Equilibrium partitioning of organic compounds

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     Sorption isotherm
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Sorption isotherm

Imagine the following experiment. You have a closed bottle with 1 L of water and 50 g soil immersed in the water (no air present). You add a tiny amount of chemical i , shake the bottle until partition equilibrium is attained. You then measure the equilibrium concentrations of i in both phases water and soil.

Then you re-add chemical i and, in the following, repeat the steps above. You repeat this 10 more times adding more and more of chemical i . Then you plot the measured data as the concentration in phase 2 (soil) vs. the concentration in phase 1 (water). This plot is referred to as a sorption isotherm:

What will the plotted curve look like? How is the partition constant of i between water and soil related to this curve? What is the maximum concentration that you can reach experimentally? How would the graph look like if i was a volatile compound and the bottle also contained 1 L of air while the experiment was carried out exactly like before?

Help: See Equilibrium partitioning in quantitative terms

 

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