In geotechnical modeling, the use of a pore fluid having viscosity greater
than that of water is a well-established method of satisfying the scaling l
aws relating to movement of pore fluid through the soil during dynamic load
ing events. This has often been achieved with either silicone oil or mixtur
es of water and glycerol. However, there are a number of inherent drawbacks
and difficulties in using silicone oil in particular, and this paper descr
ibes an alternative solution of hydroxypropyl methylcellulose (HPMC) in wat
er that has been used recently with success. This paper presents test data
documenting the variation in solution viscosity with concentration and temp
erature and the variation in specific gravity with concentration. The relat
ive performance of the fluid is illustrated with data from two centrifuge m
odel tests, one with pure water as the pore fluid and one with an HPMC solu
tion having viscosity ten times that of water.