3. Fe and FeO are in equilibrium with gas mixture of composition 71.8%CO−28.2%CO2 at 1273K. Which of the two solid phases disappears if the composition of the gas is held constant and temperature of the system is increased?
Fe(s)+1/2O2(g)=FeO(s)ΔGo=−263700+64.35TC(s)+O2(g)=CO2(g)ΔG0=−394100−0.84TC(s)+1/2O2(g)=COΔG0=−111700−87.65T
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Answer from Sia
Posted 7 months ago
Solution
1
Determine the equilibrium constant for the reaction: The equilibrium constant K for the reaction Fe(s)+21O2(g)=FeO(s) can be calculated using the Gibbs free energy change ΔG∘ at standard conditions. The relationship between ΔG∘ and K is given by ΔG∘=−RTlnK, where R is the gas constant and T is the temperature in Kelvin
2
Calculate the change in Gibbs free energy with temperature: The change in Gibbs free energy ΔG for the reaction at temperature T can be calculated using the equation ΔG=ΔG∘+64.35T for the formation of FeO from Fe and O2
3
Analyze the effect of temperature on the equilibrium: As the temperature increases, the value of ΔG for the formation of FeO becomes less negative (since 64.35T is positive and increases with T). This implies that the reaction becomes less spontaneous at higher temperatures, and the equilibrium will shift to favor the reactants, Fe(s) and O2(g)
4
Determine which solid phase disappears: Since the equilibrium shifts to favor the reactants at higher temperatures, FeO(s) will tend to decompose back into Fe(s) and O2(g). Therefore, the solid phase FeO will disappear if the temperature is increased while the gas composition is held constant
Answer
The solid phase FeO will disappear upon increasing the temperature.
Key Concept
Le Chatelier's principle and the temperature dependence of Gibbs free energy
Explanation
According to Le Chatelier's principle, increasing the temperature of an exothermic reaction will shift the equilibrium to favor the reactants. The temperature dependence of Gibbs free energy for the formation of FeO indicates that the reaction becomes less favorable at higher temperatures, leading to the disappearance of FeO.
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