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92<br />

Site<br />

categories<br />

A<br />

B<br />

C<br />

D<br />

Table 4 <strong>The</strong> adjusting coefficients suggested by Li Xiaojun (2001)<br />

Acceleration from the zoning map for site category A<br />

0.05g O.lg 0.15g 0.20g 0.30g 0.40g<br />

1.0 1.0 1.0 1.0 1.0 1.0<br />

1.5 1.45 1.40 1.33 1.25 1.18<br />

1.10 LOO 0.9 0.8 0.7 0.6<br />

0.8 0.7 0.6 0.55 0.50 0.45<br />

<strong>The</strong> values in the above two tables commonly describe the amplifying effect of ground soil layers, and<br />

the reduction effect of soil nonlinearity when acceleration is strong enough. Meanwhile one can find<br />

there is quite a large difference between the values in the two tables, especially the trend of varying<br />

with soil from stiff to soft and from thin to thick. Should it increase or decrease <strong>The</strong> most convincing<br />

answer must come from the observed data. <strong>The</strong> maximum values of normalized response spectra of<br />

760 free field ground motion records, and the corresponding magnitudes, distances and site conditions,<br />

are summarized to work out the coefficient values in this paper.<br />

To deal with the relation between the maximum values of normalized spectra and site condition, the<br />

key point is to compare them at the same magnitude and distance. <strong>The</strong> biggest difficulty is that the data<br />

sample is not large enough, and the data distribution in magnitude and distance is not homogeneous.<br />

One can rarely find sets of data of the same magnitude (ideally the same earthquake) and exact same<br />

distance for various site conditions. <strong>The</strong> qualification has to be relaxed to those of similar magnitude<br />

and distance. <strong>The</strong> authors compare the mean maximum values in each magnitude and distance group<br />

directly rather than compare the attenuation relationships for various site categories. <strong>The</strong> ratios of<br />

mean values of maximum spectrum amplitudes for various sites to the value for rock site in every<br />

group are shown hi table 5, where the number in bracket after the ratio is the sample size (i.e. number<br />

of records. <strong>The</strong> records just on the boundaries between two neighboring groups are applied twice). <strong>The</strong><br />

term Ace. is for acceleration of maximum spectral amplitude on rock site divided by 2.5<br />

Table 5 <strong>The</strong> ratios of mean values of maximum spectral amplitudes of various sites to one of rock site<br />

Distance ikm)<br />

' -— A CC - (§)<br />

Site Categories----^^_<br />

1<br />

2<br />

3<br />

4<br />

Distance (km)<br />

' " — "•—--— .^Acc. (3)<br />

Site Categories'——-^<br />

1<br />

2<br />

3<br />

4<br />

Magnitude ^5.75<br />

0-10 10-50<br />

0.2543<br />

1.00 (9)<br />

0.1365<br />

LOO (10)<br />

139 (6)<br />

0.79 (84) 0.79 (81)<br />

Magnitude 5.75 - 6.5<br />

0-30 30-50<br />

0.199<br />

1.00 (18)<br />

1.47 (8)<br />

1.96 (8)<br />

1.35 (91)<br />

0.1271<br />

1.00 (6)<br />

1.38 (6)<br />

1.10 (4)<br />

1.25 (112)<br />

50-100<br />

0.028<br />

1.00 (4)<br />

1.23 (22)<br />

50-100<br />

0.0291<br />

1.00 (6)<br />

1.53 (4)<br />

2.21 (38)<br />

100-200<br />

0.0303<br />

1.00 (2)<br />

100-200<br />

0.0357<br />

1.00 (2)<br />

0.68 (20)

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