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

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439<br />

stiffness of the springs added to give restoring<br />

forces after sliding was tuned such that the<br />

natural period of the isolation system after<br />

sliding is 3.0 seconds. Young's modulus of PVC<br />

material and the friction coefficient of the roller<br />

were evaluated by measurement. <strong>The</strong> damping<br />

ratios were evaluated by the random decrement<br />

method from the records of forced oscillation<br />

tests (Vandier, 1982). <strong>The</strong> principal dimensions<br />

and parameters of the model are listed in Table<br />

2.1.<br />

Method of Measurement<br />

Tests were performed using the bi-axial shaking<br />

table at Nagoya <strong>University</strong> which can generate<br />

horizontal and vertical motions simultaneously.<br />

<strong>The</strong> NS and UD components of El Centro 1940<br />

acceleration records which were normalized such<br />

TABLE 2.1<br />

PRINCIPAL PARAMETERS OF TEST MODEL<br />

Span<br />

Rise<br />

Radius of curvature<br />

Width<br />

Thickness<br />

Half subtended angle<br />

Total mass of arch<br />

Total mass of sub-structure<br />

Young's modulus of PVC<br />

Damping ratio<br />

non-isolated model<br />

isolated model<br />

Stiffness of a spring<br />

Friction coefficient of rollers<br />

780mm<br />

212.5 mm<br />

480.6 mm<br />

300mm<br />

I mm<br />

54.2°<br />

0.409 kg<br />

0.329 kg<br />

2.90 kN/mnf<br />

0.809 N/m<br />

0.03<br />

that the maximum horizontal acceleration is 300 gal were adopted as input horizontal and vertical<br />

ground motions, respectively. <strong>The</strong> accelerations of the shaking table were measured by means of<br />

strain-gauge type acceleration meters, and the displacement responses were measured at 7 points along<br />

the arch section and a point on the shaking table by means of an optical image tracking system.<br />

Test Results<br />

Prior to forced oscillation tests using earthquake records, sweep oscillation tests were performed to<br />

measure the natural frequencies of the non-isolated arch model, of which the results are shown in<br />

Table 2.2.<br />

Fig. 2.2 shows the measured time histories of<br />

displacement responses at the point A of the nonisolated<br />

and isolated models. <strong>The</strong>se are the<br />

displacements relative to the base-isolation system<br />

for the isolated model and to the shaking table for<br />

the non-isolated model. It is observed that large<br />

displacement responses are excited not only in the<br />

horizontal but also in the vertical directions of the<br />

non-isolated arch. This is due to the fundamental<br />

TABLE 2.2<br />

MEASURED AND PREDICTED NATURAL<br />

PERIODS OF NON-ISOLATED MODEL<br />

Mode<br />

Measured<br />

Predicted<br />

1 st mode<br />

(antisymmetric)<br />

0.632 s<br />

0.637 s<br />

2 nd mode<br />

(symmetric)<br />

0.172s<br />

0.180s<br />

(s)<br />

Horizontal disi<br />

Vertical displacanent<br />

Mon-isolated<br />

Non-isolated<br />

— Isolated<br />

FIG. 2.2<br />

MEASURED DISPLACEMENT RESPONSES<br />

AT POINT A OF ARCH

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