Earthwork Slips and Subsidences upon Public Works: Their Causes, Prevention, and ReparationNewman, John
Science
Earthwork Slips and Subsidences upon Public Works: Their Causes, Prevention, and Reparation
Newman, John
Earthwork
The construction of embankments upon soft soil is here referred to so
far as regards lateral movement, or where vertical settlement causes
such action by drawing asunder. Whenever the surface of the ground
bulges or upheaves upon earth being tipped upon it or pressure applied,
it shows that the disturbing harbingers of instability are in action and
that its sustaining power has been reached, its surface ruptured, and
any more soil placed thereon will only sink and displace the earth until
it meets the solid ground beneath, or the material becomes sufficiently
compressed and dense for it to sustain the load; such a condition of
unrest generally proceeds from over-pressure and will loosen the soil,
increase percolation, and aid disintegration. When it is known that
soft, peaty, muddy, or silty earth overlies level solid ground, and it
is certain it cannot escape, and can only be condensed by weighting
until it will permanently bear the strain required, it can be built
upon; although should there be more pressure at one place than another,
or the character of the soil vary, in certain places be swampy and in
others dry, the surrounding ground will probably rise where the weight
is the least; therefore, increased bearing area of an embankment maybe
necessary until the sustaining power of the earth is not exceeded, or
slips and subsidences will occur, for the weight of an embankment in
such a situation cannot be diminished by retaining walls, as stable
foundations are not to be obtained. It is obvious the width of the
formation cannot be reduced and therefore the only way of lessening the
load upon the base per square foot, assuming the embankment to act as a
mass, and of distributing its weight, is by flattening the slope and
making a platform under the seat of an embankment. All earths, however,
that are not hard rock subside upon being weighted, and in the case of
tenacious clay soils, upon a considerable load being applied over a
small area, a trifling contiguous uplifting of the ground will generally
be noticed. If such rise of the soil does not exceed about one-sixth of
the settlement of the clay under the load it may be disregarded as not
likely to cause a slip or serious lateral movement.
When the foundation consists of a firm stratum of gravel, sand, or solid
earth overlying soft soil such as quicksand or silt, _i.e._, mud and
sand; or alluvial deposit, care must be taken that the latter is not
forced up at a weak place by the additional weight of an embankment, and
the firm stratum undermined, as then it will sink, fissure, and be
unsafe. Any disturbance of the bed or water of an estuary or lake other
than by the tides, currents, or wind is an indication that the earth
beneath the firm soil is overloaded, and that subsidences and slips will
ensue.
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