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
It also sometimes happens that two treacherous earths have a stratum of
stable soil between them such as rock; in that event it is advisable to
leave a cess between the bottom of the slope of the upper stratum of
unstable soil and the underlying rock, so as to allow of weighting or
other works to resist movement of the toe.
With respect to the adoption of open surface rubble drains upon the
slopes, in Chapter IV., page 78, special reference is made to them as
drains, and in Chapter VI., pages 111, 112, an objection is examined;
but they are generally effective if cut at right angles to the formation
and not diagonally or transversely. When a slip is repaired by replacing
the slipped earth when dried and rammed between such drains, it should
be determined whether it would be better to cover the slope or increase
the number of drainage channels. A simpler remedy is the insertion of a
dry rubble lining on the surface of the original ground upon which a
slip has occurred, and the restoration of the slope by means of firm
earth or rammed and dried slipped soil; but the system of rammed earth
counterforts, although it has succeeded when effected during the dry
season, the earth being wetted sufficiently to make it cohesive by
ramming, will not succeed in wet or winter weather, as the soil cannot
then be consolidated by ramming operations, for it will be overcharged
with water from the effects of rain, frost, or snow. Fair or summer
weather is required to ensure success.
Should it be considered advisable, in addition to the erection of rammed
earth counterforts to a height of from one-third to one-half of that of
an embankment, a porous layer or wall of broken stone can be inserted
between the slipped material, which is not touched, so that the waters
can filter away through it and the slope be restored; and the
counterfort have a channel at its base, in order to prevent a lodgment
of water, to drain the slipped earth and the embankment, and to prevent
the counterfort becoming saturated. This method may be insufficient in
any but comparatively firm soil, and it may be necessary to make a
trench at the toe of the slope having its base 2 or 3 feet below the
seat of the slip or firm ground, it being filled with rock chippings,
shingle, gravel, burnt ballast, broken bricks, ashes, coarse clean sand,
or other material having equable frictional stability and particles that
may for earthwork purposes be considered as insoluble in water, and
therefore that form stable masses and yet act as drains; and to drain
the slopes by trenches varying in width according to the position and
depth of cutting, the depth of a trench may be little or have to be such
that it extends to the solid ground through the slip, or about 50 to 75
per cent. of its depth, which must be determined in each case, may be
sufficient. Such dry stone counterforts may be required at distances
from centre to centre of 15 to 66 feet, and are sometimes placed in the
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