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 stability of an embankment is not regulated by the cohesiveness of
the soil, as a sand or gravel embankment, or that formed of any material
whose particles are not deleteriously affected, will stand with a
sufficiently flat slope if protected against erosion, and be more stable
than a clay or any embankment in which the particles are soluble and
soon impaired by water, however great their original tenacity. If any
part of an embankment has become saturated, the internal water must be
tapped and drained; as the lower surface portion is almost certain to be
the wetter, the drains should be made at the base, trenches filled with
open porous material upon the slopes, and, perhaps, it may be necessary
to sink a few shallow wells. The slopes and formation should be covered
so that when the excess of moisture is extracted from the mass it cannot
be replaced. Porous earth counterforts can be adopted, 6 to 10 feet in
width, placed at intervals depending upon the nature and condition of
the soil and height of an embankment, or a continuous bank of similar
material at the toe to support the embankment during the temporary
weakening from drainage operations. One of the worst cases that may have
to be treated in embankments is in clay or marl soils, when the central
portion has been first tipped in a wet state in the winter months, and
after an interval the embankment completed to its required width in a
frozen condition, or nearly so, or one in which the earth becomes frozen
when deposited.
In Russia it has been found that rain-water percolating into such an
embankment cannot drain away, but accumulates and finally bursts the
slopes, and that water will exude from frozen soil when it thaws, a
considerable time elapsing before all the frozen earth has thawed; water
is thus, as it were, taken into the mass, which in all retentive soils
will be difficult to drain without turning over the earth; and it will
cause slimy surfaces and general instability. It will always be an
expensive operation to make such an embankment secure, and it cannot be
made as firm as one properly deposited. After subsidence has ceased, an
approved remedy in such a case is to cover the formation with an
impermeable layer, and to raise the embankment to the rail level with
sand, which is ultimately alone used for repairs, the slopes being
carefully trimmed and sown.
Public-domain text, read in full here on John Shaqi.
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