The dynamics of particle capture and head-loss development were studie
d in laboratory filters over extended periods. Particle-size distribut
ions and pressures were measured above the sand media and at three dep
ths. Conditions included filtration velocities of 1.8 and 5.5 mm/s and
mean media sizes of 0.39, 0.78, and 1.85 mm. The suspension was sedim
entation effluent from a softening water-treatment plant. Ripening, th
e improved removal efficiency with time, was extensive for small parti
cles, but breakthrough, the decreased removal with time, was more sign
ificant for intermediate and larger particles. Detachment of previousl
y retained particles was demonstrated to contribute substantially to b
reakoff; apparently, flocs are formed on the media surface by the sequ
ential capture of particles and break off together. Theory suggests th
at higher velocities and larger media sizes can be offset quantitative
ly, with respect to particle removal, by proportionately greater depth
s; data from this research support these ideas. Comparison with previo
us experiments with glass spheres as the media but otherwise identical
conditions showed that, for sand, initial removal was better, ripenin
g was less extensive (perhaps because of initially better removal), an
d detachment was more extensive.