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Seismic Design of Tunnels - Parsons Brinckerhoff

Seismic Design of Tunnels - Parsons Brinckerhoff

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5. Derive the ground displacement amplitude, D:<br />

As discussed before, the ground displacement amplitude is generally a function <strong>of</strong> the<br />

wavelength, L. A reasonable estimate <strong>of</strong> the displacement amplitude must consider the<br />

site-specific subsurface conditions as well as the characteristics <strong>of</strong> the input ground<br />

motion. In this design example, however, the ground displacement amplitudes are<br />

calculated in such a manner that the ground strains as a result <strong>of</strong> these displacement<br />

amplitudes are comparable to the ground strains used in the calculations based on the<br />

simplified free-field equations. The purpose <strong>of</strong> this assumption is to allow a direct and<br />

clear evaluation <strong>of</strong> the effect <strong>of</strong> tunnel-ground interaction. Thus, by assuming a sinusoidal<br />

wave with a displacement amplitude D and a wavelength L, we can obtain:<br />

For free-field axial strain:<br />

V s<br />

= 2pD<br />

2C s<br />

L fi D = Da = 0.291ft 45<br />

For free-field bending curvature:<br />

A s<br />

cos 3 45 o = 4p2 D<br />

fi D = D b = 0.226 ft<br />

2<br />

C s<br />

L 2<br />

6. Calculate the maximum axial force (Equation 3-1) and the corresponding axial strain<br />

<strong>of</strong> the tunnel lining:<br />

K a L<br />

Q max<br />

=<br />

2p<br />

K<br />

1 + 2Ê<br />

a ˆÊ<br />

L<br />

ËE c A c<br />

¯Ë<br />

ˆ¯<br />

D 2<br />

a<br />

2p<br />

526x400<br />

=<br />

2p<br />

526<br />

1+2Ê<br />

ˆÊ400ˆ<br />

x 0.291<br />

2<br />

Ë518400x62.8¯Ë<br />

2p ¯<br />

= 8619kips<br />

e axial = Q max 8619<br />

=<br />

E c A c 518400x62.8 = 0.00026<br />

45

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