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Technical Paper by JP Giroud, KL Soderman and K. Badu-Tweneboah

Technical Paper by JP Giroud, KL Soderman and K. Badu-Tweneboah

Technical Paper by JP Giroud, KL Soderman and K. Badu-Tweneboah

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GIROUD et al. D Optimal Configuration of a Double Liner System<br />

conditions are met for the simpler, but less general, Equation 4 (Bernoulli’s equation) to<br />

be applicable. According to Figure 6 of the paper <strong>by</strong> <strong>Giroud</strong> et al. (1997b), Equation 4<br />

is applicable fora defect with a diameter of2 mm <strong>and</strong> a leachate head on top of the primary<br />

liner of 0.01 m if the hydraulic conductivity of the leachate collection layer overlying<br />

the geomembrane liner is greater than 1 × 10 -1 m/s. According to Section 3.1, this condition<br />

is met. (It has also been checked that Equation 4 is applicable to the geomembrane<br />

primary liner in the three other cases considered in the comparative study.) Consequently,<br />

Equation 4 can be used as follows to calculate the rate of leachate migration through<br />

a defect in the geomembrane primary liner due to a leachate head of 0.01 m:<br />

Q 1<br />

= ¥ - 6<br />

(.)( 0 6 10 ) ()(. 2 9 81)(. 0 01) = 8.<br />

349 ¥ 10<br />

- 7 3<br />

p m /s<br />

The unit rate of leachate migration through the geomembrane primary liner is then<br />

calculated using Equation 3 as follows:<br />

q 1<br />

= ( 2. 5 ¥ 10 ) (8. 349 ¥ 10 ) = 2.<br />

087 ¥ 10<br />

- 4 - 7 -10<br />

m/s<br />

Average Head of Leachate on Top of the Secondary Liner. The methodology for calculating<br />

the average head of leachate is described in Section 2.2. The average head of<br />

leachate on top of the secondary liner due to the above calculated unit rate of leachate<br />

migration through the primary liner is calculated using Equation 1 as follows:<br />

-10<br />

( 2087 . ¥ 10 ) (50)<br />

h 2<br />

=<br />

= 2609 . ¥ 10<br />

( 2) ( 01 . ) ( 002 . )<br />

- 6 m<br />

Rate of Leachate Migration Through the Composite Secondary Liner. The methodology<br />

for calculating the rate of leachate migration through a composite liner due to a geomembrane<br />

defect is described in Section 2.3.5. The rate of leachate migration through<br />

the secondary liner resulting from the above calculated head is calculated using Equation<br />

11 as follows:<br />

L<br />

NM<br />

Q 2<br />

= 021 . 1+<br />

01 .<br />

= 4.<br />

044 ¥ 10<br />

F<br />

HG<br />

-15<br />

2.<br />

609 ¥ 10<br />

-3<br />

7 ¥ 10<br />

3<br />

m /s<br />

-6<br />

I<br />

KJ<br />

095 .<br />

O<br />

QP<br />

- - -<br />

( p ¥ 10 ) ( 2. 609 ¥ 10 ) ( 1 ¥ 10 )<br />

6 01 . 6 0. 9 11 0.<br />

74<br />

The unit rate of leachate migration through the composite secondary liner is then calculated<br />

using Equation 3 as follows:<br />

q 2<br />

= ( 2. 5 ¥ 10 ) ( 4. 044 ¥ 10 ) = 1011 . ¥ 10<br />

- 4 - 15 -18<br />

m/s<br />

382 GEOSYNTHETICS INTERNATIONAL S 1997, VOL. 4, NOS. 3-4

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