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Earthquake-Induced Liquefaction Near Lake Amatitlan, Guatemala
An analysis of data gathered from a field survey, including bore hole cores, and from laboratory measurement of soil particles, penetration resistance and other parameters, leads to the development of a soil profile and the determination of conditions which caused the soil liquefaction resulting from the earthquake motion. Field data are very consistent with experimental-analytical theory. Boundary conditions between liquefaction and non-liquefaction zones are identified and correlated with physical conditions of partical size, water content, etc.
Earthquake-Induced Liquefaction Near Lake Amatitlan, Guatemala
An analysis of data gathered from a field survey, including bore hole cores, and from laboratory measurement of soil particles, penetration resistance and other parameters, leads to the development of a soil profile and the determination of conditions which caused the soil liquefaction resulting from the earthquake motion. Field data are very consistent with experimental-analytical theory. Boundary conditions between liquefaction and non-liquefaction zones are identified and correlated with physical conditions of partical size, water content, etc.
Earthquake-Induced Liquefaction Near Lake Amatitlan, Guatemala
H. B. Seed (Autor:in) / I. Arango (Autor:in) / C. K. Chan (Autor:in) / A. Gomez-Masso (Autor:in) / R. G. Ascoli (Autor:in)
1980
42 pages
Report
Keine Angabe
Englisch
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