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Seismically Induced Delayed-Landslides in Homogeneous Cohesive Slopes and Embankments
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Curation progress:

This project was originally curated in 2009 and enhanced in 2010. Metadata were reviewed and if necessary corrected, visualization files were added. Additional documentation if missing was supplemented. This project may contain files that were not contributed by the original research team during their project.

Complete - 08/31/2011

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PI(s): , Joseph Wartman
Dates: September 05, 2007 - December 12, 2008
Facility: Drexel University, PA, United States
Rensselaer Polytechnic Institute, Troy, NY, United States
Organization(s): Drexel University, PA, United States
Description: Project is designed to track the pore pressure generation/dissipation as a function of varying shaking events. These pore pressure regimes are studied for their long term (multiple hours/days) contribution to instability in homogeneous normally consolidated clay slopes.
Website(s): NEES@Renssleaer Project Page (view)
Group Space: Project:Seismically Induced Delayed-Landslides in Homogeneous Cohesive Slopes and Embankments
Report on Data Status: View Report
Equipment: View Details
Tools: inDEED
Nicholas Malasavage, "Post-seismic Displacement Response in Normally Consolidated Clay Slopes" (view)
No files available
Tags (keywords):
  1. Landslide
  2. Clay
  3. Pore Pressure
  4. Centrifuge
Data Re-use Status: This Project does not reuse data from other projects.