@ ŒfÚŽGŽi˜ajF “y–ØŠw‰ï”NŽŸŠwpu‰‰‰ïu‰‰ŠT—vW‘æ3•” VolF 48Šª ”NF 1993”N •ÅF 20-21•Å ’˜ŽÒi˜ajF FATEMI AGHDA@S.M.C—é–Ø@“Ö–¤C–k‰€@–Fl ƒ^ƒCƒgƒ‹i˜ajF ”—ʉ»‚É‚æ‚é‰t󉻃|ƒeƒ“ƒVƒƒƒ‹‚̃}ƒCƒNƒƒ][ƒjƒ“ƒO ´˜^i˜ajF
- ƒL[ƒ[ƒhi˜ajF ƒ}ƒCƒNƒƒ][ƒjƒ“ƒOC‰tó‰»C”—ʉ»CŽ¿“Iƒf[ƒ^ ŒfÚŽGŽi‰pjF PROCEEDINGS OF ANNUAL CONFERENCE OF THE JAPAN SOCIETY OF CIVIL ENGINEERS ’˜ŽÒi‰pjF Fatemi Aghda Seyed Mahmad,Suzuki Atsumi,Kitazono Yoshito ƒ^ƒCƒgƒ‹i‰pjF MICROZONING OF LIQUEFACTION POTENTIAL BASED ON THE QUANTIFICATION OF QUALITATIVE DATA PROCESSING ´˜^i‰pjF
A using method in this work,is a method based on the application of the quantification theory,method II(Hayashi 1952),which is a mathematical-statistical method in order to convert qualitative data into quantificative relations.The seismic and geotechnical items are considered to express the basic characteristics of liquefaction potential of the study area.Based on the analysis,factors of type of soil,Dso,water table,and intensity incerments have larger range among others,and show the high degree of contribution to liquefaction susceptibility. ƒL[ƒ[ƒhi‰pjF Microzonation,Liquefaction,quantification,qualitative data ‹LŽ–‹æ•ªF - ‹æ•ª @@@ˆÏˆõ‰ï˜_•¶W