Effects of seepage flow on liquefaction resistance of uniform sand and gap-graded soil under undrained cyclic torsional shear

IF 3.3 2区 工程技术 Q2 ENGINEERING, GEOLOGICAL
Sanjei Chitravel , Masahide Otsubo , Reiko Kuwano
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引用次数: 0

Abstract

Internal erosion is the transportation of soil particles from within or beneath geotechnical structures, caused by seepage flow, that impacts the subsequent mechanical and hydraulic behaviour of the soil. However, it is difficult to predict the liquefaction resistance of eroded soil due to several factors related to the soil fabric. The present study investigates the impact of seepage flow on the undrained cyclic behaviour of two types of soil: uniform sand and gap-graded soil with a fines content of 20%, using a novel erosion hollow cylindrical torsion shear apparatus. From the results for the uniform sand, the soil fabric formed by moist tamping (MT) leads to higher liquefaction resistance than that formed by air-pluviation (AP). However, after applying seepage flow, the liquefaction resistance of the eroded MT specimens becomes even lower than that of the non-eroded AP specimen. Therefore, the liquefaction resistance of soil is expected to decrease due to the rearrangement of the initially stable coarse particles during seepage flow. On the other hand, the liquefaction resistance of the gap-graded soil tends to increase after the removal of fines as the number of stable contacts between the coarse particles is increased. Under these test conditions, the latter effect is found to be greater for the given gradation, leading to a slight increase in the liquefaction resistance of the tested gap-graded soil after internal erosion. Furthermore, the intergranular void ratio and small-strain shear modulus are seen to be well correlated with the liquefaction resistance of the tested soil.

不排水循环扭剪作用下渗流对均匀砂土和间隙级配土液化阻力的影响
内部侵蚀是指由渗流引起的土工结构内部或下方的土壤颗粒运输,影响土壤随后的机械和水力行为。然而,由于与土壤组构有关的几个因素,很难预测侵蚀土壤的抗液化性。本研究使用一种新型的侵蚀空心圆柱扭剪装置,研究了渗流对两种类型土壤(均匀砂和细粒含量为20%的间隙级配土壤)不排水循环行为的影响。从均匀砂土的结果来看,湿夯(MT)形成的土组比空气降水(AP)形成的土壤组具有更高的抗液化性。然而,在施加渗流后,受侵蚀的MT试样的抗液化能力甚至低于未受侵蚀的AP试样。因此,由于渗流过程中最初稳定的粗颗粒发生重排,预计土壤的抗液化能力会降低。另一方面,随着粗颗粒之间稳定接触的数量增加,在去除细颗粒后,间隙级配土壤的抗液化性往往会增加。在这些试验条件下,发现给定级配的后一种影响更大,导致内部侵蚀后测试间隙级配土壤的抗液化能力略有增加。此外,粒间孔隙比和小应变剪切模量与试验土壤的抗液化性密切相关。
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来源期刊
Soils and Foundations
Soils and Foundations 工程技术-地球科学综合
CiteScore
6.40
自引率
8.10%
发文量
99
审稿时长
5 months
期刊介绍: Soils and Foundations is one of the leading journals in the field of soil mechanics and geotechnical engineering. It is the official journal of the Japanese Geotechnical Society (JGS)., The journal publishes a variety of original research paper, technical reports, technical notes, as well as the state-of-the-art reports upon invitation by the Editor, in the fields of soil and rock mechanics, geotechnical engineering, and environmental geotechnics. Since the publication of Volume 1, No.1 issue in June 1960, Soils and Foundations will celebrate the 60th anniversary in the year of 2020. Soils and Foundations welcomes theoretical as well as practical work associated with the aforementioned field(s). Case studies that describe the original and interdisciplinary work applicable to geotechnical engineering are particularly encouraged. Discussions to each of the published articles are also welcomed in order to provide an avenue in which opinions of peers may be fed back or exchanged. In providing latest expertise on a specific topic, one issue out of six per year on average was allocated to include selected papers from the International Symposia which were held in Japan as well as overseas.
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