7.
Summary of the Papers
7.1.
Paper I and II
The appended papers present environmental data measurements, analyses and findings
from the field studies carried out in the Torpsbruk test site along county road 126 in
southern Sweden (Figure 17). The pavement structure consists of a 100 mm thick HMA
layer (dense graded mix, 16 mm maximum grain size and 160/220 bituminous binder
penetration grade) with 160 mm crushed gravel base and 300 mm natural sandy gravel
subbase layers. The subgrade soil at the test section is classified as sandy silt material
with more than 25% fines content resting on bedrock layer at 3.0 to 3.5 m depth.
Pavement environmental factor data collection mainly consisted of groundwater level
sensors (six groundwater rods with automatic data logger in the transverse direction of
the road), subsurface volumetric moisture content sensors (four moistures rods each
consisting of four sensors with automatic data logger) and temperature sensors (one
frost rod). A schematic overview of the test site instrumentation is illustrated in Figure
18. The structural response of the pavement was measured using a trailer-mounted
KUAB FWD device with multilevel loads.
FIGURE 17.
Location of the Torpsbruk test site along county road 126 in southern
Sweden.
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FIGURE 18.
Schematic overview of the pavement instrumentations (GW: groundwater
probes, MC: Moisture content probes).
Paper
I
mainly focuses on investigating the structural behaviour of the pavement
system during the spring-thaw period in 2010 (Figure 19). During the study period, the
pavement profile subsurface temperature and moisture content were measured and the
structural behaviour of the pavement was assessed using frequent FWD measurements.
Figure 20 shows the deflection basin variations during the thawing and the recovery
periods in 2010. As thaw penetrated the pavement structure, the moisture that was
accumulated in the pavement structure during the freezing period in the form of ice
lenses converted back into the liquid phase. Thaw penetration broke down the particle
ice-bonds which also releases excess moisture into the pavement system. This resulted
in a considerable decrease in the overall stiffness of the pavement system (Figure 20,
left). As the excess moisture was further drained out from the pavement structure, the
unbound layers regained their pre-freezing stiffness and the pavement recovered (Figure
20, right).
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