Chapter 13: Problem 119
A mixture of \(\mathrm{NaCl}\) and sucrose \(\left(\mathrm{C}_{12} \mathrm{H}_{22} \mathrm{O}_{12}\right)\) of combined mass \(10.2 \mathrm{~g}\) is dissolved in enough water to make up a 250 -mL solution. The osmotic pressure of the solution is 7.32 atm at \(23^{\circ} \mathrm{C}\). Calculate the mass percent of \(\mathrm{NaCl}\) in the mixture.
Short Answer
Step by step solution
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Van't Hoff Factor
For non-ionic compounds like sucrose, the Van't Hoff factor is typically 1, because sucrose stays intact and does not dissociate into multiple particles. This implies that each molecule of sucrose contributes a single particle to the solution's effect. Conversely, for ionic compounds like \( \text{NaCl} \), \( i = 2 \). Upon dissolving, \( \text{NaCl} \) dissociates into two ions: \( \text{Na}^+ \) and \( \text{Cl}^- \).
To calculate osmotic pressure, \( i \) is multiplied by the molarity \( M \), the ideal gas constant \( R \), and the temperature in Kelvin \( T \). Therefore, understanding and calculating the Van't Hoff Factor is necessary to predict the behavior of a solution, especially when dealing with mixtures of ionic and non-ionic substances.
Molarity Calculation
In the context of osmotic pressure, molarity is integrated into the equation \( \pi = iMRT \), where \( \pi \) is the osmotic pressure. Rearrange this equation to solve for molarity: \( M = \frac{\pi}{iRT} \). This way, you can identify how much solute is dissolved in the solution based on the observed osmotic pressure and the conditions given, like temperature.
When calculating molarity for a mixture, as in the case of \( \text{NaCl} \) and sucrose, you need the combined effect of all solutes. Each contributes to the total molarity based on their respective Van't Hoff factors and the amount present in the solution. This approach clarifies how a mixture's overall concentration impacts properties like the osmotic pressure.
Ideal Gas Constant
Constant \( R \) typically takes the value \( 0.0821 \text{ L atm/mol K} \) when calculations are done using the units of pressure in atmospheres and volume in liters. While derived from the ideal gas law \( PV = nRT \), its application extends to numerous other states of matter, including solutions.
By drawing a connection between the gas laws and colligative properties of solutions, the ideal gas constant helps in calculating how solute particles contribute to osmotic pressure in a solution. Given its universal application, understanding \( R \) is essential for assessing how changes in temperature or volume affect the concentration and pressure in any system.