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
easily, and it is therefore advisable to make them according to the
nature of the soil, situation, and requirements not less than 1 foot 6
inches to 3 feet in width at the top and 1 foot at bottom; they may be
from 1 foot to 3 feet in depth. Care should be taken that the bends are
not too abrupt or the water may make its own course. A gentle curve
considerably increases the flow. The angle of a bend should be as easy
as possible, and not exceed 26° or 2 to 1.
In sandy and loose soils, if unprotected, open drains may be difficult
to maintain even when filled with broken stone, and covered or pipe
drains be necessary, and those loosely filled with stones or faggots may
not succeed; in any case no run of the sand must be allowed, and it is
advisable to rapidly construct them. In peaty soils, from subsidence of
the ground consequent upon draining, the drains often become choked. The
depth of a drain in the formation may require to be deeper than
elsewhere, as at the toe of the slope, the weakest part, the water will
generally be most abundant.
Upon railways, the advantage of thorough drainage of the formation as
regards the stability of the permanent way and reduction of the cost of
repairs is proverbial, but here is only named in its relation to the
prevention and the reparation of slips.
When field drains are intercepted in the slopes, drain pipes or timber
ducts should be joined to them and be connected with the general
drainage of a cutting. Draining the slopes, providing outlets for the
water, and also support to the earth can be effected by means of a
counterfort of permeable material at the toe of the slope, with its
foundation a few feet below formation level, with open drains at right
angles or obliquely to it extending from the foe to the top of the
slope.[1] These open drains and trenches can be filled with stones,
gravel, hard chalk, ashes, brushwood and gravel, broken bricks, burnt
clay or other suitable material; and a simple covering of picked ashes,
&c., over a moist place in a clay cutting of little depth may be
sufficient. The distance apart of such trenches in clay cuttings
generally ranges between 10 and 33 feet; their location must be governed
by the consideration that they exist in order to prevent a localization
of water in the slopes: their width is usually from 2 feet to 8 feet,
and most frequently 4 to 6 feet, and the depth from 1 foot 6 inches to 3
feet and upwards, below the surface of the slope, but in very wet
embankments a width from 6 to 10 feet and of such a depth as the soil
will allow without extensive support. If the earth has not slipped, and
it should be found that the ground is wet for from 6 to 8 feet or so
beneath the surface, and the depth of the trench is made about half that
of the wetted soil, it is sufficient to collect the water, but if it has
slipped most probably such drains will not be effectual until carried
down below the seat of movement. At the foot of a slope these drains
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