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Simulation of dynamic compaction processes in saturated silty soils

  • SUNY Buffalo
  • University of Southern California

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

1 Scopus citations

Abstract

Dynamic compaction (DC) is a widely used ground improvement technique for densification of loose granular materials. Densification of treated deposits is achieved through high-energy impacts to ground surface. For saturated deposits, soil skeleton deformation and intergrain slippages, due to impact, cause an increase in pore water pressure leading to local liquefaction around the impact zone. In highly pervious sands, this induced pore pressure dissipates rapidly, concurrently reducing void ratio and increasing soil density. Supplementing saturated low permeable non-plastic silty deposits with drainage provisions such as wick drains improve the efficiency of DC to densify such soils and improve their resistance to liquefaction, load bearing, and settlement characteristics. A numerical simulation model has been developed to analyze the ground response and densification of saturated non-plastic silty soils during DC. Visualization tools have been developed to view and analyze changes in pore pressures and density profiles in the vicinity of the impact zone during DC processes. The simulation model and visualization tools have been used in developing design charts. Theses tools are expected to advance the use of DC for liquefaction mitigation in silty soils. Copyright ASCE 2006.

Original languageEnglish
Title of host publicationGeoCongress 2006
Subtitle of host publicationGeotechnical Engineering in the Information Technology Age
Pages284
Number of pages1
DOIs
StatePublished - 2006
EventGeoCongress 2006 - Atlanta, GA, United States
Duration: Feb 26 2006Mar 1 2006

Publication series

NameGeoCongress 2006: Geotechnical Engineering in the Information Technology Age
Volume2006

Conference

ConferenceGeoCongress 2006
Country/TerritoryUnited States
CityAtlanta, GA
Period02/26/0603/1/06

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