Results 91 to 100 of about 1,100 (141)

Study on Mechanical Properties of Permeable Polymer Treated Loess. [PDF]

open access: yesMaterials (Basel), 2022
Zhao W, Guo C, Wang C, Wang Y, Wang L.
europepmc   +1 more source

Inherit variability characterization considering piezocone test data: Application to bauxite tailings [PDF]

open access: yes
Variability characterization is a key component in the reliability assessment of geotechnical systems, particularly in scenarios involving tailings deposits, where spatial heterogeneity can critically impact design safety.
de Campos, Juliano Pasa   +3 more
core   +2 more sources

A Novel Method for Estimating the Undrained Shear Strength of Marine Soil Based on CPTU Tests

open access: yesJournal of Marine Science and Engineering
The undrained shear strength is an essential parameter in the foundation design of marine structures. Due to the complex marine environment and technical limitations, it is difficult and costly to obtain offshore samples.
Sai Fu   +4 more
doaj   +1 more source

Geotechnical Site Assessment by Seismic Piezocone Test in North of Denmark [PDF]

open access: yes, 2013
These days cone penetration tests (CPT) have gained more popularity as an alternative to the conventional laboratory tests for subsurface investigation and estimation of soil parameters.
Andersen, Lars Vabbersgaard   +3 more
core   +1 more source

Geotechnical test embankment on soft marine clay in Newington-Dover, New Hampshire [PDF]

open access: yes, 2013
During the fall of 2012, the New Hampshire Department of Transportation built a test embankment for the new alignment segment of the proposed Exit 6 Southbound On-Ramp site off Route 4 in Newington-Dover, New Hampshire. The purpose of the test embankment
Getchell, Amy
core   +1 more source

Bridge Foundation Piles in Varved Glaciolacustrine Deposits Exhibiting Very High Soil Setup [PDF]

open access: yes, 2013
A pile-supported bridge was to be constructed at a site in Vadnais Heights, Minnesota, located north of St. Paul, in an area underlain by a significant deposit of glaciolacustrine sand, silt, and clay, which extended to a depth of about 39 m.
Reuter, Gregory R.
core   +1 more source

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