deposits in a sewer is called the self-cleansing velocity. The self-cleansing
velocity in a pipe flowing full is (ASCE and WEF 1992):
for SI units
(4.41a)
for British units
(4.41b)
where V ⫽ velocity, m/s or ft/s
R ⫽ hydraulic radius, m or ft
n ⫽ Manning’s coefficient of roughness
B ⫽ dimensionless constant
⫽ 0.04 to start motion
⫽ 0.8 for adequate self-cleansing
s ⫽ specific gravity of the particle
D
p
⫽ diameter of the particle
f ⫽ friction factor, dimensionless
g ⫽ gravitational acceleration
⫽ 9.81 m/s
2
or 32.2 ft/s
2
Sewers flowing between 50% and 80% full need not be placed on
steeper grades to be as self-cleansing as sewers flowing full. The reason
is that velocity and discharge are functions of attractive force which
depends on the friction coefficient and flow velocity (Fair et al. 1966).
Figure 4.8 presents the hydraulic elements of circular sewers that pos-
sess equal self-cleansing effect.
Using Fig. 4.8, the slope for a given degree of self-cleansing of partly
full pipes can be determined. Applying Eq. (4.41) with the Manning
equation (Eq. (4.22)) or Fig. 4.3, a pipe to carry a design full discharge
Q
f
at a velocity V
f
that moves a particle of size D
p
can be selected. This
same particle will be moved by a lesser flow rate between Q
f
and some
lower discharge Q
s.
Figure 4.8 suggests that any flow ratio Q/Q
f
that causes the depth ratio
d/D to be larger than 0.5 requires no increase in slope because S
s
is less
than S
f
. For smaller flows, the invert slope must be increased to S
s
to
avoid a decrease in self-cleansing.
5 c
8B
f
gss 2 1dD
p
d
1/2
V 5
1.486R
1/6
n
[Bss 2 1dD
p
]
1/2
5 c
8B
f
gss 2 1dD
p
d
1/2
V 5
R
1/6
n
[Bss 2 1dD
p
]
1/2
282 Chapter 4