Recent studies have shown that natural organic matter (e.g., humic and fulv
ic acids) is a major foulant during ultrafiltration of surface water. The o
bjective of this study was to develop a more complete understanding of the
mechanisms governing humic acid fouling, including the effects of humic aci
d adsorption, concentration polarization, and aggregate deposition on the r
ate and extent of fouling. Data were obtained with Aldrich and Suwannee Riv
er humic acids using ultrafiltration membranes with a broad range of molecu
lar weight cutoffs. Fouled membranes were also examined using streaming pot
ential and contact angle measurements. The extent of flux decline was great
est for the largest molecular weight cutoff membranes due to the greater re
lative hydraulic resistance of the humic acid deposit formed on the surface
of these membranes. This humic acid deposit reduced the apparent zeta pote
ntial and increased the membrane contact angle. Simple static adsorption an
d concentration polarization caused relatively little flux decline. Humic a
cid aggregates had a significant effect on fouling only for the larger mole
cular weight cutoff membranes. The rate and extent of humic acid fouling in
creased at low pH, high ionic strength, and in the presence of calcium due
to changes in intermolecular electrostatic interactions. These results prov
ide important insights into the mechanisms of humic acid fouling during ult
rafiltration.