The extent and mechanisms of adsorption of marine pore water organic matter
to montmorillonite were studied in a series of batch and sequential adsorp
tion experiments. Pore water natural organic matter (pNOM) and easily extra
cted natural organic matter (eNOM) were collected from Liberty Bay (Puget S
ound, WA, USA) sediments. The pNOM and eNOM were each divided into two size
fractions using a 1000 D ultrafilter. Batch adsorption isotherms were appr
oximately linear, and the > 1000 D fractions of both pNOM and eNOM had larg
er partition coefficients (K-d) than the < 1000 D fractions. A two-componen
t fit of the sequential adsorption data indicated that pNOM and eNOM contai
ned a similar amount of NOM (30%) that was not surface reactive toward mont
morillonite. After correcting the batch adsorption K(d)s for the non-reacti
ve components, the K(d)s estimated by batch and sequential adsorption were
identical (similar to 2.7 l/kg for > 1000 D pNOM and eNOM, and similar to 1
.6 l/kg for < 1000 D pNOM and eNOM). Mechanisms of adsorption were investig
ated by systematically changing conditions (pH, temperature and ionic compo
sition) of > 1000 D fractions during batch isotherm experiments. Adsorption
of NOM was found to decrease with increased temperature, suggesting that h
ydrophobic effects were not the dominant adsorption mechanisms in this syst
em. Ion exchange was also not an important adsorption mechanism because ads
orption increased with ionic strength. The observed enhancement in adsorpti
on with ionic strength indicated that van der Waals interactions were impor
tant in the adsorption of NOM. Ligand exchange was found to be a significan
t mechanism since the presence of SO42- in solution reduced the amount of N
OM adsorbed. Ca2+ enhanced adsorption slightly more than Na+, suggesting th
at cation bridging was involved. The relative contributions of van der Waal
s interactions, ligand exchange and cation bridging were estimated to be ap
proximately 60%, 35% and 5%, respectively, for adsorption of NOM in a CaCl2
solution. (C) 2000 Elsevier Science B.V. All rights reserved.