A comparison is made between existing mathematical models and experime
ntal data that relate the reduction of the saturated hydraulic conduct
ivity (K) of a porous medium to the porosity reduction caused by micro
bial growth. The models yielded a realistic prediction of a data set o
btained with a model porous medium consisting of millimeter-size glass
spheres, but failed to predict the clogging behaviour observed in sma
ller-than-1-mm sand. A new modelling approach, semi-mechanistic in nat
ure, is proposed that gives good predictions of fine sand media as wel
l. It relaxes the assumption about uniformly-thick biofilms by allowin
g a second arrangement to occur, i.e, discrete plugs filling the pore
lumen. The new model requires input data on two intrinsic properties o
f the system, which renders it sufficiently flexible as to fit very di
fferent data sets. The two model parameters are K-min, the minimum K v
alue when all porosity is filled with microorganisms, and B-c, the bio
volume fraction at which most cell detachment from biofilm occurs.