Abstract
The vertical normal stress under a falling weight deflectometer
(FWD) was measured in a sand. The material had more than 90
percent falling within the sand fraction from 60 micrometer to 2
mm. The stress was measured with three different transducers. All
transducers were installed at a depth of 280 mm. The sand was
uniform to a depth of 700 mm and at a distance of 600 mm to either
side of the centerline. An FWD was used to exert a known vertical
force on the surface of the sand, using a loading plate 300 mm in
diameter. The average stress under the plate was about 300 kPa.
All the loads were imposed in the centerline of the three gauges,
but at different horizontal distances from FWD to transducers. An
integration of the measured stress on the plane of the transducers
results in a force 10 to 14 percent larger than the peak force
exerted by the FWD. The measured force is thus reasonably close to
the actual force. When the measured stress is compared to the the
stress predicted using Boussinesq's equation for an elastic
half-space, a very large difference is observed. At the centerline
of the load, the measured stress is about twice the theoretical
value. This difference cannot be explained by variation in the
material characteristics, including nonlinearity, or by dynamic
effects.
Original language | English |
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Book series | Transportation Research Record |
Volume | 1540 |
Pages (from-to) | 24-29 |
Publication status | Published - 1996 |