Aquifer sediments contain a wide distribution of particle sizes, but o
nly a single collector diameter (d) can be used in a filtration equati
on. To establish a method for selecting a characteristic d when media
are composed of different sized particles, we measured bacterial reten
tion in columns packed with either crushed quartz sand (separated into
three different size ranges) or borosilicate glass beads. The best me
thods for choosing d were those that produced nearly constant collisio
n efficiencies (alpha's). Characteristic diameters included: d(10) (10
% of all particles were smaller), d(90) (90% of all particles were sma
ller), d(a) (arithmetic mean), and d(g) (geometric mean), where all di
ameters were calculated using number, area, and volume size distributi
ons. Bacterial alpha's decreased in proportion to the distance travele
d in the packed bed, and were scaled by the number of bacteria-sedimen
t collisions using a dimensionless collision number (xi). These Compar
isons indicated that characteristic diameters based on the smaller par
ticles (d(a) and d(g) using number distributions, and d(10) using a vo
lume distribution) most accurately described bacterial transport in th
e different-sized porous media.