Chap. 10 Compressibility and Settlement 10-29
10.33 A consolidation test has been performed on a sample of lodgement till from a region that
was once covered with a glacier. The current vertical effective stress at the sample
location is 1800 lb/ft2 and the measured preconsolidation stress is 32,500 lb/ft2.
(a) Assuming the glacier was in place long enough for complete consolidation to occur,
and assuming the ground surface and groundwater table elevations have remained
unchanged, compute the maximum thickness of the glacier. The specific gravity of
glacial ice is about 0.87.
(b) Although glacial ice was present for a very long time, it also extended over very large
areas, so the required drainage distance for the excess pore water was very long. As a
result, all of the excess pore water pressures may not have dissipated (Chung and
Finno, 1992). Therefore, our assumption that complete consolidation occurred may
not be accurate. If so, would our computed thickness be too large or too small?
Explain.
Solution
(a)
2
0lb/ft 30,7001,80032,500 =−=
′
−
′
=
′zcm
σσσ
had dissipated. Therefore, our computed value of Hf is too small.
10.34 A highway is to be built across a wetlands with the soil profile shown in Figure 10.27
below. These wetlands are subject to flooding, so a fill must be placed to keep the
pavement above the highest flood level. According to a hydrologic analysis, the roadway
must be at elevation 7.0 ft or higher to satisfy this requirement. Sandy fill material that
has a compacted unit weight of 122 lb/ft3 is available from a nearby borrow site.
A subsurface exploration program has been completed at this site, and laboratory
tests have been performed. The results of this program are tabulated below:
Depth
(ft)
Dry unit
weight
(lb/ft3)
Moisture
content
(%) Cc/(1+e0) C
/(1+e0)
σc′
(lb/ft2)
2.0 95 28.6 0.13 0.06 3000
7.5 89 33.0 0.16 0.06 550
13.0 92 30.5 0.12 0.05 850
24.0 93 29.9 0.14 0.07 4800
All depths are measured from the original ground surface.