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
Should the soil be silty sand, or be charged with water, consequent upon
the formation of the country, it may be impossible to drain a cutting
without a complete system of wells, catchwater drains and pipes, and
even then it may be difficult to separate the water from the earth. In
building a drain-shaft it should be remembered that it may not only be
subject to a compressive strain, but also to transverse strain and
flexure from different pressures of the earth at various depths,
especially when the soil is not the same throughout, and unequally damp.
When “boils” occur in sand-cuttings, perhaps the cheapest expedient is
to place a shaft over the boil, weight the bottom sufficiently to
prevent a movement of the sand, but to allow the water to escape, and
make a discharge outlet after having ascertained its head level: _vide_
Chapter XII. On no account should a spring be stopped, as such action
will result in its diversion to some other place; but the water flowing
from it should be guided and discharged. Weighting may arrest a slip in
any sandy soil, also clay or any impervious material placed upon the
sand, or sinking a well outside a cutting to a depth of some 5 feet
below the bottom may effect a remedy by abstracting the surplus water,
but care must be taken not to disturb the sand.
Slips in embankments frequently occur from the percolation of water
through the formation to the slopes, and so to the toe, the lower
portions become disintegrated by moisture and the effects of weather,
and cause the upper parts to slide or move. To lessen percolation and to
prevent an accumulation of water upon the formation, it is usual for its
centre to be raised a few inches above the level of the top of the
slope. This is undoubtedly a good practice, as it also tends to drain
the ballast, but it may be nullified in time if the entire width of the
formation be not covered with an impermeable layer or with ballast; for
when an unprotected space remains between the toe of the slope of the
ballast and the top of the slope of an embankment, water is liable to
percolate through the cess and cause a slope to become wet and unstable;
particularly so if the ballast is broken rock and has side walls instead
of slopes, as then a depression will probably be made by the platelayers
or signalmen walking upon the cess. In all cases where the material is
treacherous or likely to slip, it is advisable to cover the top of
embankments of considerable height throughout their width with ballast
or some impervious soil, provided the permanent way is also properly
drained. This is the simplest precaution to take respecting the
preservation of the formation level or summit of an embankment. All
grass, dirt, and refuse should be regularly removed from it and anything
that obstructs free drainage. The nature of the ballast also affects the
evenness of the surface of the formation, as if it consists of broken
rock, the equal and regular packing of the sleepers is not so easily
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