Permeability of geomaterials is the most important parameter involved in th
e assessment of advection of groundwater and contaminants in the subsurface
and for the design of barriers to contain hazardous wastes. Evaluation of
the permeability of soils by employing a geotechnical centrifuge, where cen
trifugal acceleration is used to simulate the prototype conditions, is an a
rea of current research interest. This paper presents a working methodology
that can be employed for measuring the hydraulic conductivity of compacted
fine-grained soils in a geotechnical centrifuge. Two different hydraulic c
onductivity setups have been developed for silty sand and clays. The paper
also studies the effect of sample length, the limiting acceleration levels,
and the time of centrifugation on the hydraulic conductivity measurements.