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The Water Flux Based on Solution Diffusion Model describes the movement of water molecules across a semi-permeable membrane due to differences in pressure and concentration gradients. This model is fundamental in understanding membrane separation processes like reverse osmosis.
The calculator uses the solution diffusion model formula:
Where:
Explanation: The equation quantifies water transport through membranes by considering diffusion, pressure differentials, and membrane properties.
Details: Accurate water flux calculation is essential for designing and optimizing membrane separation systems, predicting system performance, and determining energy requirements in processes like desalination and water purification.
Tips: Enter all required parameters with appropriate units. Ensure pressure values are in Pascals, temperature in Kelvin, and dimensions in consistent SI units. All values must be positive.
Q1: What is membrane water diffusivity?
A: Membrane water diffusivity (D_w) is a measure of how quickly water molecules can move through a membrane material, typically expressed in m²/s.
Q2: How does temperature affect water flux?
A: Higher temperatures generally increase water flux as molecular movement increases, though the relationship depends on specific membrane properties.
Q3: What is the significance of osmotic pressure in this model?
A: Osmotic pressure represents the natural tendency of water to move from lower to higher solute concentration, opposing the applied pressure in reverse osmosis processes.
Q4: What are typical values for membrane layer thickness?
A: Membrane thickness typically ranges from nanometers to micrometers, depending on the membrane type and application.
Q5: Can this model be applied to all membrane types?
A: The solution diffusion model is most applicable to dense, non-porous membranes. For porous membranes, other models may be more appropriate.