Dissolved organic carbon (DOC) was examined in 17 Finnish lakes, 6 Fin
nish streams, and 30 Maine (USA) lakes by fractionating DOC into hydro
phobic acids and neutrals, and hydrophilic acids, bases, and neutrals.
A procedure using XAD-8, anion-exchange, and cation-exchange resins w
as used. In every sample, organic acids dominated, averaging 82% of DO
C. No major differences in DOC fractions between Maine lakes and Finni
sh lakes were found. However, differences in DOC fractions were found
between lakes with low and high DOC. The proportion of hydrophobic aci
ds increased with increasing POC, whereas the proportion of hydrophili
c acids decreased with increasing DOC. Low DOC lakes had a greater pro
portion of their DOC as hydrophilic neutrals compared with high DOC la
kes On the basis of the fractionation results, linear equations were d
eveloped for the relationships between the total DOC and the proportio
ns of hydrophobic and hydrophilic acids of the total DOC. (C) 1998 Els
evier Science Ltd.