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Damage Patterns of River Embankments Due to the 2011 Off Soils and Foundations 2012;52(5):890–909 The Japanese Geotechnical Society Soils and Foundations www.sciencedirect.com journal homepage: www.elsevier.com/locate/sandf Damage patterns of river embankments due to the 2011 off the Pacific Coast of Tohoku Earthquake and a numerical modeling of the deformation of river embankments with a clayey subsoil layer F. Okaa,n, P. Tsaia, S. Kimotoa, R. Katob aDepartment of Civil & Earth Resources Engineering, Kyoto University, Japan bNikken Sekkei Civil Engineering Ltd., Osaka, Japan Received 3 February 2012; received in revised form 25 July 2012; accepted 1 September 2012 Available online 11 December 2012 Abstract Due to the 2011 off the Pacific Coast of Tohoku Earthquake, which had a magnitude of 9.0, many soil-made infrastructures, such as river dikes, road embankments, railway foundations and coastal dikes, were damaged. The river dikes and their related structures were damaged at 2115 sites throughout the Tohoku and Kanto areas, including Iwate, Miyagi, Fukushima, Ibaraki and Saitama Prefectures, as well as the Tokyo Metropolitan District. In the first part of the present paper, the main patterns of the damaged river embankments are presented and reviewed based on the in situ research by the authors, MLIT (Ministry of Land, Infrastructure, Transport and Tourism) and JICE (Japan Institute of Construction Engineering). The main causes of the damage were (1) liquefaction of the foundation ground, (2) liquefaction of the soil in the river embankments due to the water-saturated region above the ground level, and (3) the long duration of the earthquake, the enormity of fault zone and the magnitude of the quake. In the second part of the paper, we analyze model river embankments on a foundation ground with various soil profiles, including a clayey soil layer and various ground water tables, using a dynamic liquefaction analysis method. From the analysis results, we find the effects of the soil profiles and the duration time of the earthquake motion on the deformation behavior of the river embankments. The results are consistent with those of the investigation of the features of the deformation and the failure of the embankments due to the 2011 off the Pacific Coast of Tohoku Earthquake. & 2012 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V. All rights reserved. Keywords: The 2011 off the Pacific Coast of Tohoku Earthquake; River embankment; Coupled liquefaction analysis; Elasto-plasticity; Elasto- viscoplasticity/D7/E8/E13 1. Introduction dikes, road embankments, railway foundations and coastal dikes. Due to the very high strength of this earthquake, The 2011 off the Pacific Coast of Tohoku Earthquake which had a magnitude of 9.0, many soil-made infrastruc- damaged many soil-made infrastructures, such as river tures, such as river dikes, road embankments, railway foundations and coastal dikes, were damaged. The river nCorresponding author. dikes and their related structures were damaged at 2115 E-mail address: [email protected] (F. Oka). sites over the Tohoku and Kanto areas, including Iwate, Peer review under responsibility of The Japanese Geotechnical Society. Miyagi, Fukushima, Ibaraki and Saitama Prefectures, as well as the Tokyo Metropolitan District. In the first part of the present paper, the main patterns of the damaged river embankments are presented and reviewed based on in situ 0038-0806 & 2012 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V. All rights reserved. http://dx.doi.org/10.1016/j.sandf.2012.11.010 F. Oka et al. / Soils and Foundations 52 (2012) 890–909 891 research carried out by the authors, MLIT (Ministry of 2. Damage to river embankments and river structures Land, Infrastructure, Transport and Tourism) and JICE (Japan Institute of Construction Engineering (JICE), River embankments were damaged due to the earth- 2011). quake in both the Tohoku and Kanto districts. The damage was due tone or a combination of the A summary of the damage to river embankments and following: liquefaction of the foundation ground, liquefac- river structures due to the 2011 off the Pacific Coast of tion of the soil in the river embankments since the water- Tohoku Earthquake follows: saturated region was above ground level, and the long duration of this huge earthquake, over such a huge area. 1. The number of damaged river embankments and river The damage and failure of the coastal dikes due to structures is 1195 under the jurisdiction of the Tohoku overflow and erosion from the tsunami is not within the Regional Development Bureau of MLIT. A total of 773 scope of the present study. In the second part of the paper, river embankments were damaged, with 29 of them in we analyze model river embankments on a foundation urgent need of restoration. The rivers are the Mabuchi ground with various soil profiles, including a clayey soil River (Aomori Prefecture), the Kitakami River (Iwate layer and various ground water tables, using a dynamic and Miyagi Prefectures), the Eai River, the Naruse liquefaction analysis method. From the analysis results, River, the Yoshida River, the Natori River and the we find the effects of the soil profiles and the duration time Abukuma River (Miyagi Prefecture). of the earthquake motion on the deformation behavior of 2. River embankments were damaged at 611 sites along the river embankments. The results are consistent with the 146 rivers under the jurisdiction of Miyagi Prefec- those of the investigation of the features of the deforma- ture, including the Hasama River, the Nanakita River tion and the failure of the embankments due to the 2011 and the Sunaoshi River, and river structures were off the Pacific Coast of Tohoku Earthquake. damaged at 25 sites along 21 rivers. Akita Iwate Kitakami R Eai R Tajiri Kitakami Furukawa Naruse R Shinden Yamagata Miyagi Kozuka Yoshida R Yamasaki Nakashimo Iwanuma Heavily damaged embankments Kakuda K-NET KiK-NET Abukuma R NILIM Seismometer Fig. 1. Distributions of the heavily damaged river embankments and the earthquake motion observation stations (National Research Institute for Earth Science and Disaster Prevention, MLIT), webmapc of MLIT is used in this figure. 892 F. Oka et al. / Soils and Foundations 52 (2012) 890–909 3. River embankments and river structures were damaged embankments of the Nakagawa River were damaged. at 210 sites in Fukushima Prefecture. 8. In Tokyo, sand boils occurred on the river bed of the 4. Under the jurisdiction of the Kanto Regional Develop- Arakawa River. ment Bureau of MLIT, river embankments and related river structures were damaged at 939 sites, with 55 heavily damaged embankments, 149 medium-level dam- In the Tohoku District (Aomori, Iwate, Miyagi and aged embankments and 735 minimal-level damaged Fukushima Prefectures), many river embankments were embankments. damaged due to the earthquake. River basins in the 5. In Ibaraki Prefecture, embankments were damaged at Tohoku District include the Mabuchi River Basin, the 106 sites under the jurisdiction of Ibaraki Prefecture, Kitakami River Basin, the Naruse River Basin, the Natori while river embankments under the control of the River Basin and the Abukuma River Basin. In the Tohoku Kanto Regional Development Bureau of MLIT were District, embankments were damaged at 1179 sites. From damaged at 343 sites along the embankments of the the report by JICE (2011), the patterns of the damage Tone River, Kasumigaura Lake, the Kuji River, the consisted of failures and/or washouts (25 sites), cracks (565 Naka River, the Hinuma River, a 2.7 m settlement of a sites), lateral flows (90 sites), settlements (117 sites), tributary of the Naka River and the Shin Tone River in damage to revetments (196 sites), sluice gates, etc. (81) Inajiki City. and others (105). 6. In Chiba Prefecture, the right embankments of the Tone Fig. 1 shows the main damaged sites in the northern part River were heavily damaged and the left embankments of Miyagi Prefecture and the measured accelerations at of the Edo River were damaged. several points on the ground surface; K-net (Furukawa: 7. In Saitama Prefecture, the right embankment of the Edo NS¼444, EW¼571 gal), Kitami: NS¼372, EW¼294 gal), River was damaged in Satte City, while about 50 KiK-net (Tajiri: NS¼247, EW¼263 gal), etc. D-1 Settlement Heaving Settlement of Crown D-2 Longitudinal cracks Lateral expansion of toe of the bank D-3 Settlement of the top of the shoulder and the crown Lateral expansion of the toe of the bank D4D-4 Division of the bank due to cracks Boiled Lateral expansion of the sand toe of the bank and the lateral movement of the slope Fig. 2. Typical damage and failure patterns of river embankments. F. Oka et al. / Soils and Foundations 52 (2012) 890–909 893 The damage can be largely attributed to the liquefaction of 2012). As for the liquefaction of the water-saturated soil in the foundation ground, the liquefaction of the water- the river embankments above ground level, it is possible that saturated soil in the river embankments above the ground the damage was caused by the subsidence of the river level or overflow and erosion due to the tsunami (Oka et al., embankments to levels below the water table due to the consolidation of the soft clay foundation, and the high level of water in the river embankments due to the hydraulic conditions. According to the Tohoku Regional Development Type A Bureau of MLIT (2011), failures accompanied by the observation of sand boils and a high level of water were Water table reported for the following river dikes: the right embankment Sand of the downstream of the Abukuma River in the Edano District, the left embankment of the downstream of the Abukuma River in the Noda District, the left embankment of the Eai River in the Uetani District (14.0 km–14.6 km), Type B Sand the right embankment of the Eai River in the Nakajima Otsu District (14.0 kmþ43 m–14.6 kmþ43), the right embankment of the Eai River in the Fukunuma District Water table Clay (26.6–26.8 km), and the left embankment of the upstream of the Eai River in the Fuchishiri District (27.6 km), among others.
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