INTERFACE LOAD TRANSFER DEGRADATION DURING
CYCLIC LOADING: A MICROSCALE INVESTIGATION
JASON T. DEJONG, MARK F. RANDOLPH and DAVID
J. WHITE
ABSTRACT: The shaft capacity of piles in
sand subjected to cyclic (wave) loading has been observed to
decrease significantly with loading cycles (Poulos, 1989). A
number of researchers (Boulon and Foray, 1986; Tabucanon et
al., 1995; Shahrour etal., 1999) have replicated the characteristics
of the load transfer degradation behavior in the laboratory
through cyclic interface shear testing with a constant normal
stiffness confinement condition (Vesic, 1972). However, no consensus
currently exists as to the primary microscale mechanisms that
govern cyclic interface shear behavior and load transfer degradation.
A research program was undertaken to quantify the contribution
of soil properties, cementation, confinement condition, and
displacement mode, in load transfer degradation. Monotonic and
cyclic interface shear tests were performed using a modified
interface direct shear device with a Perspex side window. The
specimen particle displacement fields were quantified during
selected cycles by capturing high resolution digital images
(1600×1200 pixels) and using Particle Image Velocimetry
(White et al., 2001a). Results indicate that the confinement
condition, which is intended to replicate the elastic response
of the far-field soil, is of primary importance as it allows
for normal stress relaxation with soil contraction adjacent
to the interface. The displacement magnitude, particle characteristics,
and particle-particle cementation were also observed to affect
the magnitude and rate of degradation. It is anticipated that
these findings will provide a fundamental rationale to identify
field conditions where shear stress degradation is likely to
occur and a basis from which more rigorous models may be developed.
Key words: CNS, constant normal stiffness,
cyclic degradation, cyclic shear, interface shear, load transfer,
particle image velocimetry, particle tracking, planar deformations
(IGC: E12)