The Flat Dilatometer Test (DMT) is an in-situ testing method used to determine the strength and deformation characteristics of fine-grained soils. This method involves a stainless blade shaped probe with a thin circular steel membrane mounted on one side. The blade has a cutting edge to penetrate the soil and is inserted into the ground at the desired depth. It is connected to a control unit on the ground surface. After the penetration, pressure by a gas tank is applied to inflate the membrane. The pressure required to initiate the movement of the membrane against the soil is recorded and is called “A-pressure”. The inflation continues until the center of the membrane is moved 1.1 mm against the soil. The required pressure to achieve that is called “B-pressure”. If the required depth is below the water table, the membrane can be slowly deflated to record “C-pressure”, which represents the pore pressure acting on the membrane. The corrected DMT results are used to obtain information on soil stratigraphy, in situ state of stress, shear strength and deformation properties.
Suggested by Professor Marchetti S., Professor, Department of Civil Engineering, L' Aquila University, Italy. List compiled in January 2003.
Most of the following 10 papers (and of other relevant papers) are downloadable from the website: http://www.marchetti-dmt.it/
Introduction The horizontal...
A Zoom Meeting (~2 hours) on “Advice for S...
Introduction Soil subgrade reaction in...
Introduction The static stiffness of a...
Introduction When a foundation i...
7th March 1961 – 3rd November 2020 The following...
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