Sediment dredged from the port of Hamburg is treated and stored upland
in a storage facility. The site is covered by a system of topsoil abo
ve a sand drainage layer and a barrier layer made of processed harbour
sludge in order to minimize the input of water after completion of th
e site. In 1995 in-situ investigations have started to study the hydra
ulic properties, the water balance and the water quality of the cover
system of the storage site Francop in Hamburg. Two lysimeters (500 m(2
) each) were constructed. During the first dry year after the construc
tion of the lysimeters discharge rates < 0.05 mm/d were measured below
the sludge barrier. The hydraulic gradients indicate downward water m
ovement in the sludge barrier during the summer and the winter of 1996
. The chemical composition of the discharge below the barrier is typic
al for sludge pore water. An increase of the discharge above the sludg
e barrier neither led to an increase of discharges nor to changes in t
he concentration of the water compounds below the barrier. We assume t
hat up to now there is no preferential flow through the sludge barrier
. The cover system including the sludge barrier performs very well. Th
e monitoring of the lysimeters is continued. (C) 1998 IAWQ. Published
by Elsevier Science Ltd.