356 CHAPTER TWELVE
and the effective stress in the soil
(12.207)
but 1/LiandiN 1 /N 2 , therefore
(12.208)
Were the soil structure of such a nature and the reservoir head Hgreat
enough to create a large amount of percolation or high seepage pressure, the
flowQwould exceed the limits for a safe foundation and the effective pressure
Pewould be reduced enough to permit soil distortion and sliding of the founda-
tion material upon itself.
To reduce under-dam seepage a cutoff wall, Fig. 12.31, can be used. Then,
Darcy’s law, as modified to include the Schliter formula, gives the following
formula for the depth of the cutoff wall:
(12.209)
in which ddepth of cutoff, ft (m)
Ka transmission constant
Hhead, ft (m)
Pporosity of the material expressed as a decimal
Vpermissible velocity, fpm (m/s)
beffective base width of the dam, ft (m)
Earth Dams
Earth dams, dikes, and levees are the commonest structures used to impound
water, and innumerable instances of their use exist in all parts of the world. The
entire range in soils, from clays to boulders or quarried stone, has been used in
their construction.
Seepage in earth dams through the dam itself and the foundation, should be
kept within the limits prescribed by use of the reservoir, and by economic con-
siderations. The flow of water through all soils except the coarser ones is of the
laminar type and is in accordance with Darcy’s law:
(12.210)
whereQquantity of flow in time, t
kcoefficient of permeability
ihydraulic gradient expressed as head lost per unit length of flow path
Asuperficial area of flow (total cross-sectional area of flow, not
merely cross-sectional area of soil pores)
QkiAt
d
KH
2 PV
b^2 PV
2 KH
peDw
s 1
1 e
N 1
N 2
H
(
peppnD
se
1 e
wDwD
H
L
w