Model tests of reinforced soil retaining sand walls by shaking table test

IF 1.827 Q2 Earth and Planetary Sciences Arabian Journal of Geosciences Pub Date : 2024-05-01 DOI:10.1007/s12517-024-11965-w
Md. Zakir Hossain, Ripon Hore, Mehedi A. Ansary
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Abstract

This research investigates the seismic response of sand-made wrap-faced retaining walls using a shaking table, focusing on the impact of varying relative densities and frequencies on the dynamic characteristics of the walls. Two types of sand have been used to prepare retaining wall model for shake table testing. They are “Local” sand and “Sylhet” sand. A 2 m × 2 m computer-controlled servo-hydraulic single degree of freedom shaking table facility in geotechnical laboratory of Bangladesh University of Engineering and Technology (BUET) has been used to test the model under sinusoidal loading. Here, different kinds of combination of seismic waves of different frequencies are selected to apply on different densities wrap-faced wall model in order to observe their dynamic characteristics. The relative densities of Sylhet sand are chosen 48%, 64%, and 80% for preparing the model wall. On the other hand, 48%, 64%, and 80% are selected for preparing Local sand model. Portable traveling pluviator (PTP) developed by (Hossain and Ansary, Innov Infrastruct Solut 3:53, 2018) has been used here to construct the uniform wrap-faced retaining wall model. Tests are performed under three different surcharge pressures like 0.7 kPa, 1.12 kPa, and 1.72 kPa. Sinusoidal tests are implemented for three base accelerations (0.1 g, 0.15 g, and 0.2 g) and for eight different frequencies (1 Hz, 2 Hz, 3 Hz, 5 Hz, 8 Hz, 10 Hz, 12 Hz, and 15 Hz). In the end, from these test results, it has been observed that acceleration amplification is inversely proportional to relative density. Further, acceleration amplifications are increased with the rise of frequencies. On the other hand, face displacement has been decreased with the increase of the relative density and frequency at same normalized elevation. The test results have been compared with (Krishna and Latha, Geosynth Int 14:355–364, 2007), although they used poorly graded sand and different scaling factor of the retaining wall model. It has been also noticed that the Sylhet sand retaining wall shows more acceleration amplification during sinusoidal loading than the Local sand retaining wall. In this research, the impact of different kinds of relative densities and frequencies on wrap-faced retaining wall model under sinusoidal testing has been observed.

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通过振动台试验进行加筋土挡沙墙模型试验
本研究利用振动台研究了砂制包面挡土墙的地震响应,重点研究了不同相对密度和频率对挡土墙动态特性的影响。为进行振动台测试,我们使用了两种类型的沙子来制作挡土墙模型。它们是 "本地 "砂和 "锡尔赫特 "砂。孟加拉国工程技术大学(BUET)岩土实验室的 2 m × 2 m 计算机控制伺服液压单自由度振动台用于在正弦荷载下测试模型。在此,我们选择了不同频率的地震波组合,应用于不同密度的包面墙模型,以观察其动态特性。西尔赫特砂的相对密度分别为 48%、64% 和 80%,用于制作模型墙。另一方面,选择 48%、64% 和 80% 制备本地砂模型。这里使用了(Hossain 和 Ansary,Innov Infrastruct Solut 3:53,2018)开发的便携式行走犁(PTP)来建造均匀的包面挡土墙模型。在 0.7 kPa、1.12 kPa 和 1.72 kPa 等三种不同附加压力下进行了测试。正弦试验针对三种基底加速度(0.1 g、0.15 g 和 0.2 g)和八种不同频率(1 Hz、2 Hz、3 Hz、5 Hz、8 Hz、10 Hz、12 Hz 和 15 Hz)进行。最后,从这些测试结果中可以看出,加速度放大与相对密度成反比。此外,加速度放大率随着频率的升高而增大。另一方面,在相同归一化标高下,面位移随着相对密度和频率的增加而减小。测试结果与(Krishna 和 Latha,Geosynth Int 14:355-364,2007 年)进行了比较,尽管他们使用了级配较差的砂和不同的挡土墙模型缩放因子。研究还注意到,在正弦加载过程中,锡尔赫特砂挡土墙比当地砂挡土墙显示出更大的加速度放大效应。本研究观察了正弦试验下不同种类的相对密度和频率对包面挡土墙模型的影响。
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来源期刊
Arabian Journal of Geosciences
Arabian Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
自引率
0.00%
发文量
1587
审稿时长
6.7 months
期刊介绍: The Arabian Journal of Geosciences is the official journal of the Saudi Society for Geosciences and publishes peer-reviewed original and review articles on the entire range of Earth Science themes, focused on, but not limited to, those that have regional significance to the Middle East and the Euro-Mediterranean Zone. Key topics therefore include; geology, hydrogeology, earth system science, petroleum sciences, geophysics, seismology and crustal structures, tectonics, sedimentology, palaeontology, metamorphic and igneous petrology, natural hazards, environmental sciences and sustainable development, geoarchaeology, geomorphology, paleo-environment studies, oceanography, atmospheric sciences, GIS and remote sensing, geodesy, mineralogy, volcanology, geochemistry and metallogenesis.
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