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Lesson 7 - nptel

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where K is the coefficient of permeability and b is the width of one flow channel, that is,<br />

the distance between two stream lines. If Nf is the total number of flow channels, then<br />

the seepage per unit width of the embankment (q) is given as<br />

h ⎛ b ⎞<br />

⎛ b ⎞ ⎛ Ν f ⎞<br />

q = ∑ Δq<br />

= Κ ⋅ ⎜ ⎟ ⋅ Ν = Κ ⋅ ⋅⎜<br />

⎟ ⋅<br />

⎜<br />

⎟<br />

f h<br />

(4)<br />

Ν d ⎝ l ⎠<br />

⎝ l ⎠ ⎝ Ν d ⎠<br />

The above calculations would give the quantity of water seeping through the body of the<br />

dam. Similar calculations have to be done for the quantity of seepage taking place<br />

through the foundation.<br />

4.7.6 Stability calculation<br />

For an embankment dam the most important cause of failure is sliding. It may occur<br />

slowly or suddenly and with or without any prior warning. Such a failure causes a<br />

pportion of the earth or rockfill to slide downwards and outwards with respect to the<br />

remaining part generally along a well-defined slide surface (Figure 53). As may be<br />

observed, the profile of the slide surface may be nearly approximated by circular arcs<br />

(Figure 53 a, b) or by wedges (Figure 53 c, d). The upstream failure surfaces in all<br />

cases may be possible, among others, during sudden drawdown of the reservoir level<br />

from elevation I to II, shown in the figures. At the time of the failure, the average<br />

shearing resistance all along the sliding surface. It is, therefore, necessary that the<br />

designers take special care to estimate the possibility of such a failure.<br />

Version 2 CE IIT, Kharagpur

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