Colloids are present in groundwater aquifers and water-permeable engineered
barrier systems and may facilitate the migration of radionuclides. A highl
y permeable mortar is foreseen to be used as backfill for the engineered ba
rrier of the Swiss repository for low- and intermediate-level waste. The ba
ckfill is considered to be a chemical environment with some potential for c
olloid generation and, due to its high porosity, for colloid mobility. Coll
oid concentration measurements were carried out using an in-situ liquid par
ticle counting system. The in-house developed counting system with three co
mmercially available sensors allowed the detection of single particles and
colloids at low concentrations in the size range 50-5000 nm. The counting s
ystem was tested using suspensions prepared from certified size standards.
The concentrations of colloids with size range 50-1000 nm were measured in
cement pore water, which was collected from a column filled with a highly p
ermeable backfill mortar. The chemical composition of the pore water corres
ponded to a Ca(OH)(2)-controlled cement system. Colloid concentrations in t
he backfill pore water were found to be typically lower than similar to0.1
ppm. The specific (geometric) surface areas of the colloid populations were
in the range 240 m(2) g(-1) to 770 m(2) g(-1). The low colloid inventories
observed in this study can be explained by the high ionic strength and Ca
concentrations of the cement pore water. These conditions are favourable fo
r colloid-colloid and colloid-backfill interactions and unfavourable for co
lloid-enhanced nuclide transport. (C) 2001 Elsevier Science Ltd. All rights
reserved.