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Jardine, R.J., Potts, D.M., StJohn, H.D., and Hight, D.W. (1991). Some practical applications of a nonlinear ground model. Proceedings, 10th European Conference on Soil Mechanics and Foundation Engineering (1), Firenze, 223-228. Johnston, A.C. and Schweig, E.S. (1996). The enigma of the New Madrid earthquakes of 1811 - 1812. Annual Review of Earth and Planetary Sciences 24, 339-384. Juang, C.H., Jiang, T. and Andrus, R.D. (2002). Assessing Probability-based Methods for Liquefaction Potential Evaluation. Vol. Journal of Geotechnical Engineering 128:7, 580-589. Lunne, T., Robertson, P.K., and Powell, JJ.M. (1997). Cone Penetration Testing in Geotechnical Practice. Blackie Academic, Routledge Publishers, New York, 312. Mayne (2001). Stress-strain-strength-flow parameters from enhanced in-situ tests. Proceedings, Intl. Conf. on In-Situ Measurement of Soil Properties & Case Histories, Bali, Indonesia, 27-48. Robertson, P.K. (1990). Soil classification using the cone penetration test. Canadian Geotechnical Journal 27:1, 151-158. Robertson, P.K. and Wride, C.E. (1998). Evaluating cyclic liquefaction potential using the cone penetration test. Canadian Geotechnical Journal 35:3, 442-459. Seed, H.B., and Idriss, I.M. (1971). Simplified procedure for evaluating soil liquefaction potential, Journal of Soil Mechanics and Foundation Division 97:9, 1249-1273. Stewart, W.P. and Campanella, R.G. (1993). Practical aspects of in situ measurements of material damping with the seismic cone penetration test. Canadian Geotechnical Journal 30:2, 211-219. Stokoe, K.H., Anderson, D.G., Hoar, RJ. and Isenhower, W.M. (1978). In-situ and lab shear velocity and modulus. Earthquake Engineering and Soil Dynamics, Vol. Ill, ASCE, New York, 1498-1502. Vucetic, M. and Dobry, R. (1991). Effect of soil plasticity on cyclic response. Journal of Geotechnical Engineering 117:1, 89-107. Woods, R.D. (1978). Measurement of Dynamic Soil Properties, State of the Art Report. Earthquake Engineering and Soil Dynamics, Vol. I, ASCE, Reston, VA, 91-178. Yasuda, S. and Tohno, I. (1988). Sites of re-liquefaction caused by the 1983 Nihonkai-Chuba earthquake. Soils and Foundations 28:2, 61-72. Youd, T.L. (1988). Recurrence of liquefaction at the same site. Proceedings of the Eighth World Conference on Earthquake Engineering. San Francisco, Vol. Ill: 231-238. Youd, T.L. and Gams, C.T. (1995). Liquefaction-induced ground-surface disruption. Journal of Geotechnical Engineering, 121:11, 805-809. Youd, T. L., et al. (2001). Liquefaction resistance of soils: Summary report from the 1996 NCEER and 1998 NCEER/NSF workshops on evaluation of liquefaction resistance of soils. Journal of Geotechnical and Geoenvironmental Engineering, 127:10, 817-833. 122
Proceedings of the International Conference on Advances and New Challenges in Earthquake Engineering Research, Hong Kong Volume ATTENUATION FUNCTION OF GROUND MOTIONS FOR GUANGDONG REGION OF SOUTHERN CHINA WONG Yuk Lung 1 , ZHENG Sihu 2 , LIUJie 2 , KANG Ying 3 , TAM Cheuk Ming 4 , LEUNG Yin Kong 4 , ZHAO Xinquan 5 1 Department of Civil and Structural Engineering, The Hong Kong Polytechnic University, Hong Kong 2 Center for Analysis and Prediction, China Seismological Bureau, Beijing, 100036 3 Seismological Bureau of Guangdong Province, Guangzhou, 510070 4 Hong Kong Observatory, Hong Kong 5 Institute of Geological and Nuclear Science, Gracefield, Lower Hutt, New Zealand ABSTRACT We made use of the first ever set of horizontal-component digital seismic data of 44 earthquake events (M L = 2.5 to 5.1) from September 1999 to October 2000, recorded by 14 stations of the Guangdong Telemetered Network to determine the attenuation function of S-wave phases of ground motions for the Guangdong Region of southern China. It was found that the geometrical spreading function of the region could be best represented by a trilinear piecewise continuous function. At a distance less than 45 km from a seismic source, the geometrical spreading coefficient was 0.97. Between 45 and 100 km, the coefficient was nearly zero. Beyond 100 km, the coefficient was 0.5. The frequency-dependent Q was estimated to be Q = 481.5f°' 31 . We then evaluated the source spectra for each of the 44 events from the records of the YHK Station of the Hong Kong Observatory's seismic monitoring network, and the proposed attenuation model. It was found that the so-obtained source spectra derived from YHK Station were comparable to those derived from the stations of Guangdong Network. Hence, the proposed attenuation function was likely to be applicable for the Hong Kong region as well. INTRODUCTION In seismology, the analysis of attenuation characteristic of ground motions provides a better understanding on wave transmission inside the earth, and the seismic source parameters. In engineering applications, the attenuation relationships of S-wave phases of ground motions are of most interest as their amplitudes are approximately five times larger than the associated P-wave phases, causing most of the earthquake damages. Therefore, a quantification of the S-wave attenuation is necessary for seismic hazard analysis of a region. Traditionally, researchers tended to study the attenuation and hazard issues for seismically active regions. After the Newcastle Earthquake in 1989 which occurred in a region of low seisrnicity and caused significant damages valued at about 700 million Australian dollars (Brunsdon, 1990), earthquake hazard analysis of a region of low seismic risk but high consequence of economic losses
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Proceedings of the International Co
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vw:. PREFACE Dunng a time when eart
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OPENING ADDRESS By Prof. Yuchen Liu
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Vll scientific support in our call
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IX INTERNATIONAL ADVISORY COMMITTEE
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XI Engineering Seismology and Geote
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Xlll Progress in the Seismic Design
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XV Crustal Deformation Measurement
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Legal Impediments There are many im
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expectation of (i) expanding the fr
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10 Some applications of wireless te
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12 Smart Materials Smart materials,
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14 research and education in a mult
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19 On September 16, 1994, buildings
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21 Some people were injured while t
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23 tallest buildings in Hong Kong w
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25 Figure 12. Tsim Sha Tsui East an
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27 OTHER ONGOING WORKS Soil-pile-st
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29 Figure 18. The pounding experime
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31 ACKNOWLEDGMENTS The writers are
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35 Table 1. Records Used in the Dev
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37 Date 8/19/1976 10/5/1977 12/16/1
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39 (2) Here Y is the ground motion
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41 1 2 3 4567810 20 3040 SO 100 200
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43 of the resultant horizontal comp
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45 200 006 005 004 003 002 Rock, Mw
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47 en o_ KOCAELI DATA (Random Hor C
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Atkinson G.M., Boore D.M., Some Com
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52 BACKGROUND AND SCOPES In order t
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configurations of cylinder, and it
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l 56 X xT / ^ V^—Ê-^/i / X\ - yX
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58 59-74 (in Japanese) [7] ISHIKAWA
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60 accuracy and efficiency, have no
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62 f •c J — c. p «3 no Fig. 2
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64 VARIOUS TESTS AND DISSEMINATION
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66 response.. The post-earthquake i
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Page 87 and 88: 71 with the potential for self-diag
Page 89 and 90: 73 Semi-active Hydraulic (SHD) Cont
Page 91 and 92: 75 Table 1 Buildings currently unde
Page 93 and 94: 77 and the inside of the damper cyl
Page 95 and 96: 79 Figure 16. MR damper installatio
Page 97 and 98: 81 sensors. New algorithms must be
Page 99 and 100: 83 Kobon T. (1998). Mission and per
Page 101 and 102: Proceedings of the International Co
Page 103 and 104: 87 for a period range less than 3.0
Page 105 and 106: 89 tens or more than a hundred acce
Page 107 and 108: 91 In order to validate the conclus
Page 109 and 110: 93 Distance (km) """"--Âcc. (g) Ma
Page 111 and 112: 95 CONCLUSION In this paper the imp
Page 113: ENGINEERING SEISMOLOGY AND GEOTECHN
Page 116 and 117: 100 analyses. This paper reviews th
Page 118 and 119: 102 A comparison of spectral amplit
Page 120 and 121: 104 the high speed with which FFT c
Page 122 and 123: 106 8. Gold, B. and C.M. Rader (197
Page 124 and 125: 108 Displacement Curves", Dept. of
Page 126 and 127: I 000,000 100,000 Number of uniform
Page 128 and 129: Response and Fourier Spectra of Dig
Page 130 and 131: 114 10 3 10 2 r | I lll| I | I | I
Page 132 and 133: 116 analysis. Other techniques incl
Page 134 and 135: It has been found that G max applie
Page 136 and 137: 120 PALEOLIQUEFACTION STUDIES IN ME
Page 140 and 141: 124 has received more attention. In
Page 142 and 143: 126 and log A tQ (/) is the mean so
Page 144 and 145: 128 O 10 s Frequency (Hz) Frequency
Page 146 and 147: 130 geometrical coefficient is near
Page 148 and 149: 132 optimizing method in many engin
Page 150 and 151: 134 Type-2 Fig.5 Three dimensional
Page 152 and 153: 136 plane plane sliding x-z section
Page 157 and 158: 141 1. System Definition define sys
Page 159 and 160: 143 f«l-.J WJjfc >. « Relations -
Page 161 and 162: 145 DS-5 Response Simulation across
Page 163 and 164: 147 CM 1 CM 2 CM 3 CM-4 CM-5 CM-6 H
Page 167 and 168: 151 Number of Pixels (Frequency) Th
Page 169 and 170: 153 Red: possible impacted areas Gr
Page 171 and 172: 155 Low reliability -(water-reflect
Page 175 and 176: Modem or Router Dial-up ISP The Int
Page 177 and 178: from observed images Fig 5 shows th
Page 179 and 180: 163 Picked up building from image p
Page 183 and 184: 167 evaluated by Seed's approximate
Page 185 and 186: 169 R(z,N)is reached to 1 or more,
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174 defined target. Performance-bas
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176 (probability of being in or exc
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178 start to dominate the hazard at
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180 MAX STORY DUCTILITY vs NORM. ST
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185 Decision Making Support Tool' U
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189 31 Array Liujiaxia Reservoir Ar
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191 IV STATION YM kCED INTERVALS OF
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193 at different stations, the diff
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197 PROBLEMS AND CHALLENGES Earthqu
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199 Database s*n/ar_- ^ " Applicati
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201 o Fig. 7 VRML authoring - model
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SMART MATERIALS AND SMART STRUCTURE
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209 vector of measured control forc
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211 To examine the effect of the co
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213 from Fig. 2, we can get the res
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Proceedings of the Intel-national C
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217 where gjî = g(X fcTl , F^+ît
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219 3 360 Deg. Fault Normal (Jan. 1
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221 Earthquake Sylmar 90 Sylinar 90
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225 0.6965, and 0.7094 Hz, which ar
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227 Two displacement sensors are po
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229 14% to 45% (under El Centre ear
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233 g ^ w (4) Notice that the stabi
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235 modes. An energy drop will be o
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237 PPF controller. The second mode
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241 In order to determine the appar
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243 RESULTS AND DISCUSSIONS Figure
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245 100 150 200 250 300 Magnetic Fl
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249 WOLFE, MASRI, CAFFREY Synthetic
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251 WOLFE, MASRI, CAFFREY Transform
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253 WOLFE MASRI,CAFFREY in parallel
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STRUCTURAL ANALYSIS AND DESIGN
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258 separating the above three effe
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260 200 300 400 SHAKE Computed RSD^
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262 where H b is the building heigh
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264 6. ACKNOWLEDGEMENTS The work de
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266 The objectives of this paper pr
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268 The comparison between abovemen
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270 determine the span of the state
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the assumption of the bi-linear for
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274 There are several outstanding e
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276 buildings with different concre
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278 160,000 - 140,000 _^ d Concrete
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280 responded in a fairly similar m
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282 CONCLUSIONS In this paper, the
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284 Li B, Park, R. and Tanaka, H. (
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For simplicity, a linear distributi
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equation can be re- written as: 288
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290 DESIGN BASE SHEAR Equating the
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292 by using the computer program S
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294 mutation. Elitist strategy mean
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296 2.3 Premature Judgment and Comb
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298 (3) F 3 : De Jone's F 5 3 (Shek
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300 3.3 Test Conclusions From the t
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30; excitation. Also, the software
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304 concrete frames as documented i
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30€ NEURAL NETWORKS Development I
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308 ACKNOWLEDGEMENTS The research r
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310 In order to ensure the entire s
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312 Examples of Seismic Design In K
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314 earthquake load can be reduced
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Proceedings of the Intel national C
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319 broken. Therefore, joint elemen
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321 the highest probability to get
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Page 341 and 342:
325 DESIGN SPECIFICATIONS Overview
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327 Strength Degradation The streng
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I 329 file £dit Vww Select Constru
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333 (1) (2) Where f t and _/£ are
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335 JL dalt (10) Where Solution of
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337 Fig.9 Distribution of first pri
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341 DISPLACMENT-BASED NSF In this p
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343 Define the displacement of the
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345 EXAMPLE The nonlinear static an
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347 REFERENCE Code for seismic desi
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350 including Hong Kong are conside
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352 structural engineers. Although
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354 4) Structural characteristics R
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356 maintain economy of design but
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358 R C3&OC11 L8C34 USC3 •••
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363 DISPLACEMENT CALCULATION FOR GR
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365 As shown in the figure, a model
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367 history of a design earthquake
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371 reflects the structure's useful
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373 have a membership degree betwee
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375 of initialization of structure,
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377 REFERENCE Zadeh, L A (1965), "F
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.0,(r+l,,)] (0 + A (3) 383 -l.y)] (
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385 The first example is come from
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387 REFERENCES Leroueil, S. (2001).
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391 maximum friction force and ther
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393 the stiffness of the bracing an
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395 splacemen (m) Bared —Braced/D
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399 Figure 1: Two-surface Model Def
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401 time, one must integrate over t
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403 CONCLUSIONS In the previous sec
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407 Response Control by Magneto-Rhe
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409 s e a ooo j| soo y 0 c l83Hz ,5
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411 *fU O A 20 7 HA I , 2 4A .'.-%-
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415 Wind Velocity (t J Relative Dis
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417 Fig. 5 4ttractor (time lag=l) F
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419 concluded that the real time re
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422 (LQR/LQG), H M and the instanta
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424 damping ratio provided by the c
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426 by Eqn. 2.9 and Eqn. 2.12, resp
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428 Fig.5.4 shows the comparison of
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Innovation is driving control devic
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432 STRUCTURAL ENERGY DURING VIBRAT
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434 Equilibrium Price of Power With
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436 CONCLUSION The scope of this re
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438 The effectiveness of the seismi
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440 anti-symmetnc mode excited by t
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442 Base Isolation System The base
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444 each member along or adjacent t
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446 2 PROJECT PARTICIPANTS Concerni
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448 3.1.2 Investigations at Seyhan
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450 Fig. 4.2: principle drawing of
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452 no TMD — TMD with optimal tun
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454 In this paper, a stochastic opt
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456 The dynamical programming equat
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458 control strategy. Model reducti
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460 (AMDs) and the proposed control
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465 Specimen 1 Specimen 1 represent
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467 increased the beam moment stren
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469 3 4@8 ~T / C 4 #5 #3 stirrups 8
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473 Phase 2: The sliding of the bot
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475 4.2 Effect of Coefficient of Fr
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477 -ZETA=Q 05 -ZETA=010 -ZETA=015
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479 031 en 03 0029 P |Q 28 ~*—MR=
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482 stiffness or coefficient of vis
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484 solved for the Hamilton Jacobi-
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486 posed to be the accelerations o
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488 vlaxacccleiation [my O O O O
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490 INTRODUCTION In recent years, t
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492 Since earthquake motion has bee
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494 confirmed in the X direction. B
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496 yielding metallic dampers, and
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498 where the coefficients a m and
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500 modal damping ratio of 2% in ea
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502 CONCLUDING REMARKS The paper re
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504 semi-active and hybrid control
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506 Iiz2i(t)l
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508 defined as 114 - [ J* [•] 2 d
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Spencer, B.F., Jr. and Sain, M.K. (
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512 with the rapid success of seism
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Figure 3 summarizes the static push
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CONCLUSIONS 516 This paper presents
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518 1 OS h : 0 6 5 5 04 Transverse
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520 TABLE 1 REPRESENTATIVE MULTISTO
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522 obtained by simply averaging a
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524 levels of peak ground accelerat
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526 8 CONCLUSIONS This paper gives
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531 350.6m 142.7m .0130') i (468')
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533 cation corresponds to a node of
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535 listed separately. Vertical mod
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539 in which H = [H(t l ), H(t 2 ),
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541 identification results of struc
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543 history to be polluted. In the
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548 environment constraints and the
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550 where F is the fundamental matr
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552 drift ratio was determined as Y
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554 were observed in the vision-sys
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556 The most well-known Bayesian so
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558 achieved by the EKF estimates I
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560 0 2 4 5 3 10 12 14 16 18 20 0 2
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562 CONCLUSION In this study, the r
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564 Figure 1 - Prototype wireless s
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566 will vary from that of the ARX
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568 A 11 25" 11 25" 1 T 1 11 25* !
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570 CONCLUSION The realization of a
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572 the structural response and ret
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574 The ratios of base shear at dif
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576 SECTION A-A COLUMN DETAIL AT TO
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578 Stress Strain Fig. 6 Superelast
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580 Genetic Algorithm(GA) and the M
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582 IDENTIFICATION ALGORITHM State
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584 the simulated structural respon
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586 GA-MCF, the number of particles
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588 instrumentation to monitor and
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590 If we compare this peak value w
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592 2.3 Sampling rate Structural mo
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594 Any remote station that has the
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596 or receives environmental infor
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598 Comparisons of Proposed E-Monit
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600 LCD display Earthquake Warning
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605 Kishwaukee River Bridge consist
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607 the table, the monthly maximum
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609 3.2 L VDTData Analysis LVDT sen
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structural response energy with fre
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615 Table 1: Fundamental natural fr
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617 JUSTS rs s." WUUR. 4 20O2 IS 44
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1-1 INDEX OF CONTRIBUTORS Volumes I
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Ths OOO F X ^s dje foe return 01 ê
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