Contents [show]
Field tests can measure the soil response in situ where the ground is not disturbed and the in-situ conditions are preserved.
The most common in-situ tests are the following:
The Surface Wave Method, but also Seismic Reflection and Seismic Refraction tests are widely used as they do not require boreholes or penetrations into the ground which can be time-consuming and expensive. Therefore, they are simple and low-cost solutions.
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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