Abstract

Research Article| August 01, 2007 Determination of Organic Soil Permeability Using The Piezocone Dissipation Test Stefan. VAN BAARS; Stefan. VAN BAARS 1Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands Search for other works by this author on: GSW Google Scholar Henke C. VAN DE GRAAF Henke C. VAN DE GRAAF 2Lankelma Geotechniek-Zuid, P.O. Box 38, 5688 ZG Oirschot, The Netherlands Search for other works by this author on: GSW Google Scholar Author and Article Information Stefan. VAN BAARS 1Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands Henke C. VAN DE GRAAF 2Lankelma Geotechniek-Zuid, P.O. Box 38, 5688 ZG Oirschot, The Netherlands Publisher: Association of Environmental & Engineering Geologists First Online: 09 Mar 2017 Online ISSN: 1558-9161 Print ISSN: 1078-7275 © 2007 Association of Engineering Geologists Environmental & Engineering Geoscience (2007) 13 (3): 197–203. https://doi.org/10.2113/gseegeosci.13.3.197 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Stefan. VAN BAARS, Henke C. VAN DE GRAAF; Determination of Organic Soil Permeability Using The Piezocone Dissipation Test. Environmental & Engineering Geoscience 2007;; 13 (3): 197–203. doi: https://doi.org/10.2113/gseegeosci.13.3.197 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEnvironmental & Engineering Geoscience Search Advanced Search Abstract Among other parameters, the hydraulic conductivity needed to predict time-dependant settlement can be estimated using a piezocone dissipation test. This test is commonly used along with cone penetration tests, soil borings, and laboratory tests in foundation site investigations. The piezocone dissipation test is based on the fact that the rate of decay of the large excess pore water pressures generated during penetration of the piezocone through saturated clays and silts depends on the hydraulic conductivity of the material. However, interpretation of the dissipation curve is often problematic, as existing methods of analysis assume a continuous decrease of pore pressure with time, whereas actual dissipation curves often exhibit nonstandard behavior, the interpretation of which is more complex. This article presents a new method of interpretation that can be used to estimate the hydraulic conductivity regardless of the shape of the dissipation curve. Examples of results using the new analysis method are compared with results obtained using laboratory odometer testing. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.