146 ENVIRONMENTAL ENGINEEWG
where Vavg = average volume of all particles and A, = average area of all particles.
Substituting Eq. (7.8) into Eq. (7.6) yields
and
(7.10)
where x = weight fraction of particles retained between any two sieves and d' =
geometric mean diameter between those sieves
1-e
hL = f (:) ( T) (5) ;.
(7.11)
This equation holds for nonstratifid beds, such as are found in a slow sand filter, since
the fraction factor does not vary with depth. When particles are stratified, as in a rapid
sand filter, we can write Eq. (7.11) as
-- dhL - [(f> (9) ($)If$.
dL
The total head loss is thus
(7.12)
hL = 1" dhL = [ (i) (9) ($)] 1 L1 f ;i' dL.
Since d L = L dx, where a!x is the proportion of particles of size d
and if the particles between adjacent sieve sizes are assumed uniform,
hL= [($) (G) ($)]E$.
(7.13)
(7.14)