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Liquefaction-induced road embankment failures

机译:液化引起的路堤破坏

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The intensive and long-lasting seismic shaking during the 2011 great east Japan earthquake left enormous amounts of scars on the ground surfaces and inflicted damage to private houses, buildings and constructed infrastructure. Many of the ground failures were associated with subsurface soil liquefaction. Forensic field investigations were conducted at one of the illustrative sites with the help of field penetration tests. The site is a road embankment over a reclaimed soil deposit located at the foot of a steep cliff along the coast of Hitachinaka city. Road pavements were broken, subsided from portion to portion and failed to perform their traffic-bearing function. Upheavals were observed on the ground surface further from the foot of the road embankment, over which liquefied subsurface soil erupted, and a nearby seafood factory was damaged. It was evident from depth-wise profiles of penetration tests that slip failures had taken place involving part of the road embankment underlain by the liquefied, loose, reclaimed soil deposit. The effect of a soft reclaimed soil deposit bounded by a stiff steep cliff and an underlying stiff mudstone layer at the site is discussed.
机译:2011年东日本大地震期间发生的强烈而持久的地震震荡在地面上留下了大量的伤痕,并对私人住宅,建筑物和已建成的基础设施造成了破坏。许多地面破坏与地下土壤液化有关。在现场渗透测试的帮助下,在其中一个说明性地点进行了法医现场调查。该场地是位于Hitachinaka市沿海陡峭悬崖脚下的填筑土壤沉积物上的路堤。道路破损,从一个地方到另一个地方平移,无法履行其交通承载功能。在距路堤脚下较远的地面上观察到动荡,液化的地下土壤喷发,附近的海鲜工厂也遭到破坏。从渗透测试的深度剖面可以明显看出,滑倒已经发生,部分路堤被液化,疏松,开垦的土壤沉积物所覆盖。讨论了在该地点以坚硬的陡峭悬崖和下层坚硬的泥岩层为边界的软填土场的影响。

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