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Sunday, October 11, 2015
SOIL CONSISTENCY
Soil consistency is the strength with which soil
materials are held together or the resistance of soils to
deformation and rupture. Soil consistency is measured for
wet, moist and dry soil samples. For wet soils, it is
expressed as both stickiness and plasticity, as defined
below. Soil consistency may be estimated in the field
using simple tests or may be measured more accurately in
the laboratory. Note: in each case, indications will be obtained
concerning the relative value of soil for fish-pond
construction, particularly when the wet-soil consistency
is determined.
Determination of wet-soil
consistency
Testing is done when the soil is saturated with water, as, for example,
immediately after a good rainfall. First, determine stickiness,
that is, the ability of soil materials to adhere to other objects. Then,
determine plasticity, that is, the ability of soil materials
to change shape, but not volume, continuously under the influence of
a constant pressure and to retain the impressed shape when the pressure
is removed.
Field test for stickiness of wet soil
Press a small amount of wet soil between your thumb and forefinger
to see if it will stick to your fingers. Then slowly open your fingers.
Rate the stickiness as follows:
0 Non-sticky, if no soil or practically no soil
sticks to your fingers;
1 Slightly sticky, if the
soil begins to stick to your fingers but comes off one or the other
cleanly and does not stretch when the fingers are opened;
**2 Sticky
**3 Very sticky
Field test for plasticity of wet soil
Roll a small amount of wet soil between the palms of your hands
until it forms a long, round strip like a wire about 3 mm thick.
Rate the plasticity as follows:
0 Non-plastic, if no wire
can be formed;
1 Slightly plastic, if
a wire can be formed but can easily be broken and returned to
its former state;
**2 Plastic
**3 Very plastic
Determination of moist-soil consistency
Field test for moist-soil consistency
Testing is done when the soil is moist but not wet, as, for
example, 24 hours after a good rainfall.
Try to crush a small amount of moist soil by pressing it between
your thumb and forefinger or by squeezing it in the palm of
your hand. Rate moist soil consistency as follows:
0 Loose, if the soil is
non-coherent (single-grain structure);
1 Very friable, if the
soil crushes easily under very gentle pressure but will stick
together if pressed again;
2 Friable, if the soil
crushes easily under gentle to moderate pressure;
**3 Firm
**4 Very firm
5 Extremely firm, if the
soil crushes only under very strong pressure, cannot be crushed
between the thumb and forefinger, but must be broken apart bit
by bit.
Determination of
dry-soil consistency
Field test for dry-soil consistency
Testing is done when the soil has been air-dried.
Try to break a small amount of dry soil by pressing it between
your thumb and forefinger or by squeezing it in the palm of
your hand. Rate dry soil consistency as follows:
0 Loose, if the soil is
non-coherent (single-grain structure):
1 Soft, if the soil is
very weakly coherent and friable. breaking to powder or individual
grains under very slight pressure;
2 Slightly hard, if the
soil resists light pressure, but can be broken easily between
thumb and forefinger;
3 Hard, if the soil resists
moderate pressure, can barely be broken between the thumb and
forefinger, but can be broken in the hands without difficulty;
4 Very hard, if the soil
resists great pressure, cannot be broken between the thumb and
forefinger but can be broken in the hands with difficulty;
5 Extremely hard, if the
soil resists extreme pressure and cannot be broken in the hands.
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