tadeoori
Bioengineer
- Feb 9, 2012
- 7
Hi Guys,
I have a problem that I'm a bit stumped with...
I have a polymer surrounding an analyte that I wish to keep dry. Think of an M&M, where the chocolate is the analyte and the candy coating is the polymer. The unit will be submersed in salt water. I'm trying to model the rate of moisture uptake by the analyte. For example, let's assume the analyte is of a rather high molecular weight, like 100 kDa.
I'm a bit confused as to how to approach the problem. Let me explain what I've done, and perhaps my conundrum will become clear.
I have the WVTR for the polymer coating (typical g*mil/100 in^2/24 hr/atm type measurement). I can calculate the rate of water vapor transfer via WVTR*area*(p2-p1)/thickness, where p2 is the vapor pressure of water on the outside and p1 is the vapor pressure of water on the inside. But can I do the calculation when I'm submersed in water? Is being submersed the same as being in 100 % RH?
In a very short time, once a little bit of water reaches the analyte, the vapor pressure of the water (calculated via Raoult's law, i.e. via molar fraction) approaches 100 % RH, and this suggests that the rate of water vapor transfer would decrease substantially. However, if I calculate osmotic pressure, there is a high osmotic pressure in the analyte that will want to draw in more water. Experimentally, I find that the analyte draws in a lot of water and liquid water forms, and this happens at a rate much higher than I calculate using the equation above.
I'm I approaching this the right way? I'm trying to reconcile the WVTR calculation using partial pressures and the steady state result predicted by osmotic pressures. Osmotic pressure calculations don't give me a rate of transfer, and I'm concerned that the rate calculations don't take into account the osmotic pressure.
Perhaps Raoult's law isn't the right way to calculate the vapor pressure of the water, considering I'm staring with dry analyte? Since the mole fraction of water increases very rapidly (18 g/mol for water, versus 100,000 g/mol for the analyte), the model predicts a very small percentage of water uptake over a long period of time, however, experiments suggest the analyte draws in a lot of water and the uptake is much more rapid than my model predicts.
Perhaps I need to stick to diffusion calculations using chemical potentials of water, or something like that?
Any help or suggestions on how to reconcile these various ideas would be greatly appreciated!
Thank you,
Tadeo
I have a problem that I'm a bit stumped with...
I have a polymer surrounding an analyte that I wish to keep dry. Think of an M&M, where the chocolate is the analyte and the candy coating is the polymer. The unit will be submersed in salt water. I'm trying to model the rate of moisture uptake by the analyte. For example, let's assume the analyte is of a rather high molecular weight, like 100 kDa.
I'm a bit confused as to how to approach the problem. Let me explain what I've done, and perhaps my conundrum will become clear.
I have the WVTR for the polymer coating (typical g*mil/100 in^2/24 hr/atm type measurement). I can calculate the rate of water vapor transfer via WVTR*area*(p2-p1)/thickness, where p2 is the vapor pressure of water on the outside and p1 is the vapor pressure of water on the inside. But can I do the calculation when I'm submersed in water? Is being submersed the same as being in 100 % RH?
In a very short time, once a little bit of water reaches the analyte, the vapor pressure of the water (calculated via Raoult's law, i.e. via molar fraction) approaches 100 % RH, and this suggests that the rate of water vapor transfer would decrease substantially. However, if I calculate osmotic pressure, there is a high osmotic pressure in the analyte that will want to draw in more water. Experimentally, I find that the analyte draws in a lot of water and liquid water forms, and this happens at a rate much higher than I calculate using the equation above.
I'm I approaching this the right way? I'm trying to reconcile the WVTR calculation using partial pressures and the steady state result predicted by osmotic pressures. Osmotic pressure calculations don't give me a rate of transfer, and I'm concerned that the rate calculations don't take into account the osmotic pressure.
Perhaps Raoult's law isn't the right way to calculate the vapor pressure of the water, considering I'm staring with dry analyte? Since the mole fraction of water increases very rapidly (18 g/mol for water, versus 100,000 g/mol for the analyte), the model predicts a very small percentage of water uptake over a long period of time, however, experiments suggest the analyte draws in a lot of water and the uptake is much more rapid than my model predicts.
Perhaps I need to stick to diffusion calculations using chemical potentials of water, or something like that?
Any help or suggestions on how to reconcile these various ideas would be greatly appreciated!
Thank you,
Tadeo