Abstract

Volatile organic compounds (VOCs) must initially be absorbed by sweat on the surface of skin for human VOC dermal exposure . The partitioning equilibrium at the air–sweat interface is given by p c = C g * / C L , where p c is the partitioning coefficient, and C g * is the gaseous concentration in equilibrium with the aqueous VOC concentration ( C L ) at a constant water temperature ( T w ). A series of thermodynamic functions of C g * ( C L , T W ) are presented, as well as the values of p c , and the heat of gaseous–liquid phase transfer (Δ H tr ) for tested VOCs, including iso-propanol (IPA, C L =12–120 mg L −1 ) and methyl ethyl ketone (MEK, C L =10–80 mg L −1 ) to determine the effects of liquid VOC concentration and salt contents of sweat on p c of hydrophilic VOCs. Experimental data reveal that the p c values of IPA and MEK drop as the liquid VOC concentrations increasing from 10 to 120 mg L −1 . However, sodium salt content in human sweat (sodium chloride and sodium lactate) induces the effect of salt, indicating the increase in p c . Notably, neither urea nor ammonia in human sweat increase p c . Artificial sweat, consisting of sodium chloride 0.47%, urea 0.05%, ammonia 0.004% and sodium lactate 0.6%, was used to evaluate the increase in the p c values of IPA and MEK. The liquid VOC concentration effect simultaneously develops together with the salt effect on the partition at the interface of air–sweat for hydrophilic VOC solutions. The p c values of IPA for artificial sweat decrease as much as 32.5% as C L increases from 12 to 120 mg L −1 at 300 K, and those of MEK drop by as much as 70.9% as C L increases from 10 to 80 mg L −1 at 300 K. This investigation provides a basis for elucidating the assessment of human dermal exposure to hydrophilic VOCs.

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