Example 2.15 in 3rd edition Example 2.14 Consider the situation shown in Figure 2.5 where on side A of the membrane we.
Download ReportTranscript Example 2.15 in 3rd edition Example 2.14 Consider the situation shown in Figure 2.5 where on side A of the membrane we.
Example 2.15 in 3rd edition Example 2.14 Consider the situation shown in Figure 2.5 where on side A of the membrane we have a solution that has a water mole fraction of 0.99. On side B of the membrane we have pure water. If the temperature is 25 oC and side B is at 1 atmosphere pressure, estimate the pressure needed on side A to stop the osmosis of water from region A. What would happen if the pressure on side A was increased to a value above this pressure? SOLUTION Assuming the solution in region A is an ideal solution we can use Equation 2.147 to calculate the osmotic pressure of region A, ie. 1atm Pa m 3 8.314 x 298K gmol K 101,325Pa PA PB x 0.01 13.6 atm 3 -6 m 18 x 10 gmol Therefore the pressure in region A would have to be 14.6 atm to prevent the osmosis of water from region B into region A. If the pressure in region A is greater than 14.6 atm, then water will move from region A into region B and this process is called reverse osmosis. Since small pressures are easy to measure, the osmotic pressure is also useful for determining the molecular weight of macromolecules. For example, letting msolute represent the mass concentration (g/liter) of the solute in the solution, then from Equation 2.147 we can write the molecular weight of the solute (MWsolute) in terms of the osmotic pressure of the solution as follows MWsolute RT m solute (2.149) Example 2.16 in 3rd edition Example 2.15 The osmotic pressure of a solution containing a macromolecule is equivalent to the pressure exerted by 8 cm of water. The mass concentration of the protein in the solution is 15 g/liter. Estimate the molecular weight of this macromolecule. SOLUTION We can use Equation 2.149 to estimate the molecular weight as follows. 100cm 1atm m 3 Pa 15g 1liter 8.314 x 298K x x x 3 molK liter 1000cm 101,325Pa m3 1in 1ft 1atm 8 cm H 2 O x x x 2.54cm 12in 33.91ft H 2 O 3 MWsolute MWsolute = 47400 g/mol Example 3.1 Calculate the filtration flowrate (cm3/sec) of a pure fluid across a 100 cm2 membrane. Assume the viscosity () of the fluid is 1.8 cP. The porosity of the membrane is 40% and the thickness of the membrane is 500 microns. The pores run straight through the membrane and these pores have a radius of 0.225 microns. The pressure drop applied across the membrane is 75 psi. ( Recall that 14.7 psi = 1 atm = 101325 Pa (or N m-2) , that 1 N = 1 kg m sec-2, and from Chapter 4 we have for the viscosity that 1 cP = 0.001 N sec m-2 = 0.001 Pa sec). SOLUTION To find the filtration flowrate we will use Equations 3.4 and 3.7. Since there are no retained solutes there are no osmotic effects and the effective pressure drop across the membrane is equal to the applied pressure drop of 75 psi. From the information about the membrane we first calculate the value of the hydraulic conductance as shown below. Ap S 0.4 , R 0.225 m icrons 2.25 105 cm , t m 500 m icrons 0.05 cm , 1.8 cP 0.0018 Pa sec , and P 75 psi 1 atm 101325Pa 5.17 105 Pa 14.7 psi 1 atm now substituting these values in Equation 3.7 : 2 0.40 2.25 105 cm cm LP 2.813 107 8 0.0018 Pa sec 0.05cm Pa sec and from Equation3.4 Q 2.813 107 Q 14.54 cm3 sec cm 100cm 2 5.17 105 Pa Pa sec Example 3.2 in 3rd edition