Pavements
are a conglomeration of materials. These materials, their associated
properties, and their interactions determine the properties of the resultant
pavement. Thus, a good understanding of these materials, how they are
characterized, and how they perform is fundamental to understanding pavement.
The materials which are used in the construction of highway are of intense
interest to the highway engineer. This requires not only a thorough
understanding of the soil and aggregate properties which affect pavement
stability and durability, but also the binding materials which may be added to
improve these pavement features.
What is Sub grade
Soil is an
accumulation or deposit of earth material, derived naturally from the
disintegration of rocks or decay of vegetation, that can be excavated readily
with power equipment in the field or disintegrated by gentle mechanical means
in the laboratory. The supporting soil beneath pavement and its special under
courses is called sub grade. Undisturbed soil beneath the pavement is called
natural sub grade. Compacted sub grade is the soil compacted by controlled
movement of heavy compactors.
Desirable
properties of Subgrade Soil
The desirable properties of sub grade soil as a
highway material are
1. Stability
2. Incompressibility
3. Permanency
of strength
4. Minimum
changes in volume and stability under adverse conditions of weather and ground
water
5. Good
drainage, and
6. Ease
of compaction
Soil Types
The wide range of soil types available as highway
construction materials have made it obligatory on the part of the highway
engineer to identify and classify different soils. A survey of locally
available materials and soil types conducted in India revealed wide variety of
soil types, gravel, moorum and naturally occurring soft aggregates, which can
be used in road construction. Broadly, the soil types can be categorized as
Laterite soil, Moorum / red soil, Desert sands, Alluvial soil, Clay including
Black cotton soil.
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Figure : Indian standard grain size soil classification system |
Gravel: These are coarse materials with particle
size under 2.36 mm with little or no fines contributing to cohesion of
materials.
Moorum: These are products of decomposition and
weathering of the pavement rock. Visually these are similar to gravel except
presence of higher content of fines.
Silts: These are finer than sand, brighter in color
as compared to clay, and exhibit little cohesion. When a lump of silty soil
mixed with water, alternately squeezed and tapped a shiny surface makes its
appearance, thus dilatancy is a specific property of such soil.
Clays: These are finer than silts. Clayey soils
exhibit stickiness, high strength when dry, and show no dilatancy. Black cotton
soil and other expansive clays exhibit swelling and shrinkage properties. Paste
of clay with water when rubbed in
between fingers leaves stain, which is not observed for silts.
Tests
on soil
Sub grade soil is an integral part of the road
pavement structure as it provides the support to the pavement from beneath. The
sub grade soil and its properties are important in the design of pavement
structure. The main function of the sub grade is to give adequate support to
the pavement and for this the sub grade should possess sufficient stability
under adverse climatic and loading conditions. Therefore, it is very essential
to evaluate the sub grade by conducting tests.
The tests used to evaluate the strength properties
of soils may be broadly divided into three groups:
·
Shear tests
·
Bearing tests
·
Penetration tests
Shear tests
are usually carried out on relatively small soil samples in the laboratory. In
order to find out the strength properties of soil, a number of representative
samples from different locations are tested. Some of the commonly known shear
tests are direct shear test, triaxial compression test, and unconfined
compression test.
Bearing tests are loading tests carried out on sub
grade soils in-situ with a load bearing area. The results of the bearing tests
are influenced by variations in the soil properties within the stressed soil
mass underneath and hence the overall stability of the part of the soil mass
stressed could be studied.
Penetration tests may be considered as small scale
bearing tests in which the size of the loaded area is relatively much smaller
and ratio of the penetration to the size of the loaded area is much greater
than the ratios in bearing tests. The penetration tests are carried out in the
field or in the laboratory.
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