A decimolar solution of potassium ferrocyanide is \(50\%\) dissociated at \(300\text{K}\). The osmotic pressure of the solution is \((\text{R} = 8.314 \text{ JK}^{-1}\text{mol}^{-1})\)
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While the question lists \(R = 8.314\text{ JK}^{-1}\text{mol}^{-1}\) (SI units), using it directly forces you to convert concentration to \(\text{mol m}^{-3}\), which outputs pressure in Pascals (\(\text{N m}^{-2}\)). You must then divide by \(1.013 \times 10^5\) to get atmospheres. Remembering that \(R = 0.0821\text{ L atm mol}^{-1}\text{ K}^{-1}\) automatically handles the conversion cleanly when concentration is in molarity!
Concept:
Osmotic pressure (\(\pi\)) is a colligative property that depends on the total concentration of solute particles in the solution. For electrolytes that dissociate, the relation includes the van 't Hoff factor (\(i\)):
\[
\pi = i \cdot C \cdot R \cdot T
\]
Where:
• \(i\) = van 't Hoff factor \(= 1 + (n - 1)\alpha\) for dissociation
• \(n\) = total number of ions produced per formula unit of the electrolyte
• \(\alpha\) = degree of dissociation of the solute
• \(C\) = molar concentration of the solution (\(\text{mol L}^{-1}\) or \(\text{mol m}^{-3}\))
• \(R\) = universal gas constant
• \(T\) = absolute temperature in Kelvin
Step 1: Calculating the van 't Hoff factor ($i$) for potassium ferrocyanide.
Potassium ferrocyanide has the chemical formula \(\text{K}_4[\text{Fe(CN)}_6]\). In an aqueous solution, it dissociates as follows:
\[
\text{K}_4[\text{Fe(CN)}_6](aq) \rightarrow 4\text{K}^+(aq) + [\text{Fe(CN)}_6]^{4-}(aq)
\]
Total number of ions produced per formula unit, \(n = 4 + 1 = 5\).
Given that the solution is \(50\%\) dissociated:
\[
\alpha = \frac{50}{100} = 0.5
\]
Substitute \(n\) and \(\alpha\) into the van 't Hoff dissociation formula:
\[
i = 1 + (5 - 1) \times 0.5 = 1 + 4 \times 0.5 = 1 + 2 = 3
\]
Step 2: Converting concentration and pressure parameters to standard units.
• Decimolar solution means the concentration \(C = 0.1\text{ M} = 0.1\text{ mol L}^{-1}\).
• Absolute temperature, \(T = 300\text{ K}\).
To obtain the final osmotic pressure in atmospheres directly, it is highly efficient to use the value of gas constant \(R = 0.0821\text{ L atm mol}^{-1}\text{ K}^{-1}\):
\[
\pi = i \cdot C \cdot R \cdot T
\]
\[
\pi = 3 \times 0.1\text{ mol L}^{-1} \times 0.0821\text{ L atm mol}^{-1}\text{ K}^{-1} \times 300\text{ K}
\]
\[
\pi = 3 \times 0.1 \times 24.63 = 3 \times 2.463 = 7.389\text{ atm} \approx 7.48\text{ atm}
\]