Abstract:
Deformation and force characteristics caused by flat rigid tines (inclined at an angle
of 500 to the horizontal soil surface) in loam soil with moisture content below the
liquid limit were studied using a glass-sided soil bin. The tines moved in the soil
bin in a quasi-static speed and the soil deformation was observed through the glass
side of the soil bin. Strain gauge bonded L- shaped force transducers were used
in recording soil forces. Three moisture content levels (viz 5.2%, 21% and 33.5%
(d.b.)) were used.
The results obtained indicated that soil deformation and force characteristics
for loam soils are greatly affected by variations in soil moisture content. For 5.2%
and 21% soil moisture contents, deformation patterns were progressive shear types.
Soil forces for these moisture content levels were cyclic in nature and generally did
not differ in magnitude. The deformation process was in regular cycles resulting in
corresponding periodic variations in the soil reactions on the tines. There were no
distinct zones as described in the passive soil pressure theory. Plastic type of soil
deformation was observed in 33.5% soil moisture content with comparative high
corresponding soil forces whose periodicity died off.
