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Earthquake Engineering Research - HKU Libraries - The University ...

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364<br />

complex as it depends on the soil-water-wall interaction. Secondly, excess pore pressure will build up m<br />

saturated soil. It is difficult to estimate excess pore pressure using simple calculation and hence it is not<br />

possible to use simple design calculation to determine the threshold acceleration or the resulting<br />

displacement. <strong>The</strong>refore, small-scale model simulation or comprehensive numerical codes need to be<br />

used.<br />

Physical Modeling<br />

Since earthquakes in the field are unpredictable, it is difficult to record seismic response of gravity walls<br />

during earthquakes in the field. In most cases, what geotechnical engineers have are the pre-earthquake<br />

information and data collected during post-earthquake investigations. <strong>The</strong> most crucial information i.e.<br />

the response of the structure during earthquakes such as the amplification of vibration, excess pore<br />

pressure, and dynamic soil-structure interaction is generally not available. In order to calibrate or verify<br />

analytical procedures or numerical simulation, realistic physical data are needed.<br />

In the absence of field data recorded in earthquakes, data generated by physical model tests such as shake<br />

table tests and centrifuge tests become very valuable. In recent years, significant progress has been made<br />

in physical modeling technique in geotechnical earthquake engineering as reported in the 2001 NSF<br />

International Workshop on <strong>Earthquake</strong> Simulation in Geotechnical <strong>Engineering</strong> (Zeng, 2002). Shake table<br />

tests conduct at Ig have been used to study seismic response of gravity quay walls by Inagaki et al (1996)<br />

after the Kobe earthquake. While the interpretation of data from Ig shake table test is complicated by the<br />

scaling law issues, centrifuge modeling has the ability to create the same stress and strain condition as<br />

expected in the field. Since most mechanical properties of soils are stress dependent, centrifuge modeling<br />

has the advantage of satisfying most of the scaling laws. In the 1990s, a group of centrifuge tests of<br />

gravity retaining walls were conducted by Zeng (1998) for the VELACS project. <strong>The</strong> result of one model<br />

test is shown in Fig. 2.1.<br />

-•<br />

water<br />

'<br />

I<br />

!<br />

" -i*<br />

l°s L 44<br />

:,<br />

5<br />

1<br />

40 \<br />

* :~"<br />

i<br />

!<br />

i\ • :i<br />

1- 96 ^|<br />

water saturated backfill<br />

Us<br />

~ initial boundary<br />

" boundary after EQl<br />

Fig, 2.1 Cross-sectional view of a gravity wall model after earthquake test (unit:m)

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