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
After ascertaining by experiment the pressure any earth will bear over a
given area, the object should be to make the soil neither drier nor
wetter than that of its natural state when experimenting, and it should
be maintained in that condition. In testing the weight which a soft
earth will support, some days should be allowed for the sinking of the
test platform, and such subsidence should be ascertained periodically by
careful levels. A month is not too long for a reliable and complete
test, as many soft soils continue to yield. In soft clay soils
considerable depression often proceeds for weeks after a load has been
applied, but except in peculiar earths such settlement will ultimately
be imperceptible, and will practically cease. A considerable margin of
stability should in all cases be allowed. Although it may not be
absolutely necessary to experiment when the nature of the ground is well
known, wherever stability is of great importance, the cost of a
practical experiment being so small, there is no sufficient reason why
an actual test of the sustaining power of the soil should not be made in
the majority of instances, for there are many earths whose friction and
cohesiveness can alone be depended upon for resistance to displacement.
In such cases the initial pressure upon the earth should not be much
exceeded.
Description of Earth. Approximate
Safe Maximum
Load in Tons
per Square
Foot.
Bog, morass, quicksand, peat moss, marsh-land, silt 0 to 0·20
Slake and mud, hard peat turf 0 to 0·25
Soft wet pasty or muddy clay, and marsh clay 0·25 to 0·33
Alluvial deposits of moderate depths in river beds, &c. 0·20 to 0·35
NOTE.—When the river bed is rocky and the deposit firm
they may safely support 0·75 ton, but not more.
Diluvial clay beds of rivers 0·35 to 1·00
Alluvial earth, loams and loamy soil (clay and 40 to 70
per cent. of sand), and clay loams (clay and about 30 0·75 to 1·50
per cent. of sand)
Damp clay 1·50 to 2·00
Loose sand in shifting river bed, the safe load increasing 2·50 to 3·00
with depth
Upheaved and intermixed beds of different sound clays 3·00
Silty sand of uniform and firm character in a river bed 3·50 to 4·00
secure from scour, and at depths below 25 feet
Solid clay mixed with very fine sand 4·00
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