📖 Explanation
Osmotic pressure manifests as the hydrostatic head resulting from solvent flow across a semi-permeable membrane, and its value is determined by the expression π=ρgh. Using the provided density ρ=1000kgm−3, acceleration due to gravity g=10ms−2, and a height h=0.08m, the pressure is calculated as 1000×10×0.08=800Pa, which is equivalent to 0.8kPa.
The relationship between osmotic pressure, solute concentration, and temperature is defined by the van 't Hoff equation π=CRT, which can be expanded as π=MVwRT where w is the mass of the solute, M is the molar mass, and V is the volume. Substituting 0.8kPa for π, 20g for w, 1L for V, 8.3kPadm3K−1mol−1 for R, and 300K for T, the equation becomes 0.8=M×120×8.3×300. Solving for M results in M=0.820×8.3×300, which equals 62250gmol−1 or 62.25kgmol−1. Rounded to the nearest integer, the molar mass is 62kgmol−1.