Natural humic surface water (pH 5.9), ion exchanged samples of the same wat
er (pH 5.5), and aqueous solutions of isolated humic substances at pH 4.5,
5.5 and 6.5, respectively, were ultrafiltered (15 degrees C, 0.5 bar) using
hydrophobic polysulfone membranes (GR51) in a cross-flow flat sheet module
. The used membrane did not completely retain natural organic matter from t
he surface water and the addition of complexing metals did not affect the r
etention any further. The changes which were induced in the membranes durin
g each filtration run were studied by simultaneous streaming potential and
flux measurements in 0.01 M KCl solutions. Zeta potentials were calculated
based on the streaming potentials and the results showed changes towards mo
re negative values for all the samples due to adsorption of organic matter
onto the surface of the membrane pores. Humic acid affected the membrane ch
arges more than fulvic acid. High ionic strength and low pH enhanced flux r
eduction and fouling. Filtration of natural waters caused more pore pluggin
g and flux reduction than filtration of solutions of the isolated humic sub
stances. (C) 1999 Elsevier Science Ltd. All rights reserved.