印尼日惹伊莫吉里遗址土壤液化的实证分析

L. Z. Mase
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引用次数: 1

摘要

在日惹特别省的南部发生了6.3兆瓦级的强烈地震,后来被称为日惹地震。地震对建筑物和公共设施造成了巨大的破坏,并引发了被称为液化的地面破坏现象。采用常规方法对地震中液化破坏程度较高的伊莫吉里遗址调查数据进行了液化严重程度的实证分析。在分析中还实现了0.3 ~ 0.4g的峰值地面加速度。结果表明,调查场地以沙质土为主。Imogiri遗址的沙质土壤在曹子地震期间被归类为可液化层,并且可能在浅深度液化。总的来说,这项研究可以警告人们在未来发生更强地震时土壤液化的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
THE EMPIRICAL ANALYSIS OF SOIL LIQUEFACTION IN IMOGIRI SITE, YOGYAKARTA, INDONESIA
A strong earthquake with magnitude of 6.3 Mw, which was later known as the JogjaEarthquake, occurred in the southern part of Yogyakarta Special Province. The earthquakehad resulted in the huge damage to the buildings, public facilities as well as triggering theground failure phenomenon, which was known as liquefaction. An empirical analysis usingthe conventional method was performed to investigate the liquefaction severity for the siteinvestigation data in Imogiri, a site with the high-level of the liquefaction damage duringthe earthquake. The peak ground accelerations varied to 0.3 to 0.4g are also implemented inthe analysis. The results show that the investigated site is dominated by sandy soils. Thesandy soil in Imogiri site is categorised as the liquefiable layer during the Jogja Earthquakeand potentially to liquefy on shallow depth. In general, this study could warn the people forthe impact of soil liquefaction if the stronger earthquake happens in the future.
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