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
When a choice of sites exists and the position of a dock is not
absolutely fixed, it may be possible to have the foundations of the
whole work in one kind of earth; if otherwise, one portion may be stable
and another unstable, always treacherous, and liable to slip and
subside. In any case settlement is not likely to be equal, and therefore
a foundation which is well able to sustain an evenly distributed load
may yield from unequal strain and excess of lateral thrust. Consequent
upon the situation of docks, the superficial beds upon which they have
to be erected frequently vary in stability and reliability; and the
location being altered in any direction may result most seriously; the
earth upon one side of a comparatively narrow river being stable in
character and on the opposite bank most treacherous. Difficulties often
arise in foundations, especially in sandy soils, from making borings and
trial pits too near the important parts of the work; they should be made
as reasonably far away as is convenient. In boring, a sand flow may
occur, when it may be necessary to fill the bore-hole and sustain the
soil by a covering, or by consolidating the sand by means of Portland
cement, and then, perhaps, reliable operations may be continued. Borings
should be considered as unreliable if merely superficial; in any case of
importance they should only be trusted for the place where they are
made, and not as indicating the nature or condition of the soil over a
considerable area. When pits cannot be sunk, it is desirable that in a
suspectedly treacherous site the bore-holes should be at every 200 or
300 feet.
Excavating pits, using test-bars, and driving piles are some of the
methods of determining the character of foundations, but care should be
taken to ascertain in boring that boulders, or thin strata of hard
gravel, are not mistaken for solid rock. In sand, mud, or soft clay they
can be made by means of an iron pipe and the water-jet system.
Experience has proved that boring with an auger is not so reliable as
boring with a tube, such as is used for artesian wells. In the case of
augers, when boulders are encountered, further boring is usually
arrested in that place and another bore-hole has to be commenced. Trial
pits, where practicable, should be preferred to boring, and they should
be sunk to a depth considerably below the lowest level of the intended
foundations, and then they may do for sump holes for pumping operations.
In testing ground by borings, several should be made, as one hole might
encounter a boulder or some hard soil, such as indurated clay, and the
latter may adhere to the auger and arrest its progress; the specimens
then brought up, being crushed and pressed together, will appear to be
firmer than the actual condition of the ground.
Public-domain text, read in full here on John Shaqi.
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