The broad geographic extent of the liquefaction over hundreds of miles was surprising to experienced engineers accustomed to seeing earthquake disaster sites, including the recent events in Chile and New Zealand.
"We've seen localized examples of soil 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 the research team.
"Entire structures were tilted and sinking into the sediments, even while they remained intact," Ashford said. "The shifts in soil destroyed water, sewer and gas pipelines, crippling the utilities and infrastructure these communities need to function. We saw some places that sank as much as 4 feet."
Some degree of soil liquefaction, in which saturated soils, particularly sand, gravel or fill, can lose much of their strength and flow during an earthquake, is common in most incidents, an OSU release said.
However, the length of the Japanese earthquake -- almost 5 minutes -- may require a reconsideration of the extent of liquefaction damage possible in similar situations, researchers said.
"With such a long-lasting earthquake, we saw how structures that might have been OK after 30 seconds just continued to sink and tilt as the shaking continued for several more minutes," Ashford said.
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