dragline, clamshell, bulldozer, backhoe, or a large
24-inch (diameter) power-driven earth auger can
expedite the digging-if the equipment is available.
Excavations below the groundwater table require the
use of pneumatic caissons or the lowering of the water
table. Load-bearing tests can also be performed on the
soil in the bottom of the pit.
The use of the hand auger is the most common
method of digging test holes. It is best suited to cohesive
soils; however, it can be used on cohesionless soils
above the water table, provided the diameter of the
individual aggregate particles is smaller than the bit
clearance of the auger. By adding a pipe extension, you
may use the earth auger to a depth of about 30 feet in
relatively soft soils. The sample is completely disturbed
but is satisfactory for determining the soil profile,
classification, moisture content, compaction
capabilities, and similar properties. Auger borings are
principally used for work at shallow depths.
Wash boring is probably the most common method
used commercially to make deep test holes in all soil
deposits except rock or other large obstructions. The test
hole is made by a chopping bit fastened to a wash pipe
inside a 2-, 4-, or 6-inch (diameter) steel casing. The
wash pipe is churned up and down, while the bit, from
which water flows under pressure, loosens the soil. The
water then carries the soil particles to the surface where
they collect inside the casing. An experienced operator
can detect from the appearance of the wash water when
a change in the type of soil being penetrated has
occurred. Wash samples are samples taken directly from
the wastewater. They are so disturbed, however, that
their value is limited. This method of sampling should
not be used if any other means is available.
Dry-sample boring makes use of the wash boring
method to sink the hole. When a change of soil type
occurs or sometimes at specified depth intervals, the
washing is stopped and the bit is replaced by a sampler.
The sampler (an open-end pipe) is driven into the
relatively disturbed soil in the bottom of the hole to
extract a sample. The sample is removed and preserved
in a sample bottle until tested in the laboratory.
The undisturbed sampling process is used to
obtain samples with negligible disturbance and
deformation for testing for shear strength,
compressibility, and permeability. These samples can
best be obtained from relatively cohesive soils. Methods
that you can use to obtain undisturbed samples are
discussed in the EA3 TRAMAN.
The core boring process is used to obtain samples
from boulders, sound rock frozen ground, and highly
resistant soils. The cutting element may consist of
diamonds, chilled shot, or steel-tooth cutters. The drill
cuts an angular ring in the rock leaving a central core
which enters the core barrel of the drill and is retained
by a holding device when the drill is removed from the
hole. This is the best method for determining the
characteristic and condition of subsurface rock
PLANNING FIELD EXPLORATIONS
The location of test holes or test pits depends upon
the particular situation. Soil tests should be made on
samples that are representative of the major soil types
in the area. In view of this, the first step in exploration
is to develop a general picture of the subgrade conditions
to assist in determining the representative soils. Field
reconnaissance should be made to study landforms and
soil conditions in ditches and cuts. Techniques have
been developed whereby aerial photographs can be used
for delineating areas of similar soil conditions. Full use
should be made of all existing data.
Subgrade Areas
To determine subgrade conditions in an area to be
used for road or for airport runway, taxiway, and apron
construction, the next step after field reconnaissance is
usually to make preliminary borings at strategic points.
An arbitrary spacing of these borings at uniform
intervals does not give a true picture and is not
recommended. Intelligent use of various procedures
permit strategic spacing of the preliminary borings to
obtain maximum information with a minimum number
of borings.
Obtain soil samples for classification purposes in
these preliminary borings. After these samples are
classified, develop soil profiles. Representative soils
should then be selected for detailed testing. Test pits or
larger diameter borings should then be made to obtain
the samples needed for testing or to permit in-place tests
to be made. The types and number of samples required
depend on the characteristics of the subgrade soils.
Subsoil investigations in areas of proposed pavement
must include measurements of in-place water content,
density, and strength to determine the depth to which
compaction must extend and to ascertain whether soft
layers exist in the subsoil.
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