A forced-gradient tracer test was conducted at the Georgetown site to
study the transport of natural organic matter (NOM) in groundwater. In
particular, the goal of this experiment was to investigate the intera
ctions between NOM and the aquifer matrix. A detailed three-dimensiona
l characterization of the hydrologic conductivity heterogeneity of the
site was obtained using slug tests. The transport of a conservative t
racer (chloride) was successfully reproduced using these conductivity
data. Despite the good simulation of the flow field, NOM breakthrough
curves could not be reproduced using a two-site sorption model with sp
atially constant parameters. Preliminary results suggest that differen
t mechanisms for the adsorption/desorption processes, as well as their
spatial variability, may significantly affect the transport and fate
of NOM.