Introduction
In the field of Environmental Chemistry is of interest to know the behavior of the pollutants in wa-ter since the transport and most of the degradation processes take place in water phase. The studied system is complex; therefore the solubility of each component should necessarily be affected by the presence of the other ones. The composition of each crude oil is unique and the oil in the environment is under very variable conditions, therefore a strong historical component exists in its current composi-tion. This makes the testing in field samples to be of fundamental interest [
1,
2,
3] since it is impossible to reproduce similar conditions in the laboratory. The oil residuals are hydrophobic but their solubility can be increased by means of the use of an organic cosolvent, as the alcohols.
This study intent to investigate on one hand, if the variations observed in the solubility and K (dis-tribution coefficient) of the oil residuals, in the presence of different cosolvent fractions can be inter-preted by the solvophobic theory and if, based on it, the solubility in water and the K’s in complex mixtures can be estimated.
Experimental
Samples of polluted soils, were product of oil spills in different times at six locations in the sur-roundings of Comodoro Rivadavia city. For the measurement of the solubility in water experiences were carried out by means of the use of water and mixtures of water and organic cosolvent (methanol).
The following relationships were used for the interpretation of the measured data [
1,
4]: log S
m = log S
w + σ f
c (
1), where S
m is the solute solubility in the water- cosolvent mixture, S
w is the solubility in water, σ is 'the potential as cosolvent' and f
c is the volume fraction of the cosolvent. According to the solvophobic theory: ln (K
m/K
w) = - a α σ f
c (
2), where K
m is the partition coefficient in water (Lkg
-1); K
w is the partition coefficient in the mixture of solvents (Lkg
-1); a is the empirical constant accounting for water-cosolvent interactions, α is the empirical constant accounting for solvent-sorbent interac-tions; and σ is the cosolvency power of a given solvent and solute accounting for solvent-solute inter-actions.
Results and Discussion
For the oldest polluted samples the solubility in water calculated according to (1) are higher in all the cases to that experimentally measured. The differences increase with decreasing σ, indicating that probably the progressive loss of the potentiality of the cosolvent to solubilize has effect on the ob-served differences. The values of K’s vary among 900 (Lkg-1) and 2,900 (Lkg-1) showing a general and marked increase when increasing age.
This information was related with the possibility of transport and it would contribute to the estimate of the mobility of oil residuals and the possibility of oil degradation.