Seismically Induced Delayed-Landslides in Homogeneous Cohesive Slopes and Embankments (NEES-2007-0412)

<p><strong>Title:</strong> Seismically Induced Delayed-Landslides in Homogeneous Cohesive Slopes and Embankments (NEES-2007-0412)</p> <p><strong>Year Of Curation: </strong>2011</p> <p><strong>Description: </strong>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.</p> <p><strong>Award: </strong>http://www.nsf.gov/awardsearch/showAward?AWD_ID=0134370</p> <p><strong>PIs & CoPIs: </strong>Joseph Wartman</p> <p><strong>Dates: </strong>September 05, 2007 - December 12, 2008</p> <p><strong>Organizations: </strong>Drexel University, PA, United States</p> <p><strong>Facilities: </strong>Drexel University, PA, United States,Rensselaer Polytechnic Institute, Troy, NY, United States</p> <p><strong>Sponsor: </strong>NSF - 0134370</p> <p><strong>Keywords: </strong>Landslide, Clay, Pore Pressure, Centrifuge</p> <p><strong>Publications: </strong>"Post-seismic Displacement Response in Normally Consolidated Clay Slopes"</p> <nb:citations></nb:citations>