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Thursday, February 28, 2013

'Liquefaction' Key To Much Of Japanese Earthquake

The findings also raise questions about whether existing building codes and technology technologies are adequately accounting for this phenomenon in other compromising locations, which in the U.S. include Portland, Ore., parts of the Willamette Valley and other areas of Oregon, working capital and California.
A preliminary report about some of the alter in Japan has just been concluded by the Geotechnical original Events Reconnaissance, or GEER advance team, in work supported by the National Science Foundation.
The broad geographic point of the liquefaction everyplace hundreds of miles was daunting to experienced engineers who are accustomed to seeing disaster sites, including the recent earthquakes in Chile and New Zealand.
Weve seen localized examples of solid ground liquefaction as extreme as this before, but the distance and extent of damage in Japan were unusually severe, said Scott Ashford, a professor of geotechnical engineering at Oregon State University and a member of this research team.
Entire structures were tilted and sinking into the sediments, yet while they remained intact, Ashford said. The shifts in change destroyed water, sewer and triggerman pipelines, crippling the utilities and infrastructure these communities need to function. We sawing machine some places that sank as much as four feet.

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Some degree of soil liquefaction is common in al approximately any major earthquake. Its a phenomenon in which saturated soils, particularly recent sediments, sand, gravel or fill, stool lose much of their strength and flow during an earthquake. This can allow structures to shift or sink and significantly explode the structural damage produced by the shaking itself.
But most earthquakes are much shorter than the recent event in Japan, Ashford said. The aloofness of the Japanese earthquake, as much as five minutes, may force researchers to reconsider the extent of liquefaction damage possible in situations such as this.
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