We examined adsorption equilibrium and kinetics of an aquatic fulvic acid (
XAD-8 resin extract) onto goethite (alpha -FeOOH). Molecular weight distrib
utions were determined using high-pressure size exclusion chromatography (H
PSEC). Overall adsorption isotherms and those of the most abundant intermed
iate molecular weight (IMW) fraction (1250-3750 Da) fit the Langmuir adsorp
tion equation, as is commonly observed for humic substances. However, this
overall fit masked the non-langmuir isotherm shape of high and low molecula
r weight (HMW, LMW, respectively) fractions. We observed preferential adsor
ption of HMW fractions at low pH and of IMW fractions at higher pH. We also
observed preferential adsorption of components with higher absorbance norm
alized to moles C (epsilon (280)), probably reflecting greater aromaticity.
Over the first 6 h of adsorption experiments, adsorbed organic carbon incr
eased and weight average molecular weight (M-w) of the organic matter remai
ning in solution decreased, consistent with slower adsorption of higher mol
ecular weight components. Observations of fractionation upon adsorption agr
eed well with a field study showing lower M-w and lower epsilon (280) organ
ic matter in deeper ground water relative to surface and shallow ground wat
er. Copyright (C) 2001 Elsevier Science Ltd.