For example, conventional static load testing gives a direct bearing
strength value for the soil, but dynamic testing adds inertia and
acceleration into the equation, and these must be factored out to
obtain a static equivalent.
Have there been any such studies done?
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--
Ed J. Garbin, Jr., E.I.
University of South Florida
--
On the WWW : http://www.eng.usf.edu/~garbin
--
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Anthony Burke
Anthon...@jcu.edu.au
I assume you are well aware of the strong effect and interaction of load
rate with pore pressure (and strength) in soil mechanics.
Rob
It was Thu, 23 Jul 1998 12:38:47 +1000, when Rob Jeffrey
<r...@dpr.csiro.au> wrote:
>Ed,
>
>I assume you are well aware of the strong effect and interaction of load
>rate with pore pressure (and strength) in soil mechanics.
>
>Rob
http://www.berminghammer.com/frstat.htm
Upon analyzing the results of many tests on both shallow and deep
foundations, it has become apparent that inertia plays a significant
role in correlating Statnamic data with Static data.
Ed G.
It was Mon, 27 Jul 1998 10:49:28 +0200, when Lars Andresen <l...@ngi.no>
wrote:
>Hello Ed J
><P>As I know, all field an laboratory tests for measuring shear-strength
>are considered to be quasi static with no inertia effects present (even
>with different loading rates within the range mentioned above). I'm
>not aware of any dynamic testing methods which may be used to reveal soil
>shear-strength (except maybe for SASW - Spectral Analysis of Surface Waves
>which determines maximum shear modulus Gmax which again can be correlated
>to shear-strength).
Lars Andresen wrote in message <35BC3F18...@ngi.no>...Hello Ed J.It is a well known fact that the measured soil shear strength generally increases with increasing loading rate. This effect is small, in the order of 1-10 %, for drained tests (e.g. triaxial) performed on dry granular specimens (see e.g. "Soil Mechanics" by Lambe and Whitman). But for a saturated soil tested under undrained conditions, the effect can be quite substantial (see e.g. Bjerrum, Simons and Torblaa, "The effect of Time on the Shear Strength of a Soft Marine Clay", Proc. Brussels Conf. on Earth Pressure Problems, Vol. 1, pp. 148-158, 1958).The loading rate considered is typically in the range from 10e-3 to 10e+1 %/min axial strain. This effects are however not connected to inertia as a strain rate of 10e+1 %/min still is considered to maintain quasi static conditions. The differences in measured shear-strength are believed to be due mainly to the inherent nature of the clay like visco-plasticity or to internal migration of pore water.
As I know, all field an laboratory tests for measuring shear-strength are considered to be quasi static with no inertia effects present (even with different loading rates within the range mentioned above). I'm not aware of any dynamic testing methods which may be used to reveal soil shear-strength (except maybe for SASW - Spectral Analysis of Surface Waves which determines maximum shear modulus Gmax which again can be correlated to shear-strength).
-
Lars Andresen
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