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
With regard to the protection of the toe or lower portion, of a slope by
means of a retaining wall, it may be the only effectual support in one
case, and not succeed in an exposed country without a complete system of
open or closed drains, and then its adoption may be superfluous. In the
following few paragraphs an endeavour is made to indicate some
situations in which retaining walls have or have not been completely
successful when erected for such purpose.
First, it is most important that ample provision be made for draining
the back of the walls, for if the egression of the surface waters be
obstructed, they must accumulate and cause hydrostatic pressure, soften
the lower portion of the earth, thereby failing to partly effect one of
the objects of their erection, and cease to protect the surface; the
probable result being that the wall is pushed forward, broken up, or
overturned. The drainage must be regulated by the quantity and velocity
of the flow, and ample weep-holes should be provided to prevent an
accumulation of water at the back. In damp soil there should be one to
about every three or four superficial yards, and an outlet at each wet
place, or a wall may not stand. The wall should be backed with a
filtering medium such as coarse gravel, hard ashes, ballast, and no
retentive earth should be used. In clay earths a retaining wall should
always have a dry porous backing, as it not only reduces any pressure
due to a head of water, but also allows of the earth swelling without
affecting the stability of the wall, as it probably would if the clay
rested against the back of the wall.
Retaining or breast walls are particularly useful in loose soil having
no cohesion, _i.e._, those of a sandy character or consisting of very
small grains, and which upon saturation by water or by the action of its
flow become in an unstable state or one of actual movement; in such, a
case not only is it requisite to protect the surface of a slope, but
support at the toe is indispensable. In cohesive soil, such as clay or
clay marls, surface protection, combined with systematic and thorough
drainage, may be all that is required to make a slope stable, and the
erection of an impervious or solid high wall be unnecessary, always
provided the earth cannot slide from being superimposed upon an inclined
stratum. In fact, retaining walls in retentive soil have been found to
induce a slip, because they neither drain the earth nor prevent the
additional impregnation of water, and they have consequently been
destroyed.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account