COMPARING THE EFFECTS OF FLUID SCALING ONLIQUEFACTION IN GEOTECHNICAL CENTRIFUGE

Publish Year: 1403
نوع سند: مقاله کنفرانسی
زبان: English
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SEE09_101

تاریخ نمایه سازی: 10 آبان 1403

Abstract:

In modeling of dynamic problems such as liquefaction in centrifuge, there are still manydiscrepancies in viscosity scaling among researchers due to the amount of effect of this scaling onother parameters like subsidence and dissipation and difficulties of model preparation. This paper aimsto shed light on the necessity of scaling the viscosity in centrifuge physical modeling, especially inproblems related to earthquakes, permeability, and subsidence. In this study, two tests were conductedon saturated model ground with water and viscous fluid-saturated (Carboxy methylcellulose and waterwhich had ۴۰ times more viscous than water) conditions. In addition, two shakes were imposed oneach model for assessing the after-shake impacts on re-liquefaction and subsidence. According to theresults, using water as a saturating fluid (CMC) can cause about ۳۵% more subsidence in ۱st shakedue to the diluted fluid which leads to inaccurate outcomes. In addition, the evident difference in thedissipation rate of pore pressure can lead to imprecise outcomes in diverse issues such asre-liquefaction.

Authors

Shayan Zare Bidaki

M.Sc. Graduate of Geotechnical Engineering, School of Civil Engineering, College of Engineering,University of Tehran, Tehran, Iran,

Abbas Ghalandarzade

Professor, School of Civil Engineering, College of Engineering, University of Tehran, Tehran, Iran

Sobhan Zamani Amirzakarya

Ph.D. Student of Earthquake Engineering, Earthquake Engineering, Faculty of Civil and EnvironmentalEngineering, Tarbiat Modares University, Tehran, Iran

Sina Ghalandarzade

M.Sc. Student of Geotechnical Engineering, School of Civil Engineering, Iran University of Science andTechnology, Tehran, Iran

Mohammad Shirazi

M.Sc. Student of Geotechnical Engineering, School of Civil Engineering, College of Engineering,University of Tehran, Tehran, Iran,