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Seismic Design of Tunnels - Parsons Brinckerhoff

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developed for a one-barrel frame with equal moment <strong>of</strong> inertia, I L , for ro<strong>of</strong> and invert slabs<br />

and equal moment <strong>of</strong> inertia, I H , for side walls is given by:<br />

F = G ÊH 2 L<br />

24 Ë EI H<br />

+ HL2<br />

EI L<br />

ˆ<br />

¯<br />

(Eq. 5-6)<br />

where<br />

E = plane strain elastic modulus <strong>of</strong> frame<br />

G = shear modulus <strong>of</strong> soil<br />

I L , I H = moments <strong>of</strong> inertia per unit width for slabs and walls, respectively<br />

Note that the expressions by Equation 5-6 and Equation 5-7 that follow are valid only<br />

for homogeneous, continuous frames with rigid connections. Reinforced framed concrete<br />

structures are examples <strong>of</strong> this type <strong>of</strong> construction.<br />

Special Case 2. The flexibility ratio derived for a one-barrel frame with ro<strong>of</strong> slab moment<br />

<strong>of</strong> inertia, I R , invert slab moment <strong>of</strong> inertia, I I , and side wall moment <strong>of</strong> inertia, I W , is<br />

expressed as:<br />

F = G ÊHL 2<br />

12 Ë EI R<br />

Y<br />

ˆ<br />

¯<br />

(Eq. 5-7)<br />

where<br />

( 1+ a2)a1 + 3a2<br />

Y= ( )2 + ( a 1+ a 2 )3a ( 2 +1) 2<br />

( 1 + a 1 + 6a 2 ) 2<br />

Ê<br />

a 1 =<br />

IR<br />

Ë ˆ¯ and a Ê<br />

2 = IR<br />

Ë<br />

ˆ¯<br />

I I<br />

I W<br />

H<br />

L<br />

E = plane strain elastic modulus <strong>of</strong> frame<br />

G = shear modulus <strong>of</strong> soil<br />

I R , I I , I W = moments <strong>of</strong> inertia per unit width<br />

Implications <strong>of</strong> Flexibility Ratios. The derivation <strong>of</strong> the flexibility ratio presented in this<br />

section is consistent with that for the circular tunnels. The theoretical implications are:<br />

• A flexibility ratio <strong>of</strong> 1.0 implies equal stiffness between the structure and the ground.<br />

Thus, the structure should theoretically distort the same magnitude as estimated for<br />

the ground in the free-field.<br />

110

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