PERILAKU REGANGAN-SIKLUS PEMBEBANAN TANAH PASIR PRAMBANAN DENGAN UJI TRIAKSIAL SIKLIS

The earthquake on Yogyakarta on May 27, 2006 caused extensive damage, one of which was damage to the �iwa temple at Prambanan complex temple. Yogyakarta as a city that had the potential of an earthquake causing the cyclic behavior of silty sand soil at the site kelanauan �iwa Temple became importa...

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Bibliographic Details
Main Authors: , Noor Rahmi, , Prof. Dr. Ir. Kabul Basah Suryolelono, Dip.H.E., DEA.
Format: Thesis
Published: [Yogyakarta] : Universitas Gadjah Mada 2011
Subjects:
ETD
Description
Summary:The earthquake on Yogyakarta on May 27, 2006 caused extensive damage, one of which was damage to the �iwa temple at Prambanan complex temple. Yogyakarta as a city that had the potential of an earthquake causing the cyclic behavior of silty sand soil at the site kelanauan �iwa Temple became important because of the potential for larger earthquakes could be occurred and threatened the stability of the structure of the temple. This study aimed to determine the effects of soil density and the PGA (Peak Ground Acceleration) of the cyclic behavior of silty sand soil on which the temple stood. The silty sand soil which had been sampled was the soil of �iwa ground around the temple and taken at a depth of 2-3 m from ground. Disturbed soil samples were tested using cyclic triaxial apparatus. Tests performed with two parameter variation of soil density variations (medium and dense) and variations on the ratio of cyclic stress, SR (for the case of an earthquake presented by the maximum ground acceleration, amax or PGA). The results showed that soil strain that occurred increased with density and a lower value of SR(Stress Ratio). Soil density factor had more influence than the SR used in cyclic loading. Soil samples did not showed the soil failure which caused by liquefaction and cyclic mobility. Different soil density on the surface and bottom of Temple would cause differences in deformation behaviour that occurred during earthquake loading. For amax = 0,2g, soil on the bottom of �iwa Temple showed relatively small deformation increment, for soil on the surface which had looser density would have bigger deformation. For amax = 0,3g and 0,4g loading, soil experienced great deformation increment, this was quite dangerous because of rapid increase in deformation colud cause damage to structures on the land.