2000
DOI: 10.1061/(asce)1090-0241(2000)126:12(1184)
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1907 Static Liquefaction Flow Failure of the North Dike of Wachusett Dam

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Cited by 86 publications
(22 citation statements)
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“…There are cases where instability or static liquefaction occurred under essentially drained conditions. In recent re-analysis of the Wachusett dam failure in 1907, Olson et al (2000) concluded that the failure was mainly triggered by static liquefaction that occurred under completely drained conditions. Through laboratory model tests, Eckersley (1990) observed that the pore water pressure increase in the gentle granular soil slope was a result of, rather than the cause of, flowslide.…”
Section: Other Concernsmentioning
confidence: 99%
“…There are cases where instability or static liquefaction occurred under essentially drained conditions. In recent re-analysis of the Wachusett dam failure in 1907, Olson et al (2000) concluded that the failure was mainly triggered by static liquefaction that occurred under completely drained conditions. Through laboratory model tests, Eckersley (1990) observed that the pore water pressure increase in the gentle granular soil slope was a result of, rather than the cause of, flowslide.…”
Section: Other Concernsmentioning
confidence: 99%
“…It implies that pre-failure instability can occur under both drained and undrained conditions and the necessary conditions for undrained and drained instability are the same. This explains why liquefaction under complete drained conditions had ocurred in the Wachuset dam failure (Olson et al, 2000); that is, because a stress path led the stress state into the zone of potential instability. Such a path can be applied to both loose and dense sand.…”
Section: Stress Ratiomentioning
confidence: 99%
“…However, there are cases where instability has occurred under essentially drained conditions. For example, in the re-analysis of the Wachusett Dam failure in 1907, Olson et al (2000) concluded that the failure was triggered mainly by static liquefaction that occurred under completely drained conditions. Through laboratory model tests, Eckersley (1990) observed that the pore water pressure increase in the gentle granular soil slope was a result, rather than the cause, of flow slide.…”
Section: Introductionmentioning
confidence: 99%
“…Liquefaction may occur under static and seismic loading. For instance, slope failure at hill side and embankment due to heavy rain or dam [1] and tailing disposal failure [2] for non-cyclic loading are also liquefaction, which is termed as static liquefaction. From the experiences of past earthquakes, it is found that sandy deposits which contain significant amount of fine-grains (silty sands, clayey sands) and/or gravel liquefy during earthquakes and cause lateral spreading [3][4][5].…”
Section: Introductionmentioning
confidence: 99%