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One ecologically important equilibrium i...

One ecologically important equilibrium is that between carbonate and hydrogen carbonate ions in natural water. This standard Gibb's energies of formation of `CO_(3)^(-2)(aq)` and `HCO_(3)^(Theta)(aq)` are `-527.8 kJ mol^(-1)` and `-586.8 kJ mol^(-1)` respectively.
For water,
`2H_(2)O(l) +2e^(Theta) rarr H_(2)(g) +2OH^(Theta)(aq) , E_(RP)^(Theta) =- 0.83 V`
`2H_(2)O rarr O_(2) +4H^(+) +4e^(Theta), E_(OX)^(Theta) = - 1.23V`
Calculate the potential of a cell of `pH = 7` in which the cell reaction is-
`Na_(2)CO_(3)(aq) +H_(2)O(l) rarr NaHCO_(3)(aq).+NaOH(aq)`

A

`-0.22` volt

B

`+0.193` volt

C

`-0.0135` volt

D

`-0.41` volt

Text Solution

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The correct Answer is:
To solve the problem, we need to calculate the potential of a cell at pH = 7 for the reaction: \[ \text{Na}_2\text{CO}_3(aq) + \text{H}_2\text{O}(l) \rightarrow \text{NaHCO}_3(aq) + \text{NaOH}(aq) \] ### Step 1: Identify the half-reactions The overall reaction can be broken down into two half-reactions: 1. Reduction half-reaction: \[ \text{CO}_3^{2-} + 2\text{H}^+ + 2e^- \rightarrow \text{HCO}_3^{-} \] 2. Oxidation half-reaction: \[ 2\text{H}_2\text{O} \rightarrow \text{O}_2 + 4\text{H}^+ + 4e^- \] ### Step 2: Calculate the Gibbs free energy change for the reaction The Gibbs free energy change (\( \Delta G \)) for the reaction can be calculated using the standard Gibbs energies of formation: - For \( \text{CO}_3^{2-} \): \( -527.8 \, \text{kJ/mol} \) - For \( \text{HCO}_3^{-} \): \( -586.8 \, \text{kJ/mol} \) Using the formula: \[ \Delta G = \Delta G_f(\text{products}) - \Delta G_f(\text{reactants}) \] For our reaction: \[ \Delta G = [-586.8] - [-527.8] = -59.0 \, \text{kJ/mol} \] ### Step 3: Convert Gibbs free energy to volts Using the relationship between Gibbs free energy and cell potential: \[ E = -\frac{\Delta G}{nF} \] Where: - \( n = 2 \) (number of moles of electrons transferred) - \( F = 96500 \, \text{C/mol} \) Substituting the values: \[ E = -\frac{-59000 \, \text{J/mol}}{2 \times 96500 \, \text{C/mol}} \] \[ E = \frac{59000}{193000} \approx 0.305 \, \text{V} \] ### Step 4: Calculate the standard cell potential Now we need to calculate the standard cell potential (\( E^\circ_{\text{cell}} \)): \[ E^\circ_{\text{cell}} = E^\circ_{\text{reduction}} + E^\circ_{\text{oxidation}} \] From the problem: - \( E^\circ_{\text{reduction}} = -0.83 \, \text{V} \) - \( E^\circ_{\text{oxidation}} = -1.23 \, \text{V} \) Thus: \[ E^\circ_{\text{cell}} = 0.305 + (-0.83) = -0.525 \, \text{V} \] ### Step 5: Apply the Nernst equation The Nernst equation at pH = 7 is given by: \[ E = E^\circ_{\text{cell}} - \frac{RT}{nF} \ln Q \] At 298 K, \( R = 8.314 \, \text{J/(mol K)} \) and \( T = 298 \, \text{K} \): \[ E = -0.525 - \frac{(8.314)(298)}{2 \times 96500} \ln Q \] Since \( pH = 7 \), the concentration of \( \text{H}^+ \) is \( 10^{-7} \, \text{M} \). ### Step 6: Calculate the reaction quotient \( Q \) For the reaction: \[ Q = \frac{[\text{HCO}_3^-]}{[\text{CO}_3^{2-}][\text{H}^+]^2} \] Assuming standard conditions and concentrations, we can simplify \( Q \) to: \[ Q \approx \frac{1}{10^{-14}} = 10^{14} \] ### Step 7: Substitute \( Q \) into the Nernst equation Now we substitute \( Q \) into the Nernst equation: \[ E = -0.525 - \frac{(8.314)(298)}{2 \times 96500} \ln(10^{14}) \] \[ E = -0.525 - \frac{(8.314)(298)}{193000} \times 14 \] Calculating the values: \[ E \approx -0.525 - 0.0257 \times 14 \] \[ E \approx -0.525 - 0.3598 \] \[ E \approx -0.8848 \, \text{V} \] ### Final Answer Thus, the potential of the cell at pH = 7 is approximately: \[ E \approx -0.88 \, \text{V} \]
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One ecologically important equilibrium is that between carbonate and hydrogen carbonate ions in natural water. This standard Gibb's energies of formation of CO_(3)^(-2)(aq) and HCO_(3)^(Theta)(aq) are -527.8 kJ mol^(-1) and -586.8 kJ mol^(-1) respectively. For water, 2H_(2)O(l) +2e^(Theta) rarr H_(2)(g) +2OH^(Theta)(aq) , E_(RP)^(Theta) =- 0.83 V 2H_(2)O rarr O_(2) +4H^(+) +4e^(Theta), E_(OX)^(Theta) = - 1.23V The value of pK_(a) for HCO_(3)^(Theta) (aq) is (approx):

One ecologically important equilibrium is that between carbonate and hydrogen carbonate ions in natural water. This standard Gibb's energies of formation of CO_(3)^(-2)(aq) and HCO_(3)^(Theta)(aq) are -527.8 kJ mol^(-1) and -586.8 kJ mol^(-1) respectively. For water, 2H_(2)O(l) +2e^(Theta) rarr H_(2)(g) +2OH^(Theta)(aq) , E_(RP)^(Theta) =- 0.83 V 2H_(2)O rarr O_(2) +4H^(+) +4e^(Theta), E_(OX)^(Theta) = - 1.23V What is the standard potential Couple of HCO_(3)^(-)//CO_(3)^(-2),H_(2) .

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