K^-1^ mol^-1^
- S⦵[NH_4_Cl] = 94.6 J K^-1^ mol^-1^
- S⦵[BaCl_2_] = 123.7 J K^-1^ mol^-1^
- S⦵[H_2_O] = 69.9 J K^-1^ mol^-1^
- S⦵[NH_3_] = 192.3 J K^-1^ mol^-1^
Step 1: Conversion of kJ mol-1 into J mol-1
To convert from kJ mol^-1^ into J mol^-1^, multiply by 1,000
164.0 kJ mol-1 = 164,000 J mol-1
Step 2: Calculate ΔS⦵surroundings
ΔS⦵surroundings = 550.3 J K-1 mol-1
Step 3: Calculate ΔS⦵system
ΔS⦵system = ΔS⦵products ΔS⦵reactants **
ΔS⦵system *= (*123.7 + (10 x 69.9) + (2 x 192.3)) (427.0 + (2 x 94.6) = +591.1 J K-1 mol-1
Step 4: Calculate ΔS⦵total
ΔS⦵total = ΔS⦵system + ΔS⦵surroundings = 591.1 550.3 = +40.8 J K-1 mol-1
The positive ΔS_total_ indicates that the reaction is spontaneous, despite being endothermic. This spontaneity is driven by the significant increase in entropy of the system, which arises from the formation of liquid water and gaseous ammonia as products.
Thermodynamic vs. kinetic stability
While total entropy determines if a reaction is thermodynamically feasible, it doesn't guarantee that the reaction will occur immediately. This is where the concept of kinetic stability becomes important.
Consider the combustion of methane:
CH4(g) + 2O2(g) ➔ CO2(g) + 2H2O(l)
At 298 K:
ΔH⦵ = 890.3 kJ mol−1
ΔStotal = +2.95 kJ mol−1
Despite having a positive ΔStotal, the combustion of methane doesn't occur spontaneously at 298 K because:
- It requires an ignition source to overcome its high activation energy.
- This makes the methane-oxygen mixture kinetically stable, even though it's thermodynamically unstable.
The impact of temperature on entropy
Temperature plays a significant role in determining changes in entropy.
When heat is added to a system:
- At lower temperatures, the increase in entropy is more substantial because molecules gain greater freedom of movement.
- At higher temperatures, the same amount of heat results in a smaller increase in entropy, as the molecules are already moving vigorously.
This dependence on temperature is crucial for understanding various natural phenomena, especially phase changes. For example, the concepts of entropy can explain why water freezes spontaneously at temperatures below its melting point.
Entropy changes during water freezing
Consider the process: H2O(l) ➔ H2O(s).
The following values are known:
- ΔH⦵ = 6.01 kJ mol-1
- S⦵(H2O(l)) = 69.9 J K-1 mol-1
- S⦵ (H2O(s)) = 47.9 J K-1 mol-1
For water to freeze spontaneously, the magnitude of ΔSsurroundings must be greater than the magnitude of ΔSsystem, resulting in a positive ΔStotal.
| Temperature (°C) | ΔS_system_ (J K^-1^ mol^-1^) | ΔS_surroundings_ (J K^-1^ mol^-1^) | ΔS_total_ (J K^-1^ mol^-1^) | Spontaneity of freezing |
|---|---|---|---|---|
| +5°C | −22.0 | +21.6 | -0.4 | Not spontaneous |
| -5°C | −22.0 | +22.4 | +0.4 | Spontaneous |
Key observations:
- ΔS_system_ remains constant because it depends on the inherent properties of water and ice.
- ΔS_surroundings_ increases at lower temperatures, as the same amount of heat released causes a larger entropy change in colder surroundings.
- At 5°C, the increase in ΔS_surroundings_ is sufficient to make ΔS_total_ positive, allowing freezing to occur spontaneously.
This example shows why we use freezers to make ice. The lower temperature increases ΔS_surroundings_, which compensates for the decrease in entropy that occurs when water freezes, making the process thermodynamically spontaneous.