Mass Transfer
Diffusivity in concentrated solutions differs from that in dilute solutions, because of the changes in

Both A & B
Neither A nor B
Viscosity with concentration
Degree of ideality of the solution

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Mass Transfer
At equilibrium the concentration of water in vapour phase (C*)in kg/m³ of air space and the amount of water (m) adsorbed per kg of dry silica gel are related by, C* = 0.0667m. To maintain dry conditions in a room of air space 100m³ containing 2.2 kg of water vapour initially, 10 kg of dry silica gel is kept in the room. The fraction of initial water remaining in the air space after a long time (during which the temperature is maintained constant) is

0.4
1
0.2

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