The Effect of Solute Concentration on the Rate of Osmosis

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The Effect of Solute Concentration on the Rate of Osmosis

Aim:

To test and observe how the concentration gradient between a potato

and water & sugar solution will affect the rate of osmosis.

Introduction:

Osmosis is defined as, diffusion, or net movement, of free water

molecules from high to low concentration through a semi-permeable

membrane.

When a substance, such as sugar (which we will be using in the

experiment we are about to analyse), dissolves in water, it attracts

free water molecules to itself, and in doing so, stops them from

moving freely.

The effect of this, is that the concentration of (free) water

molecules in that environment goes down. There are less free water

molecules, and therefore less water molecules to pass across a

semi-permeable membrane, through which sugar molecules and other

molecules attached to them are too big to diffuse across with ease.

In the diagram below on the right, we see two solutions divided by a

partially/selectively permeable membrane (i.e. one that is porous, but

allows water molecules through faster than dissolved substances).

Text Box: Originally, the two solutions were; pure water, on the left,

and sugar solution with a high sugar concentration, on the right. The

pure water solution is said to have higher water potential than the

concentrated sugar solution, because the water will flow from the area

of high concentration of free water molecules (the dilute solution),

to the area of low concentration of free water molecules (the

concentrated solution). In other words, to the sugar solution.

However, in this diagram we see that osmosis has been taking place for

a short while, because water molecules have started to diffuse to the

right, across the membrane, so that there are now many present on the

right side of the membrane, and a few sugar molecules are starting to

diffuse across the membrane in the opposite direction, to the left

side of the membrane as we see it.

Through moving from an area of lots of free water molecules, to an

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