SLOPE STABILITY
Key words: slope stability, causes, shearing strength
Introduction
Land slides are the downward and outward movements of materials on the slope. The reason for this is
the lack of required shear strength. The slope materials may be composed of
natural rock and soil, artificial fills. Slides can occur in natural slopes as
well as man- made structures and embankments.
Great care
should be taken in the selection of good construction material and also
suitable construction methods to avoid sliding of slopes.
Causes of slope failures
The causes
of slope failures may be external or internal.
External:
Steepening of the slopes, depositing of material along the edge of the slopes
and earthquakes.
Internal:
Decrease in shearing resistance due to excess pore water pressure, leaching of
salts, softening and breakage of cementation bonds.
The other
activities which may provoke land slides are: Rapid draw down, seepage of
water, erosion, heavy rainfall, excavation at the toe of the slope, excavation
at the head of the slope, blocking of the drainage.
Basic concepts of stability analysis
All sloping
surfaces are subjected to shearing stresses .The shear available should overcome the developed stresses. If
the shearing stresses are more, then a surface of rupture will be formed at the
verge of failure.
1. Finding
the most severely stressed internal surface and the connected shearing stress
along the surface Finding the shearing
strength along the surface
Instead of
resorting to rigorous mathematical analysis, a reasonable shape of failure is
assumed and then the stability of the soil above the assumed surface is
analyzed.
Rates of land movement
The
movements associated with land slides can be grouped under four heads.
- Creep, pre-failure movements, movements
during slides, post failure movements.
Creep may
range from 1 to few millimeters per
year. Heavily over consolidated clays experience post failure movements, the
speed of movements ranging from 0 to 6 m per year.
Importance of the Factor of Safety on
slope stability analysis.
It is a
measure of limiting the stress or strain so as to ensure the safety of the
structure. As such, the working stress in any earth structure is much less than
the shear strength of the soil.
The Factor
of Safety may be defined as the ratio of shearing resistance available along a slip surface to the total mobilized or developed shearing stress.
Both cohesion and friction contribute to the shearing strength
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